[Temporal and Spatial Variations of Soil Organic Carbon and the Influencing Factors in Shaanxi Province in Recent 30 Years].

Q2 Environmental Science
Xiao-Lin Feng, Yu-Yang Yan, Xin-Ran Zhang, Chu-Tian Zhang, Zeng-Chao Geng, Fei-Nan Hu, Chen-Yang Xu
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Abstract

Soil organic carbon (SOC) variation is a significant indicator for the soil quality dynamic and global carbon cycle. Therefore, it is necessary to study the regional temporal and spatial distribution of SOC pool and the influencing factors. In this study, a total of 540 soil data and environmental variables were collected from Shaanxi Province during a 30-year period from 1985 to 2015, and univariate analysis of variance and path analysis were used to explore the temporal and spatial distribution characteristics of SOC content and the influencing factors of SOC change. The results showed that the SOC contents of Shaanxi Province in both 1985 and 2015 were the highest in central Shaanxi, followed by those in southern Shaanxi, and they were significantly higher than those in northern Shaanxi. From 1985 to 2015, the increase in SOC in southern Shaanxi was the highest (21.28%), and that in central Shaanxi was 15.33%. The content of SOC in northern Shaanxi was decreased by 10.23%, caused by significant decrements in the bottom horizons of 60-80 cm and 80-100 cm. Compared with that in 1985, the increases in SOC content in the 0-100 cm soil profile (with every 20 cm as a horizon) ranged from 3.21% to 29.39% in 2015. The increase in SOC content of skeletal soils was largest, followed by that of alluvial soils. Correlation analysis and path analysis showed that SOC content was positively correlated with altitude, average annual precipitation, normalized vegetation index, and total nitrogen content and was in significant negative correlation with curvature, bulk density, and pH. Total nitrogen content was the main controlling factor affecting SOC content. The results of the study can provide reference for future carbon management measures in the region.

[近 30 年陕西省土壤有机碳时空变化及影响因素]。
土壤有机碳(SOC)的变化是衡量土壤质量动态和全球碳循环的重要指标。因此,有必要对土壤有机碳库的区域时空分布及其影响因素进行研究。本研究收集了陕西省1985-2015年30年间共540个土壤数据和环境变量,采用单变量方差分析和路径分析方法探讨了SOC含量的时空分布特征及SOC变化的影响因素。结果表明,1985 年和 2015 年陕西省 SOC 含量均以陕中地区最高,陕南地区次之,且明显高于陕北地区。从 1985 年到 2015 年,陕南 SOC 含量增幅最大(21.28%),陕中为 15.33%。陕北地区的 SOC 含量下降了 10.23%,原因是 60-80 厘米和 80-100 厘米的底层 SOC 含量明显下降。与 1985 年相比,0-100 厘米土壤剖面(以每 20 厘米为一个地层)的 SOC 含量增加了 3.21%-192%。与 1985 年相比,2015 年 0-100 厘米土壤剖面(以每 20 厘米为一个地层)的 SOC 含量增加了 3.21% 至 29.39%。骨架土的 SOC 含量增幅最大,冲积土次之。相关分析和路径分析显示,SOC 含量与海拔、年均降水量、归一化植被指数和总氮含量呈正相关,与曲率、容重和 pH 呈显著负相关。总氮含量是影响 SOC 含量的主要控制因素。研究结果可为该地区未来的碳管理措施提供参考。
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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来源期刊
环境科学
环境科学 Environmental Science-Environmental Science (all)
CiteScore
4.40
自引率
0.00%
发文量
15329
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