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Journal articles on the topic 'Hydrogeophysics'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 July 2025

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1

Moysey, Stephen. "Hydrogeophysics." Ground Water 45, no. 1 (2007): 8. http://dx.doi.org/10.1111/j.1745-6584.2006.00286.x.

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Vanderborght, Jan. "Hydrogeophysics." Vadose Zone Journal 5, no. 3 (2006): 911. http://dx.doi.org/10.2136/vzj2006.0011br.

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3

Herkelrath, William. "Hydrogeophysics." Geofluids 6, no. 2 (2006): 201. http://dx.doi.org/10.1111/j.1468-8123.2006.00137.x.

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4

Auken, Esteben, Roger Guérin, Ghislain de Marsily, and Pascal Sailhac. "Hydrogeophysics." Comptes Rendus Geoscience 341, no. 10-11 (2009): 795–99. http://dx.doi.org/10.1016/j.crte.2009.09.003.

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5

Clark, Dean. "Hydrogeophysics Workshop." Leading Edge 25, no. 9 (2006): 1032–34. http://dx.doi.org/10.1190/1.2353882.

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6

Hubbard, Susan. "The evolution of hydrogeophysics." Leading Edge 27, no. 6 (2008): 824. http://dx.doi.org/10.1190/tle27060824.1.

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7

Lambot, Sébastien, Andrew Binley, Evert Slob, and Susan Hubbard. "Ground Penetrating Radar in Hydrogeophysics." Vadose Zone Journal 7, no. 1 (2008): 137–39. http://dx.doi.org/10.2136/vzj2007.0180.

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8

Gu�rin, Roger. "Borehole and surface-based hydrogeophysics." Hydrogeology Journal 13, no. 1 (2005): 251–54. http://dx.doi.org/10.1007/s10040-004-0415-4.

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9

Tronicke, Jens, and Klaus Holliger. "Quantitative integration of hydrogeophysical data: Conditional geostatistical simulation for characterizing heterogeneous alluvial aquifers." GEOPHYSICS 70, no. 3 (2005): H1—H10. http://dx.doi.org/10.1190/1.1925744.

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High-resolution geophysical parameter information, as it can be provided, for example, by crosshole georadar and seismic tomography, has proven to provide useful spatial information to complement traditional hydrological methods such as core analyses, logging techniques, and tracer or pumping tests. Quantitative integration of these diverse database components is one of the major challenges in the field of high-resolution hydrogeophysics because of their different scales of measurement and the usually weak petrophysical relations among the measurements. In this study, we systematically explore

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10

Day-Lewis, Frederick D., and Arpita P. Bathija. "Introduction to this special section: Hydrogeophysics." Leading Edge 41, no. 8 (2022): 518. http://dx.doi.org/10.1190/tle41080518.1.

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Hydrogeophysics is a crossdisciplinary field integrating hydrogeology with geophysics for more efficient, cost-effective, and minimally invasive characterization and monitoring. Hydrogeophysics aims to provide basic insight to guide understanding of hydrologic processes and applied insight to support the assessment and (or) management of water resources and ecosystem services across multiple scales, as reviewed by Binley et al. (2015) . As in geophysical investigations for mineral and fossil energy resources, geophysical applications to hydrologic problems seek to characterize subsurface struc

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11

Lane, John W., Rosemary Knight, and Burke Minsley. "Introduction to this special section: Hydrogeophysics." Leading Edge 35, no. 9 (2016): 750–51. http://dx.doi.org/10.1190/tle35090750.1.

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12

Miller, Rick. "Introduction to this special section: Hydrogeophysics." Leading Edge 25, no. 6 (2006): 713. http://dx.doi.org/10.1190/1.2210053.

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13

Skibbe, Nico, Thomas Günther, and Mike Müller-Petke. "Improved hydrogeophysical imaging by structural coupling of 2D magnetic resonance and electrical resistivity tomography." GEOPHYSICS 86, no. 5 (2021): WB135—WB146. http://dx.doi.org/10.1190/geo2020-0593.1.

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Describing hydraulic properties in the subsurface in at least two dimensions is one of the main objectives in hydrogeophysics. However, due to the limited resolution and ambiguity of the individual methods, those images are often blurry. We have developed a methodology to combine two measuring methods, magnetic resonance tomography (MRT) and electrical resistivity tomography (ERT). To this end, we extend a structurally coupled cooperative inversion scheme to three parameters. It results in clearer images of the three main parameters: water content, relaxation time, and electrical resistivity;

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14

Vereecken, H., S. Hubbard, A. Binley, and T. Ferre. "Hydrogeophysics: An Introduction from the Guest Editors." Vadose Zone Journal 3, no. 4 (2004): 1060–62. http://dx.doi.org/10.2113/3.4.1060.

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Vereecken, H., S. Hubbard, A. Binley, and T. Ferré. "Hydrogeophysics: An Introduction from the Guest Editors." Vadose Zone Journal 3, no. 4 (2004): 1060–62. http://dx.doi.org/10.2136/vzj2004.1060.

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16

Miller, Rick, and Kamini Singha. "An introduction to this special section: Hydrogeophysics." Leading Edge 32, no. 7 (2013): 740–41. http://dx.doi.org/10.1190/tle32070740.1.

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17

Miller, Rick. "An introduction to this special section: Hydrogeophysics." Leading Edge 28, no. 10 (2009): 1210. http://dx.doi.org/10.1190/1.3249776.

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18

Hubbard, Susan, and Yoram Rubin. "Study institute assesses the state of hydrogeophysics." Eos, Transactions American Geophysical Union 83, no. 51 (2002): 602. http://dx.doi.org/10.1029/2002eo000412.

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19

Jouniaux, Laurence, Alexis Maineult, Véronique Naudet, Marc Pessel, and Pascal Sailhac. "Review of self-potential methods in hydrogeophysics." Comptes Rendus Geoscience 341, no. 10-11 (2009): 928–36. http://dx.doi.org/10.1016/j.crte.2009.08.008.

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20

Linde, Niklas, David Ginsbourger, James Irving, Fabio Nobile, and Arnaud Doucet. "On uncertainty quantification in hydrogeology and hydrogeophysics." Advances in Water Resources 110 (December 2017): 166–81. http://dx.doi.org/10.1016/j.advwatres.2017.10.014.

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21

Messias, Gerlane Cavalcante, Jose Agnelo Soares, Felipe Kipper, Igor Fernandes Gomes, Vandir Pereira Soares Júnior, and Jefferson Fidélis Alves da Silva. "HYDROGEOPHYSICS IN FRACTURED CRYSTALLINE AQUIFERS IN ENGLISH GUYANA." Brazilian Journal of Geophysics 37, no. 3 (2019): 299. http://dx.doi.org/10.22564/rbgf.v37i3.2009.

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ABSTRACT: This work is a case study in Guyana with the goal of finding groundwater in rock layers with fracture-controlled porosity using electrical resistivity imaging. This work was carried out in two phases by the Brazilian Army, in eight communities in the region of Alto Tacutu – Alto Essequibo in southeast Guyana. All work was done in accordance with a technical agreement between Brazil and Guyana. In the first phase, the surveys were completed by the team which collected resistivity data using a SuperSting R8 electrical resistivity meter with dipole-dipole and dipole-gradient arrays. The

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22

Soldovieri, Francesco, Giancarlo Prisco, and Raffaele Persico. "Application of Microwave Tomography in Hydrogeophysics: Some Examples." Vadose Zone Journal 7, no. 1 (2008): 160–70. http://dx.doi.org/10.2136/vzj2006.0147.

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23

Ferré, Ty, Laurence Bentley, Andrew Binley, et al. "Critical Steps for the Continuing Advancement of Hydrogeophysics." Eos, Transactions American Geophysical Union 90, no. 23 (2009): 200. http://dx.doi.org/10.1029/2009eo230004.

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24

Boaga, Jacopo. "The use of FDEM in hydrogeophysics: A review." Journal of Applied Geophysics 139 (April 2017): 36–46. http://dx.doi.org/10.1016/j.jappgeo.2017.02.011.

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25

Yaramanci, Ugur, and Mike Müller-Petke. "Surface nuclear magnetic resonance—A unique tool for hydrogeophysics." Leading Edge 28, no. 10 (2009): 1240–47. http://dx.doi.org/10.1190/1.3249781.

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26

Ahmed, A. Soueid, A. Revil, and L. Gross. "Multiscale induced polarization tomography in hydrogeophysics: A new approach." Advances in Water Resources 134 (December 2019): 103451. http://dx.doi.org/10.1016/j.advwatres.2019.103451.

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27

Shakas, Alexis, Niklas Linde, Ludovic Baron, et al. "Neutrally buoyant tracers in hydrogeophysics: Field demonstration in fractured rock." Geophysical Research Letters 44, no. 8 (2017): 3663–71. http://dx.doi.org/10.1002/2017gl073368.

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28

Day-Lewis, Frederick D., Mary Beth Gray, Robert L. Garfield, and Amy D. Day-Lewis. "An On-Campus Well Field for Hydrogeophysics Education and Undergraduate Research." Journal of Geoscience Education 54, no. 4 (2006): 480–86. http://dx.doi.org/10.5408/1089-9995-54.4.480.

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29

Ibrahim, Dakir, Benamara Ahmed, Aassoumi Habiba, Ouallali Abdessalam, and Ait Bahammou Youssef. "Hydrogeophysics Exploration Approximately Ain Al Atti (Region of Southeast Erfoud Morocco)." Current Research in Geoscience 10, no. 1 (2020): 16–26. http://dx.doi.org/10.3844/ajgsp.2020.16.26.

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30

de Pasquale, Giulia. "Changing the Prior Model Description in Bayesian Inversion of Hydrogeophysics Dataset." Groundwater 55, no. 5 (2017): 651–55. http://dx.doi.org/10.1111/gwat.12547.

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31

DENG, Ya-ping, Xiao-qing SHI, and Ji-chun WU. "Applications of hydrogeophysics in characterization of subsurface architecture and contaminant plumes." Journal of Groundwater Science and Engineering 4, no. 4 (2016): 354–66. http://dx.doi.org/10.26599/jgse.2016.9280040.

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32

Johnson, Timothy C., Roelof J. Versteeg, Andy Ward, Frederick D. Day-Lewis, and André Revil. "Improved hydrogeophysical characterization and monitoring through parallel modeling and inversion of time-domain resistivity andinduced-polarization data." GEOPHYSICS 75, no. 4 (2010): WA27—WA41. http://dx.doi.org/10.1190/1.3475513.

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Electrical geophysical methods have found wide use in the growing discipline of hydrogeophysics for characterizing the electrical properties of the subsurface and for monitoring subsurface processes in terms of the spatiotemporal changes in subsurface conductivity, chargeability, and source currents they govern. Presently, multichannel and multielectrode data collections systems can collect large data sets in relatively short periods of time. Practitioners, however, often are unable to fully utilize these large data sets and the information they contain because of standard desktop-computer pro

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33

Mangel, Adam R., Cian B. Dawson, David M. Rey, and Martin A. Briggs. "Drone applications in hydrogeophysics: Recent examples and a vision for the future." Leading Edge 41, no. 8 (2022): 540–47. http://dx.doi.org/10.1190/tle41080540.1.

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The recent boom of commercially available drone technology capable of supporting geophysical imaging systems has led to several practitioners adopting the platforms to collect geophysical data. This has led to significant opportunities for studying hydrologic systems, as these platforms enable more efficient data collection and data collection in difficult-to-access locations. Recent examples from snow and stream studies show the viability of these platforms for studying complex systems in difficult locations and the added value of data provided by the technology. Small unoccupied aerial syste

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34

TORAN, L., B. HUGHES, J. NYQUIST, and R. RYAN. "Using Hydrogeophysics to Monitor Change in Hyporheic Flow around Stream Restoration Structures." Environmental & Engineering Geoscience 18, no. 1 (2012): 83–97. http://dx.doi.org/10.2113/gseegeosci.18.1.83.

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35

Epuh, E. E., K. A. Sanni, and M. J. Orji. "Application of Remote Sensing, GIS and Hydrogeophysics to Groundwater Exploration in parts of Lagos Metropolis: A case study of Oshodi/Isolo LGA." March 2019 3, no. 1 (2019): 41–55. http://dx.doi.org/10.36263/nijest.2019.01.0091.

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Productivity through groundwater is quite high as compared to surface water, but groundwater resources have not yet been properly exploited. The present study is used to delineate various groundwater potential zones for the assessment of groundwater availability in Lagos metropolis using remote sensing and GIS and hydrogeophysics techniques. Landsat 8, SRTM, geological, soil, and rainfall data were used in the study to prepare various thematic maps, viz., geomorphological, slope, soil, lineament density, rainfall and land use maps. On the basis of relative contribution of each of these maps to

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36

Epuh, E. E., M. J. Orji, H. A. Iyoyojie, and O. E. Daramola. "Groundwater potential mapping in Ikorodu, Lagos State, Nigeria, using multi-criteria analysis and hydrogeophysics." Nigerian Journal of Technology 39, no. 1 (2020): 278–92. http://dx.doi.org/10.4314/njt.v39i1.31.

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The assessment of the potential groundwater recharge area is extremely important for water quality protection and proper management of ground water systems. The objective of this study was to evaluate systematic groundwater studies using the integration of remote sensing and geographic information systems (GIS) and hydrogeophysics as a tool to identify groundwater potential areas in Ikorodu, Lagos. In this study, various thematic maps (layers) derived from satellite image classification such as: Land use/ Land cover map, soil map, rainfall map, geological map, slope map derived from SRTM Digit

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37

Binley, Andrew, Susan S. Hubbard, Johan A. Huisman, et al. "The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales." Water Resources Research 51, no. 6 (2015): 3837–66. http://dx.doi.org/10.1002/2015wr017016.

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38

Banks, Eddie W., Michael Hatch, Somphasith Douangsavanh, et al. "Cooperation in hydrogeophysics: Enhancing practitioners and institutions’ groundwater assessment capacity, Vientiane Plain, Lao PDR." GEOPHYSICS 87, no. 1 (2021): WA49—WA63. http://dx.doi.org/10.1190/geo2021-0100.1.

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The lowland floodplains of the Lao People’s Democratic Republic (PDR) experience prolonged dry seasons characterized by pronounced and common water scarcity, with water supplies increasingly offset with groundwater. Groundwater assessment is still at a very rudimentary stage in Laos, making it difficult to ensure that new water supplies are developed successfully and managed sustainably. The goal of this study is to apply a variety of field hydrogeophysical techniques to this problem and in the process help build and strengthen human and institutional capacity with various stakeholder groups f

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39

Pellerin, Louise, Klaus Holliger, Lee Slater, and Ugur Yaramanci. "Special Issue on Hydrogeophysics - Methods and Processes in EAGE journal of Near Surface Geophysics." Near Surface Geophysics 6, no. 1 (2007): 71. http://dx.doi.org/10.1002/nsg.61001.

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40

Haraty, Syamsul R. "STUDI HIDROGEOFISIKA DAERAH PANAS BUMI NON-VULKANIK LAINEA KABUPATEN KONAWE SELATAN MENGGUNAKAN METODE GEOLISTRIK TAHANAN JENIS." Jurnal Rekayasa Geofisika Indonesia 4, no. 01 (2022): 53. http://dx.doi.org/10.56099/jrgi.v4i01.25684.

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Research has been carried out in the non-volcanic geothermal area of Lainea, South Konawe Regency on hydrogeophysics using the geoelectrical method of resistivity. The purpose of this study was to determine the subsurface lithology and hydrological potential in the research area. Geoelectrical resistivity measurements were carried out on 5 measurement lines using the Schlumberger configuration and data processing using the PROGRESS application. The results of the alignment between the subsurface model, resistivity table and geological conditions, the lithology of the research area consists of

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41

Knight, Rosemary, James Cannia, Joseph Doetsch, et al. "The state of the science and vision of the future: Report from the Hydrogeophysics Workshop." Leading Edge 32, no. 7 (2013): 814–18. http://dx.doi.org/10.1190/tle32070814.1.

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42

Gibson, Justin, and Trenton E. Franz. "Spatial prediction of near surface soil water retention functions using hydrogeophysics and empirical orthogonal functions." Journal of Hydrology 561 (June 2018): 372–83. http://dx.doi.org/10.1016/j.jhydrol.2018.03.046.

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43

Parsekian, Andrew, Aaron Davis, Denys Grombacher, et al. "Hydrogeophysics for Informed Water Management Decisions in the Anangu Pitjantjatjara Yankunytjatjara (APY) Lands of South Australia." ASEG Extended Abstracts 2015, no. 1 (2015): 1–3. http://dx.doi.org/10.1071/aseg2015ab240.

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44

Furlan, Lucas Moreira, César Augusto Moreira, and Vânia Silvia Rosolen. "Surface and Subsurface Hydrodynamics of Inland Wetlands in Brazil: Integrating High-Resolution Remote Sensing and Hydrogeophysics." International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLVIII-2/W10-2025 (July 7, 2025): 71–77. https://doi.org/10.5194/isprs-archives-xlviii-2-w10-2025-71-2025.

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Abstract. Inland wetlands, especially those isolated from surface water systems, present complex hydrological dynamics due to interactions between meteoric water, soil moisture, and groundwater. These ecosystems act as critical zones of recharge and discharge within a catchment, and their balance is increasingly disturbed by land use changes and climate variability. The challenge is even greater in isolated wetlands, where the absence of visible surface connectivity complicates the understanding of their hydrological role— particularly in regions subjected to seasonal heavy rainfall and high e

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45

Gonzales Amaya, Andres, Gerhard Barmen, and Galo Muñoz. "A Multidisciplinary Approach for Clarifying the Recharge Processes and Origin of Saline Water in the Semi-Arid Punata Alluvial fan in Bolivia." Water 10, no. 7 (2018): 946. http://dx.doi.org/10.3390/w10070946.

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The analysis of stable isotopes assisted in identifying that groundwater in the Punata alluvial fan is mainly recharged by heavy flash floods, and the recharge from rainfall is of less importance. In addition, the hydrochemical analysis identified the Pucara River as the main source of recharge. Other streams in the north and northwest of the fan do not seem to contribute to the recharge. The hydrochemistry also shows that there is an increase of the Na+ and Cl− concentrations in the middle and distal part of the fan. The salinization of groundwater is most likely a result of the mixing of fre

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46

Li, Mengna, Yijian Zeng, Maciek W. Lubczynski, et al. "A first investigation of hydrogeology and hydrogeophysics of the Maqu catchment in the Yellow River source region." Earth System Science Data 13, no. 10 (2021): 4727–57. http://dx.doi.org/10.5194/essd-13-4727-2021.

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Abstract. The Tibetan Plateau is the source of most of Asia's major rivers and has been called the Asian Water Tower. Detailed knowledge of its hydrogeology is paramount to enable the understanding of groundwater dynamics, which plays a vital role in headwater areas like the Tibetan Plateau. Nevertheless, due to its remoteness and the harsh environment, there is a lack of field survey data to investigate its hydrogeology. In this study, borehole core lithology analysis, soil thickness measurement, an altitude survey, hydrogeological surveys, and hydrogeophysical surveys (e.g. magnetic resonanc

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47

Francés, Alain P., Maciek W. Lubczynski, Jean Roy, Fernando A. M. Santos, and Mohammad R. Mahmoudzadeh Ardekani. "Hydrogeophysics and remote sensing for the design of hydrogeological conceptual models in hard rocks – Sardón catchment (Spain)." Journal of Applied Geophysics 110 (November 2014): 63–81. http://dx.doi.org/10.1016/j.jappgeo.2014.08.015.

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48

Yang, X., A. Klotzsche, G. Meles, H. Vereecken, and J. van der Kruk. "Improvements in crosshole GPR full-waveform inversion and application on data measured at the Boise Hydrogeophysics Research Site." Journal of Applied Geophysics 99 (December 2013): 114–24. http://dx.doi.org/10.1016/j.jappgeo.2013.08.007.

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49

Vasconcelos, Suzan S., Carlos A. Mendonça, and Nilton Silva. "Self-potential signals from pumping tests in laboratory experiments." GEOPHYSICS 79, no. 6 (2014): EN125—EN133. http://dx.doi.org/10.1190/geo2013-0444.1.

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Streaming potentials can be generated when geologic porous media are subjected to pumping tests. For a homogeneous medium, theory predicts that input and output points for water circulation generate field responses in the form of electric potentials that are equivalent to those produced by current sources that are externally driven by a power source. We evaluated tank experiments showing that this assumption is valid for common geophysical scenarios and can be used to determine charge density for porous geologic media, a key parameter in interpreting electrokinetic and interfacial properties i

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50

M.M., Mohammed, Samuel O.O., and Sanni E.B. "Hydrogeophysical Investigation of Underground Water in Sabon Kaura Community, Bauchi, Nigeria." Advanced Journal of Science, Technology and Engineering 3, no. 1 (2023): 63–74. http://dx.doi.org/10.52589/ajste-aeqakvwa.

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Hydrogeophysics is the investigation of underground formations to understand the hydrologic cycle using geophysical techniques, which aids to understand the groundwater quality and type of aquifer. One of the surface geophysical methods is the Vertical Electrical Sounding; it is effective in the investigation of layer resistivity and thicknesses of layers at various depths of interest as well as aquifer thickness. Twenty (20) VES points were sounded with maximum spread AB/2 of 60 m. The VES data was processed using IPI2 win and sounding curves obtained at most combinations which include HA, QH

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