首页> 外文会议>Proceedings of joint international agricultural conference (JIAC 2009) >Fuzzy modeling of soil water distribution using buried porous clay capsule irrigation from a subsurface point source
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Fuzzy modeling of soil water distribution using buried porous clay capsule irrigation from a subsurface point source

机译:地下点源地下多孔粘土胶囊灌溉的土壤水分模糊建模。

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Water distribution in soil is important for the design, operation, and management of irrigation system for arid and semi-arid regions. The present paper has attempted to estimate the wetted radius and vertical depth from Buried porous clay capsule irrigation using fuzzy model. A fuzzy reasoning algorithm is used to define the relationship between the saturated hydraulic conductivity, discharge, porosity, water volume applied and hydrostatic pressure head and the surface wetted radius and vertical depth. Singleton fuzzyfier, minimum Mamdani inference engine and centriod defuzzyfier are selected to determine soil water distribution using observed data of calcareous soil with clay loam texture in TMU. To obtain porous clay capsules with different discharge, we mixed 200, 400, 600 and 800 gram fine sand per kilogram clay loam and then baked porous clay capsules about 900 0C temperatures in a kiln. Water discharge from porous capsules included 200, 400, 800, 1200, and 2000 (cm3 /hr) in 2.5 meter hydrostatic pressure head. The surface wetted radius and vertical depth values of this model were also compared in the field by the analysis of residual errors. The results show a significant relation between measurement and estimation of the surface wetted radius and vertical depth of wetted zone. Also results shows that the wetted radius and vertical depth values in 2.5 meter pressure with low discharge were about 13.5 and 22 centimeter, respectively. These parameters were 14 and 45 centimeters with high discharge, respectively.
机译:土壤的水分配对于干旱和半干旱地区的灌溉系统的设计,运行和管理很重要。本文尝试用模糊模型估计埋地多孔粘土胶囊灌溉的湿润半径和垂直深度。用模糊推理算法定义饱和导水率,流量,孔隙度,施加的水量和静水压头与表面湿润半径和垂直深度之间的关系。利用TMU中具有黏土壤土质质的钙质土壤的观测数据,选择单例模糊,最小Mamdani推理机和中心反模糊器来确定土壤水分分布。为了获得具有不同排放量的多孔粘土胶囊,我们将200、400、600和800克细砂/千克粘土分别混合,然后在窑炉中以900 0C的温度烘烤多孔粘土胶囊。在2.5米静水压头中,从多孔胶囊中排出的水包括200、400、800、1200和2000(cm3 / hr)。还通过分析残留误差在现场比较了该模型的表面湿润半径和垂直深度值。结果表明,在表面润湿半径的测量和估计与润湿区域的垂直深度之间存在显着的关系。结果还表明,在低排放的2.5米压力下的湿润半径和垂直深度值分别约为13.5和22厘米。这些参数分别为14厘米和45厘米高放电。

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