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Analysis of strength development in cement-stabilized silty clay from microstructural considerations

机译:基于微观结构的水泥稳定粉质粘土强度发展分析

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This paper analyzes the strength development in cement-stabilized silty clay based on microstructural considerations. A qualitative and quantitative study on the microstructure is carried out using a scanning electron microscope, mercury intrusion pore size distribution measurements, and thermal gravity analysis. Three influential factors in this investigation are water content, curing time, and cement content. Cement stabilization improves the soil structure by increasing inter-cluster cementation bonding and reducing the pore space. As the cement content increases for a given water content, three zones of improvement are observed: active, inert and deterioration zones. The active zone is the most effective for stabilization where the cementitious products increase with cement content and fill the pore space. In the active zone, the effective mixing state is achieved when the water content is 1.2 times the optimum water content. In this state, the strength is the greatest because of the highest quantity of cementitious products. In the short stabilization period, the volume of large pores (larger than 0.1 μm) increases because of the input of coarser particles (unhydrated cement particles) while the volume of small pores (smaller than 0.1 μm) decreases because of the solidification of the cement gel (hydrated cement). With time, the large pores are filled with the cementitious products; thus, the small pore volume increases, and the total pore volume decreases. This causes the strength development over time.
机译:基于微观结构的考虑,本文分析了水泥稳定粉质粘土的强度发展。使用扫描电子显微镜,压汞孔尺寸分布测量和热重分析对微结构进行定性和定量研究。该调查中的三个影响因素是水含量,固化时间和水泥含量。水泥稳定化通过增加团簇间的胶结作用并减少孔隙空间来改善土壤结构。在给定的水含量下,随着水泥含量的增加,观察到三个改进区域:活性,惰性和劣化区域。活性区是最有效的稳定方法,其中水泥产品随水泥含量的增加而增加,并填充孔隙空间。在活性区域中,当水含量为最佳水含量的1.2倍时,可达到有效的混合状态。在这种状态下,强度最大,因为水泥产品的数量最多。在较短的稳定期,由于输入较粗的颗粒(未水合的水泥颗粒),大孔(大于0.1μm)的体积增加,而由于水泥的凝固,小孔(小于0.1μm)的体积减小。凝胶(水合水泥)。随着时间的流逝,大孔中充斥着胶凝产品。因此,小孔体积增加,而总孔体积减小。这导致强度随时间发展。

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