| 邢东地热水的化学特征、起源及利用 |
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| 引用本文： | 谢明忠. 邢东地热水的化学特征、起源及利用[J]. 中国煤田地质, 2005, 17(5): 50-51,57 |
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| 作者姓名： | 谢明忠 |
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| 作者单位： | 河北省煤田地质局,河北邢台054022 |
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| 摘 要： | 根据位于河北邢台东部太行山前大断裂东侧的金地热1号井的水质化验资料和测温资料,邢东地热水为镭、硅、氟、硫酸钙钠型高热复合矿水,具有较好的医疗价值,为核试验之前降水而成;地热温度随埋藏深度而自然增高（埋深2 900m时,井温89.9℃）,其地热类型属于盆地型中低温地热资源.
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| 关 键 词： | 热矿水 奥陶系 热储 酸性硫酸水 邢台东部 |
| 文章编号： | 1004-9177（2005）05-0050-02 |
| 收稿时间： | 2005-06-13 |
| 修稿时间： | 2005-06-13 |
Chemical Character, Origin and Use of Geothermal Water in eastern Xingtai |
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| Xie Mingzhong. Chemical Character, Origin and Use of Geothermal Water in eastern Xingtai[J]. Coal Geology of China, 2005, 17(5): 50-51,57 |
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| Authors: | Xie Mingzhong |
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| Affiliation: | Hebei Bureau of Coal Geology, Xingtai, Hebei 054022 |
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| Abstract: | According to water quality testing and temperature measuring data from JDR No.1 well located at east side of Taihang Mts.piedmont major fault in eastern Xingtai,Hebei,the geothermal water is radium,silicone,fluorine SO4-Ca,Na,type high temperature composite mineral water.The water has preferable medical value;it was formed before nuclear tests.Geothermal temperature is rising along with the deepening of the depth(well temperature is 89.9oC when it is 2900m in depth),belongs to basin type medium to low temperature geothermal resource. |
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| Keywords: | hot mineral water Ordovician System geothermal resrvoir acidic sulphate water eastern Xingtai |
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