Relevant bibliographies by topics / Ground and surface water biodiversity

Academic literature on the topic 'Ground and surface water biodiversity'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Ground and surface water biodiversity"

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Çolak, Mehmet Arda, Barış Öztaş, İbrahim Kaan Özgencil, Melisa Soyluer, Mustafa Korkmaz, Arely Ramírez-García, Melisa Metin, et al. "Increased Water Abstraction and Climate Change Have Substantial Effect on Morphometry, Salinity, and Biotic Communities in Lakes: Examples from the Semi-Arid Burdur Basin (Turkey)." Water 14, no. 8 (April 12, 2022): 1241. http://dx.doi.org/10.3390/w14081241.

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Global warming and altered precipitation patterns are predicted to intensify the water loss in semi-arid and arid regions, and such regions in Turkey will be particularly affected. Moreover, water abstraction, not least for irrigation purposes, is expected to increase markedly, posing major threats to the water balance of the lakes and thus their biodiversity. Among the closed basins in Turkey, the Burdur Closed Basin (BCB), located in the southwest of Turkey, is expected to be most affected. The BCB includes several types of aquatic ecosystems which support high biodiversity, including one Ramsar site, six Important Bird Areas, and a considerable richness of native and endemic fish species. Therefore, it is essential to analyze the potential environmental impacts of climate change and increased water abstraction on BCB lakes and their biotic communities. Here, we combined historical data on ecosystems as well as meteorological, remote sensing, and ground-truth data to analyze the changes in the temperature and precipitation of the BCB, water surface areas, and land use, as well as the potential effects on waterbird and fish communities. We calculated the water budget to elucidate water availability in the basin over the last few decades and predicted future conditions based on rainfall and temperature forecasts using climate models. The Standardized Precipitation–Evapotranspiration Index (SPEI) was used to relate the water surface area to precipitation and temperature change in the basin. Crop-farming irrigation in the BCB has increased notably since 2004, leading to intensive water abstraction from the lakes and their inflows, as well as from ground water, to meet the increased demand for irrigation. The water abstraction from the lakes, inflows to the lakes, and the groundwater in the basin has increased the water loss in the catchment substantially. Remotely sensed data on lake surface areas showed a major shrinkage of shallow lakes in the last 40 years. Moreover, the largest lake in the basin, Lake Burdur, lost nearly half of its surface area, which is worrisome since the shallower areas are the most suitable for supporting high biodiversity. Climate models (CNRM-ESM2-1GCM for temperature and GFDL-ESM4-GCM for precipitation) suggest that from 2070, the BCB will face long-term, moderate-to-severe dry periods. This, and the increased demand for water for irrigation, along with climate change, may accelerate the drying of these lakes in the near future with devastating effects on the lake ecosystems and their biodiversity.
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P S, Dr Anju, and Dr Jaya D S. "Impacts of Clay Mining Activities on Aquatic Ecosystems: A Critical Review." International Journal of Engineering and Advanced Technology 11, no. 4 (April 30, 2022): 128–34. http://dx.doi.org/10.35940/ijeat.d3495.0411422.

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The unconsolidated earth surface is a rich source of minerals, of which clay is one of the richest natural minerals, having various natural and anthropogenic properties. Natural clay is widely available as a cheaper resource, which is non toxic to ecosystems and has the property of preserving ground water and aquifers. At the same time, the ubiquitous and widespread occurrence of clay will have the property to control toxic materials. The uncontrolled exploitation or mining of clay minerals will affect the aquatic ecosystem's sustainability in many ways. Water quality is very essential for the healthy environment and human life, whereas unpredictable conditions like flooding, drought, groundwater loss, loss of biodiversity, and health impacts on the surrounding inhabitants are some of the signs of ecosystem loss. The unwanted mined clay is deposited into the surrounding area of the mining environment, resulting in top soil, ground water, and surface water pollution. The review paper describes the pollution aspects of the aquatic ecosystem with special emphasis on ground water, aquifers, fresh water (lotic and lentic), sediment, and marine ecology and hydrology.
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Singh, Sanjay. "Forestry Research in Mine Reclamation in India: Past, Present and Future." Indian Journal of Forestry 43, no. 1 (January 7, 2021): 10–18. http://dx.doi.org/10.54207/bsmps1000-2021-82p483.

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Minerals greatly influence the economic growth of any country. However, extensive mining can adversely affect the natural environment in the form of loss of biodiversity, soil erosion, contamination of surface and ground water. Therefore, restoration and reclamation of mined sites become priority areas of intervention. This review paper deals with history, current status and priorities of forestry research in the area of mine reclamation in India. The foresters need to align their activities in line with the United Nations Decade on Ecosystem Restoration during 2021-2030.
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Schirmer, M., J. Luster, N. Linde, P. Perona, E. A. D. Mitchell, D. A. Barry, J. Hollender, et al. "Morphological, hydrological, biogeochemical and ecological changes and challenges in river restoration – the Thur River case study." Hydrology and Earth System Sciences 18, no. 6 (June 27, 2014): 2449–62. http://dx.doi.org/10.5194/hess-18-2449-2014.

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Abstract. River restoration can enhance river dynamics, environmental heterogeneity and biodiversity, but the underlying processes governing the dynamic changes need to be understood to ensure that restoration projects meet their goals, and adverse effects are prevented. In particular, we need to comprehend how hydromorphological variability quantitatively relates to ecosystem functioning and services, biodiversity as well as ground- and surface water quality in restored river corridors. This involves (i) physical processes and structural properties, determining erosion and sedimentation, as well as solute and heat transport behavior in surface water and within the subsurface; (ii) biogeochemical processes and characteristics, including the turnover of nutrients and natural water constituents; and (iii) ecological processes and indicators related to biodiversity and ecological functioning. All these aspects are interlinked, requiring an interdisciplinary investigation approach. Here, we present an overview of the recently completed RECORD (REstored CORridor Dynamics) project in which we combined physical, chemical, and biological observations with modeling at a restored river corridor of the perialpine Thur River in Switzerland. Our results show that river restoration, beyond inducing morphologic changes that reshape the river bed and banks, triggered complex spatial patterns of bank infiltration, and affected habitat type, biotic communities and biogeochemical processes. We adopted an interdisciplinary approach of monitoring the continuing changes due to restoration measures to address the following questions: How stable is the morphological variability established by restoration? Does morphological variability guarantee an improvement in biodiversity? How does morphological variability affect biogeochemical transformations in the river corridor? What are some potential adverse effects of river restoration? How is river restoration influenced by catchment-scale hydraulics and which feedbacks exist on the large scale? Beyond summarizing the major results of individual studies within the project, we show that these overarching questions could only be addressed in an interdisciplinary framework.
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Kędziora, Andrzej. "The Network Of Shelterbelts As An Agroforestry System Controlling The Water Resources And Biodiversity In The Agricultural Landscape." Papers on Global Change IGBP 22, no. 1 (January 1, 2015): 63–82. http://dx.doi.org/10.1515/igbp-2015-0016.

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Abstract Long-term human activity has led to many unfavourable changes in landscape structure. The main negative effect has been a simplification of landscape structure reflecting the removal of stable ecosystems, such as forests, shelterbelts, strips of meadows and so on, which were converted into unstable ecosystems, mainly farmlands. Thanks to these changes, serious threats have been posed to the sustainable development of rural areas. The most hazardous of these involve a deteriorating of water balance, increased surface and ground water pollution, and impoverishment of biodiversity. An agroforestry system can serve as a toolkit which allows counteracting such negative changes in the landscape. This paper presents the main findings emerge from long-term investigations on the above issues carried out by the Institute for the Agricultural and Forest Environment of the Polish Academy of Sciences.
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Schirmer, M., J. Luster, N. Linde, P. Perona, E. A. D. Mitchell, D. A. Barry, O. A. Cirpka, P. Schneider, T. Vogt, and E. Durisch-Kaiser. "River restoration: morphological, hydrological, biogeochemical and ecological changes and challenges." Hydrology and Earth System Sciences Discussions 10, no. 8 (August 20, 2013): 10913–41. http://dx.doi.org/10.5194/hessd-10-10913-2013.

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Abstract. River restoration is essential as a means to enhance river dynamics, environmental heterogeneity and biodiversity. The underlying processes governing the dynamic changes need to be understood thoroughly to ensure that restoration projects meet their goals. In particular, we need to understand quantitatively how hydromorphological variability relates to ecosystem functioning and services, biodiversity and (ground)water quality in restored river corridors. Here, we provide a short overview on the literature and present a study of a restored river corridor in Switzerland combining physical, chemical, and biological observations with modeling. The results show complex spatial patterns of bank infiltration, habitat-type, biotic communities and biogeochemical processes. In particular, we found an increase in taxonomic and functional diversity for earthworms, testate amoebae and bacteria in the restored part of the river. This complexity is driven by river hydrology and morphodynamics, which are in turn actively coupled to riparian vegetation processes. Given this complexity and the multiple constraints on the uses and management of floodplains, a multi-disciplinary approach is needed to monitor the success of restoration measures and to make recommendations for future restoration projects.
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de Vries, Wim, Hans Kros, Oene Oenema, and Jan Willem Erisman. "Assessment of Nitrogen Ceilings for Dutch Agricultural Soils to Avoid Adverse Environmental Impacts." Scientific World JOURNAL 1 (2001): 898–907. http://dx.doi.org/10.1100/tsw.2001.333.

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In the Netherlands, high traffic density and intensive animal husbandry have led to high emissions of reactive nitrogen (N) into the environment. This leads to a series of environmental impacts, including: (1) nitrate (NO3) contamination of drinking water, (2) eutrophication of freshwater lakes, (3) acidification and biodiversity impacts on terrestrial ecosystems, (4) ozone and particle formation affecting human health, and (5) global climate change induced by emissions of N2O. Measures to control reactive N emissions were, up to now, directed towards those different environmental themes. Here we summarize the results of a study to analyse the agricultural N problem in the Netherlands in an integrated way, which means that all relevant aspects are taken into account simultaneously. A simple N balance model was developed, representing all crucial processes in the N chain, to calculate acceptable N inputs to the farm (so-called N ceiling) and to the soil surface (application in the field) by feed concentrates, organic manure, fertiliser, deposition, and N fixation. The N ceilings were calculated on the basis of critical limits for NO3concentrations in groundwater, N concentrations in surface water, and ammonia (NH3) emission targets related to the protection of biodiversity of natural areas. Results show that in most parts of the Netherlands, except the western and the northern part, the N ceilings are limited by NH3emissions, which are derived from critical N loads for nature areas, rather than limits for both ground- and surface water. On the national scale, the N ceiling ranges between 372 and 858 kton year–1depending on the choice of critical limits. The current N import is 848 kton year–1. A decrease of nearly 60% is needed to reach the ceilings that are necessary to protect the environment against all adverse impacts of N pollution from agriculture.
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Sishu, Feleke K., Seifu A. Tilahun, Petra Schmitter, Getachew Assefa, and Tammo S. Steenhuis. "Pesticide Contamination of Surface and Groundwater in an Ethiopian Highlands’ Watershed." Water 14, no. 21 (October 29, 2022): 3446. http://dx.doi.org/10.3390/w14213446.

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Agricultural intensification in sub-Saharan African countries has significantly increased pesticide applications. Information on pesticide residues and their transport in groundwater and streams is needed to properly manage and reduce any harm to the ecosystem and environment. This information is lacking in the volcanic soils of Ethiopian highlands. Therefore, this study was conducted to assess pesticide concentrations in ground and surface water and their risk to humans and aquatic life. The 9 km2 rural watershed Robit Bata in the Lake Tana Basin was selected. Crops were grown under rainfed and irrigated conditions. Pesticide use was assessed, and groundwater samples were collected from eight wells and surface water samples at the outlet twice in the rain phase and once in the dry phase. Samples were analyzed for chlorpyrifos, dimethoate, (α and β) endosulfan, profenofos, NO3−, and pH. Chlorpyrifos and endosulfan, which are strongly adsorbed and slowly degrading pesticides, were found in nearly all surface and groundwater samples, with maximum concentrations in surface water of 8 µg L−¹ for chlorpyrifos and 3 µg L−¹ endosulfan. Maximum groundwater concentrations were only slightly lower. The weakly adsorbed and fast degrading pesticides, dimethoate, and profenofos were detected only in the rain phase after spraying in the groundwater, indicating preferential transport to groundwater at depths of up to 9 m. The average concentration was 0.38 μg L−¹ for dimethoate in surface waters and 1.24 μg L−¹ in groundwater. Profenofos was not detected in surface water. In the groundwater, the average concentration was 0.05 μg L−¹. Surface water concentrations of chlorpyrifos and endosulfan were highly toxic to fish. The World Health Organization banned these pesticides worldwide. It should be phased out for use in Ethiopia to safeguard the ecological health of Lake Tana, which is rich in biodiversity and endemic fish species.
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Khan, Mehreen. "Impact of urbanization on water resources of Pakistan: A review." NUST Journal of Engineering Sciences 12, no. 1 (June 1, 2019): 1–8. http://dx.doi.org/10.24949/njes.v12i1.230.

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This paper summarizes the various dimensions and impacts of urbanization on Pakistan’s water resources in order to provide foundations for future water policy that will lead towards country’s socio-economic development. Urbanization is considered as a major trend of 21st century in many developing countries. Along with urbanization, increase in population growth in recent years has put a pressure on the world’s water resources in terms of water demand and pollution. Various issues related to water sector in urban areas of Pakistan have been identified including contamination of surface and ground water resources through industrial, agricultural and domestic discharge of waste and waste water, increasing floods, loss of wetlands and aquatic biodiversity, sea water intrusion and subsidence, physical reduction in water resources quantity and quality and operational and managerial incapacities. There are some other issues like unequal water distribution which together with population burden, rapid urbanization and growing industrialization are posing a huge challenge for Pakistan’s water management in 21st century. Taken together all the studies, this review suggests that to reduce vulnerability to water resources of Pakistan, there is a need for new systems of urban planning and governance institutions as the core of Pakistan’s water crisis is water management.
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Knapp, Schmauck, and Zehnsdorf. "Biodiversity Impact of Green Roofs and Constructed Wetlands as Progressive Eco-Technologies in Urban Areas." Sustainability 11, no. 20 (October 21, 2019): 5846. http://dx.doi.org/10.3390/su11205846.

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The total amount of sealed surfaces is increasing in many urban areas, which presents a challenge for sewerage systems and wastewater treatment plants when extreme rainfall events occur. One promising solution approach is the application of decentralized eco-technologies for water management such as green roofs and constructed wetlands, which also have the potential to improve urban biodiversity. We review the effects of these two eco-technologies on species richness, abundance and other facets of biodiversity (e.g., functional diversity). We find that while green roofs support fewer species than ground-level habitats and thus are not a substitute for the latter, the increase in green roof structural diversity supports species richness. Species abundance benefits from improved roof conditions (e.g., increased substrate depth). Few studies have investigated the functional diversity of green roofs so far, but the typical traits of green roof species have been identified. The biodiversity of animals in constructed wetlands can be improved by applying animal-aided design rather than by solely considering engineering requirements. For example, flat and barrier-free shore areas, diverse vegetation, and heterogeneous surroundings increase the attractiveness of constructed wetlands for a range of animals. We suggest that by combining and making increasing use of these two eco-technologies in urban areas, biodiversity will benefit.
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Dissertations / Theses on the topic "Ground and surface water biodiversity"

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Vionnet, Leticia Beatriz 1960. "Modeling of ground-water flow and surface water/ground-water interactions of the San Pedro River Basin, Cochise County, Arizona." Thesis, The University of Arizona, 1992. http://hdl.handle.net/10150/278134.

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Ground-water exploitation in the Upper San Pedro Basin has produced the formation of a cone of depression around the Sierra Vista-Fort Huachuca area. A portion of the mountain front recharge that otherwise would reach the San Pedro River is being intercepted by pumping, and portions of baseflow are being captured by pumping. The purpose of this study is to construct a simulation model capable of simulating the ground-water system as well as the ground-water-surface water interactions. The flow simulation was done by a three-dimensional, finite-difference ground-water flow model (MODFLOW) that incorporates a new stream-aquifer interaction package. Steady state simulations were performed to represent mean annual conditions. Transient simulations cover a 48 year period, starting in 1940 and ending in 1988. A sensitivity analysis of the steady state model was also performed.
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Colgan, Gary A. "Estimating surface/ground-water mixing using stable environmental isotopes." Thesis, The University of Arizona, 1989. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_etd_hy0042_m_sip1_w.pdf&type=application/pdf.

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McCary, John. "Incorporating surficial aquifer ground-water fluxes into surface-water resource management studies." [Tampa, Fla.] : University of South Florida, 2005. http://purl.fcla.edu/fcla/etd/SFE0001095.

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Rosenberry, Donald O. "Influence of fluvial processes on exchange between ground water and surface water." Connect to online resource, 2007. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:3284456.

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Anderson, Jacob. "Geochemical Tracers of Surface Water and Ground Water Contamination from Road Salt." Thesis, Boston College, 2013. http://hdl.handle.net/2345/3313.

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Thesis advisor: Rudolph Hon
The application of road de-icers has lead to increasing solute concentrations in surface and ground water across the northern US, Canada, and northern Europe. In a public water supply well field in southeastern Massachusetts, USA, chloride concentrations in ground water from an unconfined aquifer have steadily risen for the past twenty years. The objectives of this study are to understand spatial and temporal trends in road salt concentrations in order to identify contamination sources and fate. To this end, the methods of this project include field and lab work. Water samples were collected from surface, near-surface, and ground water from March 2012 to March 2013. The other major field data are specific conductance measurements from probes located in three piezometers. In the lab, all samples were analyzed for major ions with ion chromatography analysis. Additionally, trace elements were measured by inductively coupled plasma analysis on a subset of samples. The results of these hydrogeochemical procedures showed several important trends. First, the highest concentrations of sodium and chloride from near-surface samples were located near to roadways. Second, ground water samples taken from glacial sediments contained relatively high concentrations throughout the water column, whereas ground water samples from wetlands had high concentrations only near the surface. Third, there was no clear relationship between pH and cation concentrations. Finally, specific conductance data showed strong seasonal trends near to the surface, whereas values taken from deeper in the aquifer were steadily increasing. Based on these results, it is highly probable that road salt application is the dominate contamination source. The pathways of road salt in the watershed include runoff into surface water and infiltration into the vadose zone and ground water. Road salt appears to preferentially travel through glacial features rather than floodplain features. It is possible that sodium from road salt is sorbed to aquifer sediment and displaces other cations. However, the low values of trace metals suggest that cation exchange is not mobilizing heavy metals. Finally, the increasing specific conductance values deep in the aquifer suggest that road salt is retained within the aquifer and concentrations will likely increase in the future if the current road salt application procedures are continued
Thesis (MS) — Boston College, 2013
Submitted to: Boston College. Graduate School of Arts and Sciences
Discipline: Earth and Environmental Sciences
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Grundy, Ian H. "Air flow near a water surface /." Title page, table of contents and summary only, 1986. http://web4.library.adelaide.edu.au/theses/09PH/09phg889.pdf.

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Zwierschke, Kerry Hughes. "IMPACT OF TURFGRASS SYSTEMS ON THE NUTRIENT STATUS OF SURFACE WATER, AND GROUND WATER." The Ohio State University, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=osu1235150457.

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Coes, Alissa L., and Alissa L. Coes. "A GEOCHEMICAL APPROACH TO DETERMINE GROUND-WATER FLOW PATTERNS IN THE SIERRA VISTA BASIN, ARIZONA, WITH SPECIAL EMPHASIS ON GROUND-WATER/SURFACE-WATER INTERACTION." Thesis, The University of Arizona, 1997. http://hdl.handle.net/10150/622969.

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Water quality in the Sierra Vista Ground-Water Basin is of extreme importance due to the basin's unique ecosystem and predicted future population growth. Portions of the Upper San Pedro River, flowing through the Sierra Vista Basin, contain some of the few remaining perennial streamflows in the southwest. Baseflow in the perennial reaches of the river are maintained almost entirely by the regional and floodplain aquifer systems. A population increase is predicted for the Sierra Vista Basin, and an impact on groundwater quality and availability can be expected. Due to the closely linked hydrologic systems within the basin, contamination or depletion of the regional aquifer could have direct implications for the San Pedro River. Water samples were collected within the study area from the regional and floodplain aquifers, the San Pedro River, and a bedrock spring in the Huachuca Mountains. Samples were analyzed for field parameters, major-ions, and stable isotopes to describe the main chemical characteristics of the hydrologic systems within the basin. Analysis of regional aquifer geochemistry indicates a ground-water system strongly controlled by calcite precipitation. Specific conductance, deuterium and oxygen-18 values indicate a mixing of regional-aquifer ground water and San Pedro River surface water within the floodplain aquifer. Estimates of inflow to perennial reaches of the floodplain aquifer from the regional aquifer vary from 50 to 80%, depending on location. Inflow to the San Pedro River at Charleston from the regional aquifer is estimated to be about 50 to 70% of the stream discharge.
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Vionnet, Leticia Beatriz, Thomas III Maddock, and David C. Goodrich. "Investigations of stream-aquifer interactions using a coupled surface-water and ground-water flow model." Department of Hydrology and Water Resources, University of Arizona (Tucson, AZ), 1997. http://hdl.handle.net/10150/615700.

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A finite element numerical model is developed for the modeling of coupled surface-water flow and ground-water flow. The mathematical treatment of subsurface flows follows the confined aquifer theory or the classical Dupuit approximation for unconfined aquifers whereas surface-water flows are treated with the kinematic wave approximation for open channel flow. A detailed discussion of the standard approaches to represent the coupling term is provided. In this work, a mathematical expression similar to Ohm's law is used to simulate the interacting term between the two major hydrological components. Contrary to the standard approach, the coupling term is incorporated through a boundary flux integral that arises naturally in the weak form of the governing equations rather than through a source term. It is found that in some cases, a branch cut needs to be introduced along the internal boundary representing the stream in order to define a simply connected domain, which is an essential requirement in the derivation of the weak form of the ground-water flow equation. The fast time scale characteristic of surface-water flows and the slow time scale characteristic of ground-water flows are clearly established, leading to the definition of three dimensionless parameters, namely, a Peclet number that inherits the disparity between both time scales, a flow number that relates the pumping rate and the streamflow, and a Biot number that relates the conductance at the river-aquifer interface to the aquifer conductance. The model, implemented in the Bill Williams River Basin, reproduces the observed streamflow patterns and the ground-water flow patterns. Fairly good results are obtained using multiple time steps in the simulation process.
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Kikuchi, Colin. "Spatially Telescoping Measurements for Characterization of Ground Water - Surface Water Interactions along Lucile Creek, Alaska." Thesis, The University of Arizona, 2011. http://hdl.handle.net/10150/202976.

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A new spatially telescoping approach was proposed to improve measurement flexibility and account for hydrologic scale in field studies of groundwater-surface water (GW-SW) interaction. We applied this spatially telescoping approach in a study GW-SW interactions along Lucile Creek, Alaska. Catchment-scale data were used to screen areas of potentially significant GW-SW exchange, indicating groundwater contribution from a deeper regional aquifer along the middle to lower reaches of the stream. This initial assessment was tested using reach-scale estimates of groundwater contribution during base flow conditions. The reach-scale measurements indicated a large increase in discharge along the middle reaches of the stream accompanied by a shift in chemical composition towards a regional groundwater end member. Point measurements of vertical water fluxes were used to evaluate spatial and temporal variability of GW-SW exchange within representative reaches. The spatially telescoping approach identified locations of GW-SW exchange and improved interpretation of reach-scale and point-scale measurements.
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Books on the topic "Ground and surface water biodiversity"

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Ground and surface water hydrology. Hoboken, N.J: Wiley, 2011.

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Börner, H., ed. Pesticides in Ground and Surface Water. Berlin, Heidelberg: Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-79104-8.

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1926-, Börner Horst, and Beitz Horst, eds. Pesticides in ground and surface water. Berlin: Springer-Verlag, 1994.

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Saksena, R. S. Conjunctive use of surface and ground water. Roorkee: INCOH Secretariat, 2000.

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Duigon, Mark T. Ground-water and surface-water data for Washington County, Maryland. Baltimore, Md. (2300 St. Paul St., Baltimore 21218-5210): Dept. of Natural Resources, Maryland Geological Survey, 1989.

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Tompkins, Michael D. Ground-water and surface-water data for Kent County, Maryland. Baltimore, Md. (2300 St. Paul St., Baltimore 21218-5210): Dept. of Natural Resources, Maryland Geological Survey, 1994.

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Dine, James R. Ground-water and surface-water data for Frederick County, Maryland. Baltimore, Md. (711 W. 40th St., Suite 440, Baltimore 21211): Dept. of Natural Resources, Maryland Geological Survey, 1985.

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National Research Council (U.S.). Water Science and Technology Board. Committee on Ground Water Recharge in Surface-Mined Areas. Surface coal mining effects on ground water recharge. Washington, D.C: National Academy Press, 1990.

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Steele, G. V. Surface-water/ground-water interaction and implications for ground-water sustainability in the Dutch Flats Area, western Nebraska. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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Steele, G. V. Surface-water/ground-water interaction and implications for ground-water sustainability in the Dutch Flats Area, western Nebraska. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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Book chapters on the topic "Ground and surface water biodiversity"

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Purkis, Samuel, and Victor Klemas. "Surface and ground water resources." In Remote Sensing and Global Environmental Change, 122–41. West Sussex, UK: John Wiley & Sons Ltd, 2013. http://dx.doi.org/10.1002/9781118687659.ch7.

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Thomson, James A. M., James W. McKinley, Robert C. Harris, Alwyn J. Hart, Peter Hicks, and David K. Ramsden. "MTBE Occurrence in Surface and Ground Water." In MTBE Remediation Handbook, 63–72. Boston, MA: Springer US, 2003. http://dx.doi.org/10.1007/978-1-4615-0021-6_4.

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Minea, Vasile. "Surface Water Ground-Source Heat Pump Systems." In Heating and Cooling with Ground-Source Heat Pumps in Cold and Moderate Climates, 327–45. Boca Raton: CRC Press, 2022. http://dx.doi.org/10.1201/9781003032540-20.

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Ogidi, Odangowei Inetiminebi. "Impact of Pharmaceutical Compounds on the Microbial Ecology of Surface Water Resources." In Sustainable Development and Biodiversity, 323–43. Singapore: Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-19-3326-4_12.

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Galassi, S., and L. Guzzella. "Organic Phosphates in Surface, Ground and Drinking Water." In Organic Micropollutants in the Aquatic Environment, 108–15. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2989-0_16.

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Bortnikova, S. B., G. R. Kolonin, J. P. Kolmogorov, B. A. Kolotov, and D. Kalugin. "Results of the surface and ground water interaction with tailings impoundments." In Water-Rock Interaction, 867–70. London: Routledge, 2021. http://dx.doi.org/10.1201/9780203734049-216.

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Job, Chuck A., John J. Simons, and Alan D. Lease. "Methods for assessing nonpoint source contaminated ground water to surface water." In Ecological Indicators, 1540–41. Boston, MA: Springer US, 1992. http://dx.doi.org/10.1007/978-1-4615-4661-0_64.

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Brown, R. G., J. R. Stark, and G. L. Patterson. "Ground-Water and Surface-Water Interactions in Minnesota and Wisconsin Wetlands." In The Ecology and Management of Wetlands, 176–80. New York, NY: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4684-8378-9_14.

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Brown, R. G., J. R. Stark, and G. L. Patterson. "Ground-Water and Surface-Water Interactions in Minnesota and Wisconsin Wetlands." In The Ecology and Management of Wetlands, 176–80. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4684-7392-6_14.

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Rudra, Kalyan. "Interrelationship Between Surface and Groundwater: The Case of West Bengal." In Ground Water Development - Issues and Sustainable Solutions, 175–81. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-13-1771-2_10.

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Conference papers on the topic "Ground and surface water biodiversity"

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Loáiciga, Hugo A. "Ground-Water/Surface-Water Interactions in a Karst Aquifer." In Specialty Symposium on Integrated Surface and Ground Water Management at the World Water and Environmental Resources Congress 2001. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40562(267)16.

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Gentry, Randall W. "Assessing Ground Water and Surface Water Interaction Through Tracer Observation." In World Water and Environmental Resources Congress 2004. Reston, VA: American Society of Civil Engineers, 2004. http://dx.doi.org/10.1061/40737(2004)93.

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Johnson, Gary S., and Donna M. Cosgrove. "Quantifying Ground-Water Pumping Impacts on Surface Water in Idaho." In 29th Annual Water Resources Planning and Management Conference. Reston, VA: American Society of Civil Engineers, 1999. http://dx.doi.org/10.1061/40430(1999)206.

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Ranade, A. K., M. Pandey, D. Datta, Swapan Paruya, Samarjit Kar, and Suchismita Roy. "Stochastic Response Surface Based Simulation Of Ground Water Modeling." In INTERNATIONAL CONFERENCE ON MODELING, OPTIMIZATION, AND COMPUTING (ICMOS 20110). AIP, 2010. http://dx.doi.org/10.1063/1.3516304.

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Huisman, J. A., and W. Bouten. "Mapping surface soil water content with the ground wave of ground-penetrating radar." In Ninth International Conference on Ground Penetrating Radar (GPR2002), edited by Steven Koppenjan and Hua Lee. SPIE, 2002. http://dx.doi.org/10.1117/12.462252.

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Haeni, F. P., Marc L. Buursink, John E. Costa, Nick B. Melcher, Ralph T. Cheng, and William J. Plant. "Ground penetrating radar methods used in surface-water discharge measurements." In 8th International Conference on Ground Penetrating Radar, edited by David A. Noon, Glen F. Stickley, and Dennis Longstaff. SPIE, 2000. http://dx.doi.org/10.1117/12.383618.

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Kooper, K., S. Lambot, and E. C. Slob. "Incorporating near-surface layering in GPR data inversion for improved surface water content estimates." In 2007 4th International Workshop on, Advanced Ground Penetrating Radar. IEEE, 2007. http://dx.doi.org/10.1109/agpr.2007.386530.

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Cao, Jingjing, Mamattursun Eziz, Hamid Yimit, and Anwar Mohammad. "Surface and Ground Water Quality in Eli River Valley, China." In 2009 3rd International Conference on Bioinformatics and Biomedical Engineering (iCBBE 2009). IEEE, 2009. http://dx.doi.org/10.1109/icbbe.2009.5163543.

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Pekarova, Pavla. "SURFACE AND GROUND WATER POLLUTION BY NITRATES IN EASTERN SLOVAKIA." In 13th SGEM GeoConference on WATER RESOURCES. FOREST, MARINE AND OCEAN ECOSYSTEMS. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/bc3/s12.043.

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Teasley, Rebecca, John Raffensperger, and Mark Milke. "A Smart Market for Ground and Surface Water with Hydropower Generation." In World Environmental and Water Resources Congress 2010. Reston, VA: American Society of Civil Engineers, 2010. http://dx.doi.org/10.1061/41114(371)112.

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Reports on the topic "Ground and surface water biodiversity"

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Imes, J. L., and M. J. Kleeschulte. Ground-water flow and ground- and surface-water interaction at the Weldon Spring quarry, St. Charles County, Missouri. Office of Scientific and Technical Information (OSTI), December 1997. http://dx.doi.org/10.2172/578597.

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Major, Michael A. Octanol Water Partition Coefficients of Surface and Ground Water Contaminants Found at Military Installations. Fort Belvoir, VA: Defense Technical Information Center, November 1989. http://dx.doi.org/10.21236/ada228860.

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Veil, J. A., and M. G. Puder. Potential ground water and surface water impacts from oil shale and tar sandsenergy-production operations. Office of Scientific and Technical Information (OSTI), October 2006. http://dx.doi.org/10.2172/895671.

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Johnson, William K. Importance of Surface-Ground Water Interaction to Corps Total Water Management: Regional and National Examples. Fort Belvoir, VA: Defense Technical Information Center, February 1991. http://dx.doi.org/10.21236/ada236079.

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Gertsch, Jana C., Imee G. Arcibal, Charles S. Henry, and Donald M. Cropek. Lab-on-a-Chip Sensor for Monitoring Perchlorate in Ground and Surface Water. Fort Belvoir, VA: Defense Technical Information Center, February 2012. http://dx.doi.org/10.21236/ada559180.

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Schock, Kevin. Predicting Seepage of Leachate from the St. Johns Landfill to Ground and Surface Water Systems. Portland State University Library, January 2000. http://dx.doi.org/10.15760/etd.6532.

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Liszewski, M. J., and L. J. Mann. Concentrations of 23 trace elements in ground water and surface water at and near the Idaho National Engineering Laboratory, Idaho, 1988--91. Office of Scientific and Technical Information (OSTI), December 1993. http://dx.doi.org/10.2172/10191083.

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Hall, L. F. User`s Guide: Database of literature pertaining to the unsaturated zone and surface water-ground water interactions at the Idaho National Engineering Laboratory. Office of Scientific and Technical Information (OSTI), May 1993. http://dx.doi.org/10.2172/10103872.

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Bandy, P. J., and L. F. Hall. Summary of ground water and surface water flow and contaminant transport computer codes used at the Idaho National Engineering Laboratory (INEL). Version 1.0. Office of Scientific and Technical Information (OSTI), March 1993. http://dx.doi.org/10.2172/10150173.

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Bloomsburg, G., J. Finnie, D. Horn, B. King, and J. Liou. Abstracts and parameter index database for reports pertaining to the unsaturated zone and surface water-ground water interactions at the Idaho National Engineering Laboratory. Office of Scientific and Technical Information (OSTI), May 1993. http://dx.doi.org/10.2172/10103992.

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