Relevant bibliographies by topics / Groundwater-river interactions

Academic literature on the topic 'Groundwater-river interactions'

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Published: 4 June 2021
Last updated: 28 January 2023

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Journal articles on the topic "Groundwater-river interactions"

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Cai, Yi, Wenrui Huang, Fei Teng, Beibei Wang, Ke Ni, and Chunmiao Zheng. "Spatial variations of river–groundwater interactions from upstream mountain to midstream oasis and downstream desert in Heihe River basin, China." Hydrology Research 47, no. 2 (September 30, 2015): 501–20. http://dx.doi.org/10.2166/nh.2015.072.

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The Heihe River basin consists of three different characteristic regions: upstream mountain area, midstream oasis region, and downstream desert region. Understanding the river–groundwater interactions in different river reaches is important for sustainable water resources management. In this study, river–groundwater interactions in three different river regions are investigated by the analysis of geophysical characteristics, meteor-hydrological characteristics, agricultural irrigations, and channel water balance equation in the river reaches in different seasons. Results indicate that the river–groundwater interactions vary geographically in the three different regions, and change seasonally with the strongest interactions during the summer. Groundwater discharges into the river in the upstream mountainous reach (annual 2.57 × 108m3) while the river water seeps into aquifers in the downstream desert reach (annual 10.39 × 108m3). In the midstream oasis region, pumping water for agriculture irrigation significantly affects the river–groundwater interaction. The river loses water to the ground during the major- and medium-irrigation periods, and gains water from groundwater during the minor-irrigation period in the midstream reach. The characteristics of the river–groundwater interactions are primarily dominated by physiographic features and precipitation in the upstream mountainous region, by human activities and precipitation in the midstream oasis region, and by evaporation and human activities in the downstream desert region.
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Brunner, Philip, René Therrien, Philippe Renard, Craig T. Simmons, and Harrie-Jan Hendricks Franssen. "Advances in understanding river-groundwater interactions." Reviews of Geophysics 55, no. 3 (September 2017): 818–54. http://dx.doi.org/10.1002/2017rg000556.

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Wan, Yu Yu, Fu Tian Liu, and Guang Yu Lin. "Study on the Hydraulic Relationship between Molin River and Groundwater." Advanced Materials Research 490-495 (March 2012): 652–56. http://dx.doi.org/10.4028/www.scientific.net/amr.490-495.652.

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Molin River catchment is located in arid and semi-arid region in China. River water and groundwater are major water sources in this area. It is a key work to identify the interaction between river water and groundwater for not only water resources assessment and sustainable development, but residents living, industry and agriculture and environment protection. In this study, the interaction of Molin River water and groundwater has been analyzed systematically with hydrogeochemical and isotopic methods based on analyzing the characteristics of groundwater hydrodynamic field. The results show that Molin river water originates from groundwater in river source and is recharged by precipitation and groundwater with different recharge intensity along river flow. From the conclusions, it is obviously that these two parts of water cycle can not be departed, and their interactions need to be considered comprehensively in water resources assessment and development in order to avoid irreversible surface ecological environment damage in Molin River basin
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Unland, N. P., I. Cartwright, M. S. Andersen, G. C. Rau, J. Reed, B. S. Gilfedder, A. P. Atkinson, and H. Hofmann. "Investigating the spatio-temporal variability in groundwater and surface water interactions: a multi-technical approach." Hydrology and Earth System Sciences Discussions 10, no. 3 (March 22, 2013): 3795–842. http://dx.doi.org/10.5194/hessd-10-3795-2013.

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Abstract. The interaction between groundwater and surface water along the Tambo and Nicholson Rivers, southeast Australia, was investigated using 222Rn, Cl, differential flow gauging, head gradients, electrical conductivity (EC) and temperature profiling. Head gradients, temperature profiles, Cl concentrations and 222Rn activities all indicate higher groundwater fluxes to the Tambo River in areas of increased topographic variation where the potential to form large groundwater–surface water gradients is greater. Groundwater discharge to the Tambo River calculated by Cl mass balance was significantly lower (1.48 × 104 to 1.41 × 103 m3 day−1) than discharge estimated by 222Rn mass balance (5.35 × 105 to 9.56 × 103 m3 day−1) and differential flow gauging (5.41 × 105 to 6.30 × 103 m3 day−1). While groundwater sampling from the bank of the Tambo River was intended to account for the variability in groundwater chemistry associated with river-bank interaction, the spatial variability under which these interactions occurs remained unaccounted for, limiting the use of Cl as an effective tracer. Groundwater discharge to both the Tambo and Nicholson Rivers was the highest under high flow conditions in the days to weeks following significant rainfall, indicating that the rivers are well connected to a groundwater system that is responsive to rainfall. Groundwater constituted the lowest proportion of river discharge during times of increased rainfall that followed dry periods, while groundwater constituted the highest proportion of river discharge under baseflow conditions (21.4% of the Tambo in April 2010 and 18.9% of the Nicholson in September 2010).
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Baskaran, S., T. Ransley, R. S. Brodie, and P. Baker. "Investigating groundwater–river interactions using environmental tracers." Australian Journal of Earth Sciences 56, no. 1 (February 2009): 13–19. http://dx.doi.org/10.1080/08120090802541887.

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Parlov, Jelena, Zoran Kovač, and Jadranka Barešić. "The study of the interactions between Sava River and Zagreb aquifer system (Croatia) using water stable isotopes." E3S Web of Conferences 98 (2019): 12017. http://dx.doi.org/10.1051/e3sconf/20199812017.

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Water stable isotopes were used to investigate hydrological pathways and interactions between surface water and groundwater in the Zagreb aquifer system (Croatia). δ2H and δ18O values indicate a spatial variability of the influence of individual groundwater sources inside the aquifer – local precipitation and the Sava River water. Fractions of surface water in groundwater strongly depend on fluctuations of the river water level and less on the distance from the Sava River. These data extend our understanding of groundwater flow in the Zagreb aquifer system, interactions between Sava River water, local precipitation and groundwater. The results of the research allow more precise monitoring plans and definition of the sanitary protection zones of the well fields in the future.
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Hinzman, Larry D., Matthew Wegner, and Michael R. Lilly. "Hydrologic Investigations of Groundwater and Surface-water Interactions In Subarctic Alaska." Hydrology Research 31, no. 4-5 (August 1, 2000): 339–56. http://dx.doi.org/10.2166/nh.2000.0020.

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Dynamic interactions between rivers and adjacent aquifers can significantly affect near-bank geochemistry and processes associated with natural attenuation of contaminants by mixing water or introducing oxygen or nutrients. During 1997 and 1998 in a study near Fairbanks, Alaska U.S.A, the hydrologic conditions in the Chena River and in the adjacent groundwater were monitored. The river stage, groundwater elevations, and the water chemistry and temperature in both river and groundwater were measured. In the spring of 1997, the groundwater gradient close to the Chena River reversed causing surface water to enter the aquifer. Changes in temperature, specific conductance and alkalinity were used to determine the extent of bank recharge. For approximately one week during spring snowmelt of 1997, surface-water influx from the Chena River occurred approximately between the depths of 5.33 m and 9.1 m below ground surface. The effects of bank recharge extended at least 6.1 m but not to 30.5 m from the banks of the Chena River into the aquifer. Bank recharge caused 64 to 68 per cent of the groundwater, 6.1 m from the bank at a depth of 6.78 m to be displaced by surface water influx. Peak flows during 1998 were not high enough to cause flow reversals.
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Lee, Hyeonju, Min-Ho Koo, Juhyeon Lee, and Kangjoo Kim. "Changes in Stream–Aquifer Interactions Due to Gate Opening of the Juksan Weir in Korea." Water 13, no. 12 (June 10, 2021): 1639. http://dx.doi.org/10.3390/w13121639.

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The Juksan weir, installed in the Yeongsan river in South Korea from 2010 to 2012, has secured sustainable water resources and helped control flooding. However, low river flow velocities due to the weir have deteriorated the quality of the river water. For natural river restoration, the water gate was opened in 2017. In this study, the three-dimensional finite difference model Visual MODFLOW was used to analyze the effects of gate opening on stream–aquifer interactions. A conceptual model was developed to simulate the stream–aquifer dynamics caused by the operation of the water gate at the Juksan weir. Groundwater data were also analyzed to determine the impacts of weir operations on groundwater quality. Our results indicate that a lower river level due to the weir opening changed the groundwater flow, which then affected the water balance. The change in groundwater flow increased the variability of the groundwater quality which had homogenized because of induced recharge after the construction of the weir. This could affect groundwater use in agricultural areas near the weir. Therefore, further groundwater monitoring and hydrodynamic analyses are required to anticipate and address any potential issues.
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Brančić, Andjela, Anastasija Đordjević, and Dejan Nešković. "Characteristics of Groundwater–Surface Water Interaction in Areas with Scarce Input Data—Case Study of Banja River Catchment (Western Serbia)." Proceedings 2, no. 11 (August 1, 2018): 625. http://dx.doi.org/10.3390/proceedings2110625.

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Water resources monitoring traditionally refers to the observation of surface or groundwater as separate entities. However, in one watershed, almost all characteristics of surface water interact with groundwater. This research was done in order to obtain more accurate assumptions about the interaction between groundwater and surface water and establish recharge zones on the example of Banja river catchment area. This research shows the possibility to have both quantitative and qualitative analyses of groundwater–surface water interactions of some river catchment with limited input data in short period of time which can be beneficial, especially on remote locations.
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Kurth, A. M., C. Weber, and M. Schirmer. "How effective is river restoration in re-establishing groundwater – surface water interactions? – A case study." Hydrology and Earth System Sciences Discussions 12, no. 1 (January 23, 2015): 1093–118. http://dx.doi.org/10.5194/hessd-12-1093-2015.

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Abstract. In this study we investigated whether river restoration was successful in re-establishing vertical connectivity and, thereby, groundwater-surface water interactions, in a degraded urban stream. Well-tried passive Distributed Temperature Sensing (DTS) and novel active and passive DTS approaches were employed to study groundwater-surface water interactions in an experimental reach of an urban stream before and after its restoration and in two (near-) natural reference streams. Results were validated with Radon-222 analyses. Our results indicated that river restoration at the study site was indeed successful in increasing groundwater-surface water interactions. Increased surface water downwelling occurred locally at the tip of a gravel island created during river restoration. Hence, the installation of in-stream structures increased the vertical connectivity and thus groundwater-surface water interactions. With the methods presented in this publication it would be possible to routinely investigate the success of river restorations in re-establishing vertical connectivity, thereby gaining insight into the effectiveness of specific restoration measures. This, in turn, would enable the optimization of future river restoration projects, rendering them more cost-effective and successful.
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Dissertations / Theses on the topic "Groundwater-river interactions"

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Ivkovic, Karen Marie-Jeanne, and kardami@optusnet com au. "Modelling Groundwater-River Interactions for Assessing Water Allocation Options." The Australian National University. Centre for Resources, Environment and Society, 2007. http://thesis.anu.edu.au./public/adt-ANU20080901.134545.

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The interconnections between groundwater and river systems remain poorly understood in many catchments throughout the world, and yet they are fundamental to effectively managing water resources. Groundwater extraction from aquifers that are connected to river systems will reduce river flows, and this has implications for riverine ecosystem health, water security, aesthetic and cultural values, as well as water allocation and water management policies more generally. The decline in river flows as a consequence of groundwater extractions has the potential to threaten river basin industries and communities reliant on water resources. ¶ In this thesis the connectivity between groundwater and river systems and the impact that groundwater extractions have on river flows were studied in one of Australia’s most developed irrigation areas, the Namoi River catchment in New South Wales. ¶ Gauged river reaches in the Namoi River catchment were characterised according to three levels of information: 1) presence of hydraulic connection between aquifer-river systems; 2) dominant direction of aquifer-river flux; and 3) the potential for groundwater extraction to impact on river flows. The methods used to characterise the river reaches included the following analyses: 1) a comparison of groundwater and river channel base elevations using a GIS/Database; 2) stream hydrographs and the application of a baseflow separation filter; 3) flow duration curves and the percentage of time a river flows; 4) vertical aquifer connectivity from nested piezometer sites; and 5) paired stream and groundwater hydrographs. ¶ The theoretical responses for gaining, losing and variably gaining-losing river reaches were conceptualised along with the processes that operate in these systems. Subsequently, a map was prepared for the Namoi River catchment river reaches indicating aquifer-river connectivity and dominant direction of flux. Large areas of the Upper Namoi River catchment were found to have connected aquifer-river systems, with groundwater extraction bores located in close proximity to the rivers. Accordingly, the potential for groundwater extraction to impact on river flows in these areas was considered significant. The Lower Namoi was assessed as having mostly disconnected aquifer-river systems. ¶ In order to investigate the impacts of groundwater extraction on river flows in connected aquifer-river systems, a simple integrated aquifer-river model entitled IHACRES_GW was developed for use at the catchment scale. The IHACRES_GW model includes a dynamic, spatially-lumped rainfall-runoff model, IHACRES, combined with a simple groundwater bucket model that maintains a continuous water balance account of groundwater storage volumes for the upstream catchment area relative to the base of the stream, assumed to be the stream gauging station. The IHACRES_GW model was developed primarily: 1) to improve upon existing water allocation models by incorporating aquifer-river interactions; 2) to quantify the impacts of groundwater extraction on river flows within unregulated, connected aquifer-river systems; 3) to inform water policy on groundwater extraction; and 4) to be able to utilise the model in future integrated assessment of water allocations options at the catchment scale. ¶ The IHACRES_GW model was applied within the Cox’s Creek subcatchment in order to test its validity. The model was used to simulate a range of extraction scenarios which enabled the impacts of groundwater extractions on river flows to be assessed. In particular, the historical impacts of groundwater extraction on the timing, magnitude and frequency of baseflow events were quantified over a 15-year (1988-2003) simulation period. The IHACRES_GW model was also used to evaluate the implications of water sharing plans for the Cox’s Creek subcatchment. ¶ A spatially-lumped modelling approach in the management of water resources has a number of limitations, including those arising from the lack of spatial considerations. However, it offers a number of advantages including facilitating a better understanding of large-scale water management issues, assessing the impacts of water allocation and groundwater extraction on river flows at the catchment scale, and informing water sharing plans. In particular, this type of modelling approach lends itself to integrated assessments of water allocation options in which hydrological, ecological and socioeconomic data sets are combined, and where data is commonly aggregated to a larger scale of interest in response to the requirements of policy makers. The research findings from this thesis provide some insights into how to better manage the impacts of groundwater extraction in connected aquifer-river systems.
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Madlala, Tebogo Eugene. "Determination of groundwater-surface water interaction, upper Berg River catchment, South Africa." University of the Western Cape, 2015. http://hdl.handle.net/11394/5331.

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>Magister Scientiae - MSc
The present study investigated the application of a multi-method approach to determine groundwater-surface water (GW-SW) interactions to quantify and characterize the quality of water resources in a fractured rock aquifer system in upper catchment of the Berg River (G10A). Demonstrating methods for improved understanding of groundwater and surface water interactions is important for informing development of strategies that ensure effective utilization and management of water resources. Applying a single method to inform innovative strategies for water resources has proved futile. The current study shows how the use of several methods can provide the basis for devising practical strategies for water resource utilization and management. The three methods were applied as follows: First, the base flow separation was used whereby the Chapman and Lynne & Hollick digital filter algorithms were applied to time-series streamflow data from four stream gauging stations in the catchment. The computation from algorithms on three sites (gauging stations) showed that the mean Base Flow Index (BFI) value ranged between 7%-8% for the 2012-2014 periods. This means that discharges from subsurface water storages dominate stream flows throughout the study period. Secondly, the quality of groundwater and surface water was sampled using standard methods. Piper Diagrams generated on Aquachem™ software and radial charts were used to identify the predominant hydrochemical facies. Results showed that Na-Cl was the predominant GW and SW water-type. This means that both GW and SW are mainly influenced by recharging surface water as well as interaction occurring between the rock matrices and infiltrating water. Multivariate statistical analyses were used to evaluate the factors controlling GW and SW chemistry in the upper Berg River catchment and the results showed that GW and SW are influenced by natural processes. Two main factors (a. & b.) were extracted which explained 71.8% of the variation in both GW and SW physicochemical parameters. These factors include water-rock interactions and the recharge of surface water. Cluster Analysis extracted four major clusters that grouped sites with similar physicochemical characteristics together. Finally, differential stream gauging was applied to a 600m reach above the Berg River Dam. Three 200m sub-reaches were used to compute differences in flows between sub-reaches. Stream flow at each sub-reach was estimated using mass balance equations with electrical conductivity measurements during instant salt tracer injection tests. Results indicated that during both the wet season (high flow) dry season (low flow), the river continuously lost water to the subsurface. This was demonstrated by the 0.91m³/s and 2.24m³/s decrease in stream flow along the 600m reach. Dry season flow decreases were less than wet season flow decreases, indicated by markedly lower flow loss in respect to the wet season. This confirms results of the analysis of base flow separation, which indicated that discharges from subsurface storages dominate stream flows during low flow periods. The differential stream gauging approach did not provide distinct points along the selected stream reach where GW-SW interaction occurred; rather it provided a holistic representation of seasonal flow variations along the selected reach. This study showed that upper Berg River catchment is dependent on discharges from subsurface water storages to maintain dry season flows. Furthermore, this study showed that infiltration of surface water and discharge of subsurface water transfers the respective chemical signature of the contributor, meaning that the transfer of water of suitable quality will reduce contamination in the receiving water body (i.e. surface water). Transfer of water between subsurface and surface water contributed an average of 8% of the gauged flows in the catchment between 2012 and 2014, suggesting that the groundwater recharge process dominates this catchment.
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Foglia, Laura. "Alternative groundwater models to investigate river-aquifer interactions in an environmentally active alpine floodplain /." Zürich : ETH, 2006. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=16799.

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Simpson, Scott. "Modeling Stream-Aquifer Interactions During Floods and Baseflow: Upper San Pedro River, Southeastern Arizona." Thesis, The University of Arizona, 2007. http://hdl.handle.net/10150/193338.

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Streams and groundwaters interact in distinctly different ways during flood versus base flow periods. Recent research in the Upper San Pedro River using isotopic and chemical data shows that (1) near-stream, or 'riparian,' groundwater recharged during high streamflow periods is a major contributor to streamflow for the rest of the year, and (2) the amount of riparian groundwater derived from this flood recharge can vary widely (10-90%) along the river. Riparian groundwater in gaining reaches is almost entirely basin groundwater, whereas losing reaches are dominated by prior streamflow.This description of streamflow gives rise to the questions of (1) how much flood recharge occurs at the river-scale, and (2) subsequently, what is the relative importance of flood recharge and basin groundwater in maintaining the hydrologic state of the riparian system. To address these questions, a coupled hydrologic-solute model was constructed for 45 km of the Upper San Pedro riparian system.
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Wickham, Matthew Prior 1959. "The geochemistry of surface water and groundwater interactions for selected Black Mesa drainages, Little Colorado River basin, Arizona." Thesis, The University of Arizona, 1992. http://hdl.handle.net/10150/192063.

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Surface water and groundwater interactions involve complex physical processes that are not easily measured in most natural systems. Many of these processes can be indirectly evaluated by examining the geochemistry of the hydrologic system. In this investigation, a geochemical approach to investigating surface water and groundwater interactions is applied to perennial reaches of selected Black Mesa drainages in northeastern Arizona. The drainages, Moenkopi Wash and Dinnebito Wash, receive groundwater discharging from the regional Naquifer. Groundwater within the confined portion of the N-aquifer is chemically and isotopically distinct from that in the unconfined portion. Water in the majority of the confined N-aquifer exhibits a depleted δD and δ¹⁸O composition, a consequence of recharge under an earlier paleo climate. The small changes observed in chemical composition of baseflow along the streamcourse can be explained by chemical interaction with channel alluvium or minor exchange with groundwater from the alluvium.
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Naugler, Trudy Lynn. "Groundwater - surface water interactions in the Salmon River Watershed, BC : integrating spectroscopy, isotopes, water quality, and land use analyses." Thesis, University of British Columbia, 2007. http://hdl.handle.net/2429/31782.

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Understanding the sources and pathways of water pollutants is critical for protecting freshwater resources. Relationships between water quality and land use can be obscured by variable land use, seasonal variability, and interactions between surface water and groundwater. This research combines the tools of fluorescence spectroscopy, nitrate stable isotopes and water chemistry to better understand land use impacts on water quality. The Hopington aquifer, one of the most vulnerable aquifers in the Lower Fraser Valley, is a source of drinking water for the Township of Langley. This aquifer is also responsible for maintaining the summer stream flow in the Salmon River, a productive Coho salmon stream. Elevated nitrates in both ground and stream water are a concern. Twelve stream sites and eleven groundwater wells were sampled during 2006 to try and "fingerprint" different water sources. Samples were analyzed for: uv-visible absorbance, fluorescence, DOC, nutrients (ammonium, nitrate, ortho-phosphate), chloride, trace elements, and nitrate-isotopes (δ¹⁸0 and δ¹⁵N). The combination of these tools provided a more detailed look at the groundwater - surface water interactions and helped track pollutants within the system. Nitrate concentrations in the Salmon River increase where it cuts through the Hopington aquifer; concentrations peak in August when groundwater makes up the greatest proportion of the stream flow. Humic-like fluorescence was able to measure this groundwater influence because groundwater has much lower fluorescence. Nitrate isotopes showed that inorganic fertilizers were not a dominant source, but that soil N, septic tank leakage, and manure were possible sources. Stream sites influenced by groundwater had an isotopic fingerprint similar to nearby wells, showing that the nitrate source(s) were the same. A GIS-based land use analysis suggested that agricultural land use was having the greatest impact on local water quality, especially on surface waters in the wet season. Protein-like fluorescence showed potential as a tool for pollution monitoring and should be explored further.
Science, Faculty of
Resources, Environment and Sustainability (IRES), Institute for
Graduate
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Sprenger, Christoph [Verfasser]. "Surface-groundwater interactions associated with river bank filtration in Delhi (India) : investigation and modelling of hydraulic and hydrochemical processes / Christoph Sprenger." Berlin : Freie Universität Berlin, 2011. http://d-nb.info/1026069564/34.

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Fleming, Brandon J. "Effects of anthropogenic stage fluctuations on surface water/ground water interactions along the Deerfield River, Massachusetts." Amherst, Mass. : University of Massachusetts Amherst, 2009. http://scholarworks.umass.edu/theses/226/.

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Holmes, Stuart W. "Investigation of Spatial and Temporal Groundwater Thermal Anomalies at Zanesville Municipal Well Field, Ohio: Implications for Determination of River-Aquifer Connectivity Using Temperature Data." Ohio University / OhioLINK, 2016. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1462026430.

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Grapes, Timothy Rupert. "Groundwater-river interaction in a chalk catchment : the River Lambourn, UK." Thesis, University of Birmingham, 2004. http://etheses.bham.ac.uk//id/eprint/4036/.

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Chalk streams are of high ecological value and are dependent upon groundwater discharge to support flows. This study investigates chalk stream-aquifer interaction, focusing on a near-natural catchment; the River Lambourn of the West Berkshire Downs. The topographic catchment of the Lambourn is 234km², principally underlain by Upper Chalk. The river has a perennial length of c.16km, and a 7.5km seasonal section. Temporal dynamics of the recharge-storage-discharge sequence are investigated using linear regression techniques to identify the lag between recharge and discharge. The effective maximum duration of groundwater flow is 9.1 months, which is used with regional hydraulic gradients to calculate a bulk (interfluve) hydraulic conductivity of 114m/d (using Sy=1%), suggesting that interfluve permeability has been historically underestimated. Spatial flow accretion on the Lambourn is defined from 12 reaches (each 1-2km long), exhibiting mean accretion rates between -0.019 and 0.211 cumecs/km. The accretion rate profile approximates a sinusoidal pattern (λ=12km) suggesting a catchment scale litho-structural control. However, local topography and lithology also exert influence. High accretion rate reaches are associated with major dry valley intersections and elevated valley floor permeability, whilst the presence of Chalk Rock at shallow depths restricts local accretion.
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Books on the topic "Groundwater-river interactions"

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Carey, Barbara M. Groundwater/surface water interactions in the Upper Sammamish River: A preliminary analysis. Olympia, WA: Washington State Dept. of Ecology, 2003.

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Carey, Barbara M. Groundwater/surface water interactions in the Upper Sammamish River: A preliminary analysis. Olympia, WA: Washington State Dept. of Ecology, 2003.

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Caldwell, Rodney R. Groundwater and surface-water interaction within the upper Smith River Watershed, Montana, 2006-2010. Reston, Virginia: U.S. Department of the Interior, U.S. Geological Survey, 2013.

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Cowdery, T. K. Hydrogeology and ground-water/surface-water interactions in the Des Moines River Valley, Southwestern Minnesota, 1997-2001. Reston, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2005.

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Simonds, F. W. Surface water-ground water interactions along the lower Dungeness River and vertical hydraulic conductivity of streambed sediments, Clallam County, Washington, September 1999-July 2001. Tacoma, Wash: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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Simonds, F. W. Surface water-ground water interactions along the lower Dungeness River and vertical hydraulic conductivity of streambed sediments, Clallam County, Washington, September 1999-July 2001. Tacoma, Wash: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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Quantitative Assessment of Groundwater and Surface Water Interactions in the Hailiutu River Basin Erdos Plateau China. Taylor & Francis Group, 2018.

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Yang, Zhi. Quantitative Assessment of Groundwater and Surface Water Interactions in the Hailiutu River Basin, Erdos Plateau, China. Taylor & Francis Group, 2018.

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Yang, Zhi. Quantitative Assessment of Groundwater and Surface Water Interactions in the Hailiutu River Basin, Erdos Plateau, China. Taylor & Francis Group, 2018.

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Yang, Zhi. Quantitative Assessment of Groundwater and Surface Water Interactions in the Hailiutu River Basin, Erdos Plateau, China. Taylor & Francis Group, 2018.

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Book chapters on the topic "Groundwater-river interactions"

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Hussain, Syed Aaquib, Kousik Das, Soumendra Nath Bhanja, and Abhijit Mukherjee. "Potential Impact of Climate Change on Surface Water and Groundwater Interactions in Lower Reaches of Ganges River, India." In Springer Hydrogeology, 583–91. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-10-3889-1_34.

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Nawalany, M. "Combining the Analytical and Finite Element Models of the River-Groundwater Interaction." In Computational Methods in Water Resources X, 83–90. Dordrecht: Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-010-9204-3_11.

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Shamsuddin, Mohd Khairul Nizar, Wan Nor Azmin Sulaiman, Mohammad Firuz Ramli, Faradiella Mohd Kusin, and Anuar Sefie. "Numerical Simulation of Groundwater and Surface Water Interaction and Particle Tracking Movement Due to the Effect of Pumping Abstraction of Lower Muda River." In Advances in Sustainable and Environmental Hydrology, Hydrogeology, Hydrochemistry and Water Resources, 249–52. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01572-5_60.

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Kumar, M. Dinesh. "Changing Surface Water–Groundwater Interactions in Narmada River Basin." In Managing Water in River Basins, 150–77. Oxford University Press, 2010. http://dx.doi.org/10.1093/acprof:oso/9780198065364.003.0006.

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"Multispecies and Watershed Approaches to Freshwater Fish Conservation." In Multispecies and Watershed Approaches to Freshwater Fish Conservation, edited by Sarah Robertson, Brad D. Wolaver, Todd G. Caldwell, Timothy W. Birdsong, Ryan Smith, Thomas Hardy, Julie Lewey, and Joe Joplin. American Fisheries Society, 2019. http://dx.doi.org/10.47886/9781934874578.ch13.

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<em>Abstract</em>.—The Devils River is a groundwater-dominated, semiarid river in southwest Texas and considered one of the most pristine rivers in the state. It is one of the last strongholds for multiple species of regionally endemic freshwater fishes and mussels. However, groundwater pumping in the watershed poses an imminent threat to the river and its fragile ecosystem. Reductions in groundwater availability have the potential to result in concomitant reductions in spring discharge and thus instream flows. Base flow reductions would negatively impact many already imperiled aquatic species and degrade one of the state’s most remote and scenic paddling and angling destinations. Development of a comprehensive basinwide fish and mussel conservation plan is ideal due to the relatively small size of the watershed. However, challenges include the isolated location of the river and the low proportion of publicly held lands for implementing on-the-ground conservation measures. To best determine science needs, focus resources, and increase informed stewardship of the river, the Texas Parks and Wildlife Department has partnered with governmental agencies, universities, nonprofit organizations, and landowners interested in preserving this unique resource. Through collaborative research aimed at a better understanding of groundwater–surface water interactions and instream flow needs of endemic species, and by building cooperative relationships with landowners and nonprofit conservation organizations, steps are underway to preserve the esthetic, ecological, and recreational values of the Devils River.
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Fukushima, Y., J. Chen, and M. Taniguchi. "Surface and groundwater interactions in the lower reach of the Yellow River." In From Headwaters to the Ocean, 301–5. CRC Press, 2008. http://dx.doi.org/10.1201/9780203882849.ch45.

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Yang, Zhi. "Groundwater-Surface Water Interactions under Different Land Use Scenarios." In Quantitative Assessment of Groundwater and Surface Water Interactions in the Hailiutu River Basin, Erdos Plateau, China, 59–87. CRC Press, 2018. http://dx.doi.org/10.1201/9780429487385-4.

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E. Stevens, Lawrence, Raymond R. Johnson, and Christopher Estes. "Characteristics and Process Interactions in Natural Fluvial–Riparian Ecosystems: A Synopsis of the Watershed-Continuum Model." In River Basin Management - Under a Changing Climate [Working Title]. IntechOpen, 2022. http://dx.doi.org/10.5772/intechopen.107232.

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The watershed-continuum model (WCM) describes fluvial-riparian ecosystems (FREs) as dynamic reach-based ecohydrogeological riverine landscapes linking aquatic, riparian, and upland domains within watersheds. FRE domains include aquatic (channels, hyporheic zones, springs, other groundwater zones and in-channel lakes), riparian, and adjacent upland zones, all of which can interact spatio-temporally. Occupying only a minute proportion of the terrestrial surface, FREs contain and process only a tiny fraction of the Earth’s freshwater, but often are highly productive, flood-disturbed, and ecologically interactive, supporting diverse, densely-packed biotic assemblages and socio-cultural resource uses and functions. FRE biodiversity is influenced by hydrogeomorphology, ecotonal transitions, and shifting habitat mosaics across stage elevation. Thus, the WCM integrates physical, biological, and socio-cultural characteristics, elements, and processes of FREs. Here, we summarize and illustrate the WCM, integrating diverse physical and ecological conceptual models to describe natural (unmanipulated) FRE dynamics. We integrate key processes affecting FRE forms and functions, and illustrate reach-based organization across temporal and spatial scales. Such a holistic approach into natural FRE structure and functions provides a baseline against which to measure and calibrate ecosystem alteration, management, and rehabilitation potential. Integration of groundwater, fluvial, and lacustrine ecological interactions within entire basins supports long-term, seasonally-based sustainable river management, which has never been more urgently needed.
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Yang, Zhi. "A multi-method approach to quantify Groundwater/surface water interactions." In Quantitative Assessment of Groundwater and Surface Water Interactions in the Hailiutu River Basin, Erdos Plateau, China, 35–58. CRC Press, 2018. http://dx.doi.org/10.1201/9780429487385-3.

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Buono, Regina M., and Gabriel Eckstein. "Current challenges in the Rio Grande/Río Bravo Basin: old disputes in a new century." In Water Resources Allocation and Agriculture, 243–54. IWA Publishing, 2022. http://dx.doi.org/10.2166/9781789062786_0243.

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Abstract The Rio Grande River traverses 2000 kilometres of the international border between Mexico and the United States. The river and its tributaries are governed by a series of border treaties and institutions, as well as under the domestic laws of each nation. Often lauded for enabling innovative and collaborative governance, in recent years the complicated regime has come under pressure as domestic and international water governance institutions struggle under the strain of climate change, population growth, and other stressors on water supply and demand in the region. This chapter considers three of the major challenges currently facing the Rio Grande River Basin and its riparians: (1) groundwater and ground–surface interactions and related practical and policy implications; (2) engagement with local and regional stakeholders; and (3) Mexico's latest water debt under the 1944 Treaty. It also identifies shortcomings in the regime to address these concerns, as well as innovative responses and solutions that have been crafted at various levels of governance.
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Conference papers on the topic "Groundwater-river interactions"

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Yu, Weidong, and Chunhui Li. "Interactions between Polluted River and Groundwater -- A Case Study of the Weihe River, China." In 2012 International Conference on Biomedical Engineering and Biotechnology (iCBEB). IEEE, 2012. http://dx.doi.org/10.1109/icbeb.2012.253.

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Dawson, Claudia, Joe Yelderman, and Will Brewer. "GROUNDWATER/ SURFACE WATER INTERACTIONS: GRAVEL PIT LAKES IN THE BRAZOS RIVER ALLUVIUM AQUIFER." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-369719.

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Nguyen, Thuy Thanh, Akira Kawamura, Cat Minh Vu, Duong Du Bui, Hideo Amaguchi, and Naoko Nakagawa. "Interactions between the Surface Water and Groundwater of the Red River in Hanoi, Vietnam." In World Environmental And Water Resources Congress 2012. Reston, VA: American Society of Civil Engineers, 2012. http://dx.doi.org/10.1061/9780784412312.011.

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Dyer, J. R., L. J. Crossey, and A. S. Ali. "GROUNDWATER-SURFACE WATER INTERACTIONS; EFFECTS OF HYDROTHERMAL SPRING INPUTS TO JEMEZ RIVER WATER QUALITY." In 2007 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2007. http://dx.doi.org/10.56577/sm-2007.922.

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Darul, A., D. E. Irawan, and N. J. Trilaksono. "Groundwater and river water interaction on Cikapundung River: Revisited." In THE 5TH INTERNATIONAL CONFERENCE ON MATHEMATICS AND NATURAL SCIENCES. AIP Publishing LLC, 2015. http://dx.doi.org/10.1063/1.4930778.

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Ramdhan, A., A. Arifin, and R. Suwarman. "Assessing Groundwater-Citarum River Interaction and Groundwater Contribution to Flooding." In NSG2021 27th European Meeting of Environmental and Engineering Geophysics. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202120067.

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Shesterkin, V. P., and I. V. Kostomarova. "GROUNDWATER HYDROCHEMISTRY OF THE BOTCHI RIVER BASIN." In The Geological Evolution of the Water-Rock Interaction. Buryat Scientific Center of SB RAS Press, 2018. http://dx.doi.org/10.31554/978-5-7925-0536-0-2018-207-209.

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Wang, B. b., W. r. Huang, Y. Cai, F. Teng, and Q. Zhou. "Numerical investigation of the river-groundwater interaction characteristics in the downstream desert of the Heihe River, China." In 2015 International Forum on Energy, Environment Science and Materials. Paris, France: Atlantis Press, 2015. http://dx.doi.org/10.2991/ifeesm-15.2015.231.

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Huan Huan, Jinsheng Wang, Jieqiong Zheng, and Yuanzheng Zhai. "Water -rock interaction simulation of groundwater in the Yongding River alluvial fan of Beijing plain." In 2011 International Symposium on Water Resource and Environmental Protection (ISWREP). IEEE, 2011. http://dx.doi.org/10.1109/iswrep.2011.5892934.

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Born, Connor Luke. "ABSTRACT TITLE: INVESTIGATION OF GROUNDWATER-SURFACE WATER INTERACTION IN A SOUTH FLORIDA ESTUARY: SHARK RIVER SLOUGH." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320496.

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Reports on the topic "Groundwater-river interactions"

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Campbell, M. D. Monitoring groundwater and river interaction along the Hanford reach of the Columbia River. Office of Scientific and Technical Information (OSTI), April 1994. http://dx.doi.org/10.2172/10142634.

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Peterson, Robert E. Zone of Interaction Between Hanford Site Groundwater and Adjacent Columbia River. Office of Scientific and Technical Information (OSTI), October 2001. http://dx.doi.org/10.2172/787967.

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Peterson, Robert E., and Michael P. Connelly. Zone of Interaction Between Hanford Site Groundwater and Adjacent Columbia River. Office of Scientific and Technical Information (OSTI), October 2001. http://dx.doi.org/10.2172/965723.

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Provencher, S. K., B. Mayer, and S. E. Grasby. Aqueous geochemistry of the Englishman River Watershed, Parksville, British Columbia for use in assessment of potential surface water-groundwater interaction. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292678.

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PETERSEN SW. TECHNICAL EVALUATION OF THE INTERACTION OF GROUNDWATER WITH THE COLUMBIA RIVER AT THE DEPARTMENT OF ENERGY HANFORD SITE 100-D AREA. Office of Scientific and Technical Information (OSTI), November 2008. http://dx.doi.org/10.2172/943297.

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