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Geochemical evolution of groundwater in carbonate aquifers in Taiyuan, northern China |
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| Authors: | Rui Ma Yanxin WangZiyong Sun Chunmiao ZhengTeng Ma Henning Prommer |
| Institution: | a School of Environmental Studies & MOE Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, 430074 Wuhan, PR China b Department of Geological Sciences, The University of Alabama, Tuscaloosa, AL 35487, United States c CSIRO Land and Water, Floreat, Australia d School of Earth and Environment, University of Western Australia, Crawley, Western Australia, Australia |
| Abstract: | Thirty-nine samples of both cold and thermal karst groundwater from Taiyuan, northern China were collected and analyzed with the aim of developing a better understanding of the geochemical processes that control the groundwater quality evolution in the region’s carbonate aquifers. The region’s karst groundwater system was divided into three geologically distinct sub-systems, namely, the Xishan Mountain karst groundwater subsystem (XMK), the Dongshan Mountain karst groundwater subsystem (DMK) and the Beishan Mountain karst groundwater subsystem (BMK). Hydrochemical properties of the karst groundwaters evolve from the recharge zones towards the cold water discharge zones and further towards the thermal water discharge zones. In the XMK and the DMK, the hydrochemical type of the groundwater evolves from HCO3-Ca·Mg in the recharge - flow-through zone, to HCO3·SO4-Ca·Mg/SO4·HCO3-Ca·Mg in the cold water discharge zone, and further to SO4-Ca·Mg in the thermal water discharge zone. By contrast, the water type changes from HCO3-Ca·Mg to HCO3·SO4-Ca·Mg in the BMK, with almost invariable TDS and temperatures all along from the recharge to the discharge zone. The concentrations of Sr, Si, Fe, F− and of some trace elements (Al, B, Li, Mn, Mo, Co, Ni) increase as groundwater temperature increases. Different hydrogeochemical processes occur in the three karst groundwater sub-systems. In the XMK and the DMK, the geochemical evolution of the groundwater is jointly controlled by carbonate dissolution/precipitation, gypsum dissolution and dedolomitization, while only calcite and dolomite dissolution/precipitation occurs in the BMK without dedolomitization. The hydrogeochemical data of the karst groundwaters were used to construct individual geochemical reaction models for each of the three different karst groundwater sub-systems. The modeling results confirm that dedolomization is the major process controlling hydrochemical changes in the XMK and the DMK. In the thermal groundwaters, the dissolution rates of fluorite, siderite and strontianite were found to exceed those of the cold karst groundwater systems, which can explain the higher concentrations of F−, Fe and Sr2+ that are found in these waters. |
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