攀西裂谷红格温泉水文地球化学特征及地热成因

Hydro-geochemistry and Geothermal Genesis of Hongge Hot Spring in Panxi Rift

  • 摘要: 通过对红格温泉地区地下水水质及水文地球化学特征分析,结合温泉水文地质条件,探讨温泉地热成因。测试结果表明,红格温泉地热水为Na-Cl·SO4·HCO3型水,红格地区冷泉井水为Ca·Mg-HCO3型水。研究区内的碳酸盐岩、硅酸盐岩和硫酸盐岩矿物的溶解和沉淀制约了地下水中化学组分的主要特征。用三种地热温标公式分别进行计算:Na-K温标计算得热储温度为211℃,K-Mg温标计算得热储温度为72℃,而Si O2温标计算得热储温度为114℃。地下水样品氢氧同位素测试结果显示:地热水的δ2H值为-104.99‰~-103.11‰,δ18O值为-13.14‰~-13.02‰;冷泉水的δ2H值为-89.10‰~-87.87‰,δ18O值为-11.70‰~-11.56‰;冷井水的δ2H值为-86.01‰~-84.76‰,δ18O值为-11.39‰~-10.96‰。从研究区水文地质条件看,昔格达断裂为红格温泉的控热、控水、导水构造。活动断裂摩擦热、地壳岩石放射性生热和地幔来源的热能组成主要热源,大气降水为主要的地下水补给来源,其地热水循环深度可达6.4 km。地热水沿断裂破碎带上升,与碳酸盐岩地层丰富的岩溶水混合并进行热交换,同时发生化学反应后形成Na-Cl·SO4·HCO3型地下水。研究区地下水赋存丰富,水热资源潜力巨大,建议深入开展地热资源系统调查,保障地下水资源安全,保护生态环境,实现地热资源可持续开发利用。

     

    Abstract: Based on the analysis of groundwater quality and hydro-geochemistry of Hongge area,this paper discussed the geothermal genesis of the hot spring combining its hydro-geological conditions.It showed that the type of Hongge Hot Spring groundwater was Na-Cl·SO4·HCO3,and the groundwater of cold springs and wells in the Hongge area belonged to Ca·Mg-HCO3.The dissolution and precipitation of carbonate,silicate and sulfate minerals in the study area restricted the main characteristics of the chemical composition in groundwater.Three kinds of geothermometer were used to calculate the reservoir temperatures respectively:Na-K geothermometer calculated the reservoir temperature of 211℃,K-Mg geothermometer calculated 72℃,and Si O2 geothermometer calculated 114℃.The δ2H values of hot spring groundwater were-104.99‰~-103.11‰,and the δ18O values were-13.14‰~-13.02‰.The δ2H values of cold spring groundwater were 89.10‰~87.87‰,and the δ18O values were 11.70‰~11.56‰.Theδ2H values of cold well groundwater values were 86.01‰~84.76‰,and the δ18O values were 11.39‰~10.96‰.According to the hydrogeological conditions of the study area,the Xigeda fault was a heat-controlling,water-controlling and water-conducting structure of Hongge Hot Spring.The main heat source consisted of friction heat from active faults,radioactive heat generated from crustal rocks and heat from mantle.The atmospheric precipitation was the main source of groundwater recharge,and the depth of geothermal water circulation can reach 6.4 km.Geothermal water rised along fracture zone,mixed with abundant karst water in carbonate strata,and exchanged heat.At the same time,Na-Cl·SO4·HCO3 type groundwater was formed after chemical reaction.The study area was rich in groundwater and had huge potential for geothermal resources.It was suggested to carry out in-depth systematic investigation of geothermal resources to ensure the safety of groundwater resources,to protect the ecological environment and realize sustainable development and utilization of geothermal resources.

     

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