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基于胶体二氧化硅的缓释放高锰酸盐凝胶(SRP-G)的研制与表征:实验室研究。

Development and characterization of colloidal silica-based slow-release permanganate gel (SRP-G): laboratory investigations.

机构信息

Department of Geological Sciences, Ohio University, Athens, OH 45701, United States.

Department of Geological Sciences, Ohio University, Athens, OH 45701, United States.

出版信息

Chemosphere. 2014 Aug;109:195-201. doi: 10.1016/j.chemosphere.2014.01.020. Epub 2014 Mar 17.

DOI:10.1016/j.chemosphere.2014.01.020
PMID:24650708
Abstract

Slow-release permanganate (MnO4(-)) gel (SRP-G) is a hyper-saline KMnO4 solution that can be used for treating large, dilute, or deep plumes of chlorinated solvents in groundwater. Ideally, the SRP-G injected into aquifers will slowly gelate to form MnO4(-) gel in situ, and the gel will slowly releases MnO4(-). Objectives of this study were to develop SRP-G using colloidal silica as gelling solution, characterize its gelation and release kinetics, and delineate its dynamics in a saturated sandy media. The SRP-G exhibited a two-phase increase in viscosity: a lag phase characterized by little increase in viscosity followed by a short gelation phase. Gelation lag times of SRP-G solutions increased (from 0.5h to 13d) with decreasing KMnO4 concentrations (from 25 to 8 g L(-1)). Permanganate release from gelated SRP-G increased with increasing KMnO4 concentrations, and was characterized as asymptotic release with initial peak (0.9-2.2 mg min(-1)) followed by more attenuated release. Gelation lag times of SRP-G flowing in sands (linear velocity=2.1md(-1)) increased (1, 3, and 6h) with decreasing KMnO4 concentrations (25.0, 23.0, and 22.9 g L(-1)). Permanganate release from gelated SRP-Gs continued for up to 3d and was characterized as asymptotic release with an initial peak release (∼1.2 g min(-1)) followed by more attenuated release over 70h. Dilution of SRP-G by dispersion in porous media affects gelation and release kinetics. Increasing the silica concentration in the SRP-G may facilitate gelation and extend the duration of MnO4(-) release from emplaced SRP-G in porous media.

摘要

缓释高锰酸钾(MnO4(-))凝胶(SRP-G)是一种高盐度的 KMnO4 溶液,可用于处理地下水中大体积、稀释或深的氯化溶剂羽流。理想情况下,注入含水层的 SRP-G 将缓慢胶凝,在原地形成 MnO4(-)凝胶,凝胶将缓慢释放 MnO4(-)。本研究的目的是使用胶体硅作为胶凝溶液开发 SRP-G,表征其胶凝和释放动力学,并描绘其在饱和砂质介质中的动力学。SRP-G 的粘度表现出两相增加:滞后阶段的粘度增加很少,随后是短暂的胶凝阶段。SRP-G 溶液的胶凝滞后时间随 KMnO4 浓度(从 25 至 8gL(-1))的降低而增加(从 0.5h 增加至 13d)。凝胶化 SRP-G 中释放的高锰酸盐随 KMnO4 浓度的增加而增加,并且以初始峰值(0.9-2.2mgmin(-1))为特征,随后释放衰减。在砂中流动的 SRP-G(线性速度=2.1md(-1))的胶凝滞后时间随 KMnO4 浓度(25.0、23.0 和 22.9gL(-1))的降低而增加(1、3 和 6h)。凝胶化 SRP-G 中的高锰酸盐释放可持续长达 3d,并以初始峰值释放(约 1.2gmin(-1))为特征,随后在 70h 内释放衰减。SRP-G 在多孔介质中通过弥散而稀释会影响胶凝和释放动力学。增加 SRP-G 中的硅浓度可能会促进胶凝,并延长在多孔介质中放置的 SRP-G 中 MnO4(-)的释放时间。

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