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In situ chemical oxidation schemes for the remediation of ground water and soils contaminated by chlorinated solvents.

机译:原位化学氧化方案,用于修复地下水和被氯化溶剂污染的土壤。

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This study investigates various aspects of in situ chemical oxidation (ISCO) schemes based on MnO4. Batch experiments show that the interaction between MnO4, and sediment solids will not only consume the reactant, but also can release toxic metals into ground water. Various column and flow tank experiments were conducted to examine the capacity and efficiency of the oxidation scheme. Oxidation was capable of destroying chlorinated ethylenes in aqueous phase. MnO4 oxidation performs better in removal of residual DNAPL than pooled DNAPL. In zones of high NAPL saturation, Mn oxide precipitates causing pore plugging and permeability reduction. These changes potentially could cause the remedial action to fail. In an effort to mitigate the precipitation, experiments have been carried out to investigate possibilities of delaying the formation of colloidal Mn oxide and to remove the precipitates once formed. The investigation begins with the identification of the Mn oxide mineral structure and the determination of the chemical properties of the solid. Phosphate ion was added to the reaction in an attempt to slowdown colloidal formation due to its high charge and the tendency to sorb on surfaces. The results indicate that the presence of phosphate ion can lower the rate of colloid formation. However, the magnitude of effects due to the addition of phosphate is limited by the ionic strength increase and the pzc (point of zero charge) of the mineral. The dissolution kinetics of birnessite was evaluated using solutions of citric acid, oxalic acid, and EDTA. The results showed that the addition of an organic acid could greatly increase the dissolution rate of birnessite. The dissolution mechanism involves proton and ligand-promoted dissolution and reductive dissolution. A permanganate reactive barrier system (PRBS) was designed and a proof-of-concept experiment was carried out in the laboratory. The experiment demonstrated how the PRBS could delivery MnO 4 at a stable, constant, and controllable rate. This idea could be developed as a long-term reactive barrier for the remediation of chlorinated solvents in plume.
机译:本文研究了基于MnO 4 -原位化学氧化(ISCO)方案的各个方面。批处理实验表明,MnO 4 -与沉积物固体的相互作用不仅会消耗反应物,而且还会将有毒金属释放到地下水中。进行了各种塔和流动罐实验以检查氧化方案的容量和效率。氧化能够破坏水相中的氯化乙烯。 MnO 4 -氧化在去除残留DNAPL方面比合并的DNAPL更好。在高NAPL饱和度的区域中,Mn氧化物沉淀,导致孔堵塞和渗透率降低。这些更改可能会导致补救措施失败。为了减轻沉淀,已经进行了实验以研究延缓胶体Mn氧化物形成并除去形成后的沉淀的可能性。研究从鉴定锰氧化物矿物结构和确定固体的化学性质开始。由于其高电荷和易于吸附在表面上,因此向反应中添加了磷酸根离子以减缓胶体的形成。结果表明磷酸根离子的存在可以降低胶体形成的速率。但是,由于添加了磷酸盐而产生的影响的大小受到离子强度增加和矿物的pzc(零电荷点)的限制。使用柠檬酸,草酸和EDTA的溶液评估了水钠锰矿的溶解动力学。结果表明,加入有机酸可以大大提高水钠锰矿的溶解速度。溶解机理涉及质子和配体促进的溶解和还原性溶解。设计了高锰酸盐反应阻挡系统(PRBS),并在实验室中进行了概念验证实验。实验证明了PRBS可以稳定,恒定,可控的速率释放MnO 4 -。这个想法可以发展为用于补救羽状流中氯化溶剂的长期反应性屏障。

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