为了探索红壤涌泉灌的水分入渗规律，进行了不同流量下涌泉灌的水分入渗试验，依据非饱和土壤水分 运动理论建立土壤入渗数学模型，采用软件 HYDＲUS－3D 进行了求解，在模型验证后，采用数值模拟方法研究土壤水 分入渗运动。模型验证说明: 土壤含水率的模拟值与实测值相对误差较小，两种结果的吻合度比较高，涌泉灌土壤水 分运动可以用该模型来模拟。数值模拟结果说明: 随流量的增加，土壤水分运动特征值随之增大; 随着时间的延长增 减的幅度变小; 入流量越大，湿润锋运移速度越快，土壤含水率增加的速率越大; 当入渗达到稳定时，土壤含水率与流 量呈等比例增加的关系。

In order to explore the red soil bubbled irrigation water infiltration laws，the infiltration test of red soil bubbled irrigation with different flow rate was carried out based on kinematic theory of unsaturated soil moisture to establish a mathematical model of soil water infiltration，and the HYDＲUS-3D software was used to solve the model． After the model was verified through the laboratory experiment，the model was used to simulate the soil water infiltration． The results show that the simulated values and the measured values of soil moisture content relative error are small，and both have good consistency; the model can be used for irrigation of bubbled simulation of soil water movement． The numerical simulation results show that the characteristics of soil water movement increases with the increase of infiltration flow，but the amplitude decreases with time; the greater the infiltration flow rate and the faster velocity of wetting front，the greater rate of soil water content; when the infiltration is stable，the relationship between soil water content and infiltration rate is proportional increased．