充分供水条件下垂直线源灌入渗模型简化研究
Simplified infiltration model of vertical line source irrigation with sufficient water supply
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摘要: 为了定量预测和分析充分供水条件下垂直线源灌土壤入渗特性,基于HYDRUS-2D模型,设置了144种模拟情景,模拟得到了9种土壤在不同线源直径和线源长度条件下的累积入渗量。采用Philip入渗公式对模拟数据进行拟合,从而获得吸渗率和稳渗率。在此基础上,研究了吸渗率和稳渗率与灌溉参数间的关系,建立了考虑线源渗水面积和饱和导水率的充分供水垂直线源灌土壤累积入渗量简化计算模型。最后,利用试验数据验证了简化入渗模型的准确性。结果表明:同一土质的吸渗率与稳渗率均随线源渗水面积的增大而增大,且吸渗率与线源渗水面积符合线性函数关系,稳渗率与线源渗水面积符合幂函数关系。土壤累积入渗量的简化计算模型的统计指标EMAE与ERMSE分别介于1.57~2.05 L与2.38~2.88 L之间,ENSE≥0.92,计算值与实测值一致性较好,简化计算模型预测效果较好,可初步实现仅通过饱和导水率Ks这个物理参数来预测充分供水垂直线源灌的入渗量。Abstract: To quantitatively predict and analyze the soil infiltration characteristics of vertical line source irrigation with sufficient water supply, 144 simulation scenarios were set up based on HYDRUS-2 D model, and the cumulative infiltration amounts of 9 soils under different linear source diameters and lengths were simulated.The Philip infiltration formula was used to fit the simulation data and obtain soil water sorptivity rate and steady infiltration rate.On this basis, the relationship between soil water sorptivity and steady infiltration rate with irrigation parameters were studied, and the simplified calculation model of soil cumulative infiltration of vertical line source irrigation with full water supply was established and was verified by experimental data.The results showed that for the same soil texture, the soil water sorptivity and steady infiltration rate increased with the increase of the linear source seepage area.The soil water sorptivity and the linear source seepage area showed a linear function relationship.The steady infiltration rate and the line source seepage area showed a power function relationship.The statistical indicators of EMAE and ERMSE of the simplified calculation model of cumulative soil infiltration were between 1.57~2.05 L and 2.38~2.88 L,ENSE≥0.92,the calculated values were in good agreement with the measured values, and the simplified calculation model had a good prediction effect.It was possible to predict the infiltration of vertical linear source irrigation with sufficient water supply only by soil physical parameters(Ks).
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