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Lime Stabilization of Soil: A Physico-Chemical and Micro-Mechanistic Perspective

机译:土石灰稳定土壤:物理化学与微机制视角

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摘要

Lime stabilization is a well-established technique to improve the subgrade properties of different soil for pavement construction, despite construction difficulties and its ineffectiveness in certain conditions. However, a greater level of understanding is needed to know the mechanism of alteration in the properties of soils, particularly to longevity potential of ionic interaction. In the present study, mechanism of long-term strength behaviour of lime-treated soil has been brought clearly through alteration in ionic exchange (Ca2+, Mg2+, Na+ and K+), mineralogy and microstructure by performing series of physico-chemical and micro-analyses (XRD, SEM and EDAX). The results revealed that addition of lime to soil influences greatly the concentration of sodium (Na+) and calcium (Ca2+) ions with marginal alteration in potassium (K+) and magnesium (Mg2+) with curing periods. The variation in concentration of Ca2+ with curing periods has attributed to the strong cation exchange reactions at early stage and consumption of calcium in the formation of cementitious compounds with an increase in curing periods. However, concentration of Ca2+ increases after curing for longer periods, indicating the increase in solubility of cementitious compounds. Alterations in mineralogy and microstructure with an increase in curing periods of lime-treated soil substantiate the effect of changes in ionic concentration. Further, a significant increase in the strength up to 28 days and marginal up to 1 year substantiates that variation in Ca2+ and thereby, formation of cementitious compounds control the strength behaviour of lime-treated soil.
机译:石灰稳定化是一种良好的技术,以改善不同土壤的路面结构,为路面建设,尽管在某些条件下施工困难及其无效性。然而,需要更大程度的理解来了解土壤性质的变化机制,特别是离子相互作用的寿命潜力。在本研究中,通过进行离子交换(Ca2 +,Mg2 +,Na +和K +),矿物学和微观结构,通过进行一系列物理化学和微分析来清楚地带来了石灰处理的土壤的长期强度行为的机理。 (XRD,SEM和EDAX)。结果表明,将石灰与土壤的加入大大影响钠(Na +)和钙(Ca2 +)离子的浓度(k +)和镁(mg2 +)的边缘变化,具有固化期。 Ca2 +浓度的变化具有固化期,归因于早期阳离子交换反应,并在形成水泥化合物的钙的钙的消耗量随着固化期的增加。然而,固化后Ca2 +的浓度增加,表明水泥化合物的溶解度的增加。矿物学和微观结构的改变随着石灰处理土的固化期的增加证实了离子浓度变化的影响。此外,高达28天的强度显着增加,最高可达1年的实质性是Ca2 +的变化,从而形成水泥化合物的形成控制了石灰处理的土壤的强度行为。

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