镉溶液污染黏土微观结构演化规律  

Microstructure evolution of clay polluted by Cd^(2+) chemical solution

作　　者：廖朱玮[1] 陆海军[1] 陈威[1] 

机构地区：[1]武汉轻工大学多孔介质力学研究所,武汉430023

出　　处：《环境工程学报》2014年第3期1203-1207,共5页Chinese Journal of Environmental Engineering

基　　金：国家自然科学基金项目(11002102);武汉工业学院2012年研究生创新基金(2012cx008);武汉市青年科技晨光计划项目(201271031419)

摘　　要：镉溶液在压实黏土中迁移会引起黏土微观结构的变化。通过一系列扫描电子显微镜与低温氮吸附实验,观察了镉溶液污染黏土的表面微观形貌与孔隙结构的演化规律。扫描电子显微镜观察结果显示,受镉溶液污染严重的土柱上表面孔隙明显,土颗粒之间主要以点-点排列方式为主;而受镉溶液污染较弱的下表面,土颗粒之间主要以片-片状排列为主。低温氮吸附实验结果表明,Z=0 cm、Z=10 cm、Z=20 cm、Z=30 cm处,污染黏土吸附量分别为682.65、631.72、583.25和523.36 cm3/g。随土柱中土层深度的增大,黏土颗粒间微孔增多,二次孔减少,孔隙体积与比表面积减小。镉溶液污染黏土孔隙主要集中在10 nm以下。The microstructure of compacted clay was changed by the migration of cadmium solution. In order to observe the surface microtopography and pore structure of polluted clay by Cd2＋ solution,a series of scanning electron microscope（ SEM） and low temperature N2 adsorption testing were performed in laboratory. The results of SEM testing showed that the pores of upper surface samples in soil column were obvious,and the soil particle appeared point-point arrangement. However,the lower surface soil particle appeared piece-piece arrangement. The results of N2adsorption testing showed that adsorption capacities were 682. 65,631. 72,583. 25 and523. 36 cm3/ g at Z = 0 cm,Z = 10 cm,Z = 20 cm and Z = 30 cm,respectively. The amount of secondary pore,pore volume and specific surface area decreased with increasing of soil layer depth in soil column,but the amount of micropore increased. The main concentration of pore was less than 10 nm.

关 键 词：污染黏土 微观结构 孔隙 比表面积 

分 类 号：TP391.9[自动化与计算机技术—计算机应用技术]