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盐-冻耦合作用下水泥基风积沙改性土基坑填料的性能研究 被引量:2

Performance of Foundation Pit Filler with Cement-Based Drift-Sand Modified Soil under Salt-Freeze Coupling Effects
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摘要 为了研究风积沙改性土基坑填料力学性质和结构受盐-冻作用的影响规律,观测不同循环次数下样品的腐蚀程度并进行化学成分分析,开展无侧限压缩试验,评价其力学性能的衰变规律。最后利用压汞试验对风积沙改性土的孔隙分布进行测量。结果表明:在盐-冻耦合作用下,由于化学反应导致水泥凝胶体减少,改性土的腐蚀程度逐渐增加;无侧限抗压强度、弹性模量随盐-冻次数增加而呈衰减趋势,且速率先快后慢;无侧限抗压强度与孔隙体积呈负线性关系,水泥基风积沙改性土微结构中的孔隙变化是宏观性能衰变的内在原因。 In order to study the influence of salt-freeze coupling on the mechanics and structural properties of cement-based drift-sand modified soil,the corrosion degree of the soil in different cycle numbers was observed and the chemical composition was analyzed.Unconfined compression tests were carried out to evaluate the decay law of mechanical properties.Finally,the pore distributions of drift-sand modified soil were measured by mercury injection tests.The results show that the degree of corrosion of soil-cement increases gradually due to the decrease of cement gel caused by chemical reaction under the action of salt-freeze coupling.The unconfined compressive strength(UCS)and elastic modulus(E)decrease with the increase of salt-freeze times(N).Unconfined compressive strength and porosity have a good negative linear relationship,indicating that the mechanical properties of drift-sand modified soil are closely related to pore changes.The change of porosity in microstructure of cement-based drift-sand modified soil is the intrinsic cause of macroscopic decay.
作者 王丽英 骆文进 王红梅 李鑫鑫 WANG Liying;LUO Wenjin;WANG Hongmei;LI Xinxin(School of Civil Engineering,Chongqing Jianzhu College,Chongqing 400072,China;College of Urban Construction,Chongaing Energy College,Chongqing 402260,China;School of River and Ocean Engineering,Chongqing Jiaotong University,Chongqing 400074,China)
出处 《硅酸盐通报》 CAS 北大核心 2020年第9期2912-2918,共7页 Bulletin of the Chinese Ceramic Society
基金 重庆市教育委员会科学技术研究青年项目(KJQN201904306,KJQN201904309) 重庆市高等教育教学改革研究重点项目(192087)。
关键词 水泥基风积沙改性土 硫酸盐 冻融循环 力学性能 矿物成分 微结构 cement-based drift-sand modified soil sulfate freeze-thaw cycle mechanical property mineral composition microstructure
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