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Dissertationen zum Thema „Riparian soils“
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1
Rose, Michael. „Phosphorous dynamics in periodically flooded and drained riparian soils“. Thesis, University of Reading, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.367719.
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The aim of the research was to evaluate the processes that determine P stability in riparian floodplain soils, with emphasis on chemical transformations in flood-drained calcareous soil. Flooding of soil columns showed an increase in P solubility (from 0.01 to 1.2 μg ml-1) largely due to the reductive dissolution of Fe minerals (solution Fe increased from < 0.05 to > 50 μg ml-1) and increased solubility of Ca-P minerals (solution Ca increased from < 100 to > 1000 μg ml-1). The periodic drainage of the flooded soil exported the equivalent of approximately O.l5 kg ha-1 (over six flood-drain cycles). Exported P correlated with soil solution P immediately before drainage (r2 = 0.99; P < 0.001). After drainage, there was a reversal of the reactions described above, with solution Fe, Ca and P returning to preflooding levels. Over the course of the 6 flood-drain cycles inorganic P became more stable, with Ca-P and Fe-P pools increasing (from 9 and 11 % respectively both to 14 % of TP) at the expense of labile pools. Similar patterns of P release and retention were observed during batch incubation studies of aerobic - anaerobic cycles using moist soil samples. Solution P and Fe were strongly correlated in both non-calcareous (r2 = 0.96) and calcareous (r2 = 0.73) soils. The role of Ca-P mineral solubility was disguised by the dissolution of calcium carbonate. Drying of the soil can lead to P release on re-wetting (up to eight-fold). This is most likely due to a release of P from ruptured microbial cells and transformations of Fe mineral surfaces. Monitoring suggested that all of these processes were active in the field, as the water table advanced and receded, though more slowly than in the laboratory. Over a four month flood-drain cycle losses of dissolved P from the floodplain were estimated at 0.034 kg ha-1. It is unlikely that this is significant relative to upstream inputs of P to the river from point sources and other types of agricultural land in the River Thames catchment.
2
Lopez, Alfredo R. „Biodegradability of dicamba and 2,4-D in riparian wetland soils“. Thesis, This resource online, 1995. http://scholar.lib.vt.edu/theses/available/etd-06082009-170726/.
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3
Flynn, Nicola Jane. „Nitrogen interactions between floodwater and floodplain soils“. Thesis, Royal Holloway, University of London, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.311972.
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4
Williams, Emily Rose. „The Effects of Depth and Hydrological Connectivity on Heavy Metal Loading in Riparian Zones“. Thesis, Umeå universitet, Institutionen för ekologi, miljö och geovetenskap, 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-185245.
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The area between a stream and land is known as a riparian zone. These zones are highly dynamic whichcarry and accumulate heavy metals and environmental contaminants. Discrete Riparian Input Zones(DRIPs) are a subset of such zones that carry concentrated amounts of water into streams at discrete points.These are more active in their ability to channel water than riparian zones. These areas are important sincethey may retain or release metals and thereby affect the stream chemistry. To test if DRIPs accumulatemetals, 7 DRIPs and 4 Non-DRIPs were sampled along the C5 stream in the Krycklan Catchment. Soilsamples were taken from the surface down to 0.5 m depth at 0.1 m increments and were analysed for totalmercury, metals and loss on ignition. Three metals (vanadin, iron and zinc) were identified as having significant differences in concentration between DRIP and Non-DRIPS. Vanadin and Fe had significantlyhigher concentrations in Non-DRIPs, whereas iron had higher concentrations in DRIPs. Mercury,cadmium, iron, and loss on ignition (LOI) were found to decrease as depth increased, whilst Al was foundto increase with depth. Finally many elements are inter-related, but those with the strongest correlation areLOI and mercury, and iron and cadmium, both r > 0.85. LOI and mercury are strongly related as mercurybinds strongly to organic matter. The relationship of Fe and Cd is likely due to the Fe-oxide and Cdrelationship.
5
Rahe, Nathan. „RESTORATION OF RIPARIAN BUFFER FUNCTION IN RECLAIMED SURFACE MINE SOILS IN SOUTHERN ILLINOIS“. OpenSIUC, 2013. https://opensiuc.lib.siu.edu/theses/1149.
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Riparian buffers have been proven to reduce nutrient and sediment transport to streams in agricultural watersheds. Southern Illinois offers a unique opportunity to study functions of riparian buffers in reclaimed mine soils. In Perry County, Illinois three stream segments of Bonnie Creek, Galum Creek and Pipestone Creek were restored to their approximate original position following mining. Between 1980 and 2000, as part of the restoration, vegetative buffers of grasses and trees were planted along the streams to minimize nutrient and sediment inputs from adjacent restored agricultural land. Our research objective was to determine whether riparian soil function was being restored in the vegetated buffers by comparing multiple soil properties to the adjacent reclaimed soils in agricultural production. Four transects were established on each study site through the buffer and agricultural field. Ten one meter plots were evenly spaced along each transect in each of the land uses. In summers 2010 and 2011, water infiltration rates, bulk density, total carbon concentration, total nitrogen concentration, and C:N ratio measurements were made to assess the restoration of soil function. Soil water infiltration was significantly higher and bulk density was significantly lower in the riparian buffers compared to the adjacent agricultural fields. In the riparian buffer, roots likely helped to break up the soil adding pore space, which reduced the bulk density and increased the water infiltration rates. Soil total carbon, total nitrogen, and C:N ratio were significantly higher in the riparian buffers than the agricultural fields. The additional organic matter inputs from the roots of the riparian vegetation along with incorporation of litter from the soil macrofauna likely helped to increase the soil carbon and nitrogen levels compared to the agricultural fields. Even though the soil C:N ratio was significantly higher in the riparian buffers than the agricultural fields, more time is needed to restore the ratio to levels where nitrogen will be immobilized not mineralized in the riparian soils. Soil function in the riparian areas should continue to develop at a faster rate compared to the agricultural fields due to the impact of the perennial vegetation. Restoration of landscapes is not estimated by the return of structure alone, it also includes the re-establishment of function such as soil quality improvement, water quality improvement, and wildlife habitat restoration.
6
Cook, Steven Allen. „Characterization of riparian wetland soils and associated metal concentrations at the headwaters of the Stillwater River, Montana“. Thesis, Montana State University, 2007. http://etd.lib.montana.edu/etd/2007/cook/CookS0507.pdf.
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7
Lymburner, Leo. „Mapping riparian vegetation functions using remote sensing and terrain analysis“. Connect to thesis, 2005. http://repository.unimelb.edu.au/10187/2821.
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Land use practices over the last 200 years have dramatically altered the distribution and amount of riparian vegetation throughout many catchments in Australia. This has lead to a number of negative impacts including a decrease in water quality, an increase in sediment transport and a decrease in the quality of terrestrial and aquatic habitats. The task of restoring the functions of riparian zones is an enormous one and requires spatial and temporal prioritisation. An analysis of the existing and historical functions of riparian zones and their spatial distribution is a major aid to this process and will enable efficient use of remediation resources. The approach developed in this thesis combines remote sensing, field measurement and terrain analysis to describe the distribution of five riparian zone functions: sediment trapping, bank stabilization, denitrification, stream shading and large woody debris production throughout a large semi-arid catchment in central Queensland.
8
Jungst, Laura J. „Soil quality and stream channel characteristics of montane and subalpine riparian meadows, Sierra Nevada, California“. Laramie, Wyo. : University of Wyoming, 2008. http://proquest.umi.com/pqdweb?did=1799711371&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.
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9
Sessoms, Holly Nicol. „Water use potential and salt tolerance of riparian species in saline-sodic environments“. Thesis, Montana State University, 2004. http://etd.lib.montana.edu/etd/2004/sessoms/SessomsH0805.pdf.
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10
Unger, Irene M. „A multi-dimensional investigation into the effects of flooding on the physical, chemical and biotic properties of riparian soils“. Diss., Columbia, Mo. : University of Missouri-Columbia, 2008. http://hdl.handle.net/10355/5582.
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Thesis (Ph. D.)--University of Missouri-Columbia, 2008.The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file (viewed June 17, 2009). Vita. Includes bibliographical references.
11
Smedley, Scott Brian. „Denitrification potentials in soils underlying a riparian forest and an agricultural field in the coastal plain of Virginia“. Thesis, This resource online, 1993. http://scholar.lib.vt.edu/theses/available/etd-01242009-063055/.
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12
Neal, Andrew Wilson. „Soil Carbon and Nitrogen Dynamics Across the Hillslope-Riparian Interface in Adjacent Watersheds with Contrasting Cellulosic Biofuel Systems“. Thesis, Virginia Tech, 2014. http://hdl.handle.net/10919/48125.
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Climate change resulting from emissions of fossil fuel combustion has sparked considerable interest in renewable energy and fuel production research, particularly energy derived from cellulosic ethanol, which is derived from biomass such as wood and grass. Cellulosic ethanol demonstrates a more promising future as a global energy source than corn-derived ethanol because it does not displace food crops, irrigation is not required, and chemical application rates are much lower than for annual crops, such as corn. Growing cellulosic biomass for energy can help reduce greenhouse gas emissions via carbon (C) sequestration and by reducing demand for fossil fuel production. The objective of this study was to investigate how land use change affects soil properties and selected soil C and nitrogen (N) dynamics among alternative cellulosic biofuel treatments at the Weyerhaeuser Alabama Cellulosic Biofuel Research site in west-central Alabama. Composite soils for characterization, along with forest floor, were collected at year 1 and year 2 after treatment establishment at 0-15cm and 15-30cm depths at six locations along three hillslope-riparian transects in five experimental watershed treatments. Decomposition of loblolly pine needles was assessed in each watershed using an in situ litter bag method. Seasonal in situ net nitrogen mineralization was measured using a sequential core method, and an anaerobic incubation for N mineralization potential of composite soils was performed in the laboratory. Results revealed high variability of soil properties and processes within these watersheds, along with no consistent treatment effects. This study provides baseline data for these watershed treatments for future studies.Master of Science
13
Graf-Rosenfellner, Markus [Verfasser], Martin [Akademischer Betreuer] Kaupenjohann, Martin [Gutachter] Kaupenjohann und Friederike [Gutachter] Lang. „Soil organic matter in riparian floodplain soils : regionalization of stocks and stabilization processes / Markus Graf-Rosenfellner ; Gutachter: Martin Kaupenjohann, Friederike Lang ; Betreuer: Martin Kaupenjohann“. Berlin : Technische Universität Berlin, 2016. http://d-nb.info/1156274958/34.
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Borries, Blair. „Evaluating Stream and Wetland Restoration Success on Surface Mines in Southern Illinois“. OpenSIUC, 2013. https://opensiuc.lib.siu.edu/theses/1313.
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Wetlands and streams provide many ecosystem services, yet many of these services have been lost during the process of surface mining. It is often not practical to avoid wetlands and streams, and newer technologies such as large draglines have made it possible to mine through large perennial streams and their associated riparian wetland systems. Laws such as the Surface Mining Control and Reclamation Act and Clean Water Act require the restoration of these systems in approximately the same location and configuration as before mining, but do not address the long-term replacement of function. In Perry County, Illinois, three stream segments of Bonnie Creek, Galum Creek, and Pipestone Creek and their associated riparian wetland systems were among the largest ever restored following surface mining. The research objective was to determine whether or not function was restored in the three aforementioned streams and riparian wetlands following surface mining reclamation. Wetland soil properties, vegetation, and hydrology at study sites along Bonnie and Galum Creeks were compared to that of nearby natural wetlands and across a chronosequence of soil age. Water quality was assessed [alkalinity, chloride (Cl), fluoride (Fl), iron (Fe), manganese (Mn), zinc (Zn), nitrate (NO3), sulfate (SO4), total dissolved solids (TDS), and total suspended solids (TSS)] in the three restored streams for post restoration trends over time and along the length of the restored channels. Deep basins, called incline pits, were located inline of all three restored channels and are unique to streams restored on surface mines. Stream samples were collected above and below incline pits during storm events to evaluate their ability to reduce sediment concentrations. Two types of wetlands were found at the mine site: mined planned wetlands (MPWs) that had deeper water and fewer or no trees, and mined bottomland forested wetlands (MBFWs) with more shallow water depths and many trees. Significant differences were found between the two wetland types among soil properties, vegetation, and hydrology. Unlike most studies comparing wetlands restored on non-mined sites to natural wetlands, SOM, C, N, and C/N ratio in the surface 15 cm in the MBFWs were not significantly different from the natural wetlands, indicating restoration of function. Plant taxa richness was higher in both mined wetland types than in the natural wetlands at lower elevation sample points where inundation was seasonal. Overall, the mined wetlands also retained water within 30 cm of the surface for more time than the natural wetlands. However, not all function was fully regained in the mined wetlands. Several soil properties were significantly different in the mined wetlands compared to the natural wetlands. SOM, N and the C/N ratio was significantly lower in the 15-30 cm depth, and in the surface 15 cm of the lower elevation samples of the MPW. Soil texture was significantly different in the MPW. There was more sand and less silt. Plan taxa richness was also lower in the higher elevation sample points of the MPW due to the presence of the invasive Phragmites australis. Few trends were found in the soil properties across a chronosequence of soil age. Only pH showed a significant negative linear trend in both mined wetland types across soil age. Assessment of the water chemistry of the restored streams showed that for some parameters, water quality remained stable or improved with distance or time along the restored streams. However, along Bonnie and Galum Creek, a significant positive trend was seen by length of relocated channel in SO4, Fe, Mn, Zn, TDS, conductivity, and Cl. On the other hand, at Pipestone Creek, significant negative trends were evident in TDS, Mn, water temperature, conductivity, and SO4 levels over time or along the length of the relocated channel. Trends along the length of the Pipestone Creek were only found in monitoring conducted twenty years after the channel relocation was complete. Sediment concentration above and below the incline pits inline of Bonnie and Galum Creek were not significantly different based on the sampling of two storm events. An additional input from an agricultural drainage ditch to the Bonnie Pit increased sediment concentrations at the downstream sample point counteracting the reductions that were seen in the Galum pit. Research on the mined stream and riparian systems indicated that reclamation of wetlands and streams to a stable or condition similar to a natural system is possible and sets a standard for future mining operations to follow. However, several shortcomings were identified. Reduced levels of SOM and soil N in the MPWs in the surface 15 cm of the lower sample points may have been the result of longer periods of inundation that reduced nitrification and vegetation recruitment. SOM, soil N, and the C/N ratio in the 15-30 cm depth were lower in the mined wetlands suggesting that these properties take longer to recover at deeper depths, but the significant linear trend in pH show that soil in the deeper strata is changing with time. Invasion by P. Australis reduced taxa richness suggesting that invasive plants are still a problem even more than twenty years after restoration. In addition, the increase in conductivity and SO4 downstream of a visible seep in Bonnie Creek highlight the potential for contaminated groundwater to affect surface water. More consideration should be given to reclaiming not just the surface and subsoils, but also the deeper water bearing strata to ensure that surface water chemistry is not impacted by mining.
15
Altor, Anne E. „Methane and carbon dioxide fluxes in created riparian wetlands in the midwestern USA effects of hydrologic pulses, emergent vegetation and hydric soils /“. Columbus, Ohio : Ohio State University, 2007. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1180460525.
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Momoli, Renata Santos. „Dinâmica da sedimentação em solos sob matas ciliares“. Universidade de São Paulo, 2011. http://www.teses.usp.br/teses/disponiveis/11/11140/tde-08082011-102417/.
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A expansão agrícola no Cerrado brasileiro vem causando severos impactos negativos decorrentes do manejo inadequado das terras. Um destes impactos é a erosão em campos de cultivo que gera grande quantidade de sedimentos, os quais podem ser interceptados em faixas vegetadas com espécies arbóreas ou gramíneas. Várias medidas conservacionistas são indicadas para a minimização destes impactos, dentre elas a presença de cobertura florestal nativa ao longo dos cursos dágua. As matas ciliares funcionam como corredores ecológicos que favorecem a biodiversidade e colaboram na manutenção da qualidade do solo e da água. A largura fixa e simétrica dessa faixa de vegetação conforme proposto pela legislação, em algumas situações se mostra ineficiente, porém a largura ideal ainda permanece controversa. Com o objetivo de propor novas informações acerca da largura ótima para Áreas de Preservação Permanente (APP´s) o presente estudo analisa as matas ciliares de forma multidisciplinar, onde são considerados diversos fatores que influenciam na dinâmica do ecossistema ripário. Fatores climáticos, geomorfológicos e pedológicos são relacionados e focados na interação das matas ciliares com os processos erosivos e seus impactos intrínsecos. Foram utilizadas técnicas convencionais para estudos de solos, como análise estrutural, análise granulométrica em soluções dispersantes (NaOH e H2O) e micromorfologia, técnicas pertinentes a estudos geomorfológicos como uso de pinos de erosão, além de técnicas inovadoras como a dendrogeomorfologia que utiliza as árvores como testemunho temporal de processos ambientais. Dessa forma foram avaliados espaço-temporalmente os sedimentos depositados nas nascentes da zona ripária da microbacia hidrográfica do Rio Meia Ponte. A análise integrada da granulometria e da micromorfologia dos solos e sedimentos revelou a predominância da sedimentação ao longo da borda da mata ciliar. A deposição de sedimentos na área de estudo varia intensamente (coeficiente de variação de 77,76%) tanto no espaço como no tempo, tendo sido observada a deposição de até 37 cm de sedimentos em alguns locais e, a erosão de até 14 cm na superfície em outros. Sendo que de um mês para outro também foi observada alternância entre sedimentação e erosão num mesmo local. A análise dendrogeomorfológica evidenciou que nos últimos 15 anos houve a deposição de até 50 cm de sedimentos. A deposição de sedimentos na área de estudo ocorre distribuída de forma geral na área numa média de 12 cm, bem como de forma localizada próxima aos sulcos de erosão (voçorocas efêmeras) e às raízes tabulares de árvores como figueiras (Ficus insípida).Os maiores índices de sedimentação ocorreram no verão de 2008/2009 quando chuvas muito intensas atingiram o solo descoberto. A ocorrência de voçorocas que atravessam tanto o campo de cultivo quanto a zona ripária reduz a eficiência da mata ciliar na retenção de sedimentos. Outro impacto negativo de grande proporção é o soterramento das nascentes e plântulas que afetam a regeneração da floresta.Agricultural expansion in the Brazilian Savanna causes several negative impacts due to inappropriate land use. One of these impacts is represented by soil erosion in agricultural fields producing big amounts of sediment, which can be intercepted by vegetated areas with pastures or arboreous species. Several conservationist techniques are indicated to minimize these impacts, including maintenance of native vegetal coverage along water courses.Riparian forests act as ecological corridors promoting biodiversity and collaborating in water and soil quality maintenance. The symmetric and fixed width of vegetated stripes proposed by law is inefficient in some situations, and the ideal width is still controversial . With the purpose of proposing new data about the ideal width for permanent preservation areas (APPs), this study analyzes riparian forests in an integrated way taking into account several factors that influence the dynamic of riparian ecosystems. Climatic, geomorphological and pedological factors are related and focused in interaction with riparian forests, erosion processes and related intrinsic impacts. Conventional techniques were used for the soil studies such as structural analysis, particle size distribution analysis with dispersive solutions (NaOH and H2O) and micromorphology. Other techniques were used for geomorphological studies like erosion pins and dendrogeomorphology that uses trees as a temporal evidence of environmental processes. Using these techniques the spatial-temporal distribution of sediments deposited on the sources located in the riparian zone of the basin of Meia Ponte river, was studied. The integrated analysis of particle size and morphology of soils and sediments revealed the dominance of sedimentation along the edge of the riparian forest. The deposition of sediments in the study area varies greatly (coefficient of variation of 77.76%) both in space and time, the deposition was observed up to 37 cm of sediments in some locations, and erosion of up to 14 cm in surface in others. From one month to another was also observed alternation of sedimentation and erosion in one place. The dendrogeomorphic analysis showed that in the last 15 years there was deposition of sediment of up to 50 cm. Sediment deposition in the study area is generally distributed in an average of 12 cm, and locally next to rills (ephemeral gullies) and tabular roots of trees such as figs (Ficus insipida). The biggest rates of sedimentation occurred in the summer of 2008/2009 when very intense rains hit bare soil. The occurrence of gullies that cross both the field and the riparian zone and reduces the efficiency of riparian forest on sediment retention. Another negative impact is the large proportion of the springs and seedling burial that affect forest regeneration.
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Estrup, Andersen Hans. „Hydrology, nutrient processes and vegetation in floodplain wetlands“. Copenhagen : Den kgl. Veterinær- og Landbohøjskole, 2002. http://www2.dmu.dk/1_viden/2_Publikationer/3_Ovrige/rapporter/Phd_HEA.pdf.
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Gumbert, Amanda A. „INFLUENCE OF RIPARIAN BUFFER MANAGEMENT STRATEGIES ON SOIL PROPERTIES“. UKnowledge, 2013. http://uknowledge.uky.edu/pss_etds/27.
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The Kentucky Division of Water indicates that agriculture is responsible for 55% of the Commonwealth’s assessed streams not supporting their designated uses. Riparian buffers reduce nonpoint source pollution in agroecosystems by storing and cycling nutrients, stabilizing streambanks, increasing infiltration, and storing water. Specific information regarding riparian buffer management is needed for land managers to maximize buffer effectiveness at reducing agricultural contaminants impairing water quality.
Baseline soil properties (texture, pH, C and nutrients) of the riparian buffer surrounding a tributary of Cane Run Creek in Fayette County, KY were characterized prior to imposing three mowing regimes (intense, moderate, and no mow treatments) and one native grass regime. Measurements were made along parallel transects located 2-m and 8-m distances from the stream. Root biomass, aggregate distribution, and saturated hydraulic conductivity were measured along the 2-m transect in two consecutive years following treatment establishment. The 2-m transect soils had the highest C, pH, Ca, Zn, and sand content. The 8-m transect had the highest P, K, Mg, and clay content. Semivariogram analysis of C content indicated slight to moderate spatial dependency along the 2m transect and moderate to strong spatial dependency along the 8m transect. Root biomass increased with decreased mowing frequency at the surface depth after one year; the native grass treatment had significantly less root biomass in both years compared to mowing treatments. There was no significant treatment effect on aggregate size distribution at the surface depth in either year. Mean weight diameter and large macroaggregates decreased from 2011 to 2012. Vegetation treatment had no statistically significant effect on water stable aggregates or saturated hydraulic conductivity. Experimental semivariograms provided evidence of spatial structure at multiple scales in root biomass, aggregates, and soil C. Spatial variability occurred over a shorter lag distance in 2012 than 2011, suggesting an effect of imposed treatments slowly developing over time.
This study provides important insights on riparian buffer soil properties, soil sampling strategies to detect spatial variability in riparian buffers, and length of time needed to assess effects of vegetation management regimes on riparian root biomass, soil aggregates, and hydraulic conductivity.
19
Nairn, Robert W. „Biogeochemistry of newly created riparian wetlands : evaluation of water quality changes and soil development /“. Connect to resource, 1996. http://rave.ohiolink.edu/etdc/view.cgi?acc%5Fnum=osu1251216965.
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Scott, Russell Lawrence. „Riparian and rangeland soil-vegetation-atmosphere interactions in southeastern Arizona“. Diss., The University of Arizona, 1999. http://hdl.handle.net/10150/284006.
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In the riparian corridor of the San Pedro River in southeastern Arizona, the fluxes of water and energy over three riparian vegetation groupings were monitored and modeled in order to determine their annual water use and water sources. In situ micrometeorological and soil moisture measurements were made from 1996-1998 at a floodplain grassland site composed mainly of the perennial floodplain grass, Sporobolus wrightii (sacaton), and a tree/shrub grouping dominated by Prosopis velutina (mesquite). The results indicate that the grassland obtained water only from the near-surface (recent precipitation), while the mesquite accessed moisture from deeper in the vadose zone and/or from the water table. Both of these sites exhibited little interaction with the underlying groundwater, suggesting that the majority of the groundwater use from riparian vegetation is limited to the areas of dense mesquite and the forest gallery adjacent to the river. Measurements of the forest gallery water use composed mainly of Populus fremontii (cottonwood) and Salix gooddingii (willow) were available for some shorter term periods in 1997. These measurements were used to calibrate the Penman-Monteith model for evaporation in order to determine the water use from the forest gallery for the entire growing season. The total seasonal water use from the forest was considerably less than potential evaporation estimates. Observations of soil moisture under two rangeland sites in the San Pedro Basin were examined in order to determine the magnitude and the depth of root zone recharge characteristics in this semiarid region. Intermittent TDR observations made from 1990 to 1998 show that deeper root zone recharge occurred primarily during the wintertime, when the plants were senescent and evaporation demand was diminished. A physically-based variably-saturated flow model was used to determine the wintertime recharge. Using an automatic calibration algorithm, the model proved capable of reproducing the observations with small error. Simulated wintertime infiltration amounts indicated that substantial, deeper root zone recharge did occur during wet winters, but that the large year-to-year variability of this recharge implies that deeper-rooted plants would still need access to moisture in shallow root zone.
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Nakao, Megumi. „Costs of using Riparian Forest Buffer for Soil Erosion Constrol“. Connect to resource, 1998. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1216923874.
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Martin, Teri L. „Groundwater nitrate removal and soil microbial community structure in a riparian zone“. Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape17/PQDD_0011/MQ33250.pdf.
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Roosa, Benjamin. „Soil Indicators of Restored Ecological Function Following Riparian Afforestation in Southern Illinois“. OpenSIUC, 2018. https://opensiuc.lib.siu.edu/theses/2452.
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Over the last 30 years, Crab Orchard National Wildlife Refuge in Southern Illinois has made a strong and well-documented effort to convert agricultural lands to forest to further their mission of wildlife and habitat conservation. Our research seeks to assess the influence that this land use conversion has on ecological function and to establish ecological indicators of successful restoration. We examined five potential soil-based indicators of ecological function across a chronosequence of afforested sites at the refuge and compared them to nearby row crop agricultural sites and mature forest sites with similar soils and landscape positions. Collected soil samples were analyzed for total carbon, total nitrogen, labile carbon, aggregate stability, and bulk density. Soil texture analysis was also conducted to validate comparisons among sites. The data were analyzed using a multivariate analysis of variance comparing land uses as well as linear regression analyses looking at the influence of age since restoration on an index value created by subtracting the soil indicator value of the nearby agricultural site from that of the forested site. The index value was used as the dependent variable in order to control for variation among sites and isolate the influence of age. Aggregate stability and labile carbon were positively correlated with age since restoration and bulk density was negatively correlated with age since restoration. These three soil parameters were promising indicators of restored ecological function in afforested sites. Target values for these indicators were proposed. Our results help to determine the timeframe in which these ecological functions return following restoration and can be used to assess the success of current and future afforestation projects.
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Tanzosh, Joyce K. „Soil carbon dynamics and gaseous emissions in riparian zones in Coshocton, Ohio“. The Ohio State University, 2005. http://rave.ohiolink.edu/etdc/view?acc_num=osu1314631878.
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Wallace, Casey Ruth. „Riparian Graminoid Species Responses and Productivity in Compromised Environmental and Soil Conditions“. Thesis, North Dakota State University, 2019. https://hdl.handle.net/10365/31731.
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Riparian buffers have been created as a sustainable and effective way to combat the harmful effects of excess nitrogen and soil salinity in riparian settings. The goal of this research was to determine what species will I) germinate in saline environments and II) establish and produce sufficient biomass while being exposed to increased nitrogen. Incubation of eight native riparian graminoid species were evaluated for their ability to germinate in MgSO4-induced salinity. In a greenhouse study, seven riparian graminoid species were evaluated to quantify their ability to survive and take up nitrogen, mimicking buffer strips exposed to high inputs of runoff nitrogen. Slender wheatgrass and green needlegrass were able to germinate successfully when exposed to MgSO4 with EC levels up to 16 dS m-1 and 8 dS m-1, respectively. Of the graminoid species tested, smooth brome yielded sufficient biomass and nitrogen uptake percentages in a controlled setting.
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Pacific, Vincent Jerald. „Variability in soil CO2 production and surface CO2 efflux across riparian-hillslope transitions“. Thesis, Montana State University, 2007. http://etd.lib.montana.edu/etd/2007/pacific/PacificV0507.pdf.
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The spatial and temporal controls on soil COâ‚‚ production and surface COâ‚‚ efflux have been identified as an outstanding gap in our understanding of carbon cycling. I investigated both the spatial and temporal variability of soil COâ‚‚ concentrations and surface COâ‚‚ efflux across eight topographically distinct riparian-hillslope transitions in the ~300 ha subalpine upper-Stringer Creek Watershed in the Little Belt Mountains, Montana. Riparian-hillslope transitions provide ideal locations for investigating the spatial and temporal controls on soil COâ‚‚ concentrations and surface COâ‚‚ efflux due to strong gradients in respiration driving factors, including soil water content, soil temperature, and soil organic matter. I collected high frequency measurements of soil temperature, soil water content, soil air COâ‚‚ concentrations (20 cm and 50 cm), surface COâ‚‚ efflux, and soil C and N concentrations (once) at 32 locations along four transects. Soil COâ‚‚ concentrations were more variable in riparian landscape positions, as compared to hillslope positions, as well as along transects with greater upslope accumulated area. This can be attributed to a greater range of soil water content and higher soil organic matter availability. Soil gas diffusion also differed between riparian and hillslope positions. Soil gas transport limited surface COâ‚‚ efflux in riparian landscape positions due to high soil water content (despite strong concentration gradients), while efflux was gradient (production) limited in hillslope positions. This led to spring-fall reversal of maximum riparian and hillslope soil COâ‚‚ concentrations, with highest hillslope concentrations near peak snowmelt and highest riparian concentrations during the late summer and early fall. Soil temperature was a dominant control on the overall temporal variability of soil COâ‚‚. However, soil water content controlled differences in the timing of soil COâ‚‚ concentration peaks within and between riparian and hillslope positions, as exemplified by those locations closest to Stringer Creek (wetter landscape positions) peaking up to three months later than those riparian locations near the riparian-hillslope transition. This work suggests that one control on the spatial and temporal variability of watershed soil COâ‚‚ concentrations and surface COâ‚‚ efflux is a soil water content mediated tradeoff between COâ‚‚ production and transport.
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Slabbert, Etienne. „Microbial communities of riparian ecotone invaded by non-indigenous Acacias“. Thesis, Stellenbosch : Stellenbosch University, 2012. http://hdl.handle.net/10019.1/20367.
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Tufekcioglu, Mustafa. „Riparian land-use impacts on stream bank soil and phosphorus losses from grazed pastures“. [Ames, Iowa : Iowa State University], 2006.
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Nguyen, Uyen. „Multiscale Remote Sensing Analysis To Monitor Riparian And Upland Semiarid Vegetation“. Diss., The University of Arizona, 2015. http://hdl.handle.net/10150/556735.
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The health of natural vegetation communities is of concern due to observed changes in the climatic-hydrological regime and land cover changes particularly in arid and semiarid regions. Monitoring vegetation at multi temporal and spatial scales can be the most informative approach for detecting change and inferring causal agents of change and remediation strategies. Riparian communities are tightly linked to annual stream hydrology, ground water elevations and sediment transport. These processes are subject to varying magnitudes of disturbance overtime and are candidates for multi-scale monitoring. My first research objective focused on the response of vegetation in the Upper San Pedro River, Arizona, to reduced base flows and climate change. I addressed the correlation between riparian vegetation and hydro-climate variables during the last three decades in one of the remaining undammed rivers in the southwestern U.S. Its riparian forest is threatened by the diminishing base flows, attributed by different studies either to increases in evapotranspiration (ET) due to conversion of grasslands to mesquite shrublands in the adjacent uplands, or to increased regional groundwater pumping to serve growing populations in surrounding urban areas and or to some interactions of those causes. Landsat 5 imagery was acquired for pre- monsoon period, when riparian trees had leafed out but before the arrival of summer monsoon rains in July. The result has showed Normalized Difference Vegetation Index (NDVI) values from both Landsat and Moderate Resolution Imaging Spectrometer (MODIS) had significant decreases which positively correlated to river flows, which decreased over the study period, and negatively correlated with air temperatures, which have increased by about 1.4°C from 1904 to the present. The predictions from other studies that decreased river flows could negatively impact the riparian forest were supported by this study. The pre-monsoon Normalized Different Vegetation Index (NDVI) average values in the adjacent uplands also decreased over thirty years and were correlated with the previous year's annual precipitation. Hence an increase in ET in the uplands did not appear to be responsible for the decrease in river flows in this study, leaving increased regional groundwater pumping as a feasible alternative explanation for decreased flows and deterioration of the riparian forest. The second research objective was to develop a new method of classification using very high-resolution aerial photo to map riparian vegetation at the species level in the Colorado River Ecosystem, Grand Canyon area, Arizona. Ground surveys have showed an obvious trend in which non-native saltcedar (Tamarix spp.) has replaced native vegetation over time. Our goal was to develop a quantitative mapping procedure to detect changes in vegetation as the ecosystem continues to respond to hydrological and climate changes. Vegetation mapping for the Colorado River Ecosystem needed an updated database map of the area covered by riparian vegetation and an indicator of species composition in the river corridor. The objective of this research was to generate a new riparian vegetation map at species level using a supervised image classification technique for the purpose of patch and landscape change detection. A new classification approach using multispectral images allowed us to successfully identify and map riparian species coverage the over whole Colorado River Ecosystem, Grand Canyon area. The new map was an improvement over the initial 2002 map since it reduced fragmentation from mixed riparian vegetation areas. The most dominant tree species in the study areas is saltcedar (Tamarix spp.). The overall accuracy is 93.48% and the kappa coefficient is 0.88. The reference initial inventory map was created using 2002 images to compare and detect changes through 2009. The third objective of my research focused on using multiplatform of remote sensing and ground calibration to estimate the effects of vegetation, land use patterns and water cycles. Climate change, hydrological and human uses are also leading to riparian, upland, grassland and crop vegetation changes at a variety of temporal and spatial scales, particularly in the arid and semi-arid ecosystems, which are more sensitive to changes in water availability than humid ecosystems. The objectives of these studies from the last three articles were to evaluate the effect of water balance on vegetation indices in different plant communities based on relevant spatial and temporal scales. The new methodology of estimating water requirements using remote sensing data and ground calibration with flux tower data has been successfully tested at a variety sites, a sparse desert shrub environment as well as mixed riparian and cropland systems and upland vegetation in the arid and semi-arid regions. The main finding form these studies is that vegetation-index methods have to be calibrated with ground data for each new ecosystem but once calibrated they can accurately scale ET over wide areas and long time spans.
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Ensor, Breanne Leigh. „Spatial and Temporal Trends in Greenhouse Gas Fluxes from a Temperate Floodplain along a Stream-Riparian-Upland Gradient“. Thesis, Virginia Tech, 2016. http://hdl.handle.net/10919/71424.
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Increased floodplain and wetland restoration activity has raised concerns about potential impacts on the release of greenhouse gases (GHGs) to the atmosphere due to restored connectivity between aquatic and terrestrial ecosystems. Research has shown GHG fluxes from hydrologically active landscapes such as floodplains and wetlands vary spatially and temporally in response to primary controls including soil moisture, soil temperature, and available nutrients. In this study, we performed a semimonthly sampling campaign measuring GHG (CO2, CH4, and N2O) fluxes from six locations within a third-order stream floodplain. Site locations were based on dominant landscape positions and hydrologic activity along a topographic gradient including a constructed inset floodplain at the stream margin, the natural levee, an active slough, the general vegetated floodplain, a convergence zone fed by groundwater, and the upland area. Flux measurements were compared to abiotic controls on GHG production to determine the most significant factors affecting GHG flux from the floodplain. We found correlations between CO2 flux and soil temperature, organic matter content, and soil moisture, CH4 flux and pH, bulk density, inundation period length, soil temperature, and organic matter content. But minimal correlations between N2O flux and the measured variables. Spatially, our results demonstrate that constructed inset floodplains have higher global warming potential in the form of CH4 than any other site and for all other GHGs, potentially offsetting the positive benefits incurred by enhanced connectivity. However, at the reach scale, total CO2 flux from the soil remains the greater influence on climate since the area covered by these inset floodplains is comparatively much smaller than the rest of the floodplain.Master of Science
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Nelson, Amanda. „CARBON AND NITROGEN CYCLING IN GIANT CANE (ARUNDINARIA GIGANTEA (WALT.) MUHL.) RIPARIAN ECOSYSTEMS“. OpenSIUC, 2015. https://opensiuc.lib.siu.edu/dissertations/986.
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Large stands of Arundinaria gigantea (Walt.) Muhl., called canebrakes, were vital to wildlife and lowland ecosystem functions and historically covered millions of acres in the southeastern United States. Since European settlement, human disturbance (i.e, clearing for agriculture and fire suppression) has caused giant canebrakes to become critically endangered ecosystems. Increasing evidence suggests the loss of canebrakes has directly impacted riparian ecosystems, resulting in increased soil erosion, poorer water quality, and reduced flood control. Cane's ecological importance has led to an increased interest in canebrake restoration in riparian zones. To examine the role that cane plays in nutrient cycling and to attempt to determine targeted restoration sites, a four phase research strategy was designed to determine physical and chemical properties of existing riparian stands of native giant cane and their associated soils. Phase one was a GIS analysis to determine what geographical features may be used in selecting sites within a landscape suitable for canebrake restoration. First, common physical site characteristics for 140 existing southern Illinois canebrakes were determined. Soil taxonomy and pH were used to represent soil characteristics and percent slope was used as a topographic metric. These factors, combined with digital elevation models and land cover in GIS were used to identify the potential suitability of sites within the watershed for canebrake plantings and general riparian restoration. The following soil characteristics were determined to be associated with giant cane success: percentage of area containing slopes of 3 percent or less, fine to coarse-silty textures, pH of 5.3 - 6.7, effective cation exchange capacity of less than 30 units, available water holding capacity greater than 0.12, bulk density of 1.37 - 1.65 g cm-3, and percent clay of 11 - 55. Eighty-percent of existing giant cane sites were found within these slope and soil characteristics. The total area of potential riparian canebrake landscapes based on these parameters is 13,970 hectares (35,600 acres) within the Cache River watershed. The remaining three phases examined the role that cane plays in nutrient cycling. Phase two determined the pools and cycling of nitrogen and carbon in canebrakes and compared those to nearby agricultural and forested riparian areas. Phase three quantified the N2O and CO2 fluxes from canebrakes and adjacent forested areas. Phase four included methods to quantify nutrient content of leaf litter and live leaves from existing canebrakes to estimate the nutrient use efficiency of cane. Further, a decomposition study was conducted to calculate the decomposition rate of cane leaves and to explore the litter quality attributes of giant cane. The primary purpose of phase two was to compare the effects of perennial riparian vegetation (giant cane and forest) and annual crops on soil quality, nitrogen cycling, and physical properties. This was to determine if any of them have a significant influence on giant cane distribution, while focusing on nitrogen dynamics to help determine why giant cane is a successful riparian buffer species. Five study sites in the Cache River watershed that had cane, agricultural fields (corn-soybean rotation), and forested areas adjacent to one another were selected. Data were collected on soil texture, carbon/nitrogen ratios, bulk density, nitrogen content (as ammonia and nitrate), and net nitrogen mineralization rates. The crop sites had significantly lower soil C:N ratios than both forest and cane (9.8:1 vs. 10.9:1 and 10.7:1, respectively), though all sites had ratios less than 25:1, indicating a tendency toward nitrogen mineralization. Forest soils had significantly higher rates of net mineralization than cane (19.0 μg m-2 day-1 and 6.6 μg m-2 day-1, respectively), with crop not significantly different from either cane or forest (8.0 μg m-2 day-1). Cane had higher levels of soil carbon and nitrogen when compared to forest and crop soils. Cane can be successful in wetter areas than previously thought, implying that the range of conditions that will support cane is broader than previously thought. Overall, there were few identifiable soil controls on giant cane distribution, or those that differentiate long-standing canebrakes from the nearby crop and forest land. For Phase three, nitrous oxide and carbon dioxide emissions were measured monthly for one year in riparian canebrakes and forests in southern Illinois to determine the rates of greenhouse gas (GHG) fluxes in bottomland riparian areas. Carbon dioxide emissions had a strong correlation with soil temperature (p < 0.001, r2= 0.54), but not with soil water content (p > 0.05), and were greater during the warmer months. Nitrous oxide emissions had a correlation with soil water content (p=0.470, r2 = 0.11), but no relation with soil temperature (p > 0.05), nor a difference across time. Vegetation type did not appear to influence GHG fluxes. Riparian CO2 and N2O emission rates were higher than documented cropland emissions, indicating riparian restoration projects to reduce NO3 delivery to streams may affect N2O and CO2 emissions resulting in an ecosystem tradeoff between water quality and air quality. Leaf deposition, N resorption efficiency and proficiency, and decomposition rates were analyzed in riparian stands of Arundinaria gigantea in southern Illinois for the first time in Phase four. Leaf litter was collected from five established canebrakes monthly over one year and a decomposition study was conducted over 72 weeks. Live leaves, freshly senesced leaves, and decomposed leaves were analyzed for carbon and nitrogen content. Leaf litterfall biomass peaked in November at twice the monthly average for all but one site, indicating a resemblance to deciduous leaf fall patterns. Nitrogen and carbon levels decreased 48% and 30%, respectively, between live leaves and 72 weeks decomposed. High soil moisture appeared to slow decomposition rates, perhaps due to the creation of anaerobic conditions. Cane leaves have low resorption proficiency and nutrient use proficiency, suggesting that these riparian canebrakes are not nitrogen limited. These results will help improve our understanding of the role that giant cane plays in a riparian ecosystem and help focus cane restoration efforts in southern Illinois.
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Fauver, Rebecca. „The impact of the invasive species, Lonicera maackii, on soil microbial communities in Riparian Forests“. Connect to resource, 2006. http://hdl.handle.net/1811/6625.
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Thesis (Honors)--Ohio State University, 2006.Title from first page of PDF file. Document formatted into pages: contains 13 p.; also includes graphics. Includes bibliographical references (p. 12-13). Available online via Ohio State University's Knowledge Bank.
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Goble, Michael Dane. „Allometry, Morphometry and Soil Characterization of Giant Cane [Arundinaria gigantea (Walt.) Muhl.] Stands in Southern Illinois“. OpenSIUC, 2013. https://opensiuc.lib.siu.edu/theses/1103.
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The effectiveness of giant cane [Arundinaria gigantea(Walt.) Muhl.] as riparian buffer vegetation has been demonstrated through research and has gained interest from state and federal agencies to support restoration efforts. Unfortunately, little is known about the physical and chemical properties of the soils below canebrakes and how soil characteristics influence aboveground and belowground biomass production. To determine what physical attributes of the plant influence its success as riparian buffer vegetation and also to determine the interactions with underlying soils, fourteen canebrakes were sampled throughout Southern Illinois. Objective one was to develop an allometric equation to quantify belowground biomass based on aboveground parameters of canebrakes. Previous research found that successful propagation was dependent on rhizome length, the number of internodes and the number of rhizome buds present, but no data exists regarding the yield of rhizomes for a given area. By harvesting all aboveground biomass (culms and leaves) and belowground biomass (roots and rhizomes) to a depth of 25 cm from a 1-m2 plot at each site, morphometric characteristics were quantified and biomass allocation throughout the plant was determined. A significant linear relationship between total aboveground biomass (live and dead) and belowground biomass in giant cane was evident (R=0.865, p<0.001). Although this is a strong relationship, it may be impractical for a manager to harvest, process, and weigh all of the aboveground biomass to speculate the biomass below ground. Therefore, metrics were explored for predicting the length of rhizome, number of rhizome internodes and number of rhizome buds an area will yield using multiple regression and models were developed that estimate these parameters. Using the equation that predicts the number of rhizome buds for a given area, the yield of propagules can then be estimated. Although this equation does not account for all variation of belowground characteristics, it will provide a general guideline for land managers restoring giant cane. The second objective was to estimate biomass allocation of giant cane roots/rhizomes beneath canebrakes by depth (i.e., at 25-cm increments to a depth of 150 cm). Results showed that 67% of giant cane's belowground biomass was within the top 25 cm of the soil profile and accounted for 65% of all belowground biomass encountered at that depth. Giant cane rhizomes were documented to a depth of 51-75 cm deep while cane roots existed in the deepest cores at a depth of 126-150 cm with an average density of 0.08 kg m-3. Giant cane belowground biomass declined with increasing depth, but was still the dominant species at 26-50 cm, comprising 61% of all biomass encountered at that depth. These results support the utility of giant cane as an effective riparian buffer species by increasing the soil porosity and promoting infiltration while contributing a significant source of carbon to the soil profile. Chemical and physical soil properties were measured to determine if they related to canebrake characteristics. Significant correlations were found between various soil properties and canebrake characteristics, implying there is an interaction between giant cane and the underlying soil. Results from this research will improve our understanding of the dynamics of giant cane and supplement existing information to help guide restoration efforts.
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Rhoades, Erica L. „Quantifying bank erosion on the South River and its importance in assessing mercury contamination“. Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file, 82 p, 2008. http://proquest.umi.com/pqdweb?did=1597631421&sid=7&Fmt=2&clientId=8331&RQT=309&VName=PQD.
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Galera, Leonardo de Aro. „Carbon sequestration potential of the soil in the restoration of riparian forests of the Corumbataí basin (SP)“. Universidade de São Paulo, 2018. http://www.teses.usp.br/teses/disponiveis/64/64135/tde-13112018-114443/.
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The soil organic matter is the largest carbon reservoir among terrestrial reservoirs and its very important in the regulation of the climate at global scale. Strategies to increase soil organic carbon (SOC) stocks includes afforestation and reforestation and the adoption of recommended management practices (RMPs) like no-till farming and cover crops. The replacement of forestland by agriculture may deplete SOC stocks, by decreasing C input to the soil and increasing the decomposition of organic matter. The Brazilian Forest Code (FC) requires landowners to conserve native vegetation by means of Legal Reserve and Areas of Permanent Preservation (APPs), which includes Hilltop Preservation Areas and Riparian Preservation Areas. It is well known that riparian vegetation provides many ecosystem services, like biodiversity conservation and increasing water availability and quality. Another potential ecosystem service is the mitigation of climate change by accumulating carbon in the vegetation and SOM. The reforestation of riparian zones represents an important opportunity for carbon sequestration and the mitigation of climate change in Brazil, as these restorations are mandatory under the Forest Code. The goal of this study is to contribute with the discussion about the role of riparian forests in the mitigation of climate change. In order to achieve this goal, we compare the SOC stocks of forested riparian areas with the SOC stocks of agricultural areas, namely pasture and sugarcane. Forested soils had an average SOC stock of 44 Mg.ha-1 while pasture had 26 Mg.ha-1 and sugarcane 27 Mg.ha-1. Based on the estimates of the SOC stocks situation after the reforestation of the riparian zones of the 50 sub-watersheds sampled, we could foresee an accretion of 20% of organic carbon in the 0-30 cm soil layer of those areas. We hope that this work contributes to the understanding of the role of the riparian forests in the mitigation of climate change and that the inclusion of the reforestation of those ecosystems in the mitigation strategies options may highlight the urgency in sparing them from devastationA matéria orgânica do solo é o maior reservatório de carbono entre os ambientes terrestres e é muito importante na regulação do clima em escala global. As estratégias para o aumento dos estoques de carbono do solo incluem o reflorestamento e a adoção de práticas recomendadas de manejo como o plantio direto e o uso de culturas de cobertura. A substituição de florestas por áreas agrícolas pode reduzir os estoques de carbono do solo ao diminuir a aporte de carbono e aumentar a decomposição da matéria orgânica. O Código Florestal obriga proprietários de terra a conservar a vegetação nativa por meio de Reserva Legal e Áreas de Preservação Permanente, que inclui topos de morro e áreas ripárias. Sabe-se que florestas ripárias provêm diversos serviços ambientais como a conservação da biodiversidade e o aumento na disponibilidade e qualidade da água. Outro possível serviço ambiental é a mitigação das mudanças climáticas pelo acúmulo de carbono na vegetação e no solo. A restauração das zonas ripárias representa uma importante oportunidade para o sequestro de carbono no Brasil, já que são obrigatórias segundo o Código Florestal. O objetivo deste estudo é contribuir com a discussão sobre o papel das florestas ripárias na mitigação das mudanças climáticas. Foram comparados os estoques de carbono de florestas ripárias com os de áreas agrícolas, no caso pastagens e canaviais. O estoque de carbono médio dos solos florestais foi de 44 Mg.ha-1, dos de pastagem foi de 26 Mg.ha-1 e dos sob canaviais foi de 27 Mg.ha-1. Baseado nesses valores, o impacto do reflorestamento das zonas ripárias (30 m) das 50 microbacias amostradas foi estimado, e segundo essa estimativa haveria um acréscimo de 20% de carbono na camada de 0-30 cm destas áreas. Esperamos que este trabalho contribua no entendimento do papel das florestas ripárias na mitigação das mudanças climáticas e que a inclusão da restauração destes ambientes como opção de estratégia de mitigação enfatize a urgência em preservá-los
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Gu, Sen. „Release of dissolved and colloidal phosphorus from riparian wetlands : a field and laboratory assessment of the mechanisms and controlling factors“. Thesis, Rennes 1, 2017. http://www.theses.fr/2017REN1S063/document.
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Le phosphore (P) est un nutriment essentiel dans le contrôle de l'eutrophisation des eaux de surface. La majorité du P causant cette eutrophisation dans les pays occidentaux est aujourd'hui issu des sols agricoles, ce qui explique pourquoi les recherches actuelles sur l'eutrophisation se focalisent sur la compréhension des mécanismes par lequel le P est relargué de ces sols. Dans cette thèse, nous étudions ces mécanismes en nous focalisant sur la fraction dissoute (DP) du P, fraction la plus menaçante du point de vue de l'eutrophisation. Une double approche a été utilisée, combinant le suivi de la composition d'eaux du sol et d'eaux de ruisseau dans un petit bassin versant (BV) agricole représentatif (BV de Kervidy-Naizin, France) et des simulations expérimentales au laboratoire. Les suivis de terrain ont révélé que les zones humides ripariennes (RW) étaient les principales zones de relargage de DP dans le BV étudié, via deux mécanismes essentiellement déclenchée par les fluctuations des hauteurs de nappe, i) la réhumectation des sols (DRW) et ii) la dissolution réductrice des oxydes de fer du sol dans de périodes d'anoxie. Ces mêmes suivis ont révélé la présence de fortes variations spatiales de la nature chimique (inorganique et organique/colloïdale) du DP relargué. Les variations saisonnières et interannuelles de l'hydroclimat, combinées aux variations locales de topographie ont été démontrées être les deux facteurs principaux contrôlant i) la fréquence des épisodes DRW, et ii) la durée des périodes anoxiques, entraînant au final de fortes variations saisonnières et interannuelles de la dynamique de relargage du DP. Comme indiqué dans un modèle conceptuel général, la topographie est sans doute le facteur clé de contrôle des variations observées, en raison de son rôle sur i) le transfert de P à partir des parcelles agricoles amont, ii) le taux de minéralisation du P organique du sol P et iii), le déclenchement des deux mécanismes de relargage précités. Les expériences en laboratoire ont confirmé le rôle des événements DRW comme processus clé causant le relargage de DP dans les RWs. Les résultats ont démontré que le DP relargué consistait non seulement de "vrai" DP inorganique et organique, mais aussi de P colloïdal, le P colloïdal et le DP organique étant les plus réactifs aux événements DRW. Les données ont aussi révélées que ces différentes formes de P provenaient de différentes sources dans le sol (méso et macroporosité pour P colloïdal et le DP organique; microporosité pour DP inorganique), et que la quantité de P colloïdal relargué était positivement corrélée avec la teneur en matière organique et la taille de biomasse microbienne du sol. Ces mêmes expériences ont confirmé le rôle des conditions anoxiques comme conditions favorisant la libération de DP dans les RWs. La dissolution réductive de sol Fe-oxyhydroxydes n'est cependant pas le seul processus impliqué, un autre processus étant la hausse du pH causée par des réactions de réduction. Les résultats obtenus démontrent que l'augmentation de pH contrôle la libération de DP dans les sols riches en matière organique, alors que ce relargage est contrôlé principalement par la réduction des oxydes de fer dans les sols pauvres en matière organique. Les données expérimentales démontrent également que l'apport de sédiments issus des sols agricoles amont accroit le relargage de DP dans les RW, probablement en raison de la dissolution des oxydes de fer de ces mêmes sédiments par les bactéries ferroréductrices des Rws. Au final, cette thèse permet de mieux contraindre les mécanismes et facteurs responsables du relargage de DP dans les bassins versants agricoles. Une conséquence très pratique de ce travail est que la conception de stratégies pour limiter les fuites de DP dans ces bassins ne peut se faire sans une prise en compte des rôles de l'hydroclimat, de la topographie locale et des propriétés du sol sur ce relargagePhosphorus (P) is a key nutrient in controlling surface water eutrophication. Because of the decrease of urban and industrial P emissions, most of the P nowadays causing surface water eutrophication in western countries consists of P transferred from agricultural soils, explaining why current eutrophication research focused on understanding the mechanisms by which P is released from soils. In this thesis, we studied these release mechanisms for dissolved P (DP) – i.e. the most bioavailable P component for algae - using an approach combining field monitoring of soil and stream water compositions in a small, headwater catchment typical of western countries agricultural catchments (the Kervidy-Naizn catchment, France), and laboratory experimental simulations. Field monitoring data revealed that riparian wetlands (RW) are the main zones of DP release and DP production in the studied catchment, through essentially two mechanisms triggered by groundwater table fluctuations, namely i) rewetting of dry soils (DRW), and ii) reductive dissolution of soil Fe (hydr)oxides during anaerobic periods. Field monitoring data also revealed the presence of strong spatial variations in the chemical nature (inorganic vs. organic/colloidal) of the released DP, which was in relation to differences in soil properties and local topography. Seasonal and inter-annual hydroclimate variations, combined with variations in local topography were found to control the frequency of soil DRW events and duration of anaerobic periods, resulting in strong seasonal and inter-annual variations of DP release dynamics. As shown in a conceptual model, topography is likely to be the key driver of the observed spatial and temporal variations, because of its combined control on i) the transfer of P from upland fields to RW zones, ii) the mineralization rates of soil organic P and iii) the triggering of the above two release mechanisms. Laboratory leaching experiments on the same soils confirmed the role of DRW events as a major process causing DP release pulses in RWs. The data demonstrated that the released DP consisted not only of true dissolved inorganic and organic P but also of colloidal P, the latter phase being the most reactive to DRW events. The data also revealed that the different P forms came from different P sources in the soil (soil macro/mesopores for colloidal P and organic DP; soil micropores for inorganic DP) and that the amount of released colloidal P correlated positively with the organic matter contents and soil microbial biomass size of the soil. Anaerobic incubation experiments, on their hand, confirmed the role of anoxic conditions as conditions favoring the release of DP in RW. Reductive dissolution of soil Fe-oxyhydroxide was, however, not the sole process involved in that release, another process being the rise in pH caused by reduction reactions. Experimental data showed that the pH rise controlled the DP release in organic-rich soils, this release being on the contrary mainly controlled by soil Fe-oxyhydroxides reductive dissolution in organic-poor soils. Experimental data also showed that the input of soil sediments from upland fields enhanced the release of DP in RW, most likely due to the enhanced dissolution of sediment Fe-oxyhydroxides by RW Fe-reducing bacteria. Overall, this thesis allowed new constraints to be placed on the release mechanisms of DP in headwater agricultural catchments. One very practical output is that great care should be taken of hydroclimate variability, local topography, and soil property when designing and implementing management options to reduce DP release and transfer in agricultural catchments
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Moore, Erin Amanda. „An analysis of solute transport on a harvested hillslope in the southern Appalachian Mountains“. Thesis, Virginia Tech, 2008. http://hdl.handle.net/10919/32758.
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Interest in transport of dissolved nitrogen (N) and carbon (C) in forested ecosystems is growing because of potential effects of these solutes on streamwater quality and implications for C sequestration. Additional research will further the understanding about the dynamics of these soil solutes, particularly in response to harvesting of forests. Also, the purported role of riparian buffers, where logging is restricted along stream channels, in retaining soil solutes is not well studied in the steeply sloping terrain of the southern Appalachian Mountains. I examined solute transport in a first-order watershed in the Nantahala National Forest in North Carolina that was harvested in February 2006 with retention of a 10-m riparian buffer.
To quantify the movement of dissolved inorganic nitrogen (DIN), dissolved organic nitrogen (DON), and dissolved organic carbon (DOC), four transects of lysimeters, approximately 30 m apart, were installed perpendicular to the stream on one hillslope. Porous ceramic cup (2-bar) lysimeters were installed in each transect 1, 4, 10, 16, 30, and 50 m from the stream in the A horizon and B horizon, and 4, 16, and 50 m from the stream in the saprolite layer. Samples were removed from the lysimeters 24 hr after 50 centibars of tension were placed on them, and riparian groundwater well and stream samples were collected at the same time as lysimeter samples. Collection of samples from the lysimeters, wells, and stream occurred every four to six weeks for one calendar year beginning March 2007. A 16-wk laboratory N mineralization study was conducted on A horizon soils.
Mean nitrate values in the soil solution of the A horizon in the spring were 1.53mg-N/L and decreased through the growing season to 0.030mg-N/L. Mean soil solution nitrate values in the B horizon and saprolite layer were 0.40mg-N/L in the spring and summer and decreased to 0.031mg-N/L in the winter. Mean soil solution ammonium concentrations were higher in the A horizon (0.090mg-N/L) than the B horizon and saprolite layer (0.034mg-N/L) and were lowest during the summer and fall. Dissolved organic C was significantly higher in the A horizon, with values ranging from 2.3mg/L to 599mg/L, than in the relatively stable B horizon and saprolite (1.9mg/L to 36.6mg/L). Dissolved organic C was logarithmically correlated to DON (r2 = 0.64), and DON values were highest in the A horizon (0.70mg/L). Cumulative N mineralization potential ranged from 48.1mg-N/kg to 75.6mg-N/kg and was not a useful predictor for nitrate soil solution values.
Nitrate leached vertically, and a large percentage of nitrate was stored in the B horizon and saprolite. Ammonium, DON, and DOC did not appear to leach vertically because they did not increase in the B horizon or saprolite layer. Ammonium, DON, and DOC are less mobile in soil solution than nitrate. The 10-m riparian zone had little impact on nitrate, ammonium, DON, and DOC removal. Nitrate remaining in the A horizon was likely removed through plant uptake in the harvested area before reaching the riparian zone. There was no detectable difference between ammonium concentrations in the harvested area and riparian zone likely because of limited mobility. The riparian zone did not remove excess DON or DOC, and in some transects was a source of DON and DOC. Nitrate and DOC concentrations were highly variable among transects and locations within transects. This may be caused by sensitivity of these solutes to site heterogeneity. This suggests that a large number of lysimeters should be used to account for this variability in future studies to ensure accuracy.
This study observed limited vertical leaching of ammonium, DON, and DOC through the profile. However, excess nitrate was observed moving from the A horizon into the B horizon and saprolite layer, suggesting the potential for delivery to the stream via subsurface transport and the need for attenuation of nitrate by the riparian zone. Because of low concentrations of nitrate entering the riparian zone during this study, the capacity for riparian attenuation of nitrate was not demonstrated.Master of Science
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Vosse, Shelly. „The restoration potential of fynbos riparian seed banks following alien clearing“. Thesis, Stellenbosch : University of Stellenbosch, 2007. http://hdl.handle.net/10019.1/3049.
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Thesis (MScConsEcol(Conservation Ecology and Entomology)--University of Stellenbosch, 2007.Riparian areas are highly complex systems with varying levels of disturbance that are highly susceptible to invasion by alien plants. Once invaded, riparian areas play a major role in the dispersal and spread of invasive alien plants (IAPs) through the river system and, in some cases, to neighbouring landscapes. Riparian areas have therefore been prioritized by many alien clearing initiatives in South Africa. Current practice for the restoration of cleared areas is minimal and relies mainly on the un-aided recovery of native species from residual individuals and soil stored seed banks. Little research, however, has been done on the effectiveness of this approach or the extent to which riparian seed banks contribute towards community restoration. This study is part of a national research initiative (Targets for Ecosystem Repair in Riparian Ecosystems in Fynbos, Grassland and Savanna Biomes) funded by Department of Water Affairs and Forestry, in collaboration with Working for Water, The Centre for Invasion Biology and the Universities of Cape Town, Stellenbosch, Rhodes and Witwatersrand. The initiative undertook to investigate different restoration techniques on various invaded sites for their cost-effectiveness, efficiency, practicality and conservation integrity. This study has three aims. The first is to determine the composition of seed banks in un-invaded riparian areas within the fynbos biome to be used as a benchmark for future research, restoration grading and other management requirements. The second aim is to determine the composition of seed banks in heavily invaded riparian areas, and thus to assess the impact of invasion on the integrity of the seed banks. The third aim is to evaluate the restoration potential of riparian seed banks following the clearing of invasive alien plants (IAPs). Study sites were selected within four river systems in the south-western part of the Western Cape Province in South Africa: the Berg, Eerste, Molenaars and Wit Rivers. Plots were selected in both invaded (>75% IAP canopy cover; considered “closed” alien stands) and un-invaded (also termed reference, with <25% IAP canopy cover) sections of the river. Replicate plots were established along varying gradients of elevation (mountain stream and foothill) and moisture regimes (dry, wet and transitional bank zones). Soil samples were collected together with above-ground vegetation surveys and comparisons were made. Results from this study confirm those of previous studies that seed banks offer little reference to current aboveground vegetation, but rather offer insight into past vegetation history as well as future vegetation assemblages. Worldwide, many of the species that characteristically form seed banks are early successional species. A community study was done for the seed bank based on the species that germinated and were identifiable at termination of the project (6 months after initiation). Three clusters of species could be identified. One group comprised 32 generalist species that occurred in both reference and invaded sections of the rivers. A second group comprised 39 species associated with invaded sites, and a third group of 40 species that was associated with reference sites. A few sub-community groups were found within both the “reference” and “invaded” community groups which were assumed to be habitat specific. Most species were “pioneer” or relatively-short lived, early-successional species which play a vital role in the initial post-disturbance vegetation cover, and facilitate establishment of later successional species. Seed banks are notoriously variable over space and time, and floristic representation is often biased as a result of differences among species in seed production, dispersal and longevity in the soil. The general consensus is that seeds have an irregular, clustered spatial distribution that is dictated by both biological and environmental factors. Within river systems, the irregular clustering can be exceptionally skewed with the influence of pockets of high sediment deposition along the bank. Environmental factors that were found to significantly skew germination results were the presence of fire, as well as the extent and intensity of invasion (duration and cover). The high level of diversity and abundance in reference Berg River mountain stream seed banks was perceived to be a direct result of a moderate fire frequency (between 8-15 years) and the relatively natural state of the vegetation (i.e. very little invasion). Also, diversity and richness of indigenous species from the Wit and Molenaars Rivers were substantially higher in the invaded samples than the reference samples, probably because both river systems have a long history of invasion and other anthropogenic disturbances which would have an effect on the samples from “reference” sections (i.e. even a 25% presence of IAPs seems adequate enough to alter the composition of the seed bank). Correspondence analyses showed that species had clear affinities towards different levels of “key” riparian environmental variables (fire, invasion and anthropogenic disturbance). Most species were associated with moderate levels of fire frequency, invasion history, and anthropogenic disturbance. Comparisons of seed bank species assemblages between the lateral and longitudinal variables of the rivers offered insights into the habitat requirements of certain fynbos and riparian species. Most significant were the results from bank zone comparisons which showed distinct species groupings along the different moisture bands. As could be expected, riparian species were best represented within the wet bank zones and fynbos species within the dry bank zone, while species characteristic of both zones occurred in the transitional zone, making this seed bank zone the richest in species. Mountain stream sections were richer and more diverse than foothill sections over both invaded and reference samples. This is hypothesised to be linked to lower levels of anthropogenic disturbance experienced in the mountain stream sections. The impact of invasion on the riparian seed bank was most clearly shown through the correspondence analyses for the 20 most frequently occurring species. The seed bank assembly patterns were clearly defined by the state of the river (reference or invaded). Interestingly, this pattern was evident at all three spatial scales; landscape (rivers), reach (mountain stream and foothill sections) and habitat (dry, wet and transitional zones). The reference seed bank assemblage was more tightly grouped, implying that the species were more closely associated with each other and less variable than those of the invaded seed bank assemblages. The species groupings within the invaded seed banks were influenced by variables such as reach and zone, whereas the reference seed bank assemblages seem relatively unaffected by these variables. This implies that the presence of invasive alien plants creates additional variation within the seed bank which alters the natural groupings. At a broad scale, the invaded seed banks were less species rich. This means that not only will the resulting seedling community be harder to predict, but it will also have fewer species. However although generally lower in species richness, the seed banks from almost all invaded rivers interestingly showed a higher diversity of indigenous species than their reference counterparts. This is very promising in terms of rehabilitation of post-cleared riparian sites, but more information is needed to understand the seed bank composition and determine how sustainable the seed banks are for rehabilitation in the long-term. All invaded sections had fewer herbaceous perennial species but more herbaceous annual species. Graminoids made up 50% or more of the seed bank regardless of state (reference or invaded), while woody species (shrubs/shrublets) were generally more prevalent in the reference samples. These results imply that following the removal of invasive alien plants, the vegetation to regenerate from the seed bank is likely to comprise of short-lived, herbaceous species that are not necessarily an accurate reflection of the indigenous riparian community. It is however important to note that this study investigated only the species that were able to germinate over the study period (6 month germination period). Many riparian species may not have been represented because they are either late germinators or may not be present in the soil seed bank at all. In order to gain a holistic understanding of riparian community recruitment, it is recommended that seed bank studies such as this one be included in a more broad scale, long term investigation which takes into account various reproductive strategies used by riparian species. Research of this nature is in its infancy worldwide and there are many challenges involved in measuring diversity and change in these systems. However, within the scope of this study, I suggest that these results shed light on previously unanswered and important questions regarding the ecology of seed banks in the riparian ecosystems of the Western Cape.
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Arthur, Robson Clayton Jacques. „Análise da redistribuição do \"fallout\" do 137Cs na avaliação da erosão e deposição de sedimentos em sistemas de manejo de solo sob Cerrado“. Universidade de São Paulo, 2010. http://www.teses.usp.br/teses/disponiveis/64/64134/tde-06052010-151125/.
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No Brasil, a expansão das áreas agrícolas é o fator mais impactante da agricultura sobre os recursos naturais. Com a crescente ocupação do Cerrado pela agricultura, uma série de problemas ambientais decorrentes do desmatamento como a erosão e a compactação do solo estão surgindo causando transformações radicais na paisagem natural pela retirada de quase toda sua vegetação nativa. O sistema de plantio convencional (SPC) tem sido considerado uma forma de manejo inadequado pelas suas conseqüências freqüentemente irremediáveis de compactação e perdas de solo, ao passo que o sistema de plantio direto (SPD) possibilita a manutenção das condições do solo mais próximas ao ambiente natural, reduzindo assim as taxas de erosão hídrica. Este trabalho teve por objetivo avaliar a eficiência da mata ripária na retenção dos sedimentos originados por três sistemas de preparo de solo através da técnica da análise da redistribuição do fallout do 137Cs, da Equação Universal de Perdas de solo (EUPS) e de alguns parâmetros físicos e químicos indicadores das condições estruturais do solo, em Goiatuba e Jandaia-GO. Nas três áreas estudadas, com auxilio de um trado tipo caneca, foram tomados perfis de solo em três camadas de 20 cm (0-20, 20-40 e 40-60 cm) em pontos distintos localizados ao longo de transeções lineares no sentido do declive até a mata ciliar localizada a jusante das áreas de estudo. Nas matas ciliares de cada área de estudo foram abertas trincheiras e amostras de solo coletadas para avaliação da atividade de 137Cs e dos parâmetros físicos e químicos dos solos. As amostras de solo coletadas nas transeções e trincheiras (TFSA) foram analisadas quanto à atividade de 137Cs em um detector de raios gama (GEM-20180P, EG&ORTEC) acoplado a um analisador multicanal. Na comparação das médias usou-se o teste de Tukey ao nível de 5% de significância. Os resultados obtidos indicaram que os três sistemas de manejo do solo apresentaram elevadas taxas de erosão e deposição de sedimentos e as matas ciliares à jusante das áreas sob SPC, SPD e pastagem, receberam grandes quantidades de sedimentos. Entre essas, somente a mata ciliar da área de SPC foi capaz de reter os sedimentos com eficiência. As características distintas dos três locais de estudo sugerem que a eficiência da mata ciliar na retenção dos sedimentos gerados na área agrícola e na pastagem, dependente do comprimento e da declividade das vertentes e da largura da mata ciliar. Quanto aos parâmetros físicos avaliados, observou-se que a pastagem e o SPD são os sistemas de manejo de solo que apresentaram melhores condições de preservação do solo em relação ao SPC. Os sistemas de manejo do solo provocaram alterações nos parâmetros físicos e químicos, comparados com a mata ciliar, destacando-se a menor resistência à penetração sob SPC e maior no SPD e pastagem; diminuição na agregação dos solos sob SPC e SPD e aumento sob pastagem e decréscimo nos teores de matéria orgânica e cálcio sob todos os sistemas de manejoIn Brazil, the expansion of agricultural areas causes several problems on natural resources. With the increasing occupation of the Cerrado region by agriculture, a series of environmental problems like deforestation, soil erosion and soil compaction are appearing and causing radical transformations in the natural landscape due to removing almost all native vegetation. The conventional tillage system (CTS) is considered an inadequate form of soil management for its frequently irremediable consequences of soil compaction and soil erosion, and the no till system (NTS) makes the maintenance of the soil conditions possible, leving them close to the natural environment, thus reducing rates of soil erosion. The objective of this work was to evaluate the efficiency of riparian forests in the retention of sediments originated for three different tillage systems, through the fallout 137Cs redistribution technique, the Universal Soil Loss Equation (USLE) and some physical and chemical parameters that indicate the structural conditions of the soils of Goiatuba and Jandaia-GO. In the three areas, soil profiles were collected in three layers of 20 cm (0-20, 20-40 and 40-60 cm) at distinct points located along linear transects in the direction of the maximum slope until the riparian forest. In the riparian forest of each area, trenches were opened and soil was sampled to evaluate the activity of 137Cs and the physical and chemical parameters of soil. Detection of the activity of 137Cs was made with a gamma ray detector model (GEM-20180P, EG& ORTEC) connected to a multichannel analyzer. The comparison of averages was made using the Tukey test at 5% level of significance. The results indicated that, the three soil tillage systems presented high rates of soil erosion and deposition of sediments and the riparian forest of the areas under CTS, NTS and pasture, located downstream received great amounts of sediments, and that only the riparian forest of CTS was capable to trap the sediments with efficiency. The distinct characteristics of the three studied areas suggest that the efficiency of the riparian forest to retain the sediments generated in the agricultural and pasture areas, depends on the length and the slope of the transects, and of the width of riparian forest. Through the physical and chemical parameters it was observed that the pasture and the NTS were the soil tillage systems that presented the best conditions of soil preservation in relation to the CTS. The tree soil tillage systems caused alterations in the physical and chemical parameters, compared with the riparian forest, mainly by a lower resistance to penetration under CTS and a greater resistance in the NTS and pasture systems; reduction in soil aggregation under CTS and NTS and an increase under pasture, and decrease of organic matter and calcium under all tillage systems
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Kambaj, Kambol Oliver. „In situ and ex situ soil respiration in natural, Acacia-invaded and cleared riparian ecotones in the Fynbos Biome“. Thesis, Stellenbosch : Stellenbosch University, 2013. http://hdl.handle.net/10019.1/79854.
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Thesis (MScConEcol)--Stellenbosch University, 2013.ENGLISH ABSTRACT: Soil respiration (Rs) is a major component of CO2 emissions and the global carbon balance. In the context of global change it of interest to understand seasonal patterns of RS in fynbos riparian ecosystems, particularly in invaded-riparian ecotones of these Mediterranean type ecosystems (MTE's) in the Western Cape, South Africa. Riparian ecotones are three dimensional transitional zones that provide multiple ecosystem services and functions and they act as the linkage between terrestrial and aquatic ecosystems where key ecological and geomorphological processes occur. Riparian ecotones are highly prone to disturbance, and because of this reason are also vulnerable to invasion by invasive alien plants (IAPs), notably Acacia species. Invasion by IAPs is considered one of the major threats to global change and biodiversity causing extensive ecological, economical, and social impacts. In south-western Cape, more than two thirds of the riparian environment is invaded to some extent, IAPs replacing the well adapted native species along river systems. In particular, impact of IAPs on soil respiration (Rs) may be relevant, with consequences for ecosystem function and services. Clearing of invaded riparian zones initiated by the Working for Water program has been a successful in eradicating alien plants within riparian areas even though recovery after alien clearing is lagging at many sites, and knowledge on repair of ecosystem function is lacking. Various studies have generated knowledge on carbon cycling and Rs in forests, savanna, grasslands, tundra and Mediterranean shrublands, but little is known about Rs in riparian zones, and even less about soil CO2 efflux in invaded riparian fynbos riparian ecotones. The objective of this study was to contribute to a better understanding and quantifying the effect and impact of IAPs on carbon cycling between and across riparian ecotones with different invasion status: natural, invaded, and cleared. The study areas were located in the south-western Cape and measurements of Rs, soil temperature, soil moisture, root mass, litter mass, and soil properties were carried out in riparian soils of the mountain and transitional stream longitudinal river sections, and uplands fynbos areas of six different perennial river systems. In each site, four to five transects were laid out with one sampling site of each landscape position (wet bank, dry bank, and terrestrial areas) giving a total of 12 to 15 samples per site. Soil respiration measurements were taken over a period of two years, and were done seasonally. Results from this study showed that Rs was different among seasons with highest soil respiration rates in summer. Soil CO2 efflux increased in response to warm and dry conditions during summer, while seasonal soil CO2 efflux declined in autumn and winter in response to wet and cold soil conditions. The large increase in soil CO2 efflux response to warm and dry periods when temperature was 25 to 30 °C over all riparian sites and was highest in invaded sites compared to the natural and cleared sites. A significant difference was found between sites with different statuses with invaded sites leading seasonal Rs rates. Natural and cleared sites did not differ significantly in their CO2 efflux rates, suggesting that clearing of IAPs may put invaded ecosystems on a trajectory of restoration. There were also differences in terms of landscape positions; dry banks zones of the invaded sites had higher rates compared to wet banks and the uplands areas. Our results further suggest that roots are the most important component of overall Rs rates, rather than microbial respiration. When we incubated soils minus roots, little difference was evident, either when viewing the results by invasion status or by landscape position, which suggest that inherent soil differences in terms of microbial respiration were not different. We also use a trenching approach to further investigate this, and though we found Rs to decline significantly, trends later suggest that decomposition of fine and course roots likely obscured the decline in overall Rs due to root respiration. Overall, our results showed that clearing of invaded riparian zones will likely lead to successful restoration of soil functioning in terms of C cycling. Clearing of Acacia-invaded riparian ecotones will likely lead to a decline in root density, and which removes a major component of overall Rs. These results make the investigation of the C balance of invaded riparian ecotones and terrestrial areas critical in order to assess their contribution to regional C cycles.
AFRIKAANSE OPSOMMING: Grondrespirasie (Rs) is 'n belangrike komponent van CO2 uitstroming en die globale koolstofbalans. Binne die konteks van globale verandering is dit van groot belang om die seisoenale patrone van Rs in fynbos oewer ekosisteme, veral in indringer-oewer ekotone, in die Meditereense tipe ekosisteme (MTE's) in die Wes- Kaap, Suid- Afrika te verstaan. Oewerekotone is drie-dimensioneel oorgangssones wat veelvuldige ekosisteem dienste en funksies verskaf. Hulle dien as die verbinding tussen terrestriële en water-ekosisteme waar kern ekologiese en geomorfologiese prosesse plaasvind. Oewerekotone is hoogs vatbaar vir versteuringe, en as gevolg van hierdie rede, is hul ook kwesbaar vir indringing deur indringer plante (IAPs), veral Acacia spesies. Indringing deur IAPs word beskou as een van die groot bedreigings tot en met globale verandering en biodiversiteit, wat ekstensiewe ekologiese, ekonomiese, en sosiale impakte veroorsaak. In die suid- westelike Kaap word meer as twee derdes van die oeweromgewing tot 'n mate binnegedring. IAPs vervang die goed aangepaste inheemse spesies langs riviersisteme. Die impak van IAPs, spesifiek op grondrespirasie mag substansieël wees, met gevolge vir ekosisteem funksies en dienste. Opruiming van hierdie spesifieke oewer sones, geinisieer deur die Working for Water program, was suksesvol in die uitroeing van indringer plante binne oewer areas. Alhoewel herstel na indringer opruiming op baie terreine agter is, is kennis oor die herstel van ekosisteemfunksies gebrekkig. Verskeie studies het kennis ontwikkel oor koolstofsiklisering en Rs in woude, savanna, graslande, tundra en Meditereense struiklande, maar daar is minimale informasie oor oewersones,en nog minder oor grond CO2 uitstroming in indringer oewer fynbos en oewer ekotone. Die doel van hierdie studie is om 'n bydrae te lewer koolstofsiklisering beter te verstaan, en die impak van IAPs op koolstofsiklisering te kwantifiseer tussen en oor oewerekotone met verkillende indringer statusse: natuurlik, binnegedring en skoongemaak. Die studie areas was geleë in die suid- westelike Kaap, en maatstawe van Rs, grond temperature, grondvogtigheid, wortelmassa, plantafvalmassa, en grondeienskappe is uitgevoer in oewergrond van die berg en transisionele stroom longitudinale rivier seksies, asook terrestriële fynbos areas van ses verskillende standhoudende riviersisteme. In elke area is vier tot vyf transekte uitgelê met een monsternemingsarea van elke landskapsposisie (nat bank, droë bank en terrestriële areas) met 'n totaal van 12 tot 15 monsters per area. Grondrespirasie maatstawe is geneem oor 'n periode van twee jaar, en is seisoenaal uitgevoer. Resultate van die studie het getoon dat Rs verkil het tussen seisoene, met die hoogste grondrespirasietempo in die somer. Grond CO2 uitstroming het toegeneem in reaksie op warm en droë kondisies gedurende somer, terwyl seisoenale grond CO2 uitstroming afgeneem het in herfs en winter in reaksie op nat en koue grond kondisies. Die grootste toename in grond CO2 uitstroming was in reaksie op warm en droë periodes wanneer temperature gewissel het tussen 25 tot 30˚C oor alle oewersones, en was die hoogste in binnegedringde sones, vergeleke met die natuurlike en skoongemaakte terreine. 'n Beduidende verskil is gevind tussen terreine met verskillende statusse in CO2 uitstromingskoerse‚ 'n aanduiding dat opruiming van IAPs binnegedringde ekosisteme op 'n trajek van restorasie plaas. Daar was ook verskille in terme van landskapsposisies; droë bank sones van die binnegedringde terreine het hoër tempos gehad, vergeleke met die nat bank en die hoogland areas. Ons resultate dui verder aan dat wortels, eerder as mikrobiologiese respirasie, die mees belangrike komponente van Rs koerse uitmaak. Toe ons grond minus wortels inkubeer, is min verskille opgemerk, as gekyk word na die resultate deur indringer status of landskapsposisie, wat toon dit dat inherente grondveskille in terme van mikrobiologiese respirasie nie verskillend is nie. Ons het verder ook 'n sloot-benadering gebruik om verdere ondersoek hierop in te stel, en alhoewel ons bevind dat Rs aansienlik afgeneem het, dui neigings later aan dat afbraak van fyn en growwe wortels die afname in gehele Rs as gevolg van wortel respirasie waarskynlik verdoesel. Ons resultate dui daarop dat opruiming van binngedringde oewers klaarblyklik sal lei tot suksesvolle restorasie van grondfunksionering in terme van C siklisering. Opruiming van Acacia- binnegedringde oewer ekotone sal vermoedelik lei tot 'n afname in worteldigtheid, en wat 'n belangrike komponent van die gehele Rs kan verwyder. Hierdie resultate maak die ondersoek van die C balans van binngedringde oewer ekotone en terrestriële areas krities, om sodoende hulle bydrae tot streeksgewyse C siklusse te asseseer.
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Karlsson, Emil. „Multifaceted effects of competition and plant-soil feedbacks on Achillea millefolium grown in soil from a riparian meadow : Emil Karlsson - Umeå University - Thesis project - 60 hp“. Thesis, Umeå universitet, Institutionen för ekologi, miljö och geovetenskap, 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-181764.
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Competition between plant individuals and how plants alter soil properties are key processes which drive changes in plant communities over time. Estimating the relative importance of these processes and how they affect plant growth in different ecological contexts and communities is an active area of research. Furthermore, interdependencies between the two processes have been suggested to occur in many cases, but research in this area is also lacking. In this study, soil conditioned by common yarrow (Achillea millefolium) was collected from field plots and was then used in a growth chamber competition experiment, which controlled for plant-soil feedbacks. Measured soil properties such as soil pH, soil nitrogen, and soil texture were primarily used as background data in the experiment. Field parameters such as light availability, plant density, and grass to forbs ratio were used to predict optimal A. millefolium habitat in relation to other vascular plant species. The results indicate that A. millefolium was a weaker competitor than cornflower (Centaurea cyanus), while a positive plant-soil feedback effect was observed by A. millefolium grown in field soil. Intraspecific competition had a strong negative effect on A. millefolium growth when grown in non-conditioned soil, but not when grown in A. millefolium conditioned soil. Finally, competition and plant-soil feedbacks appeared to be additively affecting A. millefolium growth, meaning the plant-soil feedback effect did not have a disproportionate effect on competitive outcomes, or vice versa. The findings of this study can be of interest to conservationists or farmers who wish to predict how plant communities respond to plant competition and plant-soil feedbacks as processes.
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Fourie, Saskia. „The restoration of an alien-invaded riparian zone in grassy fynbos, South Africa“. Thesis, Rhodes University, 2013. http://hdl.handle.net/10962/d1003840.
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The most recent surveys in South Africa estimate that invasions are still increasing, despite substantial clearing efforts. Riparian systems in South Africa are particularly vulnerable to invasion by woody IAPs. This thesis addresses the restoration of alien‐invaded riparian systems, by investigating the factors that facilitate or constrain spontaneous recovery and influence the trajectories of succession. These factors include invasion history and management history, especially the use of fire. A seedling emergence approach was used to test the presence of a viable pre‐fire seedbank, and the effect of fire on the seed bank. The efficacy of some active restoration interventions was also tested, with the aim to return invasion‐resistant, indigenous vegetation with a structure and function representative of uninvaded sites. The findings of this study indicated the presence of a viable and persistent riparian soil seed bank, even after 30 years of intermtittent invasion as well as two fire cycles under invasion. It shows that the management practice of fell‐and‐burn resulted in high soil temperatures, and that this reduced the indigenous soil seed bank density, especially in the upper soil layer. Clear germination sequences and patterns of emergence over time for different species were observed during this study, with many species exhibiting delayed emergence relative to the timing of the fire event. It is proposed that manipulation of the season of fire could be used to selectively optimise the order of arrival and therefore superior recruitment of some species over others in the Eastern Cape fynbos, and thus alter the trajectories of recovery of vegetation towards a more desired state. Active restoration in the form of indigenous seed and plant additions resulted in a significantly higher indigenous cover after seven months, compared to a control (passive restoration) or restoring with grass. Indigenous cover and composition was also strongly influenced by lateral zonation, and some key guilds and species were missing or present in much lower densities compared to reference sites. Grass restoration significantly suppressed the regeneration of A. longifolia, as well as the regeneration of indigenous species. Biotic resistance can thus be achieved through restoration, and it could be a powerful tool in the management of IAPs, although the deliberate introduction of grass after clearing in fynbos also reduces biodiversity and could have unforeseen consequences to riparian function.
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Knighton, Leah Nicole. „Hydrologic and Biologic Responses of Anthropogenically Altered Lentic Springs to Restoration in the Great Basin“. BYU ScholarsArchive, 2019. https://scholarsarchive.byu.edu/etd/8578.
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Water is a limited and highly valued resource in the semi-arid Great Basin. Surface water sources are often small and widely spaced apart, comprising only 1-3% of the surface area of the overall landscape. Despite their small size, these springs and surrounding wet meadows have a substantial effect on the surrounding environment. Springs provide drinking water, forage and cover for livestock and wildlife, habitat for diversity of plant species and a resource for human-related activities. In recent years, many of these springs have become dewatered due to diversions of groundwater for municipal water and agriculture, and climatic shifts in precipitation affecting recharge. These hydrologic changes can cause a drop in the local water table that promotes a shift in the plant community from wetland-obligates to species that have more drought-tolerance. The root masses of the new plant community are insufficient to secure soils resulting in the erosion of the thalweg. This leads to channelization through the wet meadow, which drives the water table further underground. As degradation progresses, springs and wet meadows lose their ability to store water. The purpose of this thesis is to examine the responses of both the hydrologic and biologic factors to different springbox restoration techniques. Twenty-four spring sites were chosen in the Sheldon National Wildlife Refuge in northwestern Nevada. Each site was randomly assigned one of six different treatment designs. Variables for these studies included: surface soil moisture, soil moisture at varying depths, flow rates, water chemistry, plant community cover and frequency, biomass, wildlife visits and wildlife species numbers. We observed soil moisture increase over the majority of our sites, while flow rates only increased at the control sites. This may indicate that more water is being held in the soils around the spring source instead of being allowed to flow downstream. Biomass increased in four of our six treatments. All treatment types exhibited a similar effect on springs with none having a clearly more restorative effective than any others. This research suggests that springs in the Great Basin have unique characteristics and responses to restoration, and may need individualized approaches. Additionally, studies have shown that it may take many years for plant communities to recover after hydrologic restoration. Yearly variation caused by increased precipitation may be partially responsible for changes in hydrologic and biologic aspects of springs and wet meadows. Further data collection is needed to determine the true extent of treatment and yearly effects on spring restoration. In spite of the need for individualized approaches, restoration is possible. Simple solutions may be sufficient to recover hydrologic processes that maintain ecologic resilience.
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Maistrenko, Oleksandr. „Variation in Core and Accessory Parts of Genome of Escherichia Coli Isolated from Soil from Riparian Areas in New York State“. Thesis, North Dakota State University, 2016. https://hdl.handle.net/10365/28022.
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Escherichia coli is commensal bacteria and is a symbiont of the digestive system of vertebrates. Due to frequent deposition of E. coli into extrahost habitats (soil, water), approximately half of its population exists as free living organisms. It is unclear what genome-wide variation stands behind adaptation for extrahost habitat. This thesis applies a genome-wide association study approach to find genetic variation in core and accessory parts of genome of E. coli that is associated with 1) forest or agricultural field soil habitats and 2) with survival phenotype in soil microcosm. Gene composition analysis suggests that pan-genome of environmental E. coli is unlimited. Core and accessory genome contained variation associated with survival phenotype and with forest or field habitat.Federal Formula Funding (Hatch-Act)
ND-EPSCoR
Fulbright-STEP scholarship
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McGuire, Roberta Delehanty. „Transpiration, Growth And Survival Of Native Riparian And Introduced Saltcedar Trees In Mixed Stands On The San Pedro River, U.S.A“. Diss., The University of Arizona, 2015. http://hdl.handle.net/10150/556824.
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Western riparian zones have undergone significant landscape changes over the past several decades, with introduced saltcedar (Tamarix spp.) as a crucial component of this transformation. Saltcedar, now a dominating presence along many western rivers, due to its high tolerance to drought, salinity and stress, is considered to be a high-water-use plant that can desiccate disturbed river systems. Where native and saltcedar plant communities occur together, it is important to understand water use patterns and the physiological responses of each species to environmental stress factors, as a way to project an eventual course of succession processes and management options at a given site. Stress and disturbance in the form of reduced stream flows and land use changes may influence these interactions. Understanding the conditions that allow for saltcedar dominance is critical in determining riparian water budgets, and developing effective management strategies. Sap flux sensors were used to measure the physiological response of co-occurring communities of saltcedar and native trees to these environmental stress factors during the pre-monsoon period in early summer, a time of maximum stress for riparian vegetation. The results suggest that native trees are still competitive with salt cedar so that a mixed plant community is likely to continue on the San Pedro River on the condition that current groundwater levels and river flows are maintained. If base flows and depth to groundwater continue to decline, this competitive balance between saltcedar and native trees likely could change.
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Mardhiah, Ulfah [Verfasser]. „Determination of biotic and abiotic factors influencing soil structure development in a riparian system based on observational and experimental approaches / Ulfah Mardhiah“. Berlin : Freie Universität Berlin, 2015. http://d-nb.info/1068504838/34.
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Pringle, Keara Louise. „An Internship with the Ohio Environmental Protection Agency, Division of Surface Water: Understanding the Vegetation and Soil Conditions in Natural Riparian Forests“. Miami University / OhioLINK, 2017. http://rave.ohiolink.edu/etdc/view?acc_num=miami149333522985015.
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Cnossen, Peter D. „Streambank erosion: mechanisms and mitigation techniques“. Thesis, Virginia Polytechnic Institute and State University, 1987. http://hdl.handle.net/10919/101370.
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This report presents a study of the various mechanisms that may cause erosion of streambanks and the corresponding mitigation techniques used to combat them. The determination of each may depend upon a number of considerations. The source of the information comes from a variety of reports and papers, which are referenced in the text.
Of all the mitigation techniques available to prevent streambank erosion, fabrics will generally offer the most cost effective method. Fabrics have had a good service record since their inception approximately 20 years ago. Further, as the technology continues to advance, it seems likely that fabric applications in this area will only increase. However, there are some concerns that need to be addressed. These include, assessment of geotextile performance in long term use under the different forces it will be subjected to, clogging potential of fabrics for various soil distributions, and the type of fabrics, woven or nonwoven, used in these applications. These factors should become more clearly defined as long term case study data becomes available.M. Eng.
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Lakel, William. „Effects of Forestry Streamside Management Zones on Stream Water Quality, Channel Geometry, Soil Erosion, and Timber Management in the Virginia Piedmont“. Diss., Virginia Tech, 2008. http://hdl.handle.net/10919/28619.
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The major study objectives include determining if a 50-foot streamside management zone (SMZ) as described in the Virginia BMP Manual (VDOF 2002) is generally sufficient to protect stream water quality, riparian soils, and stream bank integrity in headwater streams where forest harvesting has taken place, as well as comparing other SMZ widths with regard to the same environmental protection performance. In 2003, 16 forested watersheds were clear-cut harvested for commercial timber production. Four SMZ treatments were installed across four experimental blocks during harvest. Each of the 16 watersheds was subsequently site-prepared with prescribed burning and planted with loblolly pine (Pinus taeda). Within the watersheds, the established treatments were a 100-foot width with no thinning, a 50-foot width without thinning, a 50-foot width with thinning, and a 25-foot "stringer.â Each of the four treatments was conducted within three of four blocks (Incomplete Block Design). After a two-year post-harvest monitoring period, it was determined that the SMZ treatments had no significant effect on water quality, channel geometry, or soil erosion in and around the streams. There was no apparent water quality degradation as a result of harvesting timber, and larger SMZs did not have an impact on any of the parameters studied. It was also apparent that leaving narrower SMZs or thinning within SMZs did not cause any apparent environmental degradation. It was also determined that landowners who leave SMZs on their property have very limited opportunities to manage timber within them for financial gain in the long term.Ph. D.
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Dean, Katie L. „Vertical distribution of soil water use and maintenance of stomatal conductance in the invasive exotic plant Lepidium latifolium in the riparian zone of the Walker River“. abstract and full text PDF (UNR users only), 2009. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1472950.
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