| 川西阿坝州壤古温泉成因机制研究：来自水文地球化学和地球物理勘探的证据 |
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| 引用本文： | 章旭, 张文, 吕国森, 余中友, 代倩. 2023. 川西阿坝州壤古温泉成因机制研究：来自水文地球化学和地球物理勘探的证据. 沉积与特提斯地质, 43(2): 388-403. doi: 10.19826/j.cnki.1009-3850.2023.04007 |
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| 作者姓名： | 章旭 张文 吕国森 余中友 代倩 |
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| 作者单位： | 1.四川省华地建设工程有限责任公司，四川 成都 610081; 2.成都水文地质工程地质中心，四川 成都 610081; 3.自然资源部地质灾害风险防控工程技术创新中心，四川 成都 611730; 4.中国地质科学院探矿工艺研究所，四川 成都 611734; 5.西南交通大学，四川 成都 611756 |
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| 基金项目： | 国家自然科学基金（42072313，42102334），四川省科技厅项目（2022NSFSC1084, 2022NSFSC0413, 2023YFS0356）, 四川省自然资源厅科研项目经费资助（KJ-2023-36），西南交通大学培育项目（2682021ZTPY063, 2682022ZTPY064） |
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| 摘 要： | 地热资源是一种清洁低碳、储量丰富、安全优质的可再生能源，大力开发利用地热资源，对落实“碳达峰、碳中和”战略目标具有重要意义。壤古温泉位于青藏高原东南缘川西阿坝州壤塘县，为松潘-甘孜褶皱带地热资源空白区钻获的优质地热资源，井口水温39.5℃，自流流量1500 m3/d，属富含偏硅酸、偏硼酸、锶的氟、锂优质热矿水，具有极高的医疗价值。文章以壤古温泉为研究对象，通过水文地球化学、地球物理特征研究，探讨了地热形成机制。结果表明：壤古温泉pH值6.7～7.1，溶解性总固体2050~2760 mg/L，水化学类型为HCO3-Na型，水岩作用强烈。其氢氧同位素分布于全球大气降水方程线附近，说明热水主要为大气降水补给。Na-K-Mg平衡图表现为未成熟水，表明热水受裂隙潜水或地表冷水强烈混合作用。基于传统地热温标、硅焓混合模型、Cl−校正估算热储温度为138~183.3℃，冷水混合比例为77.9~84.3%。综合地球物理勘探、钻探揭露特征，本文构建了壤古温泉成因概念模型，可为壤古温泉的开发利用提供理论支撑。
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| 关 键 词： | 壤古温泉 水文地球化学 地球物理勘探 氢氧同位素 成因模式 |
| 收稿时间： | 2023-01-12 |
| 修稿时间： | 2023-03-03 |
Geochemical, Geophysical Genesis of the Ranggu Geothermal Spring in Aba Prefecture, Western Sichuan: Evidence from Hydrogeochemical and Geophysical Exploration |
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| ZHANG Xu, ZHANG Wen, LÜ Guosen, YU Zhongyou, DAI Qian. 2023. Geochemical, Geophysical Genesis of the Ranggu Geothermal Spring in Aba Prefecture, Western Sichuan: Evidence from Hydrogeochemical and Geophysical Exploration. Sedimentary Geology and Tethyan Geology, 43(2): 388-403. doi: 10.19826/j.cnki.1009-3850.2023.04007 |
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| Authors: | ZHANG Xu ZHANG Wen LÜ Guosen YU Zhongyou DAI Qian |
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| Affiliation: | 1.Sichuan Huadi Construction Engineering Co.Ltd.,Chengdu 610081,China; 2.Chengdu Center of Hydrogeology & Engineering Geology,Chengdu 610081,China; 3.Technology Innovation Center for Risk Prevention and Mitigation of Geohazard,Ministry of Natural Resources,Chengdu 611730,China; 4.Institute of Exploration Technology,Chinese Academy of Geological Sciences,Chengdu 611734,China; 5.Southwest Jiaotong University,Chengdu 611756,China |
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| Abstract: | Geothermal resource is a clean, low-carbon, abundant, safe and high-quality renewable energy. Vigorously developing and utilizing geothermal resources is of great significance to the implementation of the strategic goal of "carbon peak, carbon neutral". Located in Rangtang County, Aba Prefecture, western Sichuan on the southeast edge of the Qinghai-Tibet Plateau, Ranggu geothermal spring is a high-quality geothermal resource drilled in the geothermal resource blank area of the Songpan-Ganzi fold zone. The wellhead water temperature is 39.5℃, and the artesian flow is 1500 m3/d. It is a high-quality thermal mineral water rich in metasilicic acid, metaborate, strontium, fluorine and lithium, and has high medical value. Based on the study of hydrogeochemical and geophysical characteristics, the paper discusses the formation mechanism of geothermal energy. The results show that the pH value of the spring is 6.7~7.1, the total dissolved solids are 2050~2760 mg/L, the hydrochemical type is HCO3-Na, and the water-rock interaction is intense. Its hydrogen and oxygen isotopes are distributed near the global atmospheric precipitation equation line, indicating that geothermal water is mainly recharged by atmospheric precipitation. The Na-K-Mg balance diagram shows immature water, indicating that the geothermal water is intensely mixed by fissure phreatic water or surface cold water. Based on the traditional geothermal temperature scale, silicon enthalpy mixing model and Cl− correction, it is estimated that the reservoir temperature is 138~183.3℃, and the mixing ratio of cold water is 77.9~84.3%. Based on the characteristics of geophysical exploration and drilling exposure, a conceptual model of the genesis of the Ranggu geothermal spring is constructed in this paper, which can provide theoretical support for the development and utilization of the Ranggu geothermal spring. |
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| Keywords: | Ranggu geothermal spring hydrochemistry geophysical prospecting hydrogen and oxygen isotopes genetic model |
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