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Three-dimensional digital soil mapping of agricultural fields by integration of multiple proximal sensor data obtained from different sensing methods

机译:通过整合从不同传感方法获得的多个近端传感器数据,对农田进行三维数字土壤制图

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The objective of the present study was to evaluate a strategy for three-dimensional (3-D) digital soil mapping on two farms in southwest Sweden. Apparent electrical conductivity (ECa) and gamma radiation data from proximal sensors and laser-scanned elevation data were used as predictors. Depth-integrated ECa measurements from a non-invasive sensor were used directly, but also calibrated against probe sensor ECa measurements to obtain layer-specific values. This allowed the predictive powers of depth-integrated and layer-specific ECa to be compared. Clay and sand fractions, and organic matter content (OM) were modelled for three depth layers by multivariate adaptive regression splines (MARSplines). Clay and sand were consistently better predicted in the topsoil than in the subsoil. MARSplines models based on layer-specific ECa data rather than on depth-integrated ECa data yielded more successful estimations of these soil properties in both subsoil layers (0.4-0.6 and 0.6-0.8 m) on both the farms but this was not always the case in the topsoil. Topsoil OM was better predicted by spatial interpolation of the calibration data than by using MARSplines models with ancillary predictors. In the two subsoil layers, the mapping procedure could not be appropriately tested, because the OM was low and homogeneous. We concluded that a 3-D soil texture map of an agricultural field could be prepared using MARSplines models based on layer-specific ECa values, gamma radiation data and a digital elevation model.
机译:本研究的目的是评估瑞典西南部两个农场的三维(3-D)数字土壤制图策略。来自近端传感器的表观电导率(ECa)和伽马辐射数据以及激光扫描的高程数据被用作预测指标。直接使用非侵入式传感器的深度积分ECa测量值,但也可以根据探针传感器ECa测量值进行校准以获得特定于层的值。这样就可以比较深度积分和特定于层的ECa的预测能力。通过多元自适应回归样条线(MARSplines)对三个深度层的粘土和砂石成分以及有机质含量(OM)进行了建模。始终比表层土更好地预测表层土中的粘土和沙子。 MARSplines模型基于特定层的ECa数据,而不是基于深度集成的ECa数据,可以在两个农场的两个次土壤层(0.4-0.6和0.6-0.8 m)中对这些土壤特性进行更成功的估计,但并非总是如此在表土上。通过对数据进行空间插值,可以比使用带有辅助预测器的MARSplines模型更好地预测表土OM。在两个底土层中,由于OM低且均匀,因此无法适当测试映射过程。我们得出的结论是,可以使用MARSplines模型基于特定于图层的ECa值,γ辐射数据和数字高程模型来准备农田的3-D土壤质地图。

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