江苏太仓浅部淤泥质土层的工程地质特征
Engineering geological characteristics of shallow mucky soil in Taicang area,Jiangsu Provience
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摘要: 太仓浅部广泛分布的淤泥质粉质粘土层具有高含水量、高压缩性和低渗透性,对开采浅层地下水引起的地面沉降研究有重要意义。本文通过一系列微观和宏观室内试验,查明该层土的矿物成分主要为伊利石,其次为绿泥石、高岭石,土中孔隙主要为中孔隙和小孔隙。在一定应力范围内,随固结压力增大,土中的中孔隙明显减小,渗透系数也明显减小,孔隙比与渗透系数之间有单对数线性关系,但当固结压力超过一定值后,土中以小孔隙为主,随固结压力增大,孔径分布变化不明显,渗透系数随孔隙比的变化也小得多。淤泥质粉质粘土层的变形以不可恢复的塑性变形为主,具有显著的蠕变性,在开采地下水引起的地面沉降中将会有明显的变形迟后。Abstract: A layer of mucky silty clay distributes extensively at a shallow depth in Taicang area,Jiangsu Provience.This soil layer is of high moisture content,high compressibility and low permeability.It has therefore an important function in land subsidence due to the pumpage of shallow groundwater.A series of laboratory tests were performed to investigate the engineering geological properties.The test results show that the soil is predominantly of clay minerals such as illite,chlorite,and kaolinite,and ...