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Stabilization of tropical kaolin soil with phosphoric acid and limeTI Stabilization of tropical kaolin soil with phosphoric acid and lime

机译:用磷酸和石灰稳定热带高岭土土壤用磷酸和石灰稳定热带高岭土

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摘要

Studies on the chemically stabilized soils have shown that the effectiveness of treatment is largely dependent on soil's natural environment. In tropical kaolin soils, phosphoric acid may be used as an alternative to traditional alkaline stabilizers for improving soil properties. This research was carried out in an effort to identify the time-dependent soil-stabilizer reactions. Data for the study of characterization of treated samples were obtained from X-ray diffractometry, energy dispersive X-ray spectrometry, field emission scanning electron microscopy, Fourier transform infrared spectroscopy, and leaching analysis. Based on the collected data, the kaolinite mineral with pH-dependent structural properties showed slightly different behavior both in basic and in acidic mediums. Also, it was found that the chemical stabilizers preferentially attacked the alumina surface of the clay particles. Therefore, it was rational to suggest that with respect to lime and phosphoric acid treatment, aluminate hydrate compounds are more likely to be formed.
机译:对化学稳定土壤的研究表明,处理的有效性在很大程度上取决于土壤的自然环境。在热带高岭土土壤中,磷酸可以用作传统碱性稳定剂的替代品,以改善土壤特性。进行这项研究是为了确定随时间变化的土壤稳定剂反应。从X射线衍射法,能量色散X射线光谱法,场发射扫描电子显微镜,傅里叶变换红外光谱法和浸出分析获得用于处理样品表征的研究数据。根据收集的数据,具有pH依赖性结构特性的高岭石矿物在碱性介质和酸性介质中的行为均略有不同。另外,发现化学稳定剂优先侵蚀粘土颗粒的氧化铝表面。因此,有理由建议就石灰和磷酸处理而言,更可能形成铝酸盐水合物。

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