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Dissertations / Theses on the topic 'Groundwater-river interactions'

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Published: 4 June 2021

Last updated: 28 January 2023

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1

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 c

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2

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<br>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

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3

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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4

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 des

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5

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-aquife

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6

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 al

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7

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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8

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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9

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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10

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 maximu

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11

Worakijthamrong, Surin. "Groundwater-River Interaction in the Context of Interbasin Transfer." Thesis, University of Bristol, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.526010.

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12

Porter, Sandra. "Groundwater/surface water interaction in the Raisin River watershed, near Cornwall, Ontario." Thesis, University of Ottawa (Canada), 1996. http://hdl.handle.net/10393/10133.

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A field study was conducted in 1994 and 1995 to understand the interaction of groundwater and surface water in the Raisin River watershed, near Cornwall, Ontario. The Raisin River lies within an agricultural region which relies heavily on groundwater use. The regional groundwater supply is predominantly from a limestone aquifer which underlies various surficial deposits (primarily glacial till). Groundwater movement appears to be in a southeasterly direction, towards the St. Lawrence River. Seepage meters, mini-piezometers, and a falling head permeameter were used to (i) measure the flux of gr

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13

Lovell, Daniel Martin. "Conjunctive management of groundwater and surface water in the Upper Ovens River Valley /." Connect to thesis, 2009. http://repository.unimelb.edu.au/10187/5724.

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14

Jahnke, Philip, and Philip Jahnke. "Modeling of groundwater flow and surface/groundwater interaction for the San Pedro River Basin from Fairbank to Redington, Arizona." Thesis, The University of Arizona, 1994. http://hdl.handle.net/10150/626882.

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15

Cameron, Stewart Graham. "A hydrogeological study of the interaction between Avon River baseflow and shallow groundwater, Christchurch, New Zealand." Thesis, University of Canterbury. Geology, 1992. http://hdl.handle.net/10092/8023.

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The relationship between shallow groundwater levels and Avon River baseflow upstream of Gloucester Street has been investigated. Avon River baseflow is supplied by shallow groundwater-fed springs. Historical and anecdotal information indicate that since European settlement of the Christchurch area in the 1850's, Avon River baseflow has declined. The baseflow decline is attributed to the progressive lowering of the Christchurch area watertable which has caused downstream migration of headwater spring positions and a reduction in spring discharge. Prior to this study minimal historical Avon Rive

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16

Banda, Vincent Santos Dzulani. "Assessing hydrogeological characteristics to establish influence of aquifer-river interaction in non-perennial river systems, Heuningnes catchment." University of the Western Cape, 2019. http://hdl.handle.net/11394/7007.

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>Magister Scientiae - MSc<br>Over half of total flows in the global river network are composed of non-perennial rivers. This indicates the importance of non-perennial river systems in supporting the biodiversity. It has been established that groundwater is one of the elements that control the flow regimes and classification (whether perennial or not) of a river system. However, the use of hydrogeological characteristics to establish the influence of groundwater on non-perennial river systems remain to be widely unpublished. This study, therefore, intends to conceptualize and explain the role o

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17

Donelan, Jack E. "Groundwater-Surface Water Interaction in the Kern River| Estimates of Baseflow from Dissolved Radon Analysis and Hydrograph Separation Techniques." Thesis, California State University, Long Beach, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10841176.

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<p> Geochemical mixing methods utilizing <sup>222</sup>Rn and chloride and statistical hydrograph separation techniques were carried out in an attempt to understand baseflow dynamics in a section of the Kern River in the Sierra Nevada of Southern California. <sup>222</sup>Rn has become a valuable tool for evaluating groundwater inflow to a river, particularly when groundwater and surface water have similar major ion geochemistry. When using geochemical methods it is important to minimize uncertainty through comparison with separate tracers and techniques, though this is complicated in this set

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18

Tien, Anh Tho. "The influence of climate variability on hydrological processes and surface and groundwater hydrochemistry : the tropical upper roper river catchment, Northern Territory, Australia." Thesis, Queensland University of Technology, 2010. https://eprints.qut.edu.au/44150/1/Anh_Tien_Thesis.pdf.

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The Upper Roper River is one of the Australia’s unique tropical rivers which have been largely untouched by development. The Upper Roper River catchment comprises the sub-catchments of the Waterhouse River and Roper Creek, the two tributaries of the Roper River. There is a complex geological setting with different aquifer types. In this seasonal system, close interaction between surface water and groundwater contributes to both streamflow and sustaining ecosystems. The interaction is highly variable between seasons. A conceptual hydrogeological model was developed to investigate the diff

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19

Vionnet, Leticia Beatriz, and Thomas Maddock. "Modeling of Ground-Water Flow and Surface/Ground-Water Interaction for the San Pedro River Basin Part I Mexican Border to Fairbank, Arizona." Department of Hydrology and Water Resources, University of Arizona (Tucson, AZ), 1992. http://hdl.handle.net/10150/614152.

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Many hydrologic basins in the southwest have seen their perennial streamflows turn to ephemeral, their riparian communities disappear or be jeopardized, and their aquifers suffer from severe overdrafts. Under -management of ground -water exploitation and of conjunctive use of surface and ground waters are the main reasons for these events.

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20

Zlatos, Caitlan McEwen. "Using Geochemical Tracers to Determine Aquifer Connectivity, Flow Paths, and Base-Flow Sources: Middle Verde River Watershed, Central Arizona." Thesis, The University of Arizona, 2008. http://hdl.handle.net/10150/193443.

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Combining geochemical data with physical data produces a powerful method for understanding sources and fluxes of waters to river systems. This study highlights this for river systems in regions of complex hydrogeology, shown here through the identification and quantification of base-flow sources to the Verde River and its tributaries within the middle Verde River watershed. Specifically, geochemical tracers (major solutes, stable and radioactive isotopes) characterize the principal aquifers (C, Redwall-Muav, and Verde Formation) and provide a conceptual understanding of the hydrologic connec

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21

Yitbarek, Baye Andarge. "Hydrogeological and hydrochemical framework of complex volcanic system in the Upper Awash River basin, Central Ethiopia : with special emphasis on inter-basins groundwater transfer between Blue Nile and Awash rivers." Poitiers, 2009. http://theses.edel.univ-poitiers.fr/theses/2009/Yitbarek-Baye-Andarge/2009-Yitbarek-Baye-Andarge-These.pdf.

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Une approche utilisant plusieurs méthodes convergentes a été mise en oeuvre pour étudier le cadre hydrogéologique du système aquifère volcanique fracturé et complexe du bassin supérieur du fleuve Awash situé sur le bord du Rift éthiopien. L'écoulement des eaux souterraines et les mécanismes de recharge des différents aquifères ont été étudiés à l'aide de méthodes conventionnelles de terrain, de l'hydrochimie, de l'hydrologie isotopique et de la modélisation numérique des flux souterrains. Des relations lithohydrostratigraphiques ont été établies à partir des logs lithologiques de forages explo

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22

Arantes, Eudes José. "Emprego de infiltrômetros na caracterização da interação entre rio e aqüífero." Universidade de São Paulo, 2003. http://www.teses.usp.br/teses/disponiveis/18/18138/tde-15062007-162427/.

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O presente trabalho visa a quantificação do escoamento de água na interação entre rio e aqüífero subterrâneo em uma bacia, através da utilização de infiltrômetros e de poços de observação de lençol freático na proximidade do rio. O Ribeirão da Onça, um afluente do rio Jacaré-Guaçú localizado no município de Brotas no estado de São Paulo, foi escolhido para a realização deste estudo sendo a sua bacia hidrográfica pertencente a importante área de recarga do aqüífero Guarani. O estudo da interação rio aqüífero foi realizado através de infiltrômetros colocados em três seções deste rio. Analisando-

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23

Kjellander, Kalle. "River-Aquifer Interaction in the Uppsala Esker - a Modelling Study of a Proposed Drinking Water Production site." Thesis, Uppsala universitet, Luft-, vatten och landskapslära, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-355671.

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The Swedish municipalities of Gävle and Älvkarleby need new sources of drinking water as the population grows. Gästrike vatten AB has employed the consultant firm Midvatten AB to assess the possibility of a new groundwater extraction site on the Uppsala esker between Älvkarleby and Skutskär in northern Uppland county. It has been observed that the natural recharge to the aquifer in the Uppsala esker might be too low to compensate for a future groundwater extraction and that there is a risk of induced infiltration from the river Dalälven if the water table is lowered. River water might bring or

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24

Smith, Donna Lee. ""Redox pumping" in the near surface Missoula aquifer iin the flood plain of the Clark Fork River surface, water and groundwater interaction and arsenic related chemistry at a compost facility near a wastewater treatment plant /." CONNECT TO THIS TITLE ONLINE, 2008. http://etd.lib.umt.edu/theses/available/etd-06062008-105818/.

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25

Du, Mingxuan. "Modélisation intégrée des écoulements souterrains et des échanges nappe-rivière dans la basse vallée du Var." Thesis, Université Côte d'Azur (ComUE), 2016. http://www.theses.fr/2016AZUR4107/document.

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La modélisation hydraulique avec modèle déterministe est une méthode largement utilisée. Cependant,lamodélisation est un ptocessus complexe, notamrnent pour les aquifères où la quantité et la qualité desdonnées ne sont pas satisfaisantes. Etantune des sources pdncipales de I'eau douce dans la basse valléedu Var, Côte d',{.zur,Frarrce,la nappe libre de lavallée est menacée parla pénurie et la pollution. Maþéle grand nombre d'études effectuées dans cette zone, la dynamique des écoulements souterrains esttoujours patiellement inconnue. Par conséquent, la métropole Nice Côte d'Azur a besoin de dév

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26

Ivkovic, Karen Marie-Jeanne. "Modelling Groundwater-River Interactions for Assessing Water Allocation Options." Phd thesis, 2006. http://hdl.handle.net/1885/49342.

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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 c

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27

Rheineck, Bruce D. "River-groundwater interactions and implications for wellhead protection at Black River Falls, Wisconsin." 1995. http://catalog.hathitrust.org/api/volumes/oclc/35210639.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 1995.<br>Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 69-74).

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28

Pfeiffer, Shaili Margreta. "Groundwater/surface water interactions in a lowland savanna on the Lower Wisconsin River floodplain." 2001. http://catalog.hathitrust.org/api/volumes/oclc/47228947.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 2001.<br>Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 156-159).

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29

Raanan, Kiperwas Hadas. "Radium Isotopes as Tracers of Groundwater-Surface Water Interactions in Inland Environments." Diss., 2011. http://hdl.handle.net/10161/4971.

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<p>Groundwater has an important role in forging the composition of surface water, supplying nutrients crucial for the development of balanced ecosystems and potentially introducing contaminants into otherwise pristine surface water. Due to water-rock interactions radium (Ra) in groundwater is typically much more abundant than in surface water. In saline environments Ra is soluble and is considered a conservative tracer (apart for radioactive decay) for Ra-rich groundwater seepage. Hence in coastal environments, where mostly fresh groundwater seep into saline surface water, Ra has been the prom

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30

Somerville, Peter Douglas. "Streamwater-groundwater interactions and implications for water sharing plans in unregulated catchments : Hunter Valley, eastern Australia." Phd thesis, 2010. http://hdl.handle.net/1885/150497.

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A key objective of the Australian National Water Iriitiative of 2004 (clause 23(x)) is that streamwater and groundwater be managed as a single connected system. The National Water Act of 2007 established water sharing plans as a mechanism for ensuring this integrated management of streamwater and groundwater and for driving the sustainable management of Australia's water resources. This thesis investigates streamwater-groundwater interactions in an unconfined alluvial aquifer system in the Widden Brook catchment in the highly productive upper Hunter Valley, eastern Australia. Widden Brook is

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31

Wickham, Matthew Prior. "The geochemistry of surface water and groundwater interactions for selected Black Mesa drainages, Little Colorado River basin, Arizona." 1992. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_e9791_1992_138_sip1_w.pdf&type=application/pdf.

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32

Nainggolan, Lamtupa, and 寧古蘭. "Implementation of Regression Kriging method to assess spatial-temporal interactions between groundwater levels and recharge in Choushui River Basin." Thesis, 2018. http://ndltd.ncl.edu.tw/handle/ezy8c5.

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碩士<br>國立中央大學<br>應用地質研究所<br>106<br>The sparse distribution of groundwater stations in Choushui River Basin limits spatial-temporal of groundwater level information in these region while this information was crucial needed to know for groundwater conservation purposes. This study reports on an effort to improve the interpolation of monthly groundwater level from groundwater stations using Ordinary Kriging (OK) and Regression Kriging (RK), spanning the period from 2006 to 2015. In order to know the effort precipitation to the groundwater level, the interpolation groundwater level of RK has used t

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33

Dixon-Jain, Prachi. "Groundwater-surface water interactions : implications for nutrient transport to tropical rivers." Phd thesis, 2008. http://hdl.handle.net/1885/9514.

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The interaction between groundwater and surface water systems is a key component of the hydrological cycle and an understanding of their connectivity is fundamental for sustainable water resource management. Water is a vehicle for mobilising dissolved constituents, including nutrients, between surface and subsurface waters and between terrestrial and marine systems. Therefore, knowledge of surface-subsurface linkages is critical not only for water quantity allocation, but also for water quality and its implications for ecosystem health. In particular, ascertaining the significance of groundwa

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34

Nzama, Stanley Mvuselelo. "Spatial and temporal assessment of groundwater-surface water interaction, Schoonspruit river catchment, North West, South Africa." Diss., 2016. http://hdl.handle.net/10500/22083.

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The study presents the spatio-temporal assessment of groundwater-surface water (GW-SW) interaction aspects in the Schoonspruit River catchment, North West of South Africa. The research study aimed at improving understanding of groundwater and surface water interaction through assessing its location and time when such interaction occurs. GW-SW interaction sites were identified using principal aquifer type characterization methods. The occurrence of the interaction was established using hydrochemistry methods and the effectiveness of the existing monitoring methods were evaluated in their consid

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35

Chen, I.-Ting, and 陳苡庭. "A Study of Interaction between Groundwater and Surface Water in Zhuoshui River Basin Using Self-Organizing Map." Thesis, 2013. http://ndltd.ncl.edu.tw/handle/46400384257321987018.

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碩士<br>淡江大學<br>水資源及環境工程學系碩士班<br>101<br>In Taiwan, Zhuoshui River alluvial fan is one of the most abundant groundwater resources that are low-cost and easy-to-use; the area has seriously suffered from overuse of groundwater. For safe yield and effective use of groundwater resources in Zhuoshui River basin, investigating the interaction relationship between surface water and groundwater is important. This study used Self-Organizing Map (SOM) to investigate the effects of hydrological factors, including precipitation and streamflow, on the variability of groundwater level. Through the topological

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36

Briody, Alyse Colleen. "Flow, nutrient, and stable isotope dynamics of groundwater in the parafluvial/hyporheic zone of a regulated river during a small pulse." Thesis, 2014. http://hdl.handle.net/2152/26921.

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Periodic releases from an upstream dam cause rapid stage fluctuations in the Colorado River near Austin, Texas. These daily pulses modulate fluid exchange and residence times in the hyporheic region, where biogeochemical reactions are pronounced. We installed two transects of wells perpendicular to the river to examine in detail the reactions occurring in this zone of surface-water and groundwater exchange. One well transect recorded physical water level fluctuations and allowed us to map hydraulic head gradients and fluid movement. The second transect allowed for water sample collection at t

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37

(7026707), Siddharth Saksena. "Integrated Flood Modeling for Improved Understanding of River-Floodplain Hydrodynamics: Moving beyond Traditional Flood Mapping." Thesis, 2019.

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<div>With increasing focus on large scale planning and allocation of resources for protection against future flood risk, it is necessary to analyze and improve the deficiencies in the conventional flood modeling approach through a better understanding of the interactions between river hydrodynamics and subsurface processes. Recent studies have shown that it is possible to improve the flood inundation modeling and mapping using physically-based integrated models that incorporate observable data through assimilation and simulate hydrologic fluxes using the fundamental laws of conservation of mas

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38

Arik, Aida D. "A study of stream temperature using distributed temperature sensing fiber optics technology in Big Boulder Creek, a tributary to the Middle Fork John Day River in eastern Oregon." Thesis, 2011. http://hdl.handle.net/1957/26338.

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The Middle Fork John Day Basin in Northeastern Oregon is prime habitat for spring Chinook salmon and Steelhead trout. In 2008, a major tributary supporting rearing habitat, Big Boulder Creek, was restored to its historic mid-valley channel along a 1 km stretch of stream 800 m upstream of the mouth. Reduction of peak summer stream temperatures was among the goals of the restoration. Using Distributed Temperature Sensing (DTS) Fiber Optic Technology, stream temperature was monitored prior to restoration in June 2008, and after restoration in September 2008, July 2009, and August 2009. Data gathe

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