气候变化和微量元素的动员MSWI从湿和干取的底层灰
Philipp Ingold1, Gisela Weibel1, Patrick Kämpfer1
1Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, 3012 Bern, Switzerland.
Journal of contaminant hydrology
|April 12, 2025
概括
底层灰的气候变化,是一种废物,影响元素排放. 由于其化学特征,干底灰具有较高的性和元素液,由于其化学特征,它比湿底灰带来更大的环境风险.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 材料科学 材料科学 材料科学
背景情况:
- 底层灰是焚烧的副产品,含有潜在的危险元素.
- 了解底层灰的气候变化行为对于评估环境风险至关重要.
- 之前的研究还没有完全阐明干底灰与湿底灰的气候变化过程和元素排放特征.
研究的目的:
- 为了研究干燥和湿底灰的气候变化特性.
- 为了确定气候对元素排放的影响.
- 了解初始水接触对底层灰行为的作用.
主要方法:
- 干燥底灰的试验性加湿.
- 定位实验以确定缓冲容量和溶解过程作为pH值的函数.
- 热力学计算以确定可溶性控制相.
- 对元素排放与pH值相关的分析和计算的可溶性曲线.
主要成果:
- 干底灰表现出高度性条件 (pH12.6) 具有涉及各种矿物阶段的多阶段溶解过程.
- 之前的气候变化降低了干燥和湿底灰的现场pH值,分别为12.1和10.3.
- 干底灰显示出比湿底灰更高的元素度和液,可能是由于溶解无机碳 (DIC) 和溶解有机碳 (DOC) 等配体.
结论:
- 气候变化过程显著影响底层灰的pH值和元素流动性.
- 干式提取的底灰造成了更高的环境风险,因为污染物的出增加了.
- 底层灰行为特征对于管理与这种废物相关的环境危害至关重要.
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