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Simulation of water flow in a field soil using pedotransfer function

机译:利用pedotransfer函数模拟田间土壤中的水流

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In this study, focus on estimating the water retention and hydraulic conductivity of unsaturated zone through soil textural analysis, carrying out simulation flow in unsaturated zone using HYDRUS 2D model, comparing the soil hydraulic properties of the unsaturated zone of tank clustered catchment. Sindapalli Uppodai a sub basin, of Vaippar river basin in Tamilnadu was selected for this study. Soil samples were collected at different location at different depths (0-30, 30-60 and 60-90 cm). HYDRUS 2D is developed for simulating water movement in unsaturated zones by integrating the two dimensional transient unsaturated water flow equation (Richard's equation) with a root water extraction term (sink), and also incorporates pedo-transfer functions (PTF)for estimating soil hydraulic properties. The measured or estimated hydraulic properties with formulations such as Darcy's law and Richards' equation were used for finding the movement of water in the unsaturated zone. The flow rate of water is often used in irrigation scheduling.
机译:在这项研究中,重点是通过土壤质地分析估算不饱和带的保水率和水力传导率,使用HYDRUS 2D模型在不饱和带中进行模拟流动,比较罐状集水区不饱和带的土壤水力特性。本研究选择了泰米尔纳德邦Vaippar流域的Sindapalli Uppodai子盆地。在不同深度(0-30、30-60和60-90厘米)的不同位置收集土壤样品。 HYDRUS 2D的开发是通过将二维瞬态非饱和水流方程(理查德方程)与根水提取项(汇)相集成来模拟非饱和区中的水运动,并且还结合了脚踏传递函数(PTF)来估算土壤的水力特性。使用达西定律和理查兹方程等公式对水力特性进行测量或估算,以发现水在非饱和区的运动。水的流量通常用于灌溉计划中。

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