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首页> 外文期刊>Archives of Agronomy and Soil Science >Evaluation of the spatial pattern of surface soil water content of a karst hillslope in Southwest China using a state-space approach
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Evaluation of the spatial pattern of surface soil water content of a karst hillslope in Southwest China using a state-space approach

机译:利用国内空间方法评估西南喀斯特喀斯特山坡表面土壤含水量的空间模式

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摘要

This study aims to evaluate the effects of soil physicochemical properties and environmental factors on the spatial patterns of surface soil water content (SWC) based on the state-space approach and linear regression analysis. For this purpose, based on a grid sampling scheme (10mx10m) applied to a 90mx120m plot located on a karst hillslope of Southwest China, the SWC at 0-16cm depth was measured 3 times across 130 sampling points, and soil texture, bulk density (BD), saturated hydraulic conductivity (K-s), organic carbon (SOC), and rock fragment content as well as site elevation (SE) were also measured at these locations. Results showed that the distribution pattern of SWC could be more successfully predicted by the first-order state-space models (R-2=67.5-99.9% and RMSE=0.01-0.14) than the classic linear regression models (R-2=10.8-79.3% and RMSE=0.11-0.24). The input combination containing silt content (Silt), K-s, and SOC produced the best state-space model, explaining 99.9% of the variation in SWC. And Silt was identified as the first-order controlling factor that explained 98.7% of the variation. In contrast, the best linear regression model using all of the variables only explained 79.3% of variation.
机译:本研究旨在基于状态空间方法和线性回归分析来评估土壤理化性质和环境因素对表面土壤水分(SWC)的空间模式的影响。为此目的,基于网格采样方案(10MX10M)应用于位于中国西南西南喀斯特山坡的90mx120M剧集,在0-16CM深度的SWC跨越130个采样点测量3次,土壤纹理,散装密度(在这些位置还测量了BD),饱和液压导电性(Ks),有机碳(SoC)和岩石片段含量以及地点升高(SE)。结果表明,SWC的分布模式可以通过比经典线性回归模型(R-2 = 0.01-0.14)更成功地预测(R-2 = 67.5-99.9%)(R-2 = 10.8 -79.3%和RMSE = 0.11-0.24)。包含淤泥含量(SILT),K-S和SOC的输入组合产生了最佳的状态空间模型,解释了SWC的差异的99.9%。并且淤泥被确定为一阶控制因素,其解释了98.7%的变异。相比之下,使用所有变量的最佳线性回归模型仅解释了79.3%的变化。

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