从沉积物迁移到无活化材料:一个关键的过程被忽视了湖泊地质工程的常见固定评估
Changhui Wang1, Xinyi Shen1,2, Bo Fan1,3
1State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China.
Water research X
|September 1, 2023
概括
使用 (P) 无活化材料进行湖泊地质工程需要仔细考虑从沉积物中P的迁移. 确保材料和沉积物之间随着时间的推移密切接触对于有效的P固定和可靠的结果至关重要.
科学领域:
- 环境科学 环境科学
- 水资源管理 水资源管理
- 地质化学 地质化学
背景情况:
- 湖泊缩往往是由沉积物的内部 (P) 污染引起的.
- 不活性化材料在湖泊地质工程中用于固定沉积物P.
- 之前的应用显示可靠性有所变化,这表明评估方法存在问题.
研究的目的:
- 研究P从沉积物迁移到固定材料中的作用.
- 评估共同的评估程序,假设沉积物与沉积物有密切接触.
- 确定影响湖泊沉积物中P固定效率的因素.
主要方法:
- 使用饮用水处理残留物 (DWTR) 和沉积物进行90天的化试验.
- 在沉积物-DWTR混合物中的P固定比较与分离的沉积物和DWTR样本.
- 分析表面水中的可溶性P和沉积物中的移动P分数以及DWTR.
主要成果:
- 沉积物-DWTR混合物显示出可溶性和可移动性P的快速和持续减少.
- 分离的样本显示了90天内从沉积物到DWTR的逐渐P迁移.
- 移动P在分离的沉积物中仍然显著,这表明P释放调节了固定.
结论:
- 使用混合物的常用评估方法可能会通过加快P迁移来高估固定率.
- 沉积物P释放动态对于有效的P固定至关重要.
- 湖泊地质工程策略必须确保材料和沉积物之间足够的接触时间,以提高可靠性.
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