地热水库在暂时地表水注入下的水化学演变和环境影响
Jinyu Shi1, Yuesuo Yang1, Ying Lu1
1Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun, 130021, China; Jilin Provincial Key Laboratory of Water Resources and Environment, Jilin University, Changchun, 130021, China.
Journal of environmental management
|February 5, 2026
概括
将地表水注入地热水库可以提高可持续性,但可能导致矿物质缩放. 这项研究对这些影响进行了建模,揭示了不同的影响区和潜在的孔隙减少,帮助管理策略.
科学领域:
- 地热能源工程 地热能源工程
- 水文地质学 水文地质学
- 地质化学 地质化学
背景情况:
- 地热能源的扩张面临着水库压力下降带来的挑战.
- 地表水注入是一种潜在的解决方案,但其影响尚不清楚.
- 由于对注射后果的理解不足,有效的管理策略受到限制.
研究的目的:
- 开发一个多物理模型框架来模拟地热水库在地表水注入下.
- 为了分析在短暂注射后的水化学和多孔性演变.
- 识别和量化撞击区域的时空演变.
主要方法:
- 综合多物理建模框架.
- 模拟热传递,流体流动和地化学反应.
- 对暂时地表水注入对水库属性的影响进行分析.
主要成果:
- 在注入井周围确定了不同的热,液压,水化学和多孔性影响区域.
- 量化了这些冲击区的时空演变.
- 观察到矿物溶解/沉变化和碳酸盐积,可降低多孔度高达0.03%.
结论:
- 地表水注入会产生动态冲击区,影响水库的行为.
- 碳酸盐的形成对水库的多孔性和注入效率构成风险.
- 开发的框架有助于优化水源选择和注入管理,以实现可持续地热资源开发.
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