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Variation of nitrate concentration in karst cave water and its sources and estimation |
SU Dan1,2, ZHOU Zhong-fa1,2, GONG Xiao-huan1,2, DING Sheng-jun1,2, DONG Hui1,2, YAN Li-hui1,2, XIONG Yong1,2 |
1. College of Geography and Environmental Science/Karst Research Institute, Guizhou Normal University, Guiyang 550001, China; 2. State Key Laboratory Breeding Base of Karst Mountain Ecological Environment in Guizhou Province, Guiyang 550001, China |
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Abstract Nitrate (NO3-) pollution of groundwater caused by anthropogenic activities has become a significant environmental problem with global concern. Accurate identification of mixing sources of NO3- pollution in aquatic environments is the key to controlling NO3- input and improving water quality. To clarify the distribution of NO3- in karst cave water, this paper selects Mahuang Cave as the research object. A comprehensive analysis of the cave hydrochemistry, the variation characteristics and sources of NO3- and the biogeochemical processes by using the hydrochemical methods and stable isotope values, the results showed that the pH of the water was 8.36 on average, and the main anions and cations were mainly HCO3-, Ca2+ and Mg2+, respectively. The hydrochemical type was Ca·Mg-HCO3 type, and the water was weakly alkaline. The δD-H2O and δ18O-H2O values were distributed near the local atmospheric precipitation line equation, indicating that atmospheric precipitation was the primary source of cave water recharge. The seasonal variation of NO3-concentration in the water was stable, with average values of 13.46mg/L and 13.93mg/L in the dry and wet seasons, respectively. The water quality met the class II water standard (in terms of N). The ratio of [NO3-] and [Cl-] and the isotopic values of NO3- indicated that fertilizer, soil N, manure&sewage, and atmospheric deposition were the mixing sources of NO3- in water. The process of NO3- conversion in water was dominated by microbial nitrification, and no significant denitrification occurred. The results estimated from the SIAR model showed that the average contribution rates of mixing pollution sources to the NO3-content in water during dry and wet seasons were CF(55%), SN(24%), M&S(12%), AD(8%), and CF (52%), SN (24%), M&S (19%), AD (5%), respectively, where CF and SN were the mainly contributing sources of nitrate concentration in the study area, followed by M&S and AD.
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Received: 06 April 2023
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