科威特北部地下水系统中硫酸盐的来源和演变
Fawzia Al-Ruwaih1, Amjad Aliewi2, Chidambaram Sabarathinam2
1Department of Earth and Environmental Sciences, Kuwait University, Kuwait City, Kuwait.
Environmental monitoring and assessment
|July 8, 2025
概括
在科威特,硫酸盐含量很高.
科学领域:
- 水文地质学 水文地质学
- 环境科学 环境科学
- 地质化学 地质化学
背景情况:
- 科威特灌水中的硫酸盐度增加威胁到作物健康.
- 科威特的性含水层面临高硫酸盐水平的风险,影响农业的可行性.
研究的目的:
- 调查和解决科威特北部古拉斯性含水层中硫酸盐度升高的问题.
- 了解控制硫酸盐水平的地球化学过程及其对地下水质量的影响.
主要方法:
- 采用数值建模和地球化学技术来分析地下水.
- 进行地质化学分析以确定离子丰度和硫酸盐度.
- 利用数值模拟来建模地下水化学驱动因素.
主要成果:
- 科威特北部的地下水是性的,主要有Na+和Cl−的离子.
- 硫酸盐度在1200至3865毫克/升之间,在农业区附近最高.
- 人类影响,硫化物氧化和矿物气候变化导致硫酸盐水平高.
- 数字模拟证实了矿物溶解,离子交换和人为因素驱动地下水化学.
结论:
- 高硫酸盐水平对地下水用于灌和消费的可用性构成重大风险.
- 可持续的水资源管理实践对于解决科威特北部的硫酸盐污染至关重要.
- 这些发现为管理含水层水质提供了必要的指导.
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