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Spatial Assessment of Soil Organic Carbon Density Through Random Forests Based Imputation

机译:基于插值法的森林估算土壤有机碳密度的空间评估

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Regional estimates of soil carbon pool have been made using various approaches that combine soil maps with sample databases. The point soil organic carbon (SOC) densities are spatialized employing approaches like regression, spatial interpolation, polygon based summation, etc. The present work investigates a data mining based spatial imputation for spatial assessment of soil organic carbon density. The study area covers Andhra Pradesh and Karnataka states of India. Field sampling was done using stratified random sampling method with land cover/use, soil type, agro-ecological regions for defining strata. The spatial data at 1 km resolution on climate, NDVI, land cover, soil type, topography was used as input for modeling the top 30 cm Soil Organic Carbon (SOC) density. To model the SOC density, a Random Forest (RF) based model with optimal parameters and input variables has been adopted. Experiment results indicate that 500 number of trees with 5 variables at each split could explain the maximum variability of soil organic carbon density of the study area. Out of various input variables used to model SOC density, land use/cover was found to be the most significant factor that influences SOC density with a distinct importance score of 34.7 followed by NDVI with a score of 12.9. The predicted mean SOC densities range between 2.22 and 13.2 Kg m~(-2) and the estimated pool size of SOC in top 30 cm depth is 923 Tg for Andhra Pradesh and 1,029 Tg for Karnataka. The predicted SOC densities using this model were in good agreement with the measured observations (R =0.86).
机译:使用多种方法将土壤图和样本数据库结合起来,可以对土壤碳库进行区域估算。利用回归,空间插值,基于多边形的求和等方法对点土壤有机碳(SOC)密度进行空间化。本工作研究了一种基于数据挖掘的空间估算方法,用于土壤有机碳密度的空间评估。研究区域涵盖印度安得拉邦和卡纳塔克邦。使用分层随机抽样方法进行田间采样,该方法采用土地覆盖/用途,土壤类型,农业生态区域来定义地层。以1 km分辨率的气候,NDVI,土地覆盖,土壤类型,地形的空间数据作为模型,用于模拟30 cm最高土壤有机碳(SOC)密度。为了建模SOC密度,已采用具有最佳参数和输入变量的基于随机森林(RF)的模型。实验结果表明,每个分割处的500棵树木具有5个变量,可以解释研究区域土壤有机碳密度的最大变异性。在用于建模SOC密度的各种输入变量中,土地使用/覆盖面积是影响SOC密度的最重要因素,其重要性指数为34.7,其次是NDVI,得分为12.9。预测的平均SOC密度范围在2.22至13.2 Kg m〜(-2)之间,安得拉邦最高30 cm深度的SOC估计池大小为923 Tg,卡纳塔克邦为1,029 Tg。使用该模型预测的SOC密度与实测值非常吻合(R = 0.86)。

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