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Laboratory Investigation on Physical-Mechanical Characteristics and Microstructure of a Clayey Gypsiferous Soil in the Presence of Chemical Accelerator

机译:化学促进剂存在下粘土型石米土壤物理力学特性和微观结构的实验室研究

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摘要

Gypsiferous soils are considered as problematic soils that cause damage to engineering infrastructures, particularly hydraulic structures. The exposition of gypsiferous soils to the steady flow leads to the dissolution of gypsum particles, significantly changing the soil engineering characteristics. In this paper, by employing physical, chemical, and mechanical experiments, the effect of raw gypsum with various percentages (0%, 3%, 6%, 9%, 12% and 15%) on the geotechnical parameters of a low plasticiy clay was investigated through leaching. Electrical conductivity test and ionic concentration analysis were used to assess the trend of gypsum dissolution. The results showed that leaching and increased gypsum content significantly degraded soil engineering characteristics, such as strength and compressibility. Acidic accelerator (diluted acetic acid) speeded up the chemical reaction rate and, at the same time, affected the geotechnical properties of the soil more than water. Mineralogical and microstructural studies (x-ray diffraction, scanning electron microscopy and energy-dispersive x-ray spectroscopy) were carried out to evaluate the interaction between gypsum and soil particles and verify laboratory test results. The x-ray diffraction patterns indicated the formation of new peaks such as calcium aluminate hydrated (CAH) and calcium silicate hydrated (CSH) and the altered structure of pure soil following the addition of raw gypsum. Scanning electron microscope images confirmed the presence of cementitious compounds and changes in the texture of gypsiferous soil in comparison with pure soil. Energy dispersive x-ray interpretation revealed changes in the chemical composition of soil blended with gypsum. The laboratory test results were corroborated by microstructural analyses.
机译:石膏的土壤被认为是有问题的土壤,导致工程基础设施损坏,特别是液压结构。石膏土壤对稳定流动的阐述导致石膏颗粒的溶解,显着改变土壤工程特征。本文通过使用物理,化学和机械实验,在低塑料粘土的岩土参数上具有各种百分比的效果(0%,3%,6%,9%,12%和15%)的效果通过浸出来研究。采用电导率试验和离子浓度分析来评估石膏溶解的趋势。结果表明,浸出和增加的石膏含量显着降低了土壤工程特性,如强度和压缩性。酸性促进剂(稀释的乙酸)加速了化学反应速率,同时影响了土壤的岩土性质而不是水。进行矿物学和微观结构研究(X射线衍射,扫描电子显微镜和能量分散X射线光谱),以评估石膏和土壤颗粒之间的相互作用,并验证实验室测试结果。 X射线衍射图案表明,在加入原料石膏后,X射线衍射图案的形成如钙铝酸钙水合(CAH)和硅酸钙水合(CSH)和纯土的改变结构。扫描电子显微镜图像确认了与纯土壤相比,含有水泥化合物的存在和含有石棉土壤质地的变化。能量分散X射线解释揭示了与石膏混合的土壤化学成分的变化。通过微观结构分析来证实实验室测试结果。

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