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Swelling characteristics of soils subjected to acid contamination

机译:酸污染土壤的溶胀特性

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The ever-increasing number of failures of industrial structures due to the heaving of acid-contaminated foundation soils has necessitated a better understanding of soil behavior under changing and extreme environmental conditions. Thus, this paper attempts to micro-mechanistically explain the swelling characteristics of soils contaminated with inorganic acids. Three soils with widely varying physical and chemical properties, namely, natural black cotton soil and commercially available bentonite and kaolin clay, were selected for the investigation. Special Teflon-made oedometer cells, which are entirely non-reactive to acid, were used to assess the swelling behavior. The soils were inundated with two concentrations of sulfuric acid and phosphoric acid and allowed to swell. The results indicate that, in montmorillonitic soils, the type of cation in the exchangeable complex plays a dominant role in governing the swelling behavior of clays during acid contamination. The mineralogical changes due to cation exchange reactions, along with the partial mineral dissolution, resulted in the acid-induced swelling in montmorillonitic soils. In the kaolin clay, the face-to-edge association of the particles due to the adsorption of H+ by broken edges led to an increase in swelling along with mineralogical changes. (C) 2017 Production and hosting by Elsevier B.V. on behalf of The Japanese Geotechnical Society.
机译:由于酸污染的基础土壤的沉浮,导致工业结构破坏的数量不断增加,因此需要更好地了解在不断变化的极端环境条件下的土壤行为。因此,本文试图从微观机理上解释受无机酸污染的土壤的溶胀特性。选择了三种物理和化学性质差异很大的土壤,即天然黑棉土和市售膨润土和高岭土,进行了研究。完全与酸不反应的特殊特氟龙制测压计电池用于评估溶胀行为。用两种浓度的硫酸和磷酸淹没土壤并使其膨胀。结果表明,在蒙脱土中,可交换配合物中的阳离子类型在控制酸污染过程中粘土的溶胀行为中起主导作用。由于阳离子交换反应引起的矿物学变化以及部分矿物溶解,导致蒙脱土中酸引起的溶胀。在高岭土中,由于断裂边缘对H +的吸附而导致的颗粒的面对面缔合导致溶胀增加以及矿物学变化。 (C)2017年由Elsevier B.V.代表日本岩土工程学会制作和托管。

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