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1. 中国地质大学(北京)地球科学与资源学院
2. 宁夏回族自治区地球物理地球化学调查院(自治区深地探测中心)
3. 中国冶金地质总局西北局五队
4. 长江大学资源与环境学院
Published:2026
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曹园园, 虎新军, 倪萍, et al. 银川盆地地热水成因机制:来自水化学和同位素的约束[J]. Bulletin of Geological Science and Technology, 2026, 45(3): 287-302.
曹园园, 虎新军, 倪萍, et al. 银川盆地地热水成因机制:来自水化学和同位素的约束[J]. Bulletin of Geological Science and Technology, 2026, 45(3): 287-302. DOI: 10.19509/j.cnki.dzkq.tb20250032.
地热资源具有可再生、能源利用效率高和节能减排等显著优势,是推动能源转型、实现“双碳”目标的重要可再生能源类型。银川盆地地热储量丰富,但因缺乏系统的水文地球化学与同位素研究,其地热水成因机制尚未明确,开发利用也缺乏科学规划与统一管理,不仅导致地热资源开发利用进程缓慢,还严重阻碍了当地经济的绿色快速发展。以银川盆地典型地热井水样为研究对象,将其按区域划分为西部、中部和东部3组,同步采集研究区深层地下冷水样品作为对照,结合区域地质构造背景,通过系统分析测试地热水与地下冷水的水化学、同位素特征,深入探讨了研究区地热水的地球化学起源、径流循环过程、热源类型,并全面剖析了地热系统的成因机制。研究发现,该区域地热水化学类型主要为Cl-Na型和Cl·SO
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-Na型;氢氧同位素特征显示,地热水补给来源以大气降水为主,补给高程在1 616~2 964 m;水化学特征结合氯、锶、硫同位素指示,地热水物质来源主要为高温条件下的水-岩相互作用、岩盐溶解及古沉积水输入。研究区地热水热储温度为78.9~109.2℃,循环深度为3 455.4~24 794.0 m;离子比例系数和
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C测年结果表明,与西部、东部地热水相比,中部地热水的水化学组分含量最高,循环周期最长,循环深度也最深。通过地热水水化学特征分析及花岗岩生热率定量计算得出,研究区地热系统的热源主要为大地热流加热。本研究明确了银川盆地地热资源的关键水文地球化学特征与成因机制,建立了地热系统成因概念模型,为后续科学合理开发利用该地热资源、推动当地经济绿色高质量发展提供了重要的理论与实践依据。
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