Abstract
Compositions of deuterium and 18O isotopes of 90 representative samples indicate that thermal groundwater in most parts of China is meteoric in origin. Latitude, altitude, and continent effects have significant bearing on the values of δD and δ18O of the hot water samples. Oxygen-18 shift is not significant in most of the thermal groundwater, especially the hot water of low-to-moderate temperature. Slight oxygen-18 shift is only found in some hot springs of high temperature in Tibet and western Yunnan and in thermal groundwater of low-to-moderate temperature in the deep-seated carbonate aquifers in the northern North China Plain (including the Tianjin area). Near-surface boiling may causes the shift of the former and the latter may be attributed to exchange of oxygen-18 between water and carbonates in the geothermal systems of taphrogenic basin-type. Hot springs in Tibet and western Sichuan have very low contents of δD and δ18O, possibly due to recharge of precipitation and snow-melting water of extremely depleted δD and δ18O values at high latitudes of several thousands of meters.
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Acknowledgments
This work was cooperatively supported by the National Natural Science Foundation of China (40572147), the Beijing Natural Science Foundation (8083030, 8042019) and the Key Project of Science and Technology from the Ministry of Education of China (No. 02026). Thanks are given to Zhang Hua, Shen Ye, Zhao Liang, Wang Wei, Yu Yuan, Fan Youli, Yang Yanyan, Chai Rui, Liu Chunhui, Yu Lan, Dai Weiyu, Liu Yongtao, Liu Yaping, Deng Zijuan and Miao Huishuai for their help in the work.
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Xun, Z., Bin, F., Haiyan, Z. et al. Isotopes of deuterium and oxygen-18 in thermal groundwater in China. Environ Geol 57, 1807–1814 (2009). https://doi.org/10.1007/s00254-008-1468-9
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DOI: https://doi.org/10.1007/s00254-008-1468-9