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Use of surface soil moisture to estimate profile water storage by polynomial regression and artificial neural networks.

机译:通过多项式回归和人工神经网络,利用地表土壤水分来估算剖面水的存储量。

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摘要

Water storage in the soil profile is an important agronomic variable but its measuring is rather difficult for farmers in production fields. We tested the possibility of using samples from the upper soil layers, which are usually taken for soil fertility evaluation, for whole profile water storage estimation. A data set of 712 water profiles from the subhumid-semiarid portion of the Pampas in Argentina was used, generated under a wide range of soil types, crops, tillage systems, soil cover, and rainfall scenarios. To calculate stored water, soil was sampled up to 140 cm in layers of 20 cm, water content was gravimetrically determined and bulk density also assessed. Polynomial regression and artificial neural networks were used for modeling, randomly partitioning the data set into 75% for model fit and 25% for independent testing. It was possible to estimate with good fit soil profile water storage using as independent variables in regression, or inputs in neural networks, water content in the upper three soil layers (0-20, 20-40, and 40-60 cm) and depth to petrocalcic layer in soils which have this type of horizon. Similar performance was attained with both modeling methods (R2
机译:土壤剖面中的蓄水量是重要的农艺变量,但对生产领域的农民而言,测水相当困难。我们测试了使用上部土壤层样本(通常用于土壤肥力评估)进行整体剖面蓄水量估算的可能性。使用了来自阿根廷潘帕斯州半湿润-半干旱地区的712个水剖面数据集,该数据集是在各种土壤类型,作物,耕作系统,土壤覆盖和降雨情景下产生的。为了计算储存的水,在20厘米的层中对140厘米以内的土壤进行采样,用重量分析法测定水含量,并评估堆积密度。使用多项式回归和人工神经网络进行建模,将数据集随机分为75%(用于模型拟合)和25%(用于独立测试)。可以使用回归分析或神经网络的输入,上三层土壤层(0-20、20-40和40-60 cm)的水含量和深度作为自变量来很好地估算土壤剖面的蓄水量具有这种类型的视野的土壤中的钙钙化层。两种建模方法均获得了相似的性能( R 2

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