用多变量统计分析和逆地化学建模来识别浅地下水中的水地化学过程
Nan Liu1, Meng Chen2,3,4, Dongdong Gao5
1College of Environmental Science and Engineering, Guilin University of Technology, Guilin, 541006, China.
Environmental monitoring and assessment
|January 6, 2025
概括
德阳市平原的地下水化学演变是由水岩相互作用和人类活动塑造的. 了解这些过程对于可持续的地下水管理和资源安全至关重要.
科学领域:
- 水文地质学 水文地质学
- 地质化学 地质化学
背景情况:
- 地下水的化学演化对于资源安全至关重要.
- 了解控制平原地区地下水化学的因素至关重要.
研究的目的:
- 在德阳市平原调查地下水的化学特征.
- 确定推动地下水组成部分的形成和演变的因素.
主要方法:
- 离子比率分析分析
- 多变量统计分析.
- 反向地质化学建模反向地化学建模
主要成果:
- 地下水主要是HCO3-Ca型的.
- 水与岩石的相互作用 (碳酸盐溶解,氧化还原,阴离子交换) 和人类的干扰是主要因素.
- 蒸发石和碳酸盐矿物质溶解/沉,以及酸盐气候变化是水地化学演变的关键.
结论:
- 由于地质和水文条件,水地化学进化途径因地质和水文条件而异.
- 提供了一个理解平原水化学演变的框架.
- 提供了类似盆地的可持续地下水管理的见解.
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