Li Yi-Fan, Wu Ting, Yao Yuan, Li Zhi-Qiang, Shen Jin-Quan, Weng Huai-Kai, Zhang Li-Ming, Xing Shi-He
College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou 350002, China.
University Key Laboratory of Soil Ecosystem Health and Regulation in Fujian, Fuzhou 350002, China.
Huan Jing Ke Xue. 2024 Oct 8;45(10):6012-6027. doi: 10.13227/j.hjkx.202309159.
Research on the mechanism of how climate change affects cultivated soil organic carbon is the basis for the management of cultivated land quality in the context of climate change. Crop phenological responses to climate change have an important effect on cultivated soil organic carbon as well. However, previous research primarily focused on the independent effects of climate change or crop phenological responses on the changes in soil organic carbon, and few studies have analyzed the changes in cultivated soil organic carbon under the combined influence of both factors or quantified their contribution rates to the changes in cultivated soil organic carbon. Based on topsoil samples in 2008 and 2021, annual pre-season and mid-season climate data from 2008 to 2021, and the phenological parameters extracted from the enhanced vegetation index (EVI) time series from 2007 to 2022, a soil organic carbon predictive model was constructed using the random forest algorithm. The total change in soil organic carbon from 2008 to 2021, the change in soil organic carbon under climate change alone, and the change in soil organic carbon under the synergistic influence of climate change and crop phenological responses were simulated. Furthermore, the contributions of climate change and crop phenological responses to the changes in cultivated soil organic carbon were distinguished and quantified. Moreover, the dominant influencing factors of soil organic carbon changes and their spatial distributions were identified and analyzed. The results were as follows: ① Under the synergistic influence of climate change and crop phenological responses, a decrease was observed in soil organic carbon in 74.15% of the cultivated land area in Fujian Province during the years 2008-2021, with an average decrease of 2.20 g·kg. Additionally, there was an increase in soil organic carbon in 25.85% of the cultivated area, with an average increase of 1.48 g·kg. ②The average contribution rates of pre-season climate, crop phenological responses to climate change, mid-season climate, and phenological changes resulting from cultivars shifts or other adjustments of agricultural measures to soil organic carbon changes were 34.08%, 28.56%, 22.75%, and 14.61%, respectively. Overall, climate change had a greater impact on the changes in cultivated soil organic carbon in Fujian Province than the crop phenological response to climate change. ③ The regions where climate change and phenological response jointly acted as dominant influencing factors held the largest area, accounting for 47.06% of the total cultivated land area in Fujian Province, and the regions where climate change was the dominant influencing factor alone held the second-largest area, accounting for 28.64% of the total cultivated land area. ④ Higher contribution rates of pre-season climate factors and phenological changes resulting from cultivar shifts or other adjustments of agricultural measures tended to be distributed in higher-altitude areas, whereas higher contribution rates of mid-season climate factors and phenological responses to climate change tended to be distributed in lower-altitude areas. These research findings can provide a theoretical basis for decision making regarding the management of cultivated land quality and the safeguarding of food security in the context of climate change.
研究气候变化影响耕地土壤有机碳的机制是气候变化背景下耕地质量管理的基础。作物物候对气候变化的响应也对耕地土壤有机碳有重要影响。然而,以往研究主要关注气候变化或作物物候响应各自对土壤有机碳变化的影响,很少有研究分析这两个因素共同影响下耕地土壤有机碳的变化情况,或量化它们对耕地土壤有机碳变化的贡献率。基于2008年和2021年的表层土壤样本、2008 - 2021年的年度季前和季中气候数据,以及从2007 - 2022年增强植被指数(EVI)时间序列中提取的物候参数,利用随机森林算法构建了土壤有机碳预测模型。模拟了2008 - 2021年土壤有机碳的总变化、仅气候变化下土壤有机碳的变化,以及气候变化和作物物候响应协同影响下土壤有机碳的变化。此外,区分并量化了气候变化和作物物候响应对耕地土壤有机碳变化的贡献。而且,识别并分析了土壤有机碳变化的主要影响因素及其空间分布。结果如下:①在气候变化和作物物候响应的协同影响下,2008 - 2021年福建省74.15%的耕地土壤有机碳呈下降趋势,平均下降2.20 g·kg。另外,25.85%的耕地土壤有机碳呈上升趋势,平均上升1.48 g·kg。②季前气候、作物物候对气候变化的响应、季中气候以及品种更替或其他农业措施调整导致的物候变化对土壤有机碳变化的平均贡献率分别为34.08%、28.56%、22.75%和14.61%。总体而言,气候变化对福建省耕地土壤有机碳变化的影响大于作物物候对气候变化响应的影响。③气候变化和物候响应共同作为主要影响因素的区域面积最大,占福建省耕地总面积的47.06%,仅气候变化作为主要影响因素的区域面积次之,占耕地总面积的28.64%。④季前气候因素以及品种更替或其他农业措施调整导致物候变化的贡献率较高的区域往往分布在高海拔地区,而季中气候因素以及作物物候对气候变化响应的贡献率较高的区域往往分布在低海拔地区。这些研究结果可为气候变化背景下耕地质量管理和保障粮食安全的决策提供理论依据。