Abiotic Reaction and Diffusion of Chlorinated Solvents in Fe2+ Bearing Intact Limestones and Mudstones

含Fe2 完整石灰岩和泥岩中氯化溶剂的非生物反应和扩散

• 批准号: 415743133
• 负责人: Professor Dr. Peter Grathwohl
• 金额: --
• 依托单位: Arbeitsgruppe Hydrogeochemie
• 依托单位国家: 德国
• 项目类别: Research Grants
• 财政年份: 2018
• 资助国家: 德国
• 起止时间: 2017-12-31 至 2022-12-31
• 项目状态: 已结题
• 来源: https://gepris.dfg.de/gepris/projekt/415743133?language=en
• 关键词: Abiotic; Reaction; Diffusion; Chlorinated; Solvents

Diffusion of groundwater contaminants into and out of water-saturated low permeability rock matrices is a very slow process and responsible for the limited success of many subsurface remediation activities. Chlorinated solvents are still among the most relevant groundwater contaminants forming large scale plumes especially in urban space despite decades of clean-up efforts. Slow diffusion results in very long residence times in the rock matrix and thus slow abiotic reactions involving Fe2+ bearing minerals (e.g. iron sulfides, magnetite, phyllosilicates) may become effective in transformation of chlorinated compounds and should be considered in assessment of natural attenuation potentials. Goals of this proposal is to measure abiotic transformation of tri- and perchloroethene during slow diffusion in rock samples from fractured aquifers and from aquitards. Since reaction rates of the parent compounds are likely too slow to be measurable experimentally, focus is on identification and analysis of transformation intermediates and products (e.g. partly chlorinated acetylenes, ethenes and ethane). Reactive diffusion experiments have to be performed with intact rock samples since crushing of minerals (e.g. quartz, pyrite) may introduce reactive surfaces resulting potentially in dehalogenation of the parent compounds. In contrast to earlier studies reactions will be related to types of minerals and their original size in the rock matrix. Results are not only relevant for long-term behavior of chlorinated solvent plumes, but in general important for radioactive waste disposal or chemical weathering (oxidation) of reduced rocks.

地下水污染物扩散进出水饱和的低渗透性岩石基质是一个非常缓慢的过程，是许多地下补救活动成效有限的原因。氯化溶剂仍然是最相关的地下水污染物之一，形成大规模的羽流，特别是在城市空间，尽管几十年的清理工作。缓慢扩散导致在岩石基质中的停留时间非常长，因此涉及含Fe2+矿物（例如硫化铁、磁铁矿、层状硅酸盐）的缓慢非生物反应可能在氯化化合物的转化中变得有效，在评估自然衰减潜力时应予以考虑。本提案的目标是测量三氯乙烯和全氯乙烯在裂隙含水层和弱透水层岩石样品中缓慢扩散过程中的非生物转化。由于母体化合物的反应速率可能太慢，无法通过实验测量，因此重点是识别和分析转化中间体和产物（例如部分氯化的乙炔、乙烯和乙烷）。反应扩散实验必须与完整的岩石样品进行，因为破碎的矿物（如石英，黄铁矿）可能会引入反应性表面，导致潜在的脱卤的母体化合物。与早期的研究相反，反应将与矿物类型及其在岩石基质中的原始大小有关。结果不仅与氯化溶剂羽流的长期行为有关，而且对于放射性废物处置或还原岩石的化学风化（氧化）具有重要意义。