Soil saturated hydraulic conductivity is an important parameter to calculate the water flux of soil profile in the irrigation and drainage system for agricultural production and resource utilization. An accurate and rapid measurement directly determines the prediction accuracy of various hydrological and hydrodynamic models. However, there are great differences in the saturated hydraulic conductivity in space, due to the different soil texture, structure, as well as physical and chemical properties. The current measurement approaches are time-consuming and laborious for the soil saturated hydraulic conductivity in the soil hydrodynamics. In this study, a rapid measurement was proposed for the soil saturated hydraulic conductivity combining the linear source inflow method and mobile phone image processing. Soil saturated hydraulic conductivity refers to the water flux per unit area of soil perpendicular to the water flow direction under the action of unit water potential gradient, when all pores of soil are filled with water. Soil infiltration rate refers to the rate at which water penetrates into the ground at any given time. The soil infiltration rate is close to a fixed value when the soil water is close to or reaches saturation in the process of infiltration. Therefore, this value is usually considered to be close to the actual soil saturated hydraulic conductivity. The specific procedure was taken as the core idea. Firstly, the soil infiltration rate was measured to consider the infiltration rate, when the water was saturated as the soil saturated hydraulic conductivity. The diffusion process of linear water flow on the soil surface was recorded by a mobile phone. The wetted area of the soil surface and the change curve with time were calculated, after the image processing operations, such as cutting, distortion correction, binarization, and count the number of target pixels in the binarized image. The water balance principle was selected to estimate the change process of soil steady-state infiltration rate using the linear source inflow method. The stable infiltration rate was taken as the soil saturated hydraulic conductivity, and then compared with the saturated hydraulic conductivity measured by the traditional constant head method. The results show that after the distortion correction and image processing, the surface wetted area of Quercus variabilis BL. forest soil, Pinus tabulaeformis Carr. forest soil and sandy loam presented an excellent power exponential relationship with the time, where the determination coefficients R2 were 0.994, 0.995, and 0.998 respectively. The steady-state infiltration rates (i.e. soil saturated hydraulic conductivity) of Quercus variabilis BL. forest soil, Pinus tabulaeformis Carr. forest soil, and sandy loam measured by the linear source inflow method were 23.40±1.21, 23.86±1.83, and 22.99±2.26 mm/h, respectively. At the same time, the values of saturated hydraulic conductivity for the three soil samples measured by the constant head standard method were 24.41±1.53, 24.26±0.37, and 23.81±0.10 mm/h respectively. The relative errors of the two methods were 4.14% 1.64% and 3.42%, respectively. It can be seen that the measurement was reasonable, simple, and accurate under the condition of sufficient water supply. The new measurement method can be widely expected to quickly acquire the soil saturated hydraulic conductivity. [ABSTRACT FROM AUTHOR]