Hydrochemistry of hot springs in geothermal fields of central, northern, and northeastern Taiwan: implication on occurrence and enrichment of arsenic

Jean, Jiin-Shuh; Liao, Libing; Kar, Saibal; Liu, Chia Chuan; Li, Zhaohui

doi:10.1007/s12665-016-6128-x

Cited by 4 publications

(1 citation statement)

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“…Considering the high capacity of the aquifer in the anticline plunge, such qualitative changes occurred in this part of the aquifer posed major challenges to supplying the city's drinking water. Given the necessity of water supply for the region, analyses of hydrochemical parameters, geochemical processes, reference ion ratios (Cartwright et al 2006;Hounslow 1995;Jean et al 2016;Mahmoudi et al 2017;Sarikhani et al 2015;Whittemore and Pollock 1979) graphs of salinity source (Richter and Kreitler 1991) and TOC (Spruill 1988) were performed to investigate the causes of quality changes and also the origin of salinity.…”

Section: Introductionmentioning

confidence: 99%

Investigation of Hydrochemical Parameters of Water Resources in Kamarderaz Anticline Plunge in the Southwest of IRAN

Aranki

asl

Vardanjani

2021

Preprint

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Changes in the quality of karstic water resources affected by the proximity to sources of salinity such as evaporate formations and oil brine pose major challenges to such water resources, especially in Khuzestan province, Iran. The karstic water resources of the Kamarderaz anticline plunge in Izeh city in Khuzestan province have hampered water supply management in the region. To determine water quality and the causes of water salinity in the study area, the hydrochemical parameters of the existing water resources were accordingly evaluated. To conduct hydrochemical studies, 21 samples were collected from different water sources of Kamarderaz anticline plunge in 2017–2018. To analyze the garnered data, Piper and Durov diagrams, composite graphs, ion exchange graphs, ion correlation diagrams, salinity source diagrams and ion ratios were used. The results showed that SO42−, Cl−, and Ca2+ in the water resources of the study area were likely due to several sources including carbonate minerals, gypsum dissolution, anhydrite, halite as well as oil brine. Besides, Br/Cl, I/Cl ion ratios as well as Br-Cl and SO4-Cl diagrams revealed the mixing of karstic freshwater with oil brine in the region. The result of TOC analysis also showed that hydrocarbon materials were present in the well of Atabaki (WT). Moreover, elemental sulfur and sulfur isotope analysis showed that the process of thermochemical sulfate reduction or bacterial sulfate reduction in the presence of hydrocarbons produced H2S gas, and eventually penetrated the WT and WH1.

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