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- W2376318122 abstract "The hot mineral water from No.2 Zhougong Well in Ya'an city, Sichuan Province is located about 1800m deep down the well in karst aquifer that composed of Triassic and Permian carbonate rocks of the Leikoubo Group, Jialingjiang Group (Triassic System) and Maokou Group (Permian System). The over-burden bedrocks of the above-mentioned water-bearing strata are clastic rocks of the Jurassic and the Upper Triassic. When the measure was started and the well was sealed off, the pressure in the well is 3 Mpa, the temperature on the mouth of the well is 75℃, the rate of flow from the well is 5000t/d. Through the measure to the hot mineral water in the well by means of 14 C and U methods, and sampling and analysis to the surface water around the nearby mountains, it is proved that the hot mineral water in No.2 Zhougong well is formed by precipitation, the recharge water probably comes from the mountains to the west and southwest, i.e. the Xingjinghe, Xinghe, Lengshuihe and Zhougonghe river basins, where the altitude is about 1500～2500m above sea level. Water in the upper part of the basin mainly exists in porosities in Quaternary deposit and Jurassic sandstone and conglomerate. But the hot mineral water in the deeper part of the basin comes from the bottom of the basin after deep circulation from precipitation to faults, fractures and karst conduits, and to the bottom in the end. So, there is no hydraulic links between the water in the upper part of the basin and the hot water in the well." @default.
- W2376318122 created "2016-06-24" @default.
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- W2376318122 date "2002-01-01" @default.
- W2376318122 modified "2023-09-28" @default.
- W2376318122 title "PRELIMINARY STUDY ON ENVIRONMENTAL ISOTOPES IN HOT MINERAL WATER FROM NO.2 ZHOUGONG WELL IN YA'AN CITY, SICHUAN PROVINCE" @default.
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