Relevant bibliographies by topics / Groundwater Electric conductivity

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  2. Dissertations / Theses
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Academic literature on the topic 'Groundwater Electric conductivity'

Author: Grafiati
Published: 4 June 2021
Last updated: 7 February 2022

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Journal articles on the topic "Groundwater Electric conductivity"

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Sejati, Sadewa Purba. "The Characteristics of Shallow Groundwater Resource in Cangkringan District Sleman Province Special Region of Yogyakarta." Media Komunikasi Geografi 18, no. 2 (2018): 166. http://dx.doi.org/10.23887/mkg.v18i2.12903.

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Cangkringan District (the research site) is one of the districts in Sleman Regency of which spatial function includeswater catchment area. Holding the predicate as a water catchment area, the research area serves as one of the groundwater supply areas for the community living in Sleman Regency. One aspect of integrated water resources management is the water resources information system aspect, in which the geohydrology information system (groundwater) is included. Based on the aspect of water resources management, the study on shallow groundwater characteristics as catchment area in the resea
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El Moukhayar, R., M. Bahir, N. Youbi, N. Chkir, H. Chamchati, and P. Caréra. "Using geochemical investigations for determining the interaction between groundwater and saline water in arid areas: case of the Wadi Ouazzi basin (Morocco)." Proceedings of the International Association of Hydrological Sciences 366 (April 10, 2015): 162–63. http://dx.doi.org/10.5194/piahs-366-162-2015.

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Abstract. The characteristics of the Essaouira basin water resources are a semi-arid climate, which is severely impacted by the climate (quantity and quality). Considering the importance of the Essaouira aquifer in the groundwater supply of the region, a study was conducted in order to understand groundwater evolution in this aquifer. The Essaouira aquifer is a coastal aquifer located on the Atlantic coastline of southern Morocco, corresponding to a sedimentary basin with an area of nearly 200 km2. The control of the fluid exchange and the influence of mixing zones between the groundwater and
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Ifeanyichukwu, Kenechukwu A., Elizabeth Okeyeh, Okechukwu E. Agbasi, Onwe I. Moses, and Ogechukwu Ben-Owope. "Using Geo-electric Techniques for Vulnerability and Groundwater Potential Analysis of Aquifers in Nnewi, South Eastern Nigeria." Journal of Geology, Geography and Geoecology 30, no. 1 (2021): 43–52. http://dx.doi.org/10.15421/112105.

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 In Nnewi, Anambra State Nigeria, twenty vertical electrical sounding (VES) were performed to delineate vulnerability and transmissivity of identified aquifer within the study area. Hydraulic parameters (transverse resistance, longitudinal conductivity, hydraulic conductivity and transmissivity) were delineated from geoelectrical parameters (depth, thickness, and apparent resistance). The geo- parameters of the aquifer: apparent resistance from 1000.590 to 1914.480, thickness from 42.850 – 66.490 m and 65.530 to 100.400 m of depth. The estimated hydraulic parameters of the
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Binotto, Raquel Barros, Elba Calesso Teixeira, Antônio Flávio Uberti Costa, and Arthur Schimidt Nanni. "Use of the geophysical method EM 34-3 in the study of groundwater contamination by coal waste and ashes." Ciência e Natura 23, no. 23 (2001): 35. http://dx.doi.org/10.5902/2179460x27122.

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The main objective of this paper is to evaluate the efficiency of the geophysical technique EM – 34 – 3 in the study of the groundwater contamination by residues from coal processing. It was applied, in the coal waste and ashes disposal site – CH 20, located in the municipal district of Charqueadas, the electromagnetic geophysical method EM – 34 – 3, which measures the electric conductivity of the medium in subsurface. It was noticed that the highest anomalous electrical conductivity values and ions content were placed inside the disposal site with the most significant contamination situated i
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Iwatake, Kaname, and Akira Ueda. "Geochemical Study on the Annual Variation of Oxygen Isotope and Chemical Composition of Groundwater in the Sho River Alluvium Fan, Toyama, Japan, as an Investigation of Selected Qualitative Aspects of Efficient Utilization of Groundwater Heat." Geosciences 11, no. 8 (2021): 352. http://dx.doi.org/10.3390/geosciences11080352.

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Seasonal variations of water temperature, electric conductivity, and oxygen isotope and chemical composition of shallow groundwaters and river waters were determined in the Sho River alluvial fan, western Toyama Prefecture, Japan, to examine groundwater heat utilization for indoor climate control. Samples were collected at 31 sites every 2 months for 1 year and at 11 representative sites monthly. In addition, the results of monthly precipitation amount and oxygen isotope composition of precipitation collected within the region during the same period were also taken into account. The sources of
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Santiago, Marlucia F., C. M. S. V. Silva, J. Mendes Filho, and H. Frischkorn. "Characterization of Groundwater in the Cariri (Ceará, Brazil) By Environmental Isotopes and Electric Conductivity." Radiocarbon 39, no. 1 (1997): 49–59. http://dx.doi.org/10.1017/s0033822200040893.

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The Cariri region is the largest sedimentary basin in the state of Ceará, Brazil. Located in the southern portion of the state, it comprises the Araripe Plateau and the Cariri Valley on its northern foot. The region's groundwaters are being heavily exploited. Using electric conductivity (EC) and 18O, 14C and 3H data, we differentiate groundwaters from various origins. We identified three horizons of springs on the slope of the Plateau through their geologic environment and the EC of their waters. Groundwaters from wells in the Cariri Valley are classified according to the aquifers exploited as
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Feo, Alessandra, Andrea Zanini, Emma Petrella, Rebeca Hernàndez-Diaz, and Fulvio Celico. "Analysis of the Saltwater Wedge in a Coastal Karst Aquifer with a Double Conduit Network, Numerical Simulations and Sensitivity Analysis." Water 11, no. 11 (2019): 2311. http://dx.doi.org/10.3390/w11112311.

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We investigate the long-distance salinity in a dual permeability coastal karst aquifer with a double conduit network using a three-dimensional variable-density groundwater flow and multispecies transport SEAWAT model. Sensitivity analyses were used to evaluate the impact of the parameters and boundary conditions on the modeling saltwater wedge in a karstic aquifer situated in the Cuban land territory, including hydraulic conductivity, vertical anisotropy and salinity concentration; both in the conduits network and the fractured medium. These analyses indicated that hydraulic conductivity of th
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SATO, Tsutomu, Norio MATSUMOTO, Makoto TAKAHASHI, et al. "Observation of water level, temperature and electric conductivity of groundwater around Usu Volcano." BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN 52, no. 4-5 (2001): 143–48. http://dx.doi.org/10.9795/bullgsj.52.143.

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Lindell, Ismo V., Murat E. Ermutlu, Keijo I. Nikoskinen, and Esko H. Eloranta. "Static image principle for anisotropic‐conducting half‐space problems: PEC and PMC boundaries." GEOPHYSICS 58, no. 12 (1993): 1861–64. http://dx.doi.org/10.1190/1.1443401.

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The image principle for an isotropic half‐space bounded by perfect electric conductor (PEC) or perfect magnetic conductor (PMC) plane is presented in most elementary textbooks on electromagnetics. It is perhaps not so well known that this principle can also be generalized to anisotropic media in the static case, because it is not covered in leading monographs of geoelectromagnetics (Wait, 1982; Negi and Saraf, 1989; Eskola, 1992). The anisotropic image method can be applied to geologic media that exhibit anisotropic electrical conductivity caused by the fractures and fissures in the rock. Such
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Nicaise, Yalo, Descloitres Marc, Alassane Abdoukarim, Mama Daouda, and Boukari Moussa. "Environmental Geophysical Study of the Groundwater Mineralization in a Plot of the Cotonou Littoral Zone (South Benin)." International Journal of Geophysics 2012 (2012): 1–10. http://dx.doi.org/10.1155/2012/329827.

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Geophysical investigations comprising electrical resistivity and electromagnetic conductivities methods were deployed in a 350 m2sector, strewn with 11 wells. Within the framework of an environmental study on a small scale in the south of Benin, the water conductivity of these wells was measured to determine in a direct way mineralization of the coastal water table in the littoral zone. This environmental study aimed to prospect by the geophysical methods the space extension of the water table mineralization obtained by direct measurements of water conductivity in the well and the depth of the
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Dissertations / Theses on the topic "Groundwater Electric conductivity"

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Allen, David Andrew. "Electrical conductivity imaging of aquifers connected to watercourses : a thesis focused on the Murray Darling Basin, Australia." University of Technology, Sydney. Faculty of Science, 2007. http://hdl.handle.net/2100/428.

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Electrical imaging of groundwater that interacts with surface watercourses provides detail on the extent of intervention needed to accurately manage both resources. It is particularly important where one resource is saline or otherwise polluted, where spatial quantification of the interacting resources is critical to water use planning and where losses from surface waterways need to be minimized in order to transport water long distances. Geo-electric arrays or transient electromagnetic devices can be towed along watercourses to image electrical conductivity (EC) at multiple depths within and
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Nygren, Anton, Edvard Nordenskjöld, and Erik Östblom. "Groundwater occurrence and quality in Bulawayo province, Zimbabwe." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-300718.

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This study focused on determining the groundwater flow paths in the crystalline subsurface rocks of the Bulawayo metropolitan, Zimbabwe, through analysing the discontinuities of the electrical properties of the ground, as well as in the magnetic field of the underlying rocks. Further, borehole water quality was analysed by measuring and mapping several chemical parameters, specifically TDS, salinity and the electrical conductivity. The electrical and magnetic anomalies were measured at two field sites within the Bulawayo province, the Harry Allen Golf Course and the Barbour Fields dumpsite, wh
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Kingsley, Janet Elizabeth. "Using electrical conductivity and temperature mapping to locate zones of groundwater discharge in the South Nation River, eastern Ontario." Thesis, University of Ottawa (Canada), 2005. http://hdl.handle.net/10393/27143.

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Groundwater-surface water interactions (GSWI's) interactions are an important part of understanding the hydrological cycle, groundwater and river systems, and in providing estimates of groundwater contributions to rivers (base flow). Seepage/leakage of groundwater into surface waters can be measured directly, but this is very labor-intensive, and therefore not feasible at the scale of a basin. An alternative method, which was used in this study, infers groundwater seepage from electrical conductivity and temperature (EC& T) of water at the bottom of the river, based on the assumption that ther
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Lasher, Candice. "Application of fluid electrical conductivity logging for fractured rock aquifer characterisation at the University of the Western Cape's Franschhoek and Rawsonville research sites." Thesis, University of the Western Cape, 2011. http://etd.uwc.ac.za/index.php?module=etd&action=viewtitle&id=gen8Srv25Nme4_3729_1338541923.

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<p>&nbsp<br>Characterisation of fractured rock aquifers is important when dealing with groundwater protection and management. Fractures are often good conduits for water and contaminants, leading to high flow velocities and the fast spread of contaminants in these aquifers. A cost effective methodology is required for the characterisation of the role of individual fractures contributing to flow to boreholes in fractured rock aquifers. Literature shows that some of the conventional methods used to characterise hydraulic properties in fractured rock aquifers are expensive, complicated, time cons
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Angheben, Anna. "Mapping and modeling of the groundwater at the dam site in Bremen. A preliminary flow model." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2017.

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Groundwater is of fundamental importance in water resources planning as it serves as storage/release entity. The hydrological characterization of the groundwater in Bremen area in the present work has been considered using two approaches. i) analysis of parameters collected during field campaign, i.e. piezometric head and electrical conductivity; ii) model elaboration and simulation with the forthcoming FREEWAT plugin for QGIS. After straightened activities in Weser up to the North Sea, the Hemelingen barrier, the peculiarity of the study area, was built to maintain a constant flow in the
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Derie, Bereket Mebrahtu. "Integration of geophysical methods for groundwater exploration in hard rock areas : application to Alla Valley, Eritrea, NE Africa." Thesis, Loughborough University, 2011. https://dspace.lboro.ac.uk/2134/12616.

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The integrated use of Electromagnetic Ground Conductivity, Ground Electrical Resistivity and Seismic Refraction geophysics methods was made in Alia valley, Eritrea for the aim of developing a methodology best suited for ground water exploration in hard rock areas with limited professional and financial resources. A total area of 25 square kilometer was covered with the geophysical surveys. The effective use of information from wells and geological information from outcrops and existing literature helped to create a preliminary conceptual hydrogeologic model that in turn provided a general pict
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Nixdorf, Erik. "Combining measurements, remote sensing and numerical modelling to assess multi-scale flow dynamics in groundwater-dependent environmental systems." Doctoral thesis, Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2018. http://nbn-resolving.de/urn:nbn:de:bsz:14-qucosa-236485.

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Groundwater flow modelling provides an important quantitative instrument for addressing issues related to the quantity and quality of groundwater and the connected water resources. Consequently, groundwater flow models have been developed and used ubiquitously in science to deepen the understanding of subsurface processes and their drivers as well as management and planning tools. The present work investigates how numerical models can be linked to field investigations and public databases to quantitatively approach questions in the area of groundwater research. The primary goal is to develop n
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YU-LIN, LIAO, and 廖玉霖. "Feasibility Study on Using Crosshole-Surface Electrical Conductivity to Evaluate Groundwater Flow Field." Thesis, 2018. http://ndltd.ncl.edu.tw/handle/4ncqz2.

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碩士<br>逢甲大學<br>環境工程與科學學系<br>106<br>The main goal of this research is to directly measure groundwater velocity and direction by monitoring soil apparent the change of soil apparent resistivity during a tracer test. The motivation is to be able to accurately and effectively measure groundwater velocity and direction using only one monitoring well. The tracer test used 250 L of de-ionized water as the tracer. The tracer was pumped into a groundwater monitoring well (MW-8) by raising the water table in the well (< 30 cm). The injection time was about 15 min and the injected water was considered as
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Yang, Chao-Sheng, and 楊晁晟. "A Study on The Relationships between Electrical Conductivity of Groundwater and Debris-Flow Occurrence." Thesis, 2003. http://ndltd.ncl.edu.tw/handle/03595347777863853380.

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碩士<br>國立臺灣大學<br>生物環境系統工程學系暨研究所<br>91<br>Abstract The main purpose of this study is to investigate the relationships between electrical conductivity of groundwater and debris-flow occurrence. If the soil deposited in the stream with a high potential of debris flow or located at the sides of the stream was eroded due to seepage for a period of time, fine particles of the soil might be carried away and subsequently, the whole soil deposit or the slope might collapse. Therefore, field dimension analyses were conducted and accordingly, seepage tanks were designed and fabricated.
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Yang, Chan-Yuan, and 楊展源. "A Study on the Relationships among Ion Concentration 、Electrical Conductivity of Groundwater and Debris-Flow Occurrence." Thesis, 2004. http://ndltd.ncl.edu.tw/handle/54204833156867039006.

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碩士<br>國立臺灣大學<br>生物環境系統工程學研究所<br>92<br>The main purpose of this study is to investigate the relationships among ion concentration 、 electrical conductivity (EC) of groundwater and debris flow occurrence. During typhoon season, very frequently, heavy rainfall resulted in the rise of groundwater table, unstability and the failure of the slope. Accordingly, in this study, the test site was investigated and flumes for seepage flow tests were designed. The site of this study was selected at Ba-Dou-Tze in Keelung. Therefore, the soil samples for the tests were collected from the site. After the soil
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Books on the topic "Groundwater Electric conductivity"

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Müller, Kerstin Andrea. Optimization of tracer experiments to characterize transport properties in heterogeneous aquifers using non-invasive measurement techniques. Forschungszentrum, Zentralbibliothek, 2006.

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Book chapters on the topic "Groundwater Electric conductivity"

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Bon, André Firmin, Sylvain Doua Aoudou, Arouna Mbouombouo Ndam, Etienne Ambomo Bineli, and Elisabeth Dassou Fita. "Groundwater Pollution Index Evaluation Test Using Electrical Conductivity in a Semi-arid Quaternary Aquifer (Kousseri-Cameroon, Lake Chad Basin): Multivariate Statistical Analysis Approach." In Advances in Sustainable and Environmental Hydrology, Hydrogeology, Hydrochemistry and Water Resources. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01572-5_70.

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PERERA, E. D. P., K. JINNO, Y. HIROSHIRO, and A. TSUTSUMI. "NUMERICAL SIMULATION OF ELECTRIC CONDUCTIVITY FLUCTUATIONS DUE TO GROUNDWATER PUMPING IN A COASTAL AQUIFER." In Advances in Geosciences. World Scientific Publishing Company, 2010. http://dx.doi.org/10.1142/9789812838124_0007.

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Dam, D., S. Christensen, and N. B. Christensen. "Characterizing the hydraulic conductivity field using electrical resistivity and inverse modeling." In Groundwater 2000. CRC Press, 2020. http://dx.doi.org/10.1201/9781003078593-5.

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Sposito, Garrison. "Soil Salinity." In The Chemistry of Soils. Oxford University Press, 2016. http://dx.doi.org/10.1093/oso/9780190630881.003.0016.

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A soil is salineif the electrical conductivity of its soil solution as obtained by extraction from a water-saturated soil paste (ECe) exceeds 4 dS m-1. (The measurement of electrical conductivity for a soil saturation extract is discussed in Methods of Soil Analysis,listed under For Further Reading at the end of this chapter.) According to this definition, about a quarter of the agricultural soils worldwide are saline, but values of ECe &gt; 1 dS m-1 are encountered typically in arid-zone soils, which cover almost one-third of the global ice-free land area. Ions released into the soil solution by mineral weathering, or introduced there by the intrusion of saline surface water or groundwater, tend to accumulate in the secondary minerals formed as the soils dry. These secondary minerals typically include clay minerals (Section 2.3), carbonates and sulfates (Section 2.5), and chlorides. Because Na, K, Ca, and Mg are brought into the soil solution relatively easily—either as displaced exchangeable cations or as cations dissolved from carbonates, sulfates, and chlorides—it is this set of four metals that contributes most to soil salinity. The corresponding set of anions that contributes to salinity is CO3, SO4, and Cl. Thus, arid-zone soil solutions are essentially electrolyte solutions containing chloride, sulfate, and carbonate salts of four metal cations. According to Eq. 4.21, an electrical conductivity of 4 dS m-1 corresponds to an ionic strength of 58 mM (log I = -1.841 + 1.009 log4 = 0.0584). This level of salinity is less than 10% of that of seawater (EC = 46.21 dS m-1), but high enough that only crops that are relatively salt tolerant can withstand it. Moderately salt-sensitive crops are affected when the electrical conductivity of a soil saturation extract approaches 2 dS m-1, corresponding to an ionic strength of 29 mM, and salt-sensitive crops are affected at 1 dS m-1 (I = 14 mM). Thus, with respect to crop salinity tolerance, a soil can be judged saline at any saturation extract ionic strength greater than 15 mM if crops are stressed.
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Conference papers on the topic "Groundwater Electric conductivity"

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Ito, Hidenori, Todd Saunders, Junya Miyamoto, Masaya Nishiyama, and Tsuyoshi Nakamura. "Establishing allowable value of Electric Conductivity for monitoring groundwater based on the benchmark dose concept and its application." In 2010 International Conference on Environmental Engineering and Applications (ICEEA). IEEE, 2010. http://dx.doi.org/10.1109/iceea.2010.5596121.

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Silva, W. P., C. D. G. C. Almeida, M. M. Rolim, J. M. Bezerra, and K. P. P. Marques. "Spatiotemporal Variability of Electrical Conductivity in Groundwater Under Vinasse Application." In II Inovagri International Meeting. INOVAGRI/INCT-EI/INCTSal, 2014. http://dx.doi.org/10.12702/ii.inovagri.2014-a184.

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McDaris, John R., and Joshua Feinberg. "USING REAL-TIME ELECTRICAL CONDUCTIVITY MEASUREMENTS TO UNDERSTAND CHLORIDE IN GROUNDWATER." In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-347832.

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Joseph, Rita Maria, Alna D. Manjaly, Sreeram Unni, Able E C, and Vinitha Sharon. "Prediction of Groundwater Quality Using Artificial Neural Network." In International Web Conference in Civil Engineering for a Sustainable Planet. AIJR Publisher, 2021. http://dx.doi.org/10.21467/proceedings.112.26.

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Assessment and prediction of water quality is a vital tool for the management of water resources systems. It is necessitous for human existence, agriculture and industry. This project delves into the prediction of groundwater quality parameters and groundwater quality criterion based on the Artificial Neural Network Modelling with the study area as Kerala, a state of India. Two models were developed. The first model employs the water quality parameters such as pH, electrical conductivity, total hardness as the input parameters and calcium, magnesium, chloride, fluoride, nitrate concentration a
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McCall, Wesley, Thomas M. Christy, and James J. Butler. "Direct Push Technology and Application to Vertical Profiling of Hydraulic Conductivity in Unconsolidated Formations." In ASME 2003 9th International Conference on Radioactive Waste Management and Environmental Remediation. ASMEDC, 2003. http://dx.doi.org/10.1115/icem2003-4590.

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Direct push (DP) methods provide a cost-effective alternative to conventional rotary drilling for investigations in unconsolidated formations. DP methods are commonly used for sampling soil gas, soil and groundwater; installing small-diameter monitoring wells; electrical logging; cone penetration testing; and standard penetration tests. Most recently, DP methods and equipment for vertical profiling of formation hydraulic conductivity (K) have been developed. Knowledge of the vertical and lateral variations in K is integral to understanding contaminant migration and, therefore, essential to des
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Akawwi, Emad. "USING ELECTRICAL CONDUCTIVITY FOR LOCATING THE SUBMARINE GROUNDWATER DISCHARGE ALONG THE EASTERN SHORES OF THE DEAD SEA-JORDAN." In SGEM2011 11th International Multidisciplinary Scientific GeoConference and EXPO. Stef92 Technology, 2011. http://dx.doi.org/10.5593/sgem2011/s02.143.

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Reports on the topic "Groundwater Electric conductivity"

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Turner, R. A., A. M. Haiblen, and S. B. Cook. Exploring for the Future—groundwater level and electrical conductivity data release: Howard East, Northern Territory. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.055.

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