Relevant bibliographies by topics / Groundwater flow

Academic literature on the topic 'Groundwater flow'

Author: Grafiati
Published: 4 June 2021
Last updated: 29 July 2024

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Contents

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Groundwater flow.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Groundwater flow"

1

Haria, A. H., and P. Shand. "Evidence for deep sub-surface flow routing in forested upland Wales: implications for contaminant transport and stream flow generation." Hydrology and Earth System Sciences 8, no. 3 (June 30, 2004): 334–44. http://dx.doi.org/10.5194/hess-8-334-2004.

Full text
Abstract:
Abstract. Upland streamflow generation has traditionally been modelled as a simple rainfall-runoff mechanism. However, recent hydrochemical studies conducted in upland Wales have highlighted the potentially important role of bedrock groundwater in streamflow generation processes. To investigate these processes, a detailed and novel field study was established in the riparian zone and lower hillslopes of the Hafren catchment at Plynlimon, mid-Wales. Results from this study showed groundwater near the river behaving in a complex and most likely confined manner within depth-specific horizons. Rapid responses to rainfall in all boreholes at the study site indicated rapid recharge pathways further upslope. The different flow pathways and travel times influenced the chemical character of groundwaters with depth. Groundwaters were shown to discharge into the stream from the fractured bedrock. A lateral rapid flow horizon was also identified as a fast flow pathway immediately below the soils. This highlighted a mechanism whereby rising groundwater may pick up chemical constituents from the lower soils and transfer them quickly to the stream channel. Restrictions in this horizon resulted in groundwater upwelling into the soils at some locations indicating soil water to be sourced from both rising groundwater and rainfall. The role of bedrock groundwater in upland streamflow generation is far more complicated than previously considered, particularly with respect to residence times and flow pathways. Hence, water quality models in upland catchments that do not take account of the bedrock geology and the groundwater interactions therein will be seriously flawed. Keywords: bedrock, groundwater, Hafren, hillslope hydrology, Plynlimon, recharge, soil water, streamflow generation
APA, Harvard, Vancouver, ISO, and other styles
2

Swenson, Guy. "Remember Groundwater Flow." Groundwater Monitoring & Remediation 38, no. 3 (May 8, 2018): 17. http://dx.doi.org/10.1111/gwmr.12284.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Hartmann, Andreas, Scott Jasechko, Tom Gleeson, Yoshihide Wada, Bartolomé Andreo, Juan Antonio Barberá, Heike Brielmann, et al. "Risk of groundwater contamination widely underestimated because of fast flow into aquifers." Proceedings of the National Academy of Sciences 118, no. 20 (May 10, 2021): e2024492118. http://dx.doi.org/10.1073/pnas.2024492118.

Full text
Abstract:
Groundwater pollution threatens human and ecosystem health in many regions around the globe. Fast flow to the groundwater through focused recharge is known to transmit short-lived pollutants into carbonate aquifers, endangering the quality of groundwaters where one quarter of the world’s population lives. However, the large-scale impact of such focused recharge on groundwater quality remains poorly understood. Here, we apply a continental-scale model to quantify the risk of groundwater contamination by degradable pollutants through focused recharge in the carbonate rock regions of Europe, North Africa, and the Middle East. We show that focused recharge is the primary reason for widespread rapid transport of contaminants to the groundwater. Where it occurs, the concentration of pollutants in groundwater recharge that have not yet degraded increases from <1% to around 20 to 50% of their concentrations during infiltration. Assuming realistic application rates, our simulations show that degradable pollutants like glyphosate can exceed their permissible concentrations by 3 to 19 times when reaching the groundwater. Our results are supported by independent estimates of young water fractions at 78 carbonate rock springs over Europe and a dataset of observed glyphosate concentrations in the groundwater. They imply that in times of continuing and increasing industrial and agricultural productivity, focused recharge may result in an underestimated and widespread risk to usable groundwater volumes.
APA, Harvard, Vancouver, ISO, and other styles
4

Setyaningsih, D. L., K. D. Setyawan, D. P. E. Putra, and Salahuddin. "Hydrogeological Conceptual Model in the Middle of Randublatung Groundwater Basin." IOP Conference Series: Earth and Environmental Science 926, no. 1 (November 1, 2021): 012078. http://dx.doi.org/10.1088/1755-1315/926/1/012078.

Full text
Abstract:
Abstract Randublatung groundwater basin is one of the groundwaters basins with massive utilization of groundwater pumping. However, the knowledge of the comprehensive hydrogeological system in this groundwater basin is limited, so this research aims to determine a comprehensive hydrogeological conceptual model of the Randublatung groundwater basin. The methodology was conducted by collecting secondary and primary data of deep and shallow wells to evaluate boundaries of pattern and direction of groundwater flow and develop the aquifer system’s geometry. The result shows that the groundwater flow boundaries are Grogol River in the west, Wado River in the East, Bengawan Solo river in the South as a river boundary, and Rembang Mountains in the North as a constant head boundary. Therefore, groundwater flows from the hills area to the Bengawan Solo River and the north as the river’s flow. Based on the log bor evaluation, the aquifer system of the study area consist of an unconfined aquifer with a maximum thickness of 20 m and three layers of confined aquifers with thickness vary between 8 to 60 m. the hydraulic conductivity of the aquifers depends on the aquifer’s lithology range from sand, gravel, limestone, and sandstone. This hydrogeological conceptual model provides essential information for numerical groundwater models in the middle of the Randublatung groundwater basin.
APA, Harvard, Vancouver, ISO, and other styles
5

Qu, W., and W. Zijl. "Interfacing groundwater head and groundwater flow calculations." Environmental Software 5, no. 2 (June 1990): 77–81. http://dx.doi.org/10.1016/0266-9838(90)90004-p.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Nyakundi, Nyambane Zachary, Mathew Kinyanjui, and Johana K Sigey. "Fluctuating Groundwater Flow in Homogeneous Finite Porous Domain." SIJ Transactions on Computer Science Engineering & its Applications (CSEA) 04, no. 02 (April 21, 2016): 01–09. http://dx.doi.org/10.9756/sijcsea/v4i2/04030070101.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Hernández-Antonio, A., J. Mahlknecht, C. Tamez-Meléndez, J. Ramos-Leal, A. Ramírez-Orozco, R. Parra, N. Ornelas-Soto, and C. J. Eastoe. "Groundwater flow processes and mixing in active volcanic systems: the case of Guadalajara (Mexico)." Hydrology and Earth System Sciences 19, no. 9 (September 24, 2015): 3937–50. http://dx.doi.org/10.5194/hess-19-3937-2015.

Full text
Abstract:
Abstract. Groundwater chemistry and isotopic data from 40 production wells in the Atemajac and Toluquilla valleys, located in and around the Guadalajara metropolitan area, were determined to develop a conceptual model of groundwater flow processes and mixing. Stable water isotopes (δ2H, δ18O) were used to trace hydrological processes and tritium (3H) to evaluate the relative contribution of modern water in samples. Multivariate analysis including cluster analysis and principal component analysis were used to elucidate distribution patterns of constituents and factors controlling groundwater chemistry. Based on this analysis, groundwater was classified into four groups: cold groundwater, hydrothermal groundwater, polluted groundwater and mixed groundwater. Cold groundwater is characterized by low temperature, salinity, and Cl and Na concentrations and is predominantly of Na-HCO3-type. It originates as recharge at "La Primavera" caldera and is found predominantly in wells in the upper Atemajac Valley. Hydrothermal groundwater is characterized by high salinity, temperature, Cl, Na and HCO3, and the presence of minor elements such as Li, Mn and F. It is a mixed-HCO3 type found in wells from Toluquilla Valley and represents regional flow circulation through basaltic and andesitic rocks. Polluted groundwater is characterized by elevated nitrate and sulfate concentrations and is usually derived from urban water cycling and subordinately from agricultural return flow. Mixed groundwaters between cold and hydrothermal components are predominantly found in the lower Atemajac Valley. Twenty-seven groundwater samples contain at least a small fraction of modern water. The application of a multivariate mixing model allowed the mixing proportions of hydrothermal fluids, polluted waters and cold groundwater in sampled water to be evaluated. This study will help local water authorities to identify and dimension groundwater contamination, and act accordingly. It may be broadly applicable to other active volcanic systems on Earth.
APA, Harvard, Vancouver, ISO, and other styles
8

Hernández-Antonio, A., J. Mahlknecht, C. Tamez-Meléndez, J. Ramos-Leal, A. Ramírez-Orozco, R. Parra, N. Ornelas-Soto, and C. J. Eastoe. "Groundwater flow processes and mixing in active volcanic systems: the case of Guadalajara (Mexico)." Hydrology and Earth System Sciences Discussions 12, no. 2 (February 3, 2015): 1599–631. http://dx.doi.org/10.5194/hessd-12-1599-2015.

Full text
Abstract:
Abstract. Groundwater chemistry and isotopic data from 40 production wells in the Atemajac and Toluquilla Valleys, located in and around the Guadalajara metropolitan area, were determined to develop a conceptual model of groundwater flow processes and mixing. Multivariate analysis including cluster analysis and principal component analysis were used to elucidate distribution patterns of constituents and factors controlling groundwater chemistry. Based on this analysis, groundwater was classified into four groups: cold groundwater, hydrothermal water, polluted groundwater and mixed groundwater. Cold groundwater is characterized by low temperature, salinity, and Cl and Na concentrations and is predominantly of Na-HCO3 type. It originates as recharge at Primavera caldera and is found predominantly in wells in the upper Atemajac Valley. Hydrothermal water is characterized by high salinity, temperature, Cl, Na, HCO3, and the presence of minor elements such as Li, Mn and F. It is a mixed HCO3 type found in wells from Toluquilla Valley and represents regional flow circulation through basaltic and andesitic rocks. Polluted groundwater is characterized by elevated nitrate and sulfate concentrations and is usually derived from urban water cycling and subordinately from agricultural practices. Mixed groundwaters between cold and hydrothermal components are predominantly found in the lower Atemajac Valley. Tritium method elucidated that practically all of the sampled groundwater contains at least a small fraction of modern water. The multivariate mixing model M3 indicates that the proportion of hydrothermal fluids in sampled well water is between 13 (local groundwater) and 87% (hydrothermal water), and the proportion of polluted water in wells ranges from 0 to 63%. This study may help local water authorities to identify and quantify groundwater contamination and act accordingly.
APA, Harvard, Vancouver, ISO, and other styles
9

Craig, D., and L. M. Johnston. "Acid Precipitation and Groundwater Chemistry at the Turkey Lakes Watershed." Canadian Journal of Fisheries and Aquatic Sciences 45, S1 (December 19, 1988): s59—s65. http://dx.doi.org/10.1139/f88-267.

Full text
Abstract:
To determine correctly the response of a basin to various acid loading events, the groundwater hydrology must be considered as a function of the basin stratigraphy and mineralogy. Groundwaters in the Turkey Lakes Watershed are well buffered and in general provide a reservoir of alkalinity for surface waters in the basin. The groundwater chemistry is dominated by the weathering of carbonates present in the tills. Groundwater can follow a variety of pathways through the subsurface. These pathways can have very different flow rates and groundwater chemistry. As a result of this the influence of groundwater on surface water is highly site specific.
APA, Harvard, Vancouver, ISO, and other styles
10

Stewart, Michael Kilgour, and Philippa Lauren Aitchison-Earl. "Irrigation return flow causing a nitrate hotspot and denitrification imprints in groundwater at Tinwald, New Zealand." Hydrology and Earth System Sciences 24, no. 7 (July 16, 2020): 3583–601. http://dx.doi.org/10.5194/hess-24-3583-2020.

Full text
Abstract:
Abstract. Nitrate concentrations in groundwater have been historically high (N≥11.3 mg L−1) in an area surrounding Tinwald, Ashburton, since at least the mid-1980s. The local community is interested in methods to remediate the high nitrate in groundwater. To do this, they need to know where the nitrate is coming from. Tinwald groundwater exhibits two features stemming from irrigation with local groundwater (i.e. irrigation return flow). The first feature is increased concentrations of nitrate (and other chemicals and stable isotopes) in a “hotspot” around Tinwald. The chemical concentrations of the groundwater are increased by recirculation of water already relatively high in chemicals. The irrigation return flow coefficient C (irrigation return flow divided by irrigation flow) is found to be consistent with the chemical enrichments. The stable isotopes of the groundwater show a similar pattern of enrichment by irrigation return flow of up to 40 % and are also enriched by evaporation (causing a loss of about 5 % of the original water mass). Management implications are that irrigation return flow needs to be taken into account in modelling of nitrate transport through soil–groundwater systems and in avoiding overuse of nitrate fertiliser leading to greater leaching of nitrate to the groundwater and unnecessary economic cost. The second feature is the presence of “denitrification imprints” (shown by enrichment of the δ15N and δ18ONO3 values of nitrate) in even relatively oxic groundwaters. The denitrification imprints can be clearly seen because (apart from denitrification) the nitrate has a blended isotopic composition due to irrigation return flow and N being retained in the soil–plant system as organic N. The nitrate concentration and isotopic compositions of nitrate are found to be correlated with the dissolved oxygen (DO) concentration. This denitrification imprint is attributed to localised denitrification in fine pores or small-scale physical heterogeneity where conditions are reducing. The implication is that denitrification could be occurring where it is not expected because groundwater DO concentrations are not low.
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "Groundwater flow"

1

Uliana, Matthew Martin. "Delineation of regional groundwater flow paths and their relation to structural features in the Salt and Toyah basins, Trans-Pecos Texas /." Digital version accessible at:, 2000. http://wwwlib.umi.com/cr/utexas/main.

Full text
Abstract:
Thesis (Ph. D.)--University of Texas at Austin, 2000.
Vita. Two folded maps in pocket. Includes bibliographical references (leaves 207-213). Available also in a digital version from Dissertation Abstracts.
APA, Harvard, Vancouver, ISO, and other styles
2

Marklund, Lars. "Topographic Control of Groundwater Flow." Doctoral thesis, KTH, Mark- och vattenteknik, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-11153.

Full text
Abstract:
Gravity is the main driving force for groundwater flow, and both landscape topography and geology distribute the effects of gravity on groundwater flow.  The groundwater table defines the distribution of the potential energy of the water. In humid regions where the bedrock permeability is relatively low and the soil depth is sufficiently shallow, the groundwater table closely follows the landscape topography and, thus, the topography controls the groundwater circulation in these regions. In this thesis, I investigate multi-scale topography-controlled groundwater flow, with the goal of systematizing the spatial distribution of groundwater flow and assessing geological parameters of importance for groundwater circulation.  Both exact solutions and numerical models are utilized for analyzing topography-controlled groundwater flow. The more complex numerical models are used to explore the importance of various simplifications of the exact solutions. The exact solutions are based on spectral representation of the topography and superpositioning of unit solutions to the groundwater flow field. This approach is an efficient way to analyze multi-scaled topography-controlled groundwater flow because the impact of individual topographic scales on the groundwater flow can be analyzed separately.  The results presented here indicate that topography is fractal and affects groundwater flow cells at wide range of spatial scales. We show that the fractal nature of the land surface produces fractal distributions of the subsurface flow patterns. This underlying similarity in hydrological processes also yields a single scale-independent distribution of subsurface water residence times which have been found in distributions of solute efflux from watersheds. Geological trends modify the topographic control of the groundwater circulation pattern and this thesis presents exact solutions explaining the impact of geological layering, depth-decaying and anisotropic hydraulic conductivity on the groundwater flow field. For instance, layers of Quaternary deposits and decaying permeability with depth both increase the importance of smaller topographic scales and creates groundwater flow fields where a larger portion of the water occupies smaller and shallower circulation cells, in comparison to homogeneous systems.
Gravitationen är den mest betydelsefulla drivkraften för grundvattenströmning. Topografin och geologin fördelar vattnets potentiella energi i landskapet. Grundvattenytans läge definierar vattnets potentiella energi, vilket är ett randvillkor för grundvattnets strömningsfält. I humida områden med en relativt tät berggrund och tillräckligt tunna jordlager, följer grundvattenytan landskapets topografi. Därav följer att grundvattenströmningen är styrd av topografin i dessa områden. I denna avhandling belyser jag den flerskaliga topografistyrda grundvattenströmningen. Min målsättning har varit att kvantitativt bestämma grundvattenströmningens rumsliga fördelning samt att undersöka hur olika geologiska parametrar påverkar grundvattencirkulationen. Jag har använt såväl numeriska modeller som analytiska lösningar, för att undersöka hur topografin styr grundvattenströmningen. De numeriska modellerna är mer komplexa än de analytiska lösningarna och kan därför användas för att undersöka betydelserna av olika förenklingar som finns i de analytiska lösningarna. De analytiska lösningarna är baserade på spektralanalys av topografin, samt superponering av enhetslösningar, där varje enhetslösning beskriver hur en specifik topografisk skala påverkar grundvattnets strömningsfält. Detta är ett effektivt tillvägagångssätt för att undersöka flerskaliga effekter av topografin, eftersom påverkan av varje enskild topografisk skala kan studeras separat. Resultaten som presenteras indikerar att topografin är fraktal och att den ger upphov till cirkulationsceller av varierande storlek som även dessa är av en fraktal natur. Denna grundläggande fördelning i grundvattnets strömningsfält ger upphov till att grundvattnets uppehållstid i marken följer ett självlikformigt mönster och kan förklara uppmätta tidsvariationer av lösta ämnens koncentrationer i vattendrag efter regn. Geologiska trender påverkar hur grundvattenströmningen styrs av topografin. De exakta lösningar som presenteras här, beskriver hur geologiska lager samt djupavtagande och anisotropisk hydraulisk konduktivitet påvekar grundvattnets strömning. Exempelvis är betydelsen av mindre topografiska skalor viktigare i områden med kvartära avlagringar och en berggrund med djupavtagande konduktivitet, än i områden med homogen bergrund utan kvartära avlagringar. Dessutom är en större andel strömmande vatten belägen närmare markytan i de förstnämnda områdena.
QC 20100802
APA, Harvard, Vancouver, ISO, and other styles
3

Poley, David Gordon 1966. "A groundwater monitoring program based upon a groundwater flow model." Thesis, The University of Arizona, 1993. http://hdl.handle.net/10150/278296.

Full text
Abstract:
This thesis concerns a groundwater modeling study south of Tucson, Arizona where 10,000 acre-feet of Central Arizona Project water may be annually recharged. South and west of the site are the Santa Cruz River and the Tohono O'odham Indian Nation. Well fields to the immediate east, west and south supply water to the City of Tucson and to farming and copper mining corporations. Operation of the corporate well fields has lead to a water table depression just west of the site. The purpose of the model is to understand of the most probable groundwater flow regime in light of aquifer recharging and groundwater mining. The model serves to compare groundwater conditions with previous investigations. Lack of data precluded the construction of a model capable of producing reliable predictive results. Hydrogeologic data gathered provide a foundation for future modeling studies. Insufficient data serve as indicators of present groundwater monitoring deficiencies.
APA, Harvard, Vancouver, ISO, and other styles
4

Hansen, Douglas Dale. "Analytic modeling of leakage in confined aquifer systems /." Diss., ON-CAMPUS Access For University of Minnesota, Twin Cities Click on "Connect to Digital Dissertations", 2002. http://www.lib.umn.edu/articles/proquest.phtml.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Radell, Mary Jo. "Three-dimensional groundwater flow model use and application Bishop Basin, Owens Valley, California /." Thesis, The University of Arizona, 1989. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_e9791_1989_192_sip1_w.pdf&type=application/pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Esposito, David M. "Criteria and methods of analysis for regulation for interference between wells." Thesis, The University of Arizona, 1985. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_e9791_1985_140_sip1_w.pdf&type=application/pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Doolen, Matthew Louis. "Sensitivity Analysis Methods and Results for Tucson Water's Central Wellfield Groundwater Flow Model, Tucson Basin, Southeastern Arizona." Thesis, The University of Arizona, 1994. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_etd_hy0087_sip1_w.pdf&type=application/pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Jacobson, Elizabeth A. "A statistical parameter estimation method using singular value decomposition with application to Avra Valley aquifer in southern Arizona." Diss., The University of Arizona, 1985. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_e9791_1985_230_sip1_w.pdf&type=application/pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Colarullo, Susan J. "Identification of an optimal ground water management strategy in a contaminated aquifer." Thesis, The University of Arizona, 1988. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_e9791_1988_602_sip1_w.pdf&type=application/pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Lang, Patrick Timothy. "Simulation of groundwater flow to assess the effects of groundwater pumping and canal lining in the Mesilla Basin of Dona Ana County, New Mexico and El Paso County, Texas." Thesis, The University of Arizona, 1994. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_etd_hy0225_sip1_w.pdf&type=application/pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Books on the topic "Groundwater flow"

1

Marek, Nawalany, ed. Natural groundwater flow. Boca Raton: Lewis Publishers, 1993.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
2

Everett, Lauren, ed. Groundwater Recharge and Flow. Washington, D.C.: National Academies Press, 2019. http://dx.doi.org/10.17226/25615.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Milan, Vuković. Groundwater dynamics: Steady flow. Littleton, Colo: Water Resources Publications, 1997.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
4

K, Sato, Iwasa Yoshiaki 1928-, and International Symposium on Groundwater (2000 : Saitama, Japan), eds. Groundwater hydraulics. Tokyo: Springer, 2003.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
5

Bear, Jacob, and Arnold Verruijt. Modeling Groundwater Flow and Pollution. Dordrecht: Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3379-8.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Custodio, E., A. Gurgui, and J. P. Lobo Ferreira, eds. Groundwater Flow and Quality Modelling. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2889-3.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Bonn, Bernadine. Dream: Analytical groundwater flow programs. Chelsea, Mich: Lewis Publishers, 1990.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
8

Dudgeon, C. R. Non-Darcy flow of groundwater. Manly Vale, N.S.W: University of New South Wales, Water Research Laboratory, 1985.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
9

NATO, Advanced Research Workshop on Advances in Analytical and Numerical Groundwater Flow and Quality Modelling (1987 Lisbon Portugal). Groundwater flow and quality modelling. Dordrecht, Holland: D. Reidel Pub. Co., 1988.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
10

Rajan, M. T. Regional groundwater modeling. New Delhi: Capital Pub. Co., 2004.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Book chapters on the topic "Groundwater flow"

1

Fowler, Andrew. "Groundwater Flow." In Interdisciplinary Applied Mathematics, 387–461. London: Springer London, 2011. http://dx.doi.org/10.1007/978-0-85729-721-1_7.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Verruijt, Arnold. "Groundwater Flow." In An Introduction to Soil Mechanics, 67–76. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-61185-3_8.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Sun, Feng, Norihiro Watanabe, and Jens-Olaf Delfs. "Groundwater Flow." In Thermo-Hydro-Mechanical-Chemical Processes in Porous Media, 107–23. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-27177-9_5.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Powrie, William. "Groundwater flow." In ICE Manual of Geotechnical Engineering, Second edition, Volume I, 187–94. Leeds: Emerald Publishing Limited, 2023. http://dx.doi.org/10.1680/icemge.66816.0187.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Misra, Debasmita, Ronald P. Daanen, and Anita M. Thompson. "Base Flow/Groundwater Flow." In Encyclopedia of Earth Sciences Series, 90–93. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_36.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Sethi, Rajandrea, and Antonio Di Molfetta. "The Groundwater Flow Equation." In Groundwater Engineering, 27–32. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-20516-4_2.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Lennon, G. P. "Unconfined Groundwater Flow." In Applications in Geomechanics, 155–72. Berlin, Heidelberg: Springer Berlin Heidelberg, 1987. http://dx.doi.org/10.1007/978-3-642-83012-9_8.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Dassargues, Alain. "Saturated groundwater flow." In Hydrogeology, 59–106. First Edition. | Boca Raton, Florida : Taylor & Francis, A CRC title, part of the Taylor & Francis imprint, a member of the Taylor & Francis Group, the academic division of T&F Informa plc, [2019]: CRC Press, 2018. http://dx.doi.org/10.1201/9780429470660-4.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Mathias, Simon A. "Transient Groundwater Flow." In Hydraulics, Hydrology and Environmental Engineering, 333–50. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-41973-7_15.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Bear, Jacob, and Arnold Verruijt. "Groundwater Motion." In Modeling Groundwater Flow and Pollution, 27–52. Dordrecht: Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3379-8_2.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "Groundwater flow"

1

Mls, J. "Modelling the tide effects in groundwater." In MULTIPHASE FLOW 2009. Southampton, UK: WIT Press, 2009. http://dx.doi.org/10.2495/mpf090331.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Polák, M., and J. Mls. "Transient groundwater flow in a single fracture." In MULTIPHASE FLOW 2007. Southampton, UK: WIT Press, 2007. http://dx.doi.org/10.2495/mpf070121.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Mls, J. "Modelling groundwater flow and pollutant transport in hard-rock fractures." In MULTIPHASE FLOW 2007. Southampton, UK: WIT Press, 2007. http://dx.doi.org/10.2495/mpf070111.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Marques, Jose Couto, Jose Rodrigues, and Maria Teresa Restivo. "Augmented reality in groundwater flow." In 2014 11th International Conference on Remote Engineering and Virtual Instrumentation (REV). IEEE, 2014. http://dx.doi.org/10.1109/rev.2014.6784201.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Burck, P., P. Barroll, A. core, and D. Rappuhn. "Taos regional groundwater flow model." In 55th Annual Fall Field Conference. New Mexico Geological Society, 2004. http://dx.doi.org/10.56577/ffc-55.433.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Hortert, Christopher E., and Daniel Bain. "CONTAMINATED GROUNDWATER FLOW CONTROL ACROSS AN INVERTED GROUNDWATER DIVIDE WITH THREE GROUNDWATER CONTROL SYSTEMS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-278648.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Marques, Jose Couto, Maria Teresa Restivo, Tiago Santos, and Alberto Cardoso. "An interactive video for groundwater flow." In 2013 International Conference on Interactive Collaborative Learning (ICL). IEEE, 2013. http://dx.doi.org/10.1109/icl.2013.6644712.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Woroniuk, Blake, Keegan Jellicoe, Jennifer McIntosh, and Grant Ferguson. "GROUNDWATER FLOW ACROSS THE INTERMEDIATE ZONE." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357681.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Özgen-Xian, Ilhan, and Adrián Navas-Montilla. "A hyperbolic Boussinesq groundwater flow model." In Proceedings of the 39th IAHR World Congress From Snow to Sea. Spain: International Association for Hydro-Environment Engineering and Research (IAHR), 2022. http://dx.doi.org/10.3850/iahr-39wc252171192022296.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Green, Jeffrey A., Jeremy A. Pavlish, Jeanette H. Leete, and E. Calvin Alexander, Jr. "Quarrying Impacts on Groundwater Flow Paths." In Ninth Multidisciplinary Conference on Sinkholes and the Engineering and Environmental Impacts of Karst. Reston, VA: American Society of Civil Engineers, 2003. http://dx.doi.org/10.1061/40698(2003)19.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Reports on the topic "Groundwater flow"

1

Benoit, N., and D. Paradis. Groundwater flow model. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/298890.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Hinton, M. J., and S. Alpay. Constraining groundwater flow in Champlain Sea muds. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2020. http://dx.doi.org/10.4095/321106.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Garven, G., and L. W. Vigrass. Modelling of deep groundwater flow in Saskatchewan. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/293499.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Klammler, Harald. Introduction to the Mechanics of Flow and Transport for Groundwater Scientists. The Groundwater Project, 2023. http://dx.doi.org/10.21083/gxat7083.

Full text
Abstract:
Starting from Newton’s laws of motion and viscosity, this book is an introduction to fundamental aspects of fluid dynamics that are most relevant to groundwater scientists. Based on a perspective of driving versus resisting forces that govern the motion of a fluid, the author derives Darcy’s law for flow through porous media by drawing an analogy to Bernoulli’s law for fluid with negligible viscosity. By combining the effects of gravity and pressure, the author identifies hydraulic head as a convenient numerical quantity to represent the force driving groundwater flow. In contrast to the physical derivation of hydraulic head, hydraulic conductivity emerges as a parameter related to the resisting frictional forces between the mobile fluid and the stationary porous medium. These frictional seepage forces also affect the effective stress state of the porous medium, thus establishing a link to soil stability and quicksand formation. Combining Darcy’s law with the law of mass conservation leads the reader to the fundamental equations of saturated groundwater flow. Finally, the effects of capillary forces are included to establish the governing equations for unsaturated and multi-phase flow. Throughout the book, the author focuses on thoroughly illustrating and deriving the equations while applying order of magnitude analyses. This approach makes it possible to extract the most information, for example in terms of the scale of response time, without requiring explicit solutions. A number of boxes and solved exercises contain further details and links to practical applications such as the water table ratio that reflects ‘fullness’ of an aquifer and the performance of slug tests for in situ measurement of hydraulic conductivity. This book makes an important contribution to groundwater science by providing a progressive introductory explanation of the physical mechanics of groundwater flow and the accompanying socioeconomic and ecological problems that may arise.
APA, Harvard, Vancouver, ISO, and other styles
5

Moran, J. E., and G. B. Hudson. Using groundwater age and other isotopic signatures to delineate groundwater flow and stratification. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/221890.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Brown, S. R., and R. W. Haupt. Study of electrokinetic effects to quantify groundwater flow. Office of Scientific and Technical Information (OSTI), April 1997. http://dx.doi.org/10.2172/471404.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Kröhn, Klaus-Peter. Groundwater flow under permafrost conditions and talik formation. International Permafrost Association (IPA), June 2024. http://dx.doi.org/10.52381/icop2024.228.1.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Ballard, S., G. T. Barker, and R. L. Nichols. The in situ permeable flow sensor: A device for measuring groundwater flow velocity. Office of Scientific and Technical Information (OSTI), March 1994. http://dx.doi.org/10.2172/10147883.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Berglund, J., A. Bobst, and A. Gebril. A groundwater flow model for the East Flathead Valley, Flathead County, Montana. Montana Bureau of Mines and Geology, July 2024. http://dx.doi.org/10.59691/cmxe7182.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Dohman, J. M., and A. E. H. Hanson. Groundwater inputs to rivers and streams: Using temperature and visual cues on the Big Hole River, southwestern Montana. Montana Bureau of Mines and Geology, April 2024. http://dx.doi.org/10.59691/bmyu6609.

Full text
Abstract:
This publication discusses the factors that influence stream temperature and flow, with a focus on groundwater discharge during summer low flow periods. It includes what indicators are being used on the Big Hole River to identify groundwater discharge zones and how groundwater affects temperature and water quality of streams.
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'Groundwater flow' for particular source types:
Journal articles Dissertations / Theses Books
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography