陈学军, 陈议城, 宋宇, 李佳明, 余思喆, 陈李洁. 2019: Cu2+污染红黏土土性异变现象分析. 工程地质学报, 27(5): 1010-1018. DOI: 10.13544/j.cnki.jeg.2019030
    引用本文: 陈学军, 陈议城, 宋宇, 李佳明, 余思喆, 陈李洁. 2019: Cu2+污染红黏土土性异变现象分析. 工程地质学报, 27(5): 1010-1018. DOI: 10.13544/j.cnki.jeg.2019030
    CHEN Xuejun, CHEN Yicheng, SONG Yu, LI Jiaming, YU Sizhe, CHEN Lijie. 2019: ANALYSIS ON VARIATION OF PHYSICAL-MECHANICAL PROPERTIES OF RED CLAY CONTAMINATED BY CU2+. JOURNAL OF ENGINEERING GEOLOGY, 27(5): 1010-1018. DOI: 10.13544/j.cnki.jeg.2019030
    Citation: CHEN Xuejun, CHEN Yicheng, SONG Yu, LI Jiaming, YU Sizhe, CHEN Lijie. 2019: ANALYSIS ON VARIATION OF PHYSICAL-MECHANICAL PROPERTIES OF RED CLAY CONTAMINATED BY CU2+. JOURNAL OF ENGINEERING GEOLOGY, 27(5): 1010-1018. DOI: 10.13544/j.cnki.jeg.2019030

    Cu2+污染红黏土土性异变现象分析

    ANALYSIS ON VARIATION OF PHYSICAL-MECHANICAL PROPERTIES OF RED CLAY CONTAMINATED BY CU2+

    • 摘要: 研究Cu2+污染物对桂林红黏土土性异变的影响。通过开展XRD、XRF及压汞试验,探讨Cu2+污染红黏土中主要矿物成分的异变规律及微观孔隙结构的变化趋势,结果表明:红黏土中主要矿物成分为高岭石、石英和针铁矿,Cu2+污染对这3种主要矿物成分的含量产生显著影响,随着Cu2+浓度的增大,高岭石和针铁矿的含量逐渐减少,石英的含量逐渐增多,其含量变化率大小关系为:高岭石>针铁矿>石英,且在浓度为2%时,高岭石的损失率高达10.69%,针铁矿的损失率达到5.38%;红黏土孔隙分布曲线为双峰分布,双峰分别分布在0.01-0.1 μm和1~10 μm之间,且在0.01~0.1 μm之间的微小孔隙占了绝对优势。随着Cu2+浓度的增加,"双峰"逐渐右移,孔隙变大;"峰宽"逐渐变宽,孔隙变多。通过开展相关力学试验,观察Cu2+污染红黏土的变形强度特性异变规律,试验结果表明:Cu2+污染对红黏土的变形强度特性影响显著。随着Cu2+浓度的增加,土体的无侧限抗压强度、抗剪强度、黏聚力C和内摩擦角φ逐渐减小,初始孔隙比e0和压缩系数α逐渐增大;当Cu2+浓度从0增大至2%时,土体应力-应变关系曲线由典型的应变软化型转变为弱应变硬化型,无侧限抗压峰值强度减少了76.91%,抗剪强度平均损失率达到69.36%。

       

      Abstract: The effect of Cu2+ on the variation of physical-mechanical properties of Guilin red clay is studied. XRD、XRF and mercury intrusion tests are carried out to investigate the variation law of main mineral components and the change trend of micro-pore structure in Cu2+ contaminated red clay. The results show that the main mineral components in red clay are kaolinite, quartz and goethite. Cu2+ pollutant has a significant impact on the content of these three main mineral components. With the increase of Cu2+ concentration, the content of kaolinite and goethite gradually decrease, while the content of quartz gradually increases. The change rate of content is kaolinite>goethite>quartz. When the Cu2+ concentration is 2%, the content loss rate of kaolinite and goethite are as high as 10.69% and 5.38%, respectively. The pore distribution curve of red clay is bimodal. The double peaks are distributed between 0.01~0.1 μm and 1~10 μm respectively. The micro-pores between 0.01~0.1 μm account for the absolute advantage. With the increase of Cu2+ concentration, the "double peak" move to the right gradually, and the pores become larger, the "peak width" widens gradually, and the pores become more numerous. A series of tests are conducted to observe the variation law of the deformation strength characteristics of red clay contaminated by Cu2+. They include unconfined compressive strength test, direct shear test and compression consolidation test. The results show that Cu2+ contamination has a significant effect on the deformation strength properties of red clay. With the increase of Cu2+ concentration, the unconfined compressive strength, shear strength and its index(C, φ) of the red clay decrease gradually, the initial void ratio e0 and the compression coefficient α increase gradually. When the Cu2+ concentration increases from 0 to 2%, the unconfined compressive stress-strain curve of soil changes from typical strain softening type to weak strain hardening one, the peak value of unconfined compressive strength decreases by 76.91% and the average loss rate of shear strength reaches 69.36%.

       

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