A study of water infiltration and water-bearing condition of the L1—S4 layers in Luochuan,Shaanxi

Through water infiltration experiment of the L1—S4 layers in Luochuan using the double-ring method and through determination of porosity,magnetization and CaCO3 content,this paper examines the water infiltration difference,the development of the water-containing space and their causes between the loess and the red ancient soil.The results indicate that the stable infiltration rates of the loess layers are bigger than that of the paleosol layers,and the time when ...