2014
DOI: 10.7857/jsge.2014.19.2.007
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Chemical Characteristics of Groundwater in Carbonate Rock Areas of Korea

Abstract: This study was conducted to understand the chemical characteristics of groundwater in carbonate areas of Korea. In this study, data on pH, electric conductivity (EC), Ca , and HCO 3 − were collected from 97 wells which were installed in various carbonate rock regions of Korea. The pH values ranged from 5.7 to 9.9, and the average value was 7.3. The concentration range showed differences between the maximum value of HCO , and HCO 3 − might be not only water-rock interactions, but also irrigation return flow, be… Show more

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Cited by 6 publications
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“…The order of their abundance is SO 4 2-> Cl ->HCO 3 -, contributing on average, 34.51, 33.71 and 31.78% of the total anions, respectively. If halite dissolution is responsible for sodium, Na/Cl ratio should be approximately equal to 1, whereas ratio greater than 1 is typically interpreted as Na released from silicate weathering reaction (Meyback, 1987;Kabir et al, 2014;Pazand, 2020). In the present study, Samples (except number 60) having Na/Cl ratio greater than 1 (Figure 3) hence silicate weathering was the probable source of sodium.…”
Section: Chemical Characteristics Of Groundwatermentioning
confidence: 55%
“…The order of their abundance is SO 4 2-> Cl ->HCO 3 -, contributing on average, 34.51, 33.71 and 31.78% of the total anions, respectively. If halite dissolution is responsible for sodium, Na/Cl ratio should be approximately equal to 1, whereas ratio greater than 1 is typically interpreted as Na released from silicate weathering reaction (Meyback, 1987;Kabir et al, 2014;Pazand, 2020). In the present study, Samples (except number 60) having Na/Cl ratio greater than 1 (Figure 3) hence silicate weathering was the probable source of sodium.…”
Section: Chemical Characteristics Of Groundwatermentioning
confidence: 55%