洪水灌增加了从含水层沉积物释放到地下水中的
Xinyi Cao1, Xu Han2, Yaoxuan Chen3
1College of Water Sciences, Beijing Normal University, Beijing 100875, China.
Journal of contaminant hydrology
|January 14, 2024
概括
在田的洪水灌显著增加了地下水含量,因为它改变了含水层的化学成分. 这一过程释放结合的,对水质产生负面影响,需要农业规划的注意.
科学领域:
- 环境科学 环境科学
- 水文地质学 水文地质学
- 地质化学 地质化学
背景情况:
- 农业活动是非点污染的主要来源,影响水层中的外源和地源污染物.
- 地质地下水可以呈现高度,但农业实践的影响,如洪水灌对命运仍然不清楚.
研究的目的:
- 研究洪水灌对地下水中的时间和空间分布的影响.
- 为了确定负责洪水灌下缩度变化的水地化学机制.
主要方法:
- 为了模拟洪水灌条件,进行了实验室实验.
- 分析在地下水中的时间和空间分布特征.
主要成果:
- 发现洪水灌增加了水表介质中的释放量,显著提高了地下水中的度.
- 主要机制涉及到水库可降解性的增加,导致氧化铁的减少性溶解和铁结合的释放.
- pH值的变化也会通过酸矿物质的溶解释放.
结论:
- 洪水灌通过增加的度,对大米种植地区的地下水质量产生负面影响.
- 了解这些水地化学过程对于农业规划和地下水污染控制至关重要.
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