地质化学特征及其空间变化在邻科威特主要油田的地下水中
Chidambaram Sabarathinam1, Mohamed Al-Senafy2, Ali Asker3
1Water Research Center, Kuwait Institute for Scientific Research, Safat, Kuwait City, Kuwait. csabarathinam@kisr.edu.kw.
Environmental monitoring and assessment
|April 24, 2025
概括
科威特的地下水 科威特的地下水
科学领域:
- 水地地化学 水地地化学
- 环境科学 环境科学
- 地质化学 地质化学
背景情况:
- 科威特的地下水依赖于两个主要的含水层:较年轻的科威特含水层和较旧的Dammam形成.
- 这些含水层的地下水是盐水到盐水,在油田附近存在潜在的污染风险.
研究的目的:
- 分析科威特主要油田地下水的地化学特性.
- 确定控制地下水化学和盐度的过程.
主要方法:
- 从三个油田 (北方,东南,西部) 收集了地下水样本.
- 使用了地化学特征,矿物和指数和统计分析 (主要成分分析).
主要成果:
- 硫酸盐和酸盐是所有地区的主导离子.
- 确定了不同的水类型:Na-Cl-SO4 (北),Na-Ca-Cl (东南) 和Na-Ca-Mg-Cl-SO4 (西).
- 矿物溶解 (多洛米特,石膏,酸盐) 和微生物过程显著影响了地下水化学.
结论:
- 地质化学变化归因于石质学,地下水的盐度和普遍存在的物理化学条件.
- 来自含水层矩阵的离子溶解,酸盐气候变化和化是关键过程.
- 具体的矿物溶液 (碳酸盐,化物,硫酸盐,酸盐) 根据地区而异.
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