In order to research engineering geological properties of the soil in Zhenlai of western Jilin,especially the dispersivity of soil,the authors carried out the basic physicochemical test and dispersivity identification test.The results show that the dispersivity of the soil increases with the increase of depth within 0-30 cm (surface soil);it decreases as the depth increases within in 30-100 cm.Furthermore,the statistical analysis of the dispersivity indexes and physicochemical propertity indexes show that the DP is positively linear correlated with total soluble salt content,sodium ion content,ESP,pH and organic matter content.Meanwhile,it is negatively linear correlated with clay content,and the linear relationship is better.Through the study of the dispersion mechanism of soil samples,it can be concluded that sodium montmorillonite,higher percentage of exchangeable sodium and high pH are the main reasons for the dispersion of soils in western Jilin. In order to research engineering geological properties of the soil in Zhenlai of western Jilin, especially the dispersivity of soil, the authors carried out the basic physicochemical test and dispersivity identification test. Results show that the dispersivity of the soil increases with the increase of depth within 0-30 cm (surface soil); it decreases as the depth increases within 30-100 cm. Ferrthermore, the statistical analysis of the dispersivity indexes and physicochemical propertity indexes show that the DP is positively linear correlated with total soluble salt content, sodium ion content, ESP, pH and organic matter content. While it is negatively linear correlated with clay content, and the linear relationship is better. Through the study of the dispersion mechanism of soil samples, it can be concluded that sodium montmorillonite, higher percentage of exchangeable sodium and high pH are the main reasons for the dispersion of soils in western Jilin.