黄土丘陵区土壤有机碳含量影响因素分析及空间估算[j]。

Q2 Environmental Science
Rong-Yan-Ting Huo, Jing Liu, Rui Zhang, Gui-Ling Lin, Rui Dai
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引用次数: 0

摘要

土壤有机碳(SOC)是评价土壤肥力的重要指标。了解其空间分布格局及其影响因素对提高农业可持续性和保障国家粮食安全至关重要。以陕西省延安市抚县为研究对象,从地形、气候、植被和土壤4类环境因子中选取22个与有机碳形成相关的环境变量。采用随机森林(RF)、支持向量机(SVM)和地理加权回归(GWR) 3种数字土壤制图方法建立土壤有机碳含量估算模型。分析了整个研究区、园地、耕地和林地0 ~ 20 cm土壤深层有机碳含量的影响因素及空间分布特征。结果表明:①抚县全区土壤有机碳(SOC)平均值为8.54 g·kg-1,其中园地为6.44 g·kg-1,耕地为7.49 g·kg-1,林地为10.22 g·kg-1。变异系数分别为36.90%、19.24%、29.88%和32.56%,均处于中等变异程度。②在抚县全区,地形、气候、植被和土壤因子对土壤有机碳的分布均有显著影响,且各因子对土壤有机碳的影响差异显著。在林地中,坡度(SLP)、年平均温度(MAT)和容重(BD)对有机碳有显著的负向影响,而年平均降水量(MAP)和总氮(TN)对有机碳有显著的正向影响。在园地中,pH、TN和TK对土壤有机碳均有显著的正向影响。在耕地上,MAP对土壤有机碳有显著的负向影响,TN对土壤有机碳有显著的正向影响。③比较不同估计模型的性能,本研究使用的射频估计模型具有最高的R2,最低的均方根误差(RMSE)和平均绝对误差(MAE)值,最小的模型预测误差。在实测值与估计值的线性拟合中,RF模型的拟合精度R2达到0.85以上,是所有模型中估计性能最好的模型。④利用RF模型对抚县土壤有机碳含量进行空间估算,结果显示出东低西高的分布格局。研究结果可为黄土丘陵区土地利用结构优化调整提供决策参考,为土壤有机碳的准确估算提供技术支持。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
[Influencing Factors Analysis and Spatial Estimation of Soil Organic Carbon Content in the Hilly Areas of the Loess Plateau].

Soil organic carbon (SOC) is a crucial indicator for assessing soil fertility. Understanding its spatial distribution patterns and influencing factors is essential for enhancing agricultural sustainability and securing national food security. This study focused on the Fuxian County, Yan'an City, and Shaanxi Province, selecting 22 environmental variables related to SOC formation from four types of environmental factors: topography, climate, vegetation, and soil. Three digital soil mapping methods, random forest (RF), support vector machine (SVM), and geographically weighted regression (GWR), were employed to establish SOC content estimation models. The influencing factors and spatial distribution characteristics of SOC content at 0-20 cm soil depth for the entire study area, garden land, cultivated land, and forest land were analyzed. The results showed that: ① The average ω(SOC) across the entire region of the Fuxian County was 8.54 g·kg-1, with garden land at 6.44 g·kg-1, cultivated land at 7.49 g·kg-1, and forest land at 10.22 g·kg-1. The coefficients of variation were 36.90%, 19.24%, 29.88%, and 32.56%, respectively, all of which fall into the moderate degree of variation. ② In the entire region of the Fuxian County, topography, climate, vegetation, and soil factors all significantly affected the distribution of SOC, with notable differences in their effects on SOC. In forest land, slope (SLP), mean annual temperature (MAT), and bulk density (BD) had significant negative effects on SOC, while mean annual precipitation (MAP) and total nitrogen (TN) had significant positive effects on SOC. In garden land, pH, TN, and total potassium (TK) all had significant positive effects on SOC. In cultivated land, MAP had a significant negative effect on SOC, while TN had a significant positive effect. ③ Comparing the performance of different estimation models, the RF estimation model used in this study had the highest R2, the lowest root mean square error (RMSE) and mean absolute error (MAE) values, and the smallest model prediction error. In the linear fitting between measured and estimated values, the RF model's fitting accuracy R2 reached above 0.85, demonstrating the best estimation performance among the models. ④ Utilizing the RF model for spatial estimation of SOC content in the Fuxian County revealed a distribution pattern of lower concentrations in the east and higher in the west. The results can provide decision-making reference for the optimization and adjustment of land-use structure in hilly areas of the Loess Plateau and offer technical support for the accurate estimation of SOC.

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环境科学
环境科学 Environmental Science-Environmental Science (all)
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