硫改性腐蚀的光谱诱导极化 沉积物中的铁
Hilary P Emerson1, James E Szecsody1, Christopher Halter2
1Pacific Northwest National Laboratory, 902 Battelle Blvd, Richland, WA 99354, United States of America.
Journal of contaminant hydrology
|October 5, 2024
概括
光谱诱导极化 (SIP) 能够有效地监测地下修复中的硫改性铁 (SMI). SIP检测到SMI转换,有助于表征和监测受污染的网站.
科学领域:
- 地质物理学 地质物理学
- 环境科学 环境科学
- 地质化学 地质化学
背景情况:
- 光谱诱导极化 (SIP) 对于理解地下污染物修复至关重要.
- SIP应用需要进一步研究动态,生物地化学状态.
- 硫改性铁 (SMI) 是潜在的地下修改,但其SIP反应没有特征.
研究的目的:
- 评估SIP用于对硫改性铁 (SMI) 的非侵入性监测.
- 在相关的地下条件下调查SMI的SIP响应.
- 评估SIP在污染场所的SMI特征和监测方面的实用性.
主要方法:
- 实验室规模的研究使用带有SMI和砂或汉福德遗址沉积物的柱子.
- 在和条件下进行了长达77天的地化学和SIP分析.
- SIP测量侧重于复杂导电性,相极值,充电能力和放松时间.
主要成果:
- 观察到SMI的可辨别的SIP阶段峰值在0.1和1.0赫兹之间,可检测到0.3重量%SMI.
- 最初的SIP变化表明极化增加和长度尺度减少.
- 较长期 (77天) 的SIP分析显示形成较少的极化相和增加的粒子大小/连接性.
结论:
- 对于SMI转型,SIP表现出一种独特的反应.
- SIP可以潜在地监测作为地下障碍物放置的SMI或在现场注入的SMI.
- 这项研究提供了使用SIP用于SMI污染现场整治的基础数据.
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