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Holowaty, Nadja Deyglun. "Floodplain management in Quebec : a case study of the Mille Iles River floodplains". Thesis, McGill University, 1985. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63232.
Pełny tekst źródłaWolfe, Brian Paul. "Floodplains and the Proximate Principle: A Case for Floodplain Linear Parks in Roanoke, Virginia". Thesis, Virginia Tech, 2005. http://hdl.handle.net/10919/33151.
Pełny tekst źródłaMaster of Landscape Architecture
Sims, Neil C., i n/a. "The landscape-scale structure and functioning of floodplains". University of Canberra. Resource, Environmental & Heritage Sciences, 2004. http://erl.canberra.edu.au./public/adt-AUC20050706.095439.
Pełny tekst źródłaNatho, Stephanie. "Modelling nutrient retention in floodplains". Doctoral thesis, Humboldt-Universität zu Berlin, Mathematisch-Naturwissenschaftliche Fakultät II, 2013. http://dx.doi.org/10.18452/16854.
Pełny tekst źródłaAlthough there are detailed studies on nutrient retention in single wetlands and floodplains, the role of riparian floodplains for nutrient retention is not investigated very well on a landscape scale, since knowledge on the most important parameters for nutrient retention, inundated floodplains and incoming load, is insufficient. Additionally, a method for describing these parameters as discharge dependent variables is missing. Therefore, the present work analyzes the flooding frequencies on floodplains of three study rivers, Elbe, Main and Rhine. The relation of inundated floodplain extent and current discharge conditions based on detailed results of the established Software Flys is deduced empirically. Based on these subsequently generalized results, finally event related average inundated floodplain extent respectively, incoming nutrient loads are calculated by considering the effects of the hydrologic conditions of each river system. Therefore, available geodata as well as data on water quality and discharge is processed and serves as input data for yearly and monthly empirical retention models. The calculated nutrient retention in floodplains varies with hydrological connectivity of the floodplain to the surface waters as well as with the current hydrologic condition of the river system. For this reason the finally developed concept of event related nutrient retention is suggested as the most realistic in combination with hydro-exponential retention models. The Elbe floodplains are the most natural, and in years with high floods nutrient retention in the floodplains contributes up to 9% respectively 10% of the monthly transported load of TP and NO3-N, which is significant. The transfer of the results to a German-wide application is possible due the generalization of the methods carried out. With the presented results the hydrology dependent role of floodplains for nutrient balances in river systems can be quantified on a landscape scale.
Shepherd, V. "Beetle diversity of chalk river floodplains". Thesis, University College London (University of London), 2014. http://discovery.ucl.ac.uk/1420432/.
Pełny tekst źródłaBrill, Katie Ellen. "Impacts of inundation and season on greenhouse gas fluxes from a low-order floodplain". Thesis, Virginia Tech, 2013. http://hdl.handle.net/10919/19213.
Pełny tekst źródłaMaster of Science
Leigh, Catherine. "Floodplain River Function in Australia's Wet/Dry Tropics, With Special Reference to Aquatic Macroinvertebrates and the Gulf of Carpentaria". Thesis, Griffith University, 2009. http://hdl.handle.net/10072/367453.
Pełny tekst źródłaThesis (PhD Doctorate)
Doctor of Philosophy (PhD)
Griffith School of Environment
Science, Environment, Engineering and Technology
Full Text
Pernik, Maribeth. "Mixing processes in a river-floodplain system". Thesis, Georgia Institute of Technology, 1985. http://hdl.handle.net/1853/19514.
Pełny tekst źródłaRose, 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.
Pełny tekst źródłaTaylor, Mark P. "Holocene sedimentation in River Severn catchments". Thesis, Aberystwyth University, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.337496.
Pełny tekst źródłaKruske, Montana L., i Dr Eileen G. Ernenwein. "Paleochannel or Palisade? Preliminary Geophysical Investigations of a Linear Feature at the Runion Archaeological Site, Washington County, Tennessee". Digital Commons @ East Tennessee State University, 2019. https://dc.etsu.edu/asrf/2019/schedule/74.
Pełny tekst źródłaSims, Neil C. "The landscape-scale structure and functioning of floodplains". Connect to this title online, 2004. http://cicada.canberra.edu.au/public/adt-AUC20050706.095439/.
Pełny tekst źródłaTitle from PDF title page (viewed on July 20, 2005). Pages 185-194 lacking in digital version of thesis. Includes bibliographical references (p. 155-184).
Weatherholt, Laura. "Floodplains on the prairie: an ecological schoolyard design". Kansas State University, 2012. http://hdl.handle.net/2097/13767.
Pełny tekst źródłaDepartment of Landscape Architecture, Regional and Community Planning
Mary Catherine (Katie) Kingery-Page
Man has been learning in the outdoors since the beginning of humankind. Modern times have reduced the amount of time people spend learning and exploring outside. This causes humans to be disconnected from the natural environment. By making schoolyards more environmentally focused, conducive to outdoor education and play, formal education can return to the original classroom–nature– and inspire people to reconnect with their environment. Much literature supports the ideas of aligning the efforts of play and education, environmental interpretation and education, and outdoor education with formal education; by incorporating all of these elements in a schoolyard, the potential for enriched learning is greatly increased. This project explores nature interpretation strategies used by public botanic gardens and translates these strategies to an ecological schoolyard. At Northview Elementary School in Manhattan, Kansas, the students face a simple, sterile play-yard with flooding limiting site use after storm events. The design for Northview Elementary will integrate stormwater features with school needs into a new ecological master plan for campus. Interpreting this landscape using the strategies adapted from botanical gardens for educational approaches, methods, and interpretive displays, provides the school and community a resource to enhance their lives, education, and the environment.
Truchan, Jessie J. "Genesis of Carbonate Lakes on Perennial Siliciclastic Floodplains". Ohio University / OhioLINK, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1242778273.
Pełny tekst źródłaWerth, David E. Jr. "Predicting Resistance and Stability of Vegetation in Floodplains". DigitalCommons@USU, 1997. https://digitalcommons.usu.edu/etd/4459.
Pełny tekst źródłaAnderson, Michelle Louise. "The edge effect lateral habitat ecology of an alluvial river flood plain /". Diss., [Missoula, Mont.] : The University of Montana, 2009. http://etd.lib.umt.edu/theses/available/etd-10012008-134442/.
Pełny tekst źródłaWestwater, David. "Modelling hydrodynamic and shallow water processes over vegetated floodplains". Thesis, Cardiff University, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.391534.
Pełny tekst źródłaBrooker, Michael R. "Physical and Chemical Characterization of Self-Developing Agricultural Floodplains". The Ohio State University, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=osu1513778530623727.
Pełny tekst źródłaYu, Dapeng. "Diffusion-based modelling of flood inundation over complex floodplains". Thesis, University of Leeds, 2005. http://etheses.whiterose.ac.uk/3360/.
Pełny tekst źródłaLeigh, Catherine. "Floodplain river function in Australia's wet/dry tropics, with specific reference to aquatic macroinvertebrates and the Gulf of Carpentaria". Thesis, Griffith University, 2009. https://eprints.qut.edu.au/119606/1/Leigh_2009_02Thesis.pdf.
Pełny tekst źródłaBogoni, Manuel. "Long-term evolution of meandering rivers flowing above heterogeneous floodplains". Doctoral thesis, Università degli studi di Padova, 2017. http://hdl.handle.net/11577/3424896.
Pełny tekst źródłaLe piane alluvionali e i relativi fiumi costituiscono complessi sistemi dinamici la cui simulazione numerica richiede la modellazione di processi idrodinamici, morfodinamici, chimici e biologici agenti mutuamente su varie scale temporali (dai giorni ai secoli). La morfologia e la stratigrafia della piana alluvionale sono determinate dalla mutua interazione tra flussi idrici, erosione e deposito di sedimenti dovuti a ripetuti eventi di piena. Barre alluvionali, canali abbandonati, caratteristiche dei sedimenti e della vegetazione giocano un ruolo chiave nella storia migratoria del fiume che scorre sulla superficie alluvionale. Il primo argomento di questa tesi riguarda l'interazione mutua tra fiume e piana alluvionale, prodotta dai processi sedimentologici che modificano la struttura della superficie alluvionale influendo sulla migrazione del fiume e, allo stesso tempo, sono determinati dai processi legati dalla migrazione stessa. Tali processi consistono in progressivi depositi nella parte interna delle curve (point bars) fino ai cutoffs che portano alla formazione di anse abbandonate, contribuendo ad alterare la resistenza all'erosione del suolo da parte del fiume stesso. Il secondo argomento riguarda la presenza di condizioni al contorno interne che sono in grado di influire sulle caratteristiche del campo di moto, il quale è legato alla distribuzione della curvatura planimetrica dei meandri. La presenza di una singolarità (e.g., variazione di portata dovuta alla confluenza con un affluente) genera perturbazioni al campo di moto che si propagano verso monte e verso valle, influendo sulla dinamica a breve e a lungo termine del fiume. Metodi statistici spettrali e multivariati permettono di analizzare e confrontare oggettivamente le geometrie dei meandri fluviali, sia naturali che generati numericamente.
Bonyongo, Mpaphi Casper. "Vegetation ecology of the seasonal floodplains in the Okavango Delta, Botswana". Diss., Connect to this title online, 1999. http://upetd.up.ac.za/thesis/available/etd-03012007-103712/.
Pełny tekst źródłaVega, Luisa F. [Verfasser]. "Ecology of seasonal shallow lakes in neotropical floodplains / Luisa F. Vega". Konstanz : Bibliothek der Universität Konstanz, 2014. http://d-nb.info/1081016256/34.
Pełny tekst źródłaTeo, Fang Yenn. "Study of the hydrodynamic processes of rivers and floodplains with obstructions". Thesis, Cardiff University, 2010. http://orca.cf.ac.uk/54161/.
Pełny tekst źródłaRezaei, Bahram. "Overbank flow in compound channels with prismatic and non-prismatic floodplains". Thesis, University of Birmingham, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.564484.
Pełny tekst źródłaClubb, Fiona Jane. "Controls on fluvial networks in upland landscapes : from hillslopes to floodplains". Thesis, University of Edinburgh, 2017. http://hdl.handle.net/1842/28817.
Pełny tekst źródłaBechtold, James Scott. "Fluvial sediment influences on floodplain soil biogeochemistry /". Thesis, Connect to this title online; UW restricted, 2007. http://hdl.handle.net/1773/5358.
Pełny tekst źródłaDenys, Frank. "Transverse transport of suspended sediment across the main channel - floodplain shear boundary /". Link to the online version, 2007. http://hdl.handle.net/10019/415.
Pełny tekst źródłaMichaelides, Katerina. "The effects of hillslope-channel coupling on catchment hydrological response in Mediterranean areas". Thesis, King's College London (University of London), 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.326964.
Pełny tekst źródłaBarsoum, Nadia. "A comparison of vegetative and non-vegetative regeneration strategies in Populus nigra and Salix alba". Thesis, University of Cambridge, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.364532.
Pełny tekst źródłaSpurgeon, V. Leanne. "Sedimentology of historic and prehistoric deposits in the drainage basin of Deep River and Muddy Creek on the Piedmont of North Carolina". Morgantown, W. Va. : [West Virginia University Libraries], 2000. http://etd.wvu.edu/templates/showETD.cfm?recnum=1268.
Pełny tekst źródłaTitle from document title page. Document formatted into pages; contains viii, 152 p. : ill. (some col.), maps. Includes abstract. Includes bibliographical references (p. 62-64).
Shah, Mohammad Aminur Rahman. "Decision Support Framework for Sustainability Assessment of Flood Mitigation Projects". Thesis, Griffith University, 2017. http://hdl.handle.net/10072/371222.
Pełny tekst źródłaThesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Eng & Built Env
Science, Environment, Engineering and Technology
Full Text
Louca, Vasilis. "The ecology of fishes and mosquitoes of the lower Gambia River floodplains". Thesis, Durham University, 2009. http://etheses.dur.ac.uk/2082/.
Pełny tekst źródłaAzinheira, David Lee. "Complementary Effects of In-Stream Structures and Inset Floodplains on Solute Retention". Thesis, Virginia Tech, 2013. http://hdl.handle.net/10919/51046.
Pełny tekst źródłaMaster of Science
Molinari, Bianca S. "Aquatic Productivity and Connectivity in a Tropical River Floodplain". Thesis, Griffith University, 2021. http://hdl.handle.net/10072/405196.
Pełny tekst źródłaThesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Environment and Sc
Science, Environment, Engineering and Technology
Full Text
Savanhu, G. M. (George Mutangamberi). "Controls on channel form and floodplain character along the Bulstrode River, southern Quebec, Canada". Thesis, McGill University, 1993. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=69683.
Pełny tekst źródłaThe second objective is to relate the variations in gradient, sediment calibre and channel geometry to the changes in floodplain character along the river valley.
The river is about 85 km long and flows across the Appalachian highlands and foothills in southern Quebec. This study focuses on six alluvial reaches along the river, ranging from 0.7 to 1.5 km in length. The channel gradient ranges from 0.0036 to 0.0001. The decline in gradient is associated with rapid downstream fining from small cobble and gravel-bed in the 'upvalley reaches' to a sand-bedded channel in the 'downvalley' reaches.
The discharge remains fairly constant over the river length, averaging about 140 m$ sp3$/sec. Channel depth, particularly the thalweg depth, increases appreciably in the downstream direction. The channel width decreases appreciably in the downstream direction. The channel capacity varies significantly without a clear pattern in the steeper cobble-gravel bed reaches and generally declines in the more hydraulically efficient, gentler and more hydraulically efficient fine gravel-sand bed downstream reaches.
This study finds that floodplain characteristics vary with specific stream power and within-channel processes, but not in the same manner as suggested in the Nanson and Croke (1992) model. (Abstract shortened by UMI.)
Horn, R. P. "Flow resistance of woody vegetation and velocity estimation for flow over wooded floodplains". Thesis, University of Cambridge, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.604233.
Pełny tekst źródłaNicholas, Andrew Paul. "Modelling overbank deposition on floodplains : a case study of the River Culm, Devon". Thesis, University of Exeter, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239297.
Pełny tekst źródłaClitherow, Leonie Rose. "Terrestrial-aquatic food web linkages across floodplains of different ages, Glacier Bay, Alaska". Thesis, University of Birmingham, 2016. http://etheses.bham.ac.uk//id/eprint/6676/.
Pełny tekst źródłaSouthwell, Mark, i n/a. "Floodplains as dynamic mosaics : sediment and nutrient patches in a large lowland riverine landscape". University of Canberra. n/a, 2008. http://erl.canberra.edu.au./public/adt-AUC20081217.144116.
Pełny tekst źródłaKharat, Deepak Bhimrao. "Practical aspects of integrated 1D2D flood modelling of urban floodplains using LiDAR topography data". Thesis, Heriot-Watt University, 2009. http://hdl.handle.net/10399/2272.
Pełny tekst źródłaJayakaran, Anand D. "The formation of benches in agricultural channels in Ohio". Columbus, Ohio : Ohio State University, 2006. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1149002547.
Pełny tekst źródłaDikgola, Kobamelo. "Spatial and temporal variation of inundation in the Okavango Delta, Botswana; with special reference to areas used for flood recession cultivation". University of the Western Cape, 2015. http://hdl.handle.net/11394/4677.
Pełny tekst źródłaThe Okavango Delta is recognized as one of the famous inland wetlands and its sustainable use is important for socio-economic development of Botswana. The Okavango delta comprises permanent swamps, seasonal swamps, and drylands on islands within the delta and the surrounding areas, sustained by Okavango river inflows from upstream and local rainfall. TheOkavango River splits into several distributary channels within the delta. Areas which are flooded annually vary in response to varying inflows into the delta. Peak inflows into the delta occur during the February to May period. Due to the low gradient over the delta, these inflows move slowly resulting in peak outflows from the delta occurring during the June to August period. The inundated area over the entire delta increases from May until it reaches maximum inAugust and starts to decrease from September, reaching minimum inundated area in the months of December and January. The incoming flood wave into the delta and maximum inundation is out of phase with the local rainfall season.Communities living within and around the delta derive their livelihoods from tourism, hunting, fishing, livestock rearing, and crop production. Crop production is carried out on drylands and within floodplains. Some of the households take advantage of the increase in soil moisture arising from this inundation along floodplains to cultivate their crops as the floods recede. This practice is locally referred to as molapo farming which highly depends on inundation of floodplains. The availability of floodplain inundation highly depends on the magnitude of inflows into the delta and the local rainfall which are highly variable resulting in uncertainty regarding successful crop production, availability of livestock grazing areas, and uncertainty in reliance on the wetlands resources such as fishing. The uncertainty experienced in timing of extreme events which cause flooding of resulting in water reaching areas or floodplains where it is not wanted, and also uncertainity in timing of low flows, therefore water not reaching some parts of the delta.Several hydrological studies have been carried out with the aim of improving the understanding of the spatial and temporal dynamics of flows throughout the delta including predicting areas that are likely to be inundated each year. The significant gap addressed by this research is to improve the understanding of the spatial and temporal influence of magnitude and timing of flows on floodplain inundation. Local rainfall on the delta is highly variable over time and space due to its convective nature. This research also addresses the rainfall temporal and spatial variations and its implications on floodplain inundation. The knowledge about spatial extent and duration of floodplain inundation should assist in predicting each year the viability of molapo farming. Three research site, Shorobe, Tubu and Xobe are selected as case studies to understand the dynamics of floodplain inundation induced either by inflows or local rainfall. Local rainfall during the December to March period enables the crops to reach maturity. The onset of the rainy season is very important in supporting sowing of crop seeds. Local rainfall on the delta varies considerably. Aerial rainfall interpolation shows a change in rainfall magnitudes over space in different rainfall months, i.e different parts of the delta receive different rainfall magnitudes in different months of the rainy season. The spatial variation is mainly associated with the migration of the ITCZ southwards first through East Africa during October andNovember and down over Southern Africa in December to February. The movement of the ITCZ brings rainfall concentration on the northern and eastern parts of the Okavango Delta during December to January and bringing rainfall concentration to the northwestern part of the delta around February. However, rainfall spatial correlation between stations can be poor even within the first 150 km therefore implying neighboring places do not experience floodplain inundation by rainfall at the same time. The poor spatial correlation of rainfall between neighboring stations reflects the erratic nature of rainfall in the Okavango Delta characterised by localized thunderstorms. Change detection shows change points in rainfall which can be associated with ENSO episodes. A change point is identified in 1976 and 1977 which can be associated with the El Nino episodes during those years and two change points identified in 1999 and 2004 which can be associated with the La Nina episodes, therefore rainfall induced floodplain inundation can also be associated with wet and dry ENSO episodes. Rainfall does not show any significant trends except for an increasing trend on 10th percentile of Shakawe rainfall. Rainfall also does not show any cyclic behavior. Rainfall over the Okavango Delta can be divided into three unique homogenious sub-regions; sub-region 1: the northern part following the GEV probability distribution and being the region with highest rainfall amounts; sub-region 2: the lower northern and the outlet parts of the Okavango Delta following the GPA distribution with moderate rainfall; and sub-region 3: the middle part of the delta extending to the western and the eastern fringes of the delta, following the P3 distribution and having the lowest rainfall.The main characteristic that defines the Okavango Delta flows at Mohembo is its cyclic behavior. Three significant cycles are identified, close to 10, 20 and 40 years. No significant trends are identified, only a decreasing trend in minimum flows. Change points are identified in 1979 and 1988 and these can be explained by the existing cyclicity since no major land use changes have taken place in the Okavango River Basin upstream before 1989. The existence of cyclicity in Okavango River flows at Mohembo also explains the periodic wetting and drying of different floodplains in the delta. A long period of low flows was experienced from 1983 until 2003 and floodplain inundation extent was greatly reduced, more especially during the 1993-2003. During the 1993-2003 period, flows could no longer reach Maun Bridge along Thamalakne River, therefore leaving molapo floodplains around Boteti River, Gomoti River and Thaoge River to dry out. The 10 and 40 year return floods are important as they indicate the probability of a flood magnitude which has potential to result in major inundation in the Okavango Delta. Therefore, flood magnitudes with recurrence interval 10 and 40 years have high probability of occurring and can cause major floodplain inundation as they can be above the 2009 flood of 969 m3/s, which was the return of major inundation of Okavango Delta floodplains after a long period of dryness. The Ngoqa-Maunachira distributary channel of the Okavango River receives 32% of flow volumes entering the Okavango Delta at Mohembo. 12 % of the Mohembo flow volumes reach the Jao-Boro distributary whilst 1% is received by the Thaoge distributary. Therefore more inundation is experienced along the Ngoqa-Maunachira system compared to the other two. Only about 2% of the Mohembo flow volumes leave the Okavango Delta through Boteti River. Long term shifting of flow direction amongst reaches along the Okavango Delta distributaries is evident more especially along the Ngoqa-Maunachira River system. This results in shifting of inundation. Sub-surface water respond significantly to local rainfall and inflows with high soil moisture conditions retained at 60 cm and 100 cm below the ground.
Jung, Kwansue 1959. "The comparative sediment processes in channel and overbank". Thesis, The University of Arizona, 1989. http://hdl.handle.net/10150/277205.
Pełny tekst źródłaNecsoiu, Dorel Marius. "A Data Fusion Framework for Floodplain Analysis using GIS and Remotely Sensed Data". Thesis, University of North Texas, 2000. https://digital.library.unt.edu/ark:/67531/metadc2557/.
Pełny tekst źródłaLind, Pollyanna 1970. "Holocene Floodplain Development of the Lower Sycan River, Oregon". Thesis, University of Oregon, 2009. http://hdl.handle.net/1794/10171.
Pełny tekst źródłaWater and pumice accumulated behind a dam that, upon failure, scoured the c1aydominated floodplain and deposited pumice sands across the Sycan Valley. The pumice originated from the eruption of Mount Mazama (approximately 7660 ybp), and dam failure occurred very shortly afterwards. In response to the flood the lower Sycan River underwent episodes of channel aggradation and degradation. This study presents the history of channel evolution for the lower Sycan River from 11,000 years ago to present, based on floodplain stratigraphy and radiocarbon chronology. Seven primary periods of channel and floodplain development are identified: I. Early Holocene Dynamic Equilibrium; II: Sycan Outburst Flood; III. Initial Channel Formation; IV. Degradation & Widening; V. Aggradation & Lateral Migration; VI. (Secondary) Degradation & Widening; VII. Modern Dynamic Equilibrium. The active floodplain of the modern lower Sycan River is flanked by terraces of the rapidly abandoned Sycan Outburst Flood deposits.
Committee in Charge: Dr. Patricia McDowell, Chair; Dr. Jim E. O'Connor; Dr. Andrew Marcus
Potter, Karen. "Battle for the floodplains : an institutional analysis of water management and spatial planning in England". Thesis, University of Liverpool, 2012. http://livrepository.liverpool.ac.uk/11853/.
Pełny tekst źródłaIsmail, Zulhilmi. "A study of overbank flows in non-vegetated and vegetated floodplains in compound meandering channels". Thesis, Loughborough University, 2007. https://dspace.lboro.ac.uk/2134/7905.
Pełny tekst źródłaFranklin, Louise Bartlett. "Floodplain management in Georgia : its techniques, funding, and program design". Thesis, Georgia Institute of Technology, 1997. http://hdl.handle.net/1853/20802.
Pełny tekst źródłaNatho, Stephanie [Verfasser], Gunnar [Akademischer Betreuer] Nützmann, Mathias [Akademischer Betreuer] Zessner i Dagmar [Akademischer Betreuer] Haase. "Modelling nutrient retention in floodplains : development of a concept to empirically derive the average inundated floodplain extent and incoming nutrient loads / Stephanie Natho. Gutachter: Gunnar Nützmann ; Mathias Zessner ; Dagmar Haase". Berlin : Humboldt Universität zu Berlin, Mathematisch-Naturwissenschaftliche Fakultät II, 2013. http://d-nb.info/1044956267/34.
Pełny tekst źródła