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2020 Vol. 47, No. 6
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XU Hongfei, ZHOU Xun, WANG Mengmeng, LIU Yu, WU Yanqiu, ZHUO Linyang. 2020. Characteristics and origin of the Denggeng and Mabu hot spring in Lushui County, Yunnan Province[J]. Geology in China, 47(6): 1739-1754. doi: 10.12029/gc20200611
Citation: XU Hongfei, ZHOU Xun, WANG Mengmeng, LIU Yu, WU Yanqiu, ZHUO Linyang. 2020. Characteristics and origin of the Denggeng and Mabu hot spring in Lushui County, Yunnan Province[J]. Geology in China, 47(6): 1739-1754. doi: 10.12029/gc20200611
shu

Characteristics and origin of the Denggeng and Mabu hot spring in Lushui County, Yunnan Province

  • 1.

    School of Water Resources and Environment, China University of Geosciences(Beijing), Beijing 100083, China

  • 2.

    MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences(Beijing), Beijing 100083, China

    • Fund Project: Supported by National Natural Science Foundation of China (No. 41772261)
More Information
  • Author Bio: XU Hongfei, male, born in 1995, master, mainly engages in hydrogeology research; E- mail:1468017872@qq.com
  • Corresponding author: ZHOU Xun, male, born in 1963, professor, supervisor of doctor candidates, mainly engages in coastal groundwater, geothermal water(hot spring), underground brine(salt spring), mineral water and circulation and simulation of groundwater research; E-mail:zhouxun@cugb.edu.cn 
Received Date:  21 October 2019
Revised Date:  19 October 2020
Publish Date:  25 December 2020
    Abstract

  • Located in the Lushui County of Yunnan Province,the Denggeng hot spring and the Mabu hot spring emerge on the western bank of the Nujiang River valley. Sand of the Quaternary (Q42),basalt of the Upper Carboniferous Woniusi Group (C3w) and limestone of the Lower Formation of Triassic Hewan Group (T2h1) underlie the study area. The temperature of hot springs range from 48.9 to 69.6℃,and TDS from 0.493 to 0.782 g/L. The hydrochemical types of hot water are of HCO3·Ca-Mg type and HCO3·Ca-Na type. The hot springs are of low to moderate temperature and weak acid. The F- concentrations of the hot springs range from 0.78 to 2.13 mg/L,and the H2SiO3 concentrations from 41.0 to 70.2 mg/L. Li,Sr,Rb,Cs and Ba are relatively abundant in the hot water. The values of δ2H and δ18O of the spring water indicate that the hot springs in the study area are meteoric in origin. The elevation of the hot spring's recharge area is estimated to be from 1260 to 1435 m,the temperature of the recharge area varies in the range of 6.18-9.02℃,and the temperature of the geothermal reservoirs varies in the range of 100 -127.5℃. The content of Ca2+ and HCO3- in hot water is rich,and the percentages of milliequivalent concentrations of anions and cations are high,accounting for more than 60% and 82% respectively. Calcite and aragonite in the hot water are in the saturated state,the content of CO2 in water is high and the pCO2 in the hot water is much higher than atmospheric pCO2. The hydrochemical and hydrodynamic conditions are favorable to CaCO3 deposition. Travertines are precipitating near YLS3-1,YLS3-3 and YLS3-4 of the Denggeng hot spring and YLS4-1 of the Mabu hot spring. Thermal groundwater rises up to the land surface on the western bank of the Nujiang River valley after groundwater receives recharge from infiltration of precipitation in the recharge areas of the mountainous areas to the west of the Nujiang River,undergoes deep circulation and obtains heat from heat flow. The hot springs are of the deep infiltration-cycle type and are of low to moderate temperature. The hot water mixes with the shallow cold water when it rises to the land surface. The proportion of mixing cold water is about 60%-73%,and the circulation depth of the hot water ranges from 2375.2 to 3161.7 m.

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