Geospatial modeling approaches for mapping topsoil organic carbon stock in northern part of Mongolia

S. M, Purevdorj Ts.
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引用次数: 1

Abstract

Soil organic carbon (SOC) is one of the most important indicators of soil quality and agricultural productivity. This paper presents the application of Regression Kriging (RK), geographically weighted regression (GWR) and Geographically Weighted Regression Kriging (GWRK) for prediction of topsoil organic carbon stock in Tarialan. A total of 25 topsoil (0-30 cm) samples were collected from Tarialan soum of Khuvsgul aimag in Mongolia. In this study, seven independent variables were used including normalised difference vegetation index (NDVI), soil adjusted vegetation index (SAVI), normalised difference moisture index (NDMI), land surface temperature (LST) and terrain factors (DEM, Slope, Aspect). We used root-mean-square error (RMSE), mean error (ME) and determination coefficient (R2) to evaluate the performance of these methods. Validation results showed that performance of the GWRK, GWR, and RK approaches were good with not only low values of root-mean-square error (1.38 kg/m2, 1.48 kg/m2, 0.69 kg/m2), mean error (0.28 kg/m2, -0.22 kg/m2, 0.17 kg/m2) but also high values of R2 (0.76, 0.72, 0.94). The estimated SOC stock values ranged from 0.28-16.26 kg/m2, 0.72–15.24 kg/m2, 0.16–15.83 kg/m2 using GWRK, GWR, RK approaches in the study area. The highest average SOC stock value was in the wetland (6.47 kg/m2, 6.08 kg/m2, 6.44 kg/m2) and the lowest was in cropland (1.63 kg/m2, 1.48 kg/m2, 1.80 kg/m2) using these approaches. According to the validation, GWRK, GWR, and RK approaches produced satisfactory results for estimating and mapping SOC stock. However, Regression Kriging was the best model, followed by GWRK and GWR to predict topsoil organic carbon stock in Tarialan.
绘制蒙古北部表层有机碳储量的地理空间建模方法
土壤有机碳(SOC)是衡量土壤质量和农业生产力的重要指标之一。本文介绍了回归克里格法(RK)、地理加权回归法(GWR)和地理加权回归克里格方法(GWRK)在塔里阿兰表层有机碳储量预测中的应用。从蒙古Khuvsgul省的Tarialan soum共采集了25份表层土(0-30 cm)样本。在本研究中,使用了七个自变量,包括归一化差异植被指数(NDVI)、土壤调整植被指数(SAVI)、归一化差异水分指数(NDMI)、地表温度(LST)和地形因子(DEM、坡度、纵横比)。我们使用均方根误差(RMSE)、平均误差(ME)和确定系数(R2)来评估这些方法的性能。验证结果表明,GWRK、GWR和RK方法的性能良好,不仅均方根误差值较低(1.38 kg/m2、1.48 kg/m2和0.69 kg/m2)、平均误差值(0.28 kg/m2、-0.22 kg/m2和0.17 kg/m2),而且R2值较高(0.76、0.72和0.94),RK方法在研究领域。使用这些方法,平均SOC存量值最高的是湿地(6.47 kg/m2、6.08 kg/m2、6.44 kg/m2),最低的是农田(1.63 kg/m2、1.48 kg/m2和1.80 kg/m2)。根据验证,GWRK、GWR和RK方法在估计和绘制SOC存量方面产生了令人满意的结果。然而,回归克里格法是预测塔里阿兰表层有机碳储量的最佳模型,其次是GWRK和GWR。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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