| 天水及其南北地区地热水水化学特征及起源 |
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| 引用本文： | 温煜华,王乃昂,朱锡芬,张华安,马宏伟,陈立.天水及其南北地区地热水水化学特征及起源[J].地理科学,2011,31(6):668-673. |
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| 作者姓名： | 温煜华 王乃昂 朱锡芬 张华安 马宏伟 陈立 |
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| 作者单位： | 兰州大学资源环境学院 兰州大学干旱区水循环与水资源研究中心, 甘肃 兰州 730000 |
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| 基金项目： | 国家自然科学基金项目(50879033)资助 |
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| 摘 要： | 运用水化学和同位素示踪的原理追溯地热水的水岩相互作用和起源,得出武山和天水地热水为pH较高(7.94~9.06)的低TDS(226~255 mg/L)HCO3型水,通渭和清水地热水为pH较低(7.1~8.07)的较高TDS(915~1 793 mg/L)SO4型水,地热水的水化学特征主要受不同的围岩及与围岩相互作用的程度所控制。地热水的δD和δ18O值说明地热水起源于大气降水,且未受水-岩同位素交换明显影响。综合应用各种地热温标,估算地热水的热储温度为70~111℃,属于中低温地热资源。对年均降雨量约500 mm的天水及其南北地区,应采取采、停交替的地热水利用方式。
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| 关 键 词： | 天水及南北地区 水化学 同位素 地热温标 |
| 收稿时间： | 2010-09-04 |
| 修稿时间： | 2010-12-08 |
Hydrochemistry of Geothermal Water in Tianshui and Its Northern-southern Area |
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| WEN Yu-hua,WANG Nai-ang,ZHU Xi-fen,ZHANG Hua-an,MA Hong-wei,CHEN Li.Hydrochemistry of Geothermal Water in Tianshui and Its Northern-southern Area[J].Scientia Geographica Sinica,2011,31(6):668-673. |
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| Authors: | WEN Yu-hua WANG Nai-ang ZHU Xi-fen ZHANG Hua-an MA Hong-wei CHEN Li |
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| Institution: | College of Earth and Environmental Science, Center for Hydrologic Cycle and Water Resources in Arid Region, Lanzhou University, Lanzhou, Gansu 730000, China |
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| Abstract: | A geochemical study of geothermal water has been carried out in the Tianshui and its northern-southern area.Geothermal water of Wushan and Tianshui is bicarbonate water of low salinity characterized by pH in 7.94-9.06 and low total dissolved solids(TDS)(226-255 mg/L),which were probably formed by water-rock interaction between meteoric rain,biotite plagioclase gneiss rock and carbonate sediment in reservior.While geothermal water of Tongwei and Qingshui is sulfate water with characteristics of pH in 7.1-8.0... |
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| Keywords: | Tianshui and northern-southern area hydrochemistry isotope geothemometry |
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