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Functional evaluation of methods for predicting the soil water characteristic

机译:预测土壤水分特征的方法的功能评估

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Functional sensitivity analysis was used for 66 different soil horizons to evaluate methods of predicting the soil water characteristic (theta(psi)). Error in predicted hydraulic properties was identified through examination of outputs from the SWIM soil water simulation model. The variability in these outputs arose solely from error in prediction of the soil hydraulic properties. The simulation scenario was the determination of drainage and evapotranspiration over 5-years from a perennial pasture in southern Victoria, Australia. The functional evaluation considered hydraulic conductivity as a function of water content (K(theta)) being independent of error in theta(psi) prediction, as well as K(theta) being estimated from predicted theta(psi) data. Inaccurate hydraulic property prediction caused error in drainage calculation approximately equal and opposite to that for evapotranspiration whilst profile water storage was almost unaffected. Water balance error resulting from the two-point method of theta(psi) prediction was small with simulated drainage less than 4 mm/year different, on average, from that generated using measured theta(psi) data. The two-point method will be sufficiently accurate for many simulation applications and the one-point method is a useful alternative. The multiple regression equations, which do not use measured hydraulic property inputs, were the least accurate of the three methods of theta(psi) prediction and should be applied with caution. When K(Bf was estimated using theta(psi) data generated with the multiple regression method the hydraulic property specification was sufficiently imprecise to cause large additional error in drainage prediction. Functional sensitivity analysis is useful for assessing pedotransfer functions and for determining the accuracy and precision required in hydraulic characterisation surveys. (C) 2000 Elsevier Science B.V. All rights reserved. [References: 28]
机译:使用功能敏感性分析对66种不同的土壤层进行评估,以评估预测土壤水分特征(theta(psi))的方法。通过检查SWIM土壤水模拟模型的输出来确定预测的水力特性中的错误。这些输出的可变性完全是由土壤水力特性预测中的误差引起的。模拟场景是确定澳大利亚维多利亚州南部多年生牧场过去5年的排水和蒸散量。功能评估认为,水力传导率是水含量(K(θ))的函数,而与θ(psi)预测的误差无关,并且K(θ)是根据预测的θ(psi)数据估算的。不正确的水力特性预测会导致排水计算中的误差与蒸发蒸腾大致相等并相反,而剖面蓄水几乎不受影响。由两点式theta(psi)预测法得出的水平衡误差很小,模拟排水量平均少于4毫米/年,与使用测得的theta(psi)数据所产生的平均值平均相差。两点法对于许多仿真应用将足够准确,而单点法是一种有用的替代方法。不使用测得的水力特性输入的多元回归方程是theta(psi)预测的三种方法中精度最低的,应谨慎使用。当使用多元回归法生成的theta(psi)数据估算K(Bf)时,水力特性指标不够精确,在排水预测中会引起较大的附加误差,功能敏感性分析对于评估pedotransfer函数以及确定精度和精度很有用。 (C)2000 Elsevier Science BV保留所有权利[参考文献:28]

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