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首页> 外文期刊>Bulletin of engineering geology and the environment >Effects of carbonate on the structure and properties of loess and the corresponding mechanism: an experimental study of the Malan loess, Xi'an area, China
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Effects of carbonate on the structure and properties of loess and the corresponding mechanism: an experimental study of the Malan loess, Xi'an area, China

机译:碳酸盐对黄土结构和性质的影响及其机理:中国西安马兰黄土的实验研究

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摘要

The structural, physical and morphological characteristics of loess will change as a result of the dissolution of mineral components, mainly carbonate, when it is exposed to acid rain, industrial acid leakage or other acidic environments. This study investigates the physical and structural characteristics of the Malan loess, Xi'an area, China, after carbonate dissolution. The presence of carbonate is determined by scanning electron microscopy (SEM)/energy-dispersive X-ray (EDX) and X-ray diffraction (XRD) analysis. The loess was soaked with 0.2 mol/L acetic acid. The degree of degradation of the loess, carbonate and other minerals was determined by the abundances of elements in the solution. Microstructural analysis combined with the loess characteristics of adsorption, water stability, compressive yield stress and shear strength are used to explain the changes in the soil structure after carbonate dissolution. The results show that bonds in the cementation are irreversibly lost during the remoulding process, and additional bonds are destroyed with the removal of large amounts of carbonate, causing the skeletal particle surface area, specific surface area, adsorption capacity and water stability to decrease. The compressive yield stress and cohesion of the soil are considerably more sensitive at higher water contents. Calcium carbonate is the main carbonate component in the loess, and the secondary calcium carbonate connects the skeletal particles by coating and bridging; the strong cementation stops the particles from dispersing in water. The change in strength and deformation of the soil change its microstructure, which indicates that the secondary calcium carbonate affects the soil structure and stability by reducing the aggregate wettability and changing the mechanical strength of the soil aggregate. This paper will contribute to elucidating the formation and destruction of loess.
机译:当暴露于酸雨,工业酸泄漏或其他酸性环境中时,由于矿物成分(主要是碳酸盐)的溶解,黄土的结构,物理和形态特征将发生变化。本研究调查了碳酸盐溶解后中国西安地区马兰黄土的物理和结构特征。碳酸盐的存在通过扫描电子显微镜(SEM)/能量色散X射线(EDX)和X射线衍射(XRD)分析确定。黄土用0.2 mol / L乙酸浸泡。黄土,碳酸盐和其他矿物质的降解程度取决于溶液中元素的含量。用微观结构分析结合黄土的吸附特性,水稳定性,压缩屈服应力和剪切强度来解释碳酸盐溶解后土壤结构的变化。结果表明,在重塑过程中,胶结物中的键不可逆地丢失,另外的键因去除大量碳酸盐而被破坏,从而导致骨骼颗粒的表面积,比表面积,吸附能力和水稳定性降低。在较高的水分含量下,压缩屈服应力和土壤的凝聚力更加敏感。黄土中主要的碳酸钙成分是碳酸钙,次生的碳酸钙则通过包覆和桥接的方式连接骨骼颗粒。牢固的胶结作用阻止了颗粒在水中的分散。土壤强度和变形的变化会改变其微观结构,这表明次生碳酸钙通过降低集料的润湿性和改变土壤集料的机械强度而影响土壤结构和稳定性。本文将有助于阐明黄土的形成和破坏。

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