Готові списки джерел за темами / Hydrogeology

Добірка наукової літератури з теми "Hydrogeology"

Автор: Grafiati
Опубліковано: 4 червня 2021
Оновлено: 30 липня 2024

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Статті в журналах з теми "Hydrogeology"

1

Ren, Jian Min, Yang Yang, and Xing Wei Hu. "Application of GIS and FEFLOW in Forecasting Groundwater Flow Field of Minqin Basin." Advanced Materials Research 368-373 (October 2011): 2128–31. http://dx.doi.org/10.4028/www.scientific.net/amr.368-373.2128.

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Conditions were considered of complex geology and the hydrogeology of Minqin, the 3d numerical simulation model of groundwater system was built by FEFLOW software in the study area. Author found that hydrogeologic parameters which have been debugged many times corresponded with the hydrogeology prospecting results well. Verification results show that the model has better simulation effect and higher reliability in checking the model. Facts show that prediction of groundwater flow field has high reliability in the study area.
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2

Nelson, Gordon L. "Hydrogeology." Wetlands 25, no. 3 (September 2005): 788. http://dx.doi.org/10.1672/0277-5212(2005)025[0788:r]2.0.co;2.

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3

Caruso, Phil, Carlos Ochoa, W. Jarvis, and Tim Deboodt. "A Hydrogeologic Framework for Understanding Local Groundwater Flow Dynamics in the Southeast Deschutes Basin, Oregon, USA." Geosciences 9, no. 2 (January 24, 2019): 57. http://dx.doi.org/10.3390/geosciences9020057.

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Understanding local hydrogeology is important for the management of groundwater resources and the ecosystems that depend on them. The main objective of this study conducted in central Oregon, USA was to characterize the hydrogeologic framework of a part of the semiarid Upper Deschutes Basin. Information on local geology and hydrology was synthesized to construct a hydrogeologic framework and a conceptual model of groundwater movement in shallow and previously unmapped deeper aquifers. Study results show that local geology drives many of the surface water and groundwater connections that sustain groundwater-related ecosystems and ranching-related activities in the geographical area of interest. Also, the findings of this study suggest that ecohydrological investigations can be used to mitigate concerns regarding groundwater development. Likewise, newly-developed conceptual models of the hydrogeology of previously unstudied areas within a groundwater basin undergoing regulation offer opportunities to not only address concerns regarding integrated surface water–groundwater interactions but also provide supplemental sources of water for nearby areas undergoing groundwater depletion through proposed bulk water transfers.
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4

Li, Sheng, Xue Hai Fu, and Yan Yan Ge. "Evaluation Research on the Hydrogeology Conditions of Coal Bed Methane Row Production." Applied Mechanics and Materials 295-298 (February 2013): 3200–3204. http://dx.doi.org/10.4028/www.scientific.net/amm.295-298.3200.

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This paper confirms that the mining of the coal bed methane (CBM) are most significantly influenced by the hydrogeology parameters of the reservoir itself, the hydrogeology parameters, the supply properties and the geological structure of the roof and floor and other neighboring water-bearing rocks hydraulically associated with the coal bed as well as the difficulty degree of CBM mining; a evaluation indicator system structure of the hydrogeology conditions are established based on the foresaid conclusions and the CBM mining hydrogeology conditions are divided into “beneficial, moderate and adverse” grades; this paper finally divides the threshold to grade the hydrogeology condition evaluation indicators and a complete CBM mining hydrogeology conditions evaluation indicator system is founded to evaluate the hydrogeology conditions.
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5

HAYASHI, Masaki. "Alpine hydrogeology." Journal of Groundwater Hydrology 62, no. 1 (February 28, 2020): 43–58. http://dx.doi.org/10.5917/jagh.62.43.

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6

Ingebritsen, S. E., and Michael Manga. "Earthquake Hydrogeology." Water Resources Research 55, no. 7 (July 2019): 5212–16. http://dx.doi.org/10.1029/2019wr025341.

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7

Sukop, Michael C. "Coastal Hydrogeology." Groundwater 58, no. 3 (January 14, 2020): 414–15. http://dx.doi.org/10.1111/gwat.12980.

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8

Naymik, Thomas G. "Contaminant Hydrogeology." Geochimica et Cosmochimica Acta 57, no. 15 (August 1993): 3820. http://dx.doi.org/10.1016/0016-7037(93)90162-p.

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9

Baker, Victor R., James M. Dohm, Alberto G. Fair�n, Ty P. A. Ferr�, Justin C. Ferris, Hideaki Miyamoto, and Dirk Schulze-Makuch. "Extraterrestrial hydrogeology." Hydrogeology Journal 13, no. 1 (February 26, 2005): 51–68. http://dx.doi.org/10.1007/s10040-004-0433-2.

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10

Schwille, F. "Hydrogeology. An introduction to general and applied hydrogeology." Earth-Science Reviews 31, no. 3-4 (October 1991): 289. http://dx.doi.org/10.1016/0012-8252(91)90030-j.

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Дисертації з теми "Hydrogeology"

1

Barker, John A. "Diffusion in hydrogeology." Universitätsbibliothek Leipzig, 2016. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-193862.

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The field of hydrogeology is primarily concerned with the flow of water below the ground surface and with transport, normally of solutes and heat, within that water. Many disciplines have contributed to this endeavor which requires skills from across the spectrum of science, engineering and beyond. The diffusion equation describes not only solute transport but also the flow of water, via Darcy’s law. Of particular interest is transport in fractured rock where most of the flow is through the fractures while most of the storage is in the rock pores: a ‘double-porosity’ system. Hydrogeology remains a field that welcomes those who bring techniques from other areas of science to address problems as varied as water supply, radioactive waste disposal and geothermal energy.
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2

Barker, John A. "Diffusion in hydrogeology." Diffusion fundamentals 6 (2007) 50, S. 1-18, 2007. https://ul.qucosa.de/id/qucosa%3A14229.

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The field of hydrogeology is primarily concerned with the flow of water below the ground surface and with transport, normally of solutes and heat, within that water. Many disciplines have contributed to this endeavor which requires skills from across the spectrum of science, engineering and beyond. The diffusion equation describes not only solute transport but also the flow of water, via Darcy’s law. Of particular interest is transport in fractured rock where most of the flow is through the fractures while most of the storage is in the rock pores: a ‘double-porosity’ system. Hydrogeology remains a field that welcomes those who bring techniques from other areas of science to address problems as varied as water supply, radioactive waste disposal and geothermal energy.
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3

Cooksey, Kirsty. "Hydrogeology of the Mackenzie Basin." Thesis, University of Canterbury. Geological Sciences, 2008. http://hdl.handle.net/10092/1983.

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The intermontane Mackenzie Basin is located within the central South Island of New Zealand. The glacial basin contains three glacial lakes which are used for hydroelectric power generation via a canal system that links the lakes. The basin is an area of climate extremes, low rainfall, high summer temperatures, and snowy winters. The area is predominantly used for pastoral farming, however farming practices are changing and, combined with an increasing population, there is a need to define the groundwater resources to enable sustainable resource management. Little is currently known about the hydrogeological system within the Mackenzie Basin, and what is known is from investigations carried out during the construction of the canal system from 1935 to 1985. There are four glacial formations that overlie Tertiary sequences and Torlesse bedrock. However, due to the glacial processes that have been ongoing over at least the last 300 ka, determining the occurrence and extent of groundwater within the outwash gravels is difficult. It is suggested that the permeability of the formations decreases with depth, therefore horizontal and vertical hydraulic conductivity decrease with depth. A shallow groundwater table is present within the Post Glacial Alluvial Gravels which is recharged directly from fast flowing streams and rivers as well as rainfall. It appears that this shallow system moves rapidly through the system and it is unlikely that the water infiltrates downwards to recharge the deeper groundwater system. It is thought that a deep groundwater system flows preferentially through the Mt John Outwash Gravels, being the second youngest glacial formation. Water chemistry and age dating tracer analysis indicate that the deeper groundwater is over 80 years old and that the groundwater system is recharging slowly. The shallow groundwater in the Post Glacial Alluvial Gravels and within the major fans to the east of the basin is 10 to 20 years in age. Baseline data such as water chemistry, groundwater levels, and surface water gaugings have been collected which can be used for future investigations. More data needs to be collected to create a long term record to further define the hydrogeological system and to determine the best way to manage the resource for long term sustainable use in the future.
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4

Vincent, Craig Nicholas. "Hydrogeology of the Upper Selwyn Catchment." Thesis, University of Canterbury. Geological Sciences, 2005. http://hdl.handle.net/10092/1137.

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Farming practices within the upper Selwyn plains have significantly expanded, and are becoming more dependent on groundwater as a reliable source of irrigation. This expansion has resulted in the rapid development of the groundwater resource and water levels in many wells have reached record low levels. Groundwater resources can be found within at least three aquifers within the glacial gravel deposits of the upper Selwyn plains. Aquifer 1 occurs between approximately 0-30 m, aquifer 2 between 40-85 m and aquifer 3 greater than 100 m below the surface. Aquifers 1 and 2 occur within close proximity to the Selwyn River and its tributaries. Aquifer 1 is unconfined, aquifer 2 semi-confined and aquifer 3 semi-confined to confined. Significant leakage of groundwater occurs between the different aquifers. Recharge sources to the aquifers include rainfall infiltration and river seepage. Water levels and groundwater chemistry suggest that the Selwyn River provides the dominant source of recharge to aquifers 1 and 2 in areas immediately surrounding the river and to the south of the current course of the river between Greendale and Dunsandel.
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5

Loris, Phoebe. "Hydrogeology of the Waipara alluvial basin." Thesis, University of Canterbury. Geology, 2000. http://hdl.handle.net/10092/7655.

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The Waipara alluvial basin, located 50 kilometres north of Christchurch on the South Island of New Zealand is experiencing rapid transformation in land use from pastoral farming to horticulture. In the last five years the use of the groundwater resources has increased significantly. Knowledge is lacking about the availability and sustainability of the groundwater resources. Groundwater resources can be found throughout the basin in the Quaternary Canterbury and Teviotdale Gravels, and the late Pliocene/Early Pleistocene Kowai Formation. The hydrogeological system can be described as a complex network of discrete, lithologically and hydraulically heterogeneous and aniosotropic semipermeable to permeable channels. The physical and hydraulic nature of the aquifers (or water-bearing units) makes identification and characterisation of the resources difficult. However, the resources can be distinguished in terms of the observed hydrogeologic properties (i.e. lithology, yield, transmissivity, and chemistry). Chemical and isotope sampling indicate that recharge to the basin aquifers is occurring through the uplifted and fractured Tertiary sequences formed along the eastern and western margins of the basin, and through infiltration of local rainfall in the unconfined and semi-confined portions of the aquifer. Groundwater residence times are long (20- 40+ years). Long residence times, slow recharge, and low hydraulic conductivity suggests that if the groundwater resources are not properly monitored and managed, there is great potential for 'mining' the resource(s), or in other words for depleting the resource faster than it can be recharged. Long term monitoring and management strategies have been recommended for future work to help gain more knowledge and understanding of the Waipara hydrogeological system, and ensure sustain ability for future development.
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6

Carpenter, Stan H. "Hydrogeology of northern Daviess County, Indiana." Virtual Press, 1992. http://liblink.bsu.edu/uhtbin/catkey/865949.

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In 1988, ninety ground-water samples were collected in northern Daviess County, Indiana. Sampled wells were completed in the Pennsylvanian Age Racoon Creek Group and underlying Mississippian units. Twenty-one inorganic parameters were targeted for laboratory analysis.The computer program DATAGEN4 was utilized to generate saturation indices for target mineral species. Thirteen, thirty-six, twenty-four, eighty-six, and thirteen samples were saturated with barite, calcite, dolomite, hematite, and siderite, respectively. All samples were undersaturated with respect to gypsum and fluorite.Trilinear diagrams were plotted, and the prevalent chemical characters of the samples were determined. Generally, samples collected from depths of less than 225 feet were characterized as Ca-HCO3 waters. Deeper wells yielded Na-HCO3 and Na-HCO3-Cl type waters.The naturally-occurring chemical processes that result in the water types (decomposition of organic material, carbonate dissolution, and cation exchange) are described. The influence of coal units and upwelling brines on ground-water chemistry is also discussed.
Department of Geology
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7

Stanger, Gordon. "The hydrogeology of the Oman Mountains." Thesis, Open University, 1986. http://oro.open.ac.uk/57011/.

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Northern Oman is an arid area almost entirely dependent upon groundwater recharged by highly sporadic rainfall. Precipitation estimates are hampered by a lack of any reliable altitude-rainfall relationship. Below 700 m there is no statistically significant relationship. The isotopic composition of groundwater is strongly influenced by the rainfall amount (related to storm frequency), and not just by altitude/temperature. Storm events with long return periods are of disproportionate importance to recharge. Despite the huge volume of carbonate formations, holokarstic development is generally immature, and groundwater storage is greatest in alluvial piedmont surrounding main limestone massifs. Isotopes, chemistry and hydrologic measurements show that post-storm evaporative losses are very large. The origin of limestone springs and their chemical and physical anomalies are described. Structure rather than petrology controls groundwater flow in the limestones, hence regional differences in structural style produce contrasting hydrologic regimes between the various massifs. The Semail nappe mantle sequence is the only other hard-rock formation of groundwater significance. Though much less productive than the carbonates, these ultramafics display extraordinary chemical activity, yielding bicarbonate waters from the weathered zone, whilst more deeply circulating groundwaters produce hyperalkaline springs by low-temperature serpentinisation. Associated processes include solute reduction, hydrogen evolution, hydroxide and carbonate precipitation, hydroxide-basic rock reaction, salt enrichment and water-rock isotopic exchange. Throughout the interior catchments, groundwater mostly flows into narrow buried alluvial channels which are often constricted at hard-rock nodal points, thus facilitating very efficient interception and recovery by the "falaj" system. Traditional agriculture has evolved to cope with fluctuating groundwater supply but is sensitive to increased abstraction. On the Batinah plain, greatly increased coastal abstraction has locally induced moderate to severe salinisation. Existing process studies are insufficiently quantified to provide the resolution necessary to manage groundwater resources, especially in high-risk coastal areas.
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8

Smart, Michael Charles. "Hydrogeology of the Queenstown 1:500 000 map region (Sheet 3126)." Thesis, Rhodes University, 1999. http://hdl.handle.net/10962/d1005583.

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The Groundwater characteristics of a portion of the Eastern Cape are depicted on a General Hydrogeological Map (Queenstown 3126) at 1 :500 000 scale. The purpose of the map and accompanying text is to provide a synoptic overview of the hydrogeology of the area. The "fractured and intergranular" aquifer type predominates in the more humid eastern part of the study area where the lithologies are more highly weathered whereas the fractured type predominates in the drier west. For the bulk of the area borehole yields are in the 0.5 - 2.0 ℓ/sec range. Higher yields (in the 2.0 - 5.0 ℓ/sec range) are common only in a small area in the south-west of the map. Lowest yields (0.1 - 0.5 ℓ/sec) are obtained in an area immediately north of East London and in the Dwyka Group near the NE coast. It is important to note that these yield ranges are merely a measure of the central tendency, and that higher yields - in excess of 3 ℓ/sec - could well be obtainable at optimal hydrogeological target features within these areas. Highest borehole yields are obtained in folded areas (restricted to the southern edge of the study area) followed by rocks with dolerite intrusions (common over the bulk of the study area). Other targets include fractured sedimentary and volcanic rock and unconsolidated deposits. Yields obtained from dolerite contact zones vary across the area; differences correspond to spatial variations in the style of intrusion. Highest success rates are obtained in areas intruded by a combination of dykes, ring-shaped sheets and irregular sheets while poor results are obtained in areas intruded by thick massive sills. Air photo and satellite image interpretation, geological mapping, magnetic, electrical resistivity and electromagnetic geophysical methods can be used to locate drilling target features. Groundwater quality is good since electrical conductivities over much of the area are lower than 70 mS/m and rarely exceed the South African Water quality guideline limit for human consumption of 300 mS/m. The volume of groundwater abstractable ranges between approximately 2 000 m³/km²/annum and 80 000 m³/km²/annum and is limited by either volumes of recharge or subsurface storage.
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9

Davis, Stanley N., and Augusta G. Davis. "Hydrogeology in the United States 1780-1950." Department of Hydrology and Water Resources, University of Arizona (Tucson, AZ), 2005. http://hdl.handle.net/10150/615795.

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Most modern textbooks that deal with subsurface water, or hydrogeology, include a brief summary of the historical development of the science. In our book, we have expanded on this general theme without introducing the more technical aspects of the topic. We have, however, emphasized two important points that are commonly overlooked. First, most of the fundamental contributions made during the 1800's were not American but were primarily European. Second, 1885 was the date of the first ground -water publication of the United States Geological Survey, but it did not mark the birth of hydrogeology in the United States. Some American contributions were made about 80 years earlier. The authors are grateful for the assistance of many individuals. T. N. Narasimhan, M. P. Anderson, F. M. Phillips, D. B. Stephens, J. V. Brahana, C. W. Fetter, D. Deming, and D. I. Siegel were given the initial version of our book and provided numerous useful comments.
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10

Pool, Donald Robert 1955. "Hydrogeology of McMullen Valley, west-central Arizona." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/191959.

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The hydrogeology of McMullen Valley, west-central Arizona, was investigated using geologic, geophysical, and hydrologic data and a numerical model of the ground-water system. Geologic information and gravity modeling indicate that the main structure of McMullen Valley is a syncline. Basin fill that accumulated in the structural depression is the main aquifer and is divided into upper and lower units. A fine-grained facies in separates the aquifer into shallow and deep systems. A numerical model was used to analyze the ground-water system for both steady-state and transient conditions. The steady-state model aided in evaluating the distribution of hydraulic properties. The transient model was used to analyze system response to pumping stress. Water-level declines are controlled by the distribution of pumpage, specific-yield, and the fine-grained facies of lower basin fill. Significant water-level declines may extend to aquifer boundaries in most of the basin.
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Книги з теми "Hydrogeology"

1

Nonner, Johannes C. Introduction to hydrogeology. 2nd ed. Boca Raton, Fla: CRC Press, 2010.

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2

Back, William, Joseph S. Rosenshein, and Paul R. Seaber, eds. Hydrogeology. U.S.A: Geological Society of America, 1988. http://dx.doi.org/10.1130/dnag-gna-o2.

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3

Hölting, Bernward, and Wilhelm G. Coldewey. Hydrogeology. Berlin, Heidelberg: Springer Berlin Heidelberg, 2019. http://dx.doi.org/10.1007/978-3-662-56375-5.

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4

Dassargues, Alain. Hydrogeology. 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.

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5

1925-, Back William, Rosenshein Joseph S, Seaber Paul R, and Decade of North American Geology Project., eds. Hydrogeology. Boulder, Colo: Geological Society of America, 1988.

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6

Davis, Stanley N. Hydrogeology. Malabar, Fla: Krieger Pub. Co., 1991.

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7

Brassington, Rick. Field hydrogeology. Chichester, Eng: John Wiley & Sons, 1993.

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8

Brassington, Rick. Field Hydrogeology. Hoboken, New Jersey: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781118397404.

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9

1920-, LaMoreaux Philip E., ed. Environmental hydrogeology. 2nd ed. Boca Raton: Tayor & Francis, 2008.

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10

T, Bean Robert, and Association of Engineering Geologists. Meeting, eds. Hydrogeology Symposium. Lawrence, KS: Association of Engineering Geologists, 1985.

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Частини книг з теми "Hydrogeology"

1

Deb, Pradipta Kumar. "Hydrogeology." In SpringerBriefs in Water Science and Technology, 9–12. Cham: Springer International Publishing, 2013. http://dx.doi.org/10.1007/978-3-319-02988-7_2.

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2

Sachse, Agnes, Leslie Jakobs, and Olaf Kolditz. "Hydrogeology." In OpenGeoSys-Tutorial, 13–17. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13335-5_2.

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3

Shekhar, Shashi, and Hui Xiong. "Hydrogeology." In Encyclopedia of GIS, 461. Boston, MA: Springer US, 2008. http://dx.doi.org/10.1007/978-0-387-35973-1_573.

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4

Percopo, Carlo, and Maurizio Guerra. "Hydrogeology." In Encyclopedia of Earth Sciences Series, 1–4. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-12127-7_161-1.

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5

Naik, Prakash Chandra. "Hydrogeology." In SpringerBriefs in Water Science and Technology, 39–68. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-66511-5_4.

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6

Jones, Brian. "Hydrogeology." In Geology of the Cayman Islands, 265–89. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-08230-6_11.

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7

Purkait, B. "Hydrogeology." In The Brahmaputra Basin Water Resources, 113–38. Dordrecht: Springer Netherlands, 2004. http://dx.doi.org/10.1007/978-94-017-0540-0_7.

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8

Şen, Zekâi. "Hydrogeology." In Earth Systems Data Processing and Visualization Using MATLAB, 89–114. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01542-8_4.

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9

Percopo, Carlo, and Maurizio Guerra. "Hydrogeology." In Encyclopedia of Earth Sciences Series, 496–99. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-73568-9_161.

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10

Cartwright, Keros, and Bruce R. Hensel. "Hydrogeology." In Geotechnical Practice for Waste Disposal, 66–93. Boston, MA: Springer US, 1993. http://dx.doi.org/10.1007/978-1-4615-3070-1_4.

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Тези доповідей конференцій з теми "Hydrogeology"

1

Murdoch, Larry, Scott DeWolf, Leonid Germanovich, Soheil Roudini, and Robert Moak. "Recent Developments in Hydrogeologic Applications for Strain Tensor Analyses." In 31st Clemson Hydrogeology Symposium. US DOE, 2023. http://dx.doi.org/10.2172/2373046.

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2

Burkart, Michael. "HYDROGEOLOGY IN SUPPORT OF LITIGATION: INFLUENCING POLICY WITH HYDROGEOLOGY." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-312558.

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3

A. van Overmeeren, R. "Georadar for hydrogeology." In 55th EAEG Meeting. European Association of Geoscientists & Engineers, 1993. http://dx.doi.org/10.3997/2214-4609.201411534.

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4

López, Robin D., Mark Anthony Nawman, Mark Anthony Nawman, Sarah Elizabeth Heraldo, and Sarah Elizabeth Heraldo. "FLOWS IN HYDROGEOLOGY." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286666.

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5

Kiss, J., L. Vertesy, G. Csillag, K. Gondar, and L. Koloszar. "Hydrogeology Supported by Geophysic." In 1st EEGS Meeting. European Association of Geoscientists & Engineers, 1995. http://dx.doi.org/10.3997/2214-4609.201407448.

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6

Murdoch, Larry, Scott DeWolf, Rob Moak, and Leonid Germanovich. "Recent Developments in Hydrogeologic Applications for Strain Tensor Analyses." In 31st Clemson Hydrogeology Symposium, Clemson, South Carolina. US DOE, 2023. http://dx.doi.org/10.2172/2373030.

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7

Russo, Nicholas. "HYDROGEOLOGY OF SLIPPERY ROCK UNIVERSITY." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328461.

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8

Yaramanci, Ugur. "Magnetic resonance technology for hydrogeology." In International Conference on Engineering Geophysics, Al Ain, United Arab Emirates, 9-12 October 2017. Society of Exploration Geophysicists, 2017. http://dx.doi.org/10.1190/iceg2017-067.

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9

Wilson, Alicia. "SUBSEAFLOOR HYDROGEOLOGY: MOVING BEYOND WATERSHEDS." In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-393251.

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Komatina-Petrovic, S. "Implementation Of Geophysics In Contaminant Hydrogeology." In 4th Congress of the Balkan Geophysical Society. European Association of Geoscientists & Engineers, 2005. http://dx.doi.org/10.3997/2214-4609-pdb.26.p2-08.

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Звіти організацій з теми "Hydrogeology"

1

Hinton, M. J., S. Alpay, and C. Logan. Stop 1-2B: Hydrogeology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/289562.

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2

Rawling, Geoffrey, and Shari Kelley. Sunshine Valley hydrogeology study. New Mexico Bureau of Geology and Mineral Resources, 2020. http://dx.doi.org/10.58799/ofr-607.

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3

Newton, Talon, Stacy Timmons, Geoffrey Rawling, Frederick Partey, Trevor Kludt, Lewis Land, Mike Timmons, and Patrick Walsh. Sacramento Mountains hydrogeology study. New Mexico Bureau of Geology and Mineral Resources, 2009. http://dx.doi.org/10.58799/ofr-518.

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4

Rudolph, D. L. A renaissance in regional hydrogeology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2019. http://dx.doi.org/10.4095/313599.

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5

Denham, M. E. SRS Geology/Hydrogeology Environmental Information Document. Office of Scientific and Technical Information (OSTI), August 1999. http://dx.doi.org/10.2172/10526.

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6

Ingebritsen, S. E., and M. A. Scholl. Annotated bibliography hydrogeology of Kilauea Volcano, Hawaii. Office of Scientific and Technical Information (OSTI), October 1993. http://dx.doi.org/10.2172/10189656.

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7

Savard, M. M., M. Nastev, D. Paradis, R. Lefebvre, R. Martel, V. Cloutier, V. Murat, et al. Regional hydrogeology of the fractured aquifer system. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292546.

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8

Benoit, N., G. Forest, M. Nastev, N. Roy, D. Blanchette, and A. Fréchette. Hydrogeology of the Chaudière River Watershed, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/293152.

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9

Lowry, Thomas Stephen, Allen R. Lappin, Glen L. Gettemy, Richard Pearson Jensen, Bill Walter Arnold, Scott Carlton James, Moo Yul Lee, and Diane A. Meier. Preliminary study on hydrogeology in tectonically active areas. Office of Scientific and Technical Information (OSTI), September 2006. http://dx.doi.org/10.2172/893123.

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10

Last, George V., Eugene J. Freeman, Kirk J. Cantrell, Michael J. Fayer, Glendon W. Gee, William E. Nichols, Bruce N. Bjornstad, and Duane G. Horton. Vadose Zone Hydrogeology Data Package for Hanford Assessments. Office of Scientific and Technical Information (OSTI), June 2006. http://dx.doi.org/10.2172/896355.

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