| 绵竹三箭水S1井温泉补给源的同位素示踪研究 |
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| 引用本文： | 徐进勇,王多义,尹观.绵竹三箭水S1井温泉补给源的同位素示踪研究[J].矿物岩石,2003,23(2):75-78. |
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| 作者姓名： | 徐进勇 王多义 尹观 |
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| 作者单位： | 1. 成都理工大学,四川,成都,610059;四川省地学核技术重点实验室,四川,成都,610059
2. 成都理工大学,四川,成都,610059 |
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| 摘 要： | 根据绵竹三箭水S1井相关地质区域内各水体的氢、氧同位素组成和放射性同位素氚浓度,结合该区的地质背景,利用同位素示踪手段,基本确定该井温泉地下水的成因为大气降水渗入补给主体含水层补给源在西北部1700m左右的“彭灌杂岩”高山区一带、补给量相对稳定,水温不会有大波动,有远期开发价值。
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| 关 键 词： | 温泉 大气降水 同位素示踪 氧同位素 氢同位素 地下水 成因 渗入补给 |
| 文章编号： | 1001-6872(2003)02-0075-04 |
| 修稿时间： | 2002年9月17日 |
ISOTOPIC TRACER OF THERMAL SPRING OF S1 WELL AT SANJIAN,MIANZHU |
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| XU Jin-yong ,WANG Duo-yi ,YIN Guan .Chengdu University of Technology,Chengdu ,China, .Applied Nuclear Technigues in Geosciences Key Laboratory of Sichuan Province,Chengdu ,China.ISOTOPIC TRACER OF THERMAL SPRING OF S1 WELL AT SANJIAN,MIANZHU[J].Journal of Mineralogy and Petrology,2003,23(2):75-78. |
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| Authors: | XU Jin-yong WANG Duo-yi YIN Guan Chengdu University of Technology Chengdu China Applied Nuclear Technigues in Geosciences Key Laboratory of Sichuan Province Chengdu China |
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| Institution: | XU Jin-yong 1,2,WANG Duo-yi 1,YIN Guan 1 1.Chengdu University of Technology,Chengdu 610059,China, 2.Applied Nuclear Technigues in Geosciences Key Laboratory of Sichuan Province,Chengdu 610059,China |
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| Abstract: | Based on the hydrogen and oxygen isotope compositions and radioactive isotope-tritium concentration of the water body of S1 well and its related geological background in Mianzhu,we could determine the contributing factor of thermal spring by using isotope tracer technique.S1 well is mainly caused by meteoric water recharging andthe recharge resource of the main aquifer is in the north-west "Pengguan complex" with an altitude of 1 700 metre or so.The amount of recharge is steady and the temperature is not fluctuated.So the S1 well have the value of long-term exploitation. |
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| Keywords: | hot spring meteric water isotope tracer |
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