Academic literature on the topic 'Groundwater Chemistry'

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Journal articles on the topic "Groundwater Chemistry"

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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 (1988): s59—s65. http://dx.doi.org/10.1139/f88-267.

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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 g
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Kitessa, Wagari Mosisa, Adisu Befekadu Kebede, Fayera Gudu Tufa, et al. "Hydrogeochemical Characterization and Processes Controlling Groundwater Chemistry of Complex Volcanic Rock of Jimma Area, Ethiopia." Water 16, no. 23 (2024): 3470. https://doi.org/10.3390/w16233470.

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The sustainable management of groundwater in the Jimma area is complicated by a lack of comprehensive studies on its chemical makeup and the geochemical processes influencing its hydrochemistry. This research aims to fill that gap by examining 51 groundwater samples from various sources, including deep groundwaters, shallow groundwaters, hand-dug well groundwaters, surface waters, and springs within the area primarily consisting of complex volcanic rocks. The goal is to describe the hydrogeochemical characteristics and determine the key processes affecting groundwater composition in this volca
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Liu, Chunyan, Qinxuan Hou, Yetao Chen, and Guanxing Huang. "Hydrogeochemical Characteristics and Groundwater Quality in a Coastal Urbanized Area, South China: Impact of Land Use." Water 14, no. 24 (2022): 4131. http://dx.doi.org/10.3390/w14244131.

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Land use transformation accompanied with various human activities affects groundwater chemistry and quality globally, especially in coastal urbanized areas because of complex human activities. This study investigated the impact of land use on groundwater chemistry and quality in a coastal alluvial aquifer (CAA) of the Pearl River Delta where urbanization continues. A fuzzy synthetic evaluation method was used to evaluate the groundwater quality. Besides, factors controlling groundwater chemistry and quality in the CAA were discussed by using a principal components analysis (PCA). Nearly 150 gr
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Datta, P. S., and S. K. Tyagi. "Major Ion Chemistry of Groundwater in Delhi Area: Chemical Weathering Processes and Groundwater Flow Regime." Journal Geological Society of India 47, no. 2 (1996): 179–88. http://dx.doi.org/10.17491/jgsi/1996/470205.

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Abstract Groundwater is moderately to highly saline in all parts of Delhi area. No definite explanation has emerged so far about the source of salinity. Study of major ion chemistry of groundwater has been conducted to identify the source of major ions in terms of chemical weathering processes. The chemistry of groundwater is dominated by carbonate weathering. The excess of sodium ion over chloride ion can be attributed to silicate weathering to a certain extent. The groundwater in northern and western parts of the area is primarily alkaline and secondarily saline and in the southern and south
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Liu, Ji Lai, Tian Ming Huang, and Jie Li. "Groundwater Recharge Environments and Hydrogeochemical Evolution in Beijing, China: Multi-Tracer Approach." Advanced Materials Research 518-523 (May 2012): 3647–51. http://dx.doi.org/10.4028/www.scientific.net/amr.518-523.3647.

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The groundwater recharge environments and hydrogeochemical characteristics in Beijing were investigated using a combination of chemical indicators, stable isotopes, and radiocarbon dating. There are two distinct zones for those groundwaters: modern water (1000 a) are depleted, which implies that the palaeowaters were recharged in relatively cold climate. The TDS for all groundwater samples range from 312 to 914 mg/L. Groundwaters are supersaturated with respect to calcite and the δ13C value is stable (around -13‰), which suggests dissolution of calcite is limited. Dissolution of halite, sulfat
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Wu, Ruohan, Laura A. Richards, Ajmal Roshan, and David A. Polya. "Artificial Intelligence Modelling to Support the Groundwater Chemistry-Dependent Selection of Groundwater Arsenic Remediation Approaches in Bangladesh." Water 15, no. 20 (2023): 3539. http://dx.doi.org/10.3390/w15203539.

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Groundwater arsenic (As) still poses a massive public health threat, especially in South Asia, including Bangladesh. The arsenic removal efficiency of various technologies may be strongly dependent on groundwater composition. Previously, others have reported that the molar ratio [Fe]−1.8[P][As], in particular, can usefully predict the potential efficiency of groundwater As removal by widespread sorption/co-precipitation-based remediation systems. Here, we innovatively extended the application of artificial intelligence (AI) machine learning models to predict the geospatial distribution of [Fe]
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Wang, Wanping, Shilong Zhang, Shengbin Wang, et al. "Spatial Variations and Regulating Processes of Groundwater Geochemistry in an Urbanized Valley Basin on Tibetan Plateau." Applied Sciences 14, no. 21 (2024): 9804. http://dx.doi.org/10.3390/app14219804.

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Groundwater resource is crucial for the development of agriculture and urban communities in valley basins of arid and semiarid regions. This research investigated the groundwater chemistry of a typical urbanized valley basin on the Tibetan Plateau to understand the hydrochemical status, quality, and controlling mechanisms of groundwater in arid urbanized valley basins. The results show groundwater is predominantly fresh and slightly alkaline across the basin, with approximately 54.17% of HCO3-Ca type. About 12.5% and 33.33% of sampled groundwaters are with the hydrochemical facies of Cl-Mg·Ca
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Neal, C., A. J. Robson, P. Shand, et al. "The occurrence of groundwater in the Lower Palaeozoic rocks of upland Central Wales." Hydrology and Earth System Sciences 1, no. 1 (1997): 3–18. http://dx.doi.org/10.5194/hess-1-3-1997.

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Abstract. A series of boreholes of up to 50 m depth, drilled into Lower Palaeozoic mudstone, shale and greywacke bedrock in the headwater catchment areas of the River Severn at Plynlimon in Central Wales, shows an extensive chemically- and hydrologically-active shallow groundwater fracture flow system. Groundwater chemistry varies in space and time with lowest water levels and highest alkalinities occurring during the drier summer months. The groundwaters are enriched in base cations, silica, sulphate and alkalinity relative to surface waters indicating significant silicate weathering sources
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Hernández-Antonio, A., J. Mahlknecht, C. Tamez-Meléndez, et al. "Groundwater flow processes and mixing in active volcanic systems: the case of Guadalajara (Mexico)." Hydrology and Earth System Sciences Discussions 12, no. 2 (2015): 1599–631. http://dx.doi.org/10.5194/hessd-12-1599-2015.

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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.
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Schwab, Valérie F., Martina Herrmann, Vanessa-Nina Roth, et al. "Functional diversity of microbial communities in pristine aquifers inferred by PLFA- and sequencing-based approaches." Biogeosciences 14, no. 10 (2017): 2697–714. http://dx.doi.org/10.5194/bg-14-2697-2017.

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Abstract. Microorganisms in groundwater play an important role in aquifer biogeochemical cycles and water quality. However, the mechanisms linking the functional diversity of microbial populations and the groundwater physico-chemistry are still not well understood due to the complexity of interactions between surface and subsurface. Within the framework of Hainich (north-western Thuringia, central Germany) Critical Zone Exploratory of the Collaborative Research Centre AquaDiva, we used the relative abundances of phospholipid-derived fatty acids (PLFAs) to link specific biochemical markers with
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Dissertations / Theses on the topic "Groundwater Chemistry"

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Carlyle, Graham Charles. "Groundwater phosphorus chemistry in a river riparian zone." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0017/MQ59163.pdf.

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Mahmood, Hosam Rifaat. "Groundwater chemistry and water table variations in Bahrain." Thesis, Loughborough University, 1993. https://dspace.lboro.ac.uk/2134/11707.

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An evaluation has been carried out of the groundwater system in Bahrain. It has involved the collection of water samples from all the water bearing formations to study the quality of the groundwater. Each water sample was tested physically, chemically, and bacteriologically. Additionally, the five day biochemical oxygen demand test and hydrogen sulphide were detected. The period of the actual sampling and testing extended from mid-1990 to the beginning of 1992. The results obtained have been compared to the results of an earlier study conducted between 1978 and 1979. The investigation has also
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Kolesnik, Lindgren Julian. "Aquifer Thermal Energy Storage : Impact on groundwater chemistry." Thesis, KTH, Hållbar utveckling, miljövetenskap och teknik, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-232110.

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Groundwater is potentially a useful source for storing and providing thermal energy to the built environment. In a nordic context, aquifer thermal energy storage, (ATES) has not been subject to a wider extent of research concerning environmental impact. This thesis intends to study the impact on groundwater chemistry from an ATES that has been operational since 2016 and is located in the northern part of Stockholm, on a glaciofluvial deposit called the Stockholm esker. Analysis of groundwater sampling included a period of 9 months prior to ATES operation as well as a 7 month period after opera
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Seger, Emily M. "Seepage Lake Chemistry as an Indicator of Climate Change." Fogler Library, University of Maine, 2004. http://www.library.umaine.edu/theses/pdf/SegerEM2004.pdf.

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Grant, Jane D. "The significance of groundwater-surface water interactions on hyporheic physico-chemistry and stream ecology in two Scottish mountain rivers." Thesis, Available from the University of Aberdeen Library and Historic Collections Digital Resources. Online version available for University members only until Apr. 7, 2010, 2008. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?application=DIGITOOL-3&owner=resourcediscovery&custom_att_2=simple_viewer&pid=26046.

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Doremus, Llyn, and David Kreamer. "Groundwater Movement and Water Chemistry at Bryce Canyon National Park." Arizona-Nevada Academy of Science, 2000. http://hdl.handle.net/10150/296565.

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Stanley, James. "Groundwater chemistry and microbiology in a wet-tropics agricultural catchment." Thesis, Queensland University of Technology, 2019. https://eprints.qut.edu.au/134265/1/James_Stanley_Thesis.pdf.

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Groundwater ecosystems can moderate the concentrations of agricultural contaminants that discharge into marine zones like the Great Barrier Reef. However, the analysis of microorganisms in our wet-tropics groundwater aquifers has received little attention. This study monitored seasonal changes in groundwater chemistry in aquifers underlying sugarcane in north Queensland and identified microorganisms that inhabit the groundwater and soil. The results indicate a strong connectivity between agricultural soil ecosystems and groundwater aquifers. There was spatial variability in groundwater chemist
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Shanyengana, Shanyengana E. "Groundwater chemistry and supplementary sources of freshwater in Arid environments : groundwater salinisation, solar desalination & fog collection." Thesis, Stellenbosch : Stellenbosch University, 2002. http://hdl.handle.net/10019.1/52870.

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Thesis (DPhil)--Stellenbosch University, 2002.<br>ENGLISH ABSTRACT: Freshwater is the most fundamental of all life-supporting resources that determine our social, economic and political wellbeing. It is, however, only a small percentage of the world's water resources and is also unevenly distributed. Arid regions make-up about forty percent of the world's land area and have a large proportion of the world population, however, they only have a small fraction of the freshwater compared to other areas. Conventional freshwater sources in arid environments such as surface water in rivers, l
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Garcia, Garcia Sandra. "The impact of groundwater chemistry on the stability of bentonite colloids." Licentiate thesis, KTH, Chemistry, 2007. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-4504.

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<p>I det svenska djupförvaret för kärnbränsle ska kompakterad bentonit användas som barriär mellan kopparkapslar med utbränt kärnbränsle och berget. I kontakt med vattenförande sprickor kan bentonitbarriären under vissa omständigheter avge montmorillonitkolloider. Förutom att barriärens egenskaper urholkas pga förlusten av material kan kolloiderna, om de är stabila, underlätta transporten av sorberade radionuklider ut mot biosfären.</p><p>Den här studien fokuserar på att undersöka vilka effekter grundvattenkemin har på montmorillonitkolloiders stabilitet. Grundvattnets sammansättning, pH och j
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García, García Sandra. "The impact of groundwater chemistry on the stability of bentonite colloids /." Stockholm : Kemi, Kungliga Tekniska högskolan, 2007. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-4504.

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Books on the topic "Groundwater Chemistry"

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J, Brown L. Poverty Bay flats' groundwater chemistry. Dept. of Scientific and Industrial Research, New Zealand Geological Survey, 1987.

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Hiscock, Kevin M. Groundwater chemistry study in the vicinity of Norwich. University of Birmingham, 1986.

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Deutsch, W. J. Groundwater geochemistry: Fundamentals and applications to contamination. Lewis Publishers, 1997.

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ʻImanuʼel, Mazor, ed. Chemical and isotopic groundwater hydrology: The applied approach. 2nd ed. M. Dekker, 1997.

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Drever, James I. The geochemistry of natural waters: Surface and groundwater environments. 3rd ed. Prentice Hall, 1997.

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Zekt︠s︡er, I. S. Groundwater and the Environment. Taylor and Francis, 2000.

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Steinkampf, W. C. Ground-water geochemistry of the Columbia Plateau aquifer system, Washington, Oregon, and Idaho. U.S. Geological Survey, 1996.

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Zaĭt͡sev, Ivan Kireevich. Gidrogeokhimii͡a SSSR. "Nedra," Leningradskoe otd-nie, 1986.

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Steinkampf, W. C. Controls on ground-water chemistry in the Horse Heaven Hills, south-central Washington. U.S. Dept. of Interior, Geological Survey, 1985.

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Steinkampf, W. C. Ground-water geochemistry of the Columbia Plateau aquifer system, Washington, Oregon, and Idaho. U.S. Geological Survey, 1996.

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Book chapters on the topic "Groundwater Chemistry"

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Grøn, Christian. "AOX in groundwater." In Environment & Chemistry. Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0061-8_4.

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Eang, Khy Eam, Ratana Kheang, Bunhuot Ruos, et al. "Chemistry of Groundwater in the Floodplain." In Water and Life in Tonle Sap Lake. Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-6632-2_26.

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Fendeková, Miriam. "Groundwater Drought Occurrence in Slovakia." In The Handbook of Environmental Chemistry. Springer International Publishing, 2018. http://dx.doi.org/10.1007/698_2018_269.

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Balamurugan, Gopal, Sekar Vikneshvaran, Mayakrishnan Gopiraman, Vadivel Porchezhiyan, Andivelu Ilangovan, and Somasundaram Saravanamoorthy. "CHAPTER 10. Functional Nanocomposites for Groundwater Treatment." In Chemistry in the Environment. Royal Society of Chemistry, 2021. http://dx.doi.org/10.1039/9781839165283-00246.

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Berkowitz, Brian, Ishai Dror, and Bruno Yaron. "Contaminant-Induced Irreversible Changes in Groundwater Chemistry." In Contaminant Geochemistry. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-54777-5_17.

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Garba, Ahmed, Muhammad Mukhtar, and Aishatu Hussein Santuraki. "A Multivariate Analysis of Groundwater Chemistry Data." In Water Resources in Arid Lands: Management and Sustainability. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-67028-3_13.

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Stupp, Hans Dieter. "Spreading of MTBE and Chlorinated Hydrocarbons in Groundwater: Comparison of Groundwater Transport and Plume Dimensions." In The Handbook of Environmental Chemistry. Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-72641-8_6.

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Wang, Chi-Yuen, and Michael Manga. "Groundwater and Stream Composition." In Lecture Notes in Earth System Sciences. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-64308-9_9.

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AbstractChanges of groundwater chemistry have long been observed. We review some studies of the earthquake-induced changes of groundwater and streamflow composition. When data are relatively abundant and the hydrogeology is relatively simple, the observed changes may provide valuable insight into earthquake-induced changes of hydrogeological processes. Progress in this aspect, however, has been slow not only because systematic measurements are scare but also because of the distribution of chemical sources and sinks in the crust are often complex and unknown. Most changes are consistent with th
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Mahmoud, M. A. "Groundwater and Agriculture in the Nile Delta." In The Handbook of Environmental Chemistry. Springer International Publishing, 2017. http://dx.doi.org/10.1007/698_2017_94.

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Debor, Linde, and Leen Bastiaens. "Bioremediation of groundwater contaminated with MTBE/TBA." In The Handbook of Environmental Chemistry. Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-72641-8_8.

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Conference papers on the topic "Groundwater Chemistry"

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Chiang, K. T., D. S. Dunn, and G. A. Cragnolino. "Effect of Simulated Groundwater Chemistry on Stress Corrosion Cracking of Alloy 22." In CORROSION 2005. NACE International, 2005. https://doi.org/10.5006/c2005-05463.

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Abstract Slow strain rate tests were performed to evaluate the effect of simulated groundwater chemistry variations on the stress corrosion cracking (SCC) susceptibility of mill-annealed Alloy 22. Tests were conducted in which the constituent anionic species were removed selectively from simulated concentrated water (SCW). SCC was observed in SCW and its variations [removal of nitrate, sulfate, fluoride or chloride] at a high anodic potential of 0.4 VSCE at 95°C (203°F). Although the bicarbonate ion is the predominant constituent in SCW causing SCC, a synergistic effect exists between the bica
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Jain, Vijay, Darrell Dunn, Narasi Sridhar, and Lietai Yang. "Effect of Measurement Methods and Solution Chemistry on the Evaluation of the Localized Corrosion of Candidate High-Level Waste Container Materials." In CORROSION 2003. NACE International, 2003. https://doi.org/10.5006/c2003-03690.

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Abstract The formation of concentrated brines and inorganic salts is predicted to occur due to groundwater evaporation within the emplacement drifts of the proposed Yucca Mountain repository. These brines are important because they can increase the boiling point of the aqueous solutions well above 100 °C and a liquid phase can be stable at very low values of relative humidity. In addition, they provide a source of concentrated anions that could initiate or inhibit localized corrosion of the waste package (WP). Critical potentials such as the repassivation potential for crevice corrosion are us
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Adina, Pacala. "ARSENIC REMOVAL FROM GROUNDWATER BY COAGULATION PROCESS: PERFORMANCE AND LIMITATIONS INFLUENCED BY THE GROUNDWATER SOURCES CHEMISTRY USED FOR DRINKING WATER PURPOSE IN THE WEST REGION OF ROMANIA." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024v/3.2/s11.03.

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Arsenic (As) contaminated groundwater is a critical issue of concern, in view of its toxicity through drinking water and health impacts on the human body. In this regard, the World Health Organization (WHO, 1993) has recommended 10 ?g/L for dissolved As concentration in water as standard value for drinking purposes. Special attention should be paid to the monitoring the quality of the groundwater, the chemistry and composition of arsenic-contaminated water are the major factors, determining the applied technologies for removal of arsenic. The coagulation-flocculation process is well known as p
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Elboujdaini, M., J. Li, V. Gertsman, et al. "Stress Corrosion Cracking: Microstructural and Material Properties for Crack Initiation of 16" X-52 Line Pipe Steel." In CORROSION 2004. NACE International, 2004. https://doi.org/10.5006/c2004-04553.

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Abstract To better understand the mechanism for stress corrosion cracking (SCC) the advanced analytical tools, including high-resolution scanning electron microscope (SEM), focus ion beam (FIB) and transmission electron microscope (TEM) were used. The complexity of stress corrosion cracking results from the dependence of SCC on composition of the steel, applied stress, water chemistry in the field, and ionic concentrations in the groundwater near the pipe surface, may all have an effect on crack initiation and propagation.
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Csontos, Aladar A., Yi-Ming Pan, Darrell S. Dunn, Leitai Yang, and Gustavo A. Cragnolino. "Pb-Assisted Stress Corrosion Cracking Susceptibility of Alloy 22." In CORROSION 2006. NACE International, 2006. https://doi.org/10.5006/c2006-06508.

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Abstract The susceptibility of mill-annealed (MA), solution annealed (SA), and short-term thermally aged (STA) Alloy 22 and gas tungsten arc welded (GTAW) Alloy 22 to Pb-assisted stress corrosion cracking (PbSCC) is evaluated in supersaturated PbCl2 and Pb(NO3)2 solutions. Parameters varied include potential, Pb concentration, solution chemistry, and pH to evaluate the effects of Pb-bearing species on the SCC resistance of Alloy 22. Chemical speciation calculations determined the type and concentration of Pb-bearing species that may evolve during the evaporation-condensation cycles of J-13 gro
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Tachera, Diamond K., and Nicole Lautze. "INTEGRATING PRECIPITATION AND GROUNDWATER CHEMISTRY TO INTERPRET GROUNDWATER FLOW IN THE HAWAIIAN ISLANDS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300369.

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Sadawarti, Alpashi L., Shubham P. Masurkar, N. Anusha, J. Refonaa, and Ramesh Cheripelli. "Groundwater Chemistry Of Umred Taluka, Nagpur District, Maharashtra." In 2024 IEEE International Conference on Interdisciplinary Approaches in Technology and Management for Social Innovation (IATMSI). IEEE, 2024. http://dx.doi.org/10.1109/iatmsi60426.2024.10502635.

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McGibbon, Chris, Laura J. Crossey, Karl Karlstrom, and Tanner Grulke. "GROUNDWATER CONTROLS ON WATER CHEMISTRY IN THE JEMEZ RIVER." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-306143.

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Vesković, Jelena, and Antonije Onjia. "IDENTIFICATION AND ALLOCATION OF HEAVY METAL POLLUTION SOURCES IN GROUNDWATER NEAR LADJEVCI AIRPORT USING POSITIVE MATRIX FACTORIZATION RECEPTOR MODEL." In 17th International Conference on Fundamental and Applied Aspects of Physical Chemistry. Society of Physical Chemists of Serbia, 2024. https://doi.org/10.46793/phys.chem24ii.475v.

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This study investigated sources of heavy metal pollution in groundwater near Ladjevci airport in Serbia. Groundwater was collected from 42 monitoring wells and analyzed for nine heavy metals (As, Cd, Pb, Cr, Cu, Ni, Sb, Zn, and Hg). Positive matrix factorization (PMF) receptor model was utilized to identify and apportion groundwater pollution sources. The results showed that traffic and road construction-related activities, agricultural practices, and natural/geogenic processes were the three main factors affecting heavy metal concentration in groundwater. The leading cause of groundwater poll
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Liu, Wei, and Zhongjing Wang. "Groundwater Chemistry in the Badain Jaran Desert Region of China." In 2008 2nd International Conference on Bioinformatics and Biomedical Engineering (ICBBE '08). IEEE, 2008. http://dx.doi.org/10.1109/icbbe.2008.589.

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Reports on the topic "Groundwater Chemistry"

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Kerrisk, J. F. Groundwater chemistry at Yucca Mountain, Nevada, and vicinity. Office of Scientific and Technical Information (OSTI), 1987. http://dx.doi.org/10.2172/60103.

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Hurlow, Hugh A., Paul C. Inkenbrandt, and Trevor H. Schlossnagle. Hydrogeology, Groundwater Chemistry, and Water Budget of Juab Valley, Eastern Juab County, Utah. Utah Geological Survey, 2022. http://dx.doi.org/10.34191/ss-170.

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Juab Valley is a north-south-trending basin in the eastern Basin and Range Province. Juab Valley is bounded on the east by the Wasatch normal fault and the Wasatch Range and San Pitch Mountains, bounded on the west by Long Ridge and the West Hills. Juab Valley is at the southern end of Utah’s Wasatch Front, an area of projected rapid population growth and increased groundwater use. East-west-trending surface-water, groundwater, and water-rights boundaries approximately coincide along the valley’s geographic midline at Levan Ridge, an east-west trending watershed divide that separates the north
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Dyke, L. Regional groundwater and stream chemistry survey, Oak Ridges Moraine, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210858.

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Chapman, J. B., and B. F. Lyles. Groundwater chemistry at the Nevada Test Site: Data and preliminary interpretations. Office of Scientific and Technical Information (OSTI), 1993. http://dx.doi.org/10.2172/138650.

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Desbarats, A. J., and J. B. Percival. Groundwater chemistry of uranium-thorium-rare earth element deposits, Bancroft area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297779.

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Moore, G. K. Inorganic soil and groundwater chemistry near Paducah Gaseous Diffusion Plant, Paducah, Kentucky. Office of Scientific and Technical Information (OSTI), 1995. http://dx.doi.org/10.2172/196453.

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Kidder, J. A., M. B. McClenaghan, M I Leybourne, et al. Geochemical data for stream and groundwaters around the Casino Cu-Au-Mo porphyry deposit, Yukon (NTS 115 J/10 and 115 J/15). Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328862.

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This open file reports geochemical data for stream and groundwater samples collected around the Casino porphyry Cu-Au-Mo deposit, one of the largest and highest-grade deposits of its kind in Canada. The calc-alkaline porphyry is hosted in a Late Cretaceous quartz monzonite and associated breccias in the unglaciated region of west central Yukon. Water chemistry around the deposit was investigated because: (i) the deposit has not yet been disturbed by mining; (ii) the deposit was known to have metal-rich waters in local streams; and (iii) the deposit has atypically preserved ore zones. Stream wa
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Bunce, Lauren, Tim Lowenstein, and Elliot Jagniecki. Spring, River, and Lake Water Analyses from the Great Salt Lake Basin, Northern Utah. Utah Geological Survey, 2022. http://dx.doi.org/10.34191/ofr-745.

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The accompanying database is a compilation of major and minor ion chemistry data from spring, river, and lake water samples collected in and around Great Salt Lake (GSL), northern Utah. The purpose of this database is to provide an updated analysis of previously sampled spring, river, and lake water chemistries by Kirby and others (2019) (https://doi.org/10.34191/ofr-699) and to add additional locations and water chemistry of unsampled springs in the area around GSL to better understand solute load and groundwater contribution.
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Abrajano, T., J. Bates, W. Ebert, and T. Gerding. Effect of gamma radiation on groundwater chemistry and glass leaching as related to the NNWSI repository site. Office of Scientific and Technical Information (OSTI), 1986. http://dx.doi.org/10.2172/59924.

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Apps, J. A., J. T. Birkholzer, N. Spycher, et al. Groundwater Chemistry Changes as a Result of CO2 Injection at the ZERT Field Site in Bozeman, Montana. Office of Scientific and Technical Information (OSTI), 2009. http://dx.doi.org/10.2172/980778.

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