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SIMPLE MODEL TO ESTIMATE FIELD-MEASURED SOILWATER LIMITS

机译:估算田间土壤水极限的简单模型

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Engineering and modeling applications often require reasonable estimates of the upper and lower limits of plant extractable water. Laboratory measurements of these limits do not always coincide with field observations. Statistical models to estimate soil water retention can be complicated, and usually are not based on field measurements. The objective of this work was to develop simple, generic equations to estimate the field-measured limits of the soil water reservoir based on soil survey data such as texture and bulk density. We used linear regression to estimate the gravimetric upper limit from sand and clay content; the volumetric upper limit can be estimated from the gravimetric upper limit and bulk density. We used non-linear regression to estimate the volumetric plant extractable water from sand content. The lower limit can be estimated as the difference between the upper limit and the plant extractable water. We adjusted the predictions for coarse fragments and organic C and we placed reasonable upper and lower boundaries to our estimates. The equation for the drained upper limit has a RMSE of 0.030 kg kg–1 and uses two coefficients. The equation for the plant extractable water has a RMSE of 0.030 m3 m–3 and uses three coefficients. We tested the simple model with an independent data set. The RMSE of our model was similar or better than that of a more complex statistical model.
机译:工程和建模应用程序通常需要合理估计植物可提取水的上限和下限。这些限值的实验室测量值并不总是与现场观察结果一致。估计土壤保水量的统计模型可能很复杂,并且通常不基于实地测量。这项工作的目的是开发简单的通用方程式,以基于土壤调查数据(例如质地和堆积密度)估算土壤水库的实测极限。我们使用线性回归从沙子和黏土含量估计重量上限。体积上限可以根据重量上限和堆积密度来估算。我们使用非线性回归从砂含量估算植物可提取的体积水。下限可以估计为上限与植物提取水之间的差。我们调整了对粗碎屑和有机碳的预测,并对估算值设置了合理的上下边界。排放上限的方程式的RMSE为0.030 kg kg-1,并使用两个系数。植物可提取水的方程的RMSE为0.030 m3 m–3,并使用三个系数。我们使用独立的数据集测试了简单模型。我们模型的RMSE与更复杂的统计模型相似或更好。

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