Zhu Chongchong, Zhong Wenhui, Han Cheng, Deng Huan, Jiang Yunbin
Jiangsu Provincial Key Laboratory of Materials Cycling and Pollution Control, School of Geography, Nanjing Normal University, Nanjing, 210023, China.
Jiangsu Provincial Key Laboratory of Materials Cycling and Pollution Control, School of Geography, Nanjing Normal University, Nanjing, 210023, China; Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing, 210023, China.
J Environ Manage. 2023 Jun 1;335:117590. doi: 10.1016/j.jenvman.2023.117590. Epub 2023 Feb 28.
Straw returning is suggested as a sustainable agricultural practice to promote soil organic carbon (SOC) sequestration, whose magnitude can be influenced by climatic, edaphic and agronomic factors simultaneously. However, the driving factors regulating straw returning-induced SOC increase in China's uplands remain uncertain. This study conducted a meta-analysis by collecting data from 238 trials at 85 field sites. The results showed that straw returning significantly increased SOC content by an average of 16.1% ± 1.5% with an average sequestration rate of 0.26 ± 0.02 g kg yr. The improvement effects were significantly better in the northern China (NE-NW-N) than in the eastern and central (E-C). SOC increases were more pronounced in C-rich and alkaline soils, in cold and dry climates, and under larger amounts of straw-C and moderate nitrogen fertilizer inputs. Longer experimental period resulted in higher SOC increase rates but lower SOC sequestration rates. Furthermore, partial correlation analysis and structural equation modelling revealed that total straw-C input was the key driving factor of SOC increase rate whereas straw returning duration was the dominant limiting factor of SOC sequestration rate across China. Climate conditions were potential limiting factors of SOC increase rate in NE-NW-N and SOC sequestration rate in E-C. It was suggested that straw returning with large application amounts should be more strongly recommended in uplands in NE-NW-N especially in the straw applications at the beginning, from the perspective of SOC sequestration.
秸秆还田被认为是一种促进土壤有机碳(SOC)固存的可持续农业实践,其固存规模会同时受到气候、土壤和农艺因素的影响。然而,在中国旱地,调控秸秆还田导致SOC增加的驱动因素仍不明确。本研究通过收集来自85个田间试验点的238项试验数据进行了荟萃分析。结果表明,秸秆还田显著提高了SOC含量,平均提高了16.1%±1.5%,平均固存率为0.26±0.02 g kg⁻¹ yr⁻¹。中国北方地区(东北-西北-华北)的改善效果明显优于东部和中部地区(华东-华中)。在富含碳和碱性的土壤、寒冷干燥的气候条件下,以及秸秆碳投入量较大和施氮量适中的情况下,SOC的增加更为显著。试验期越长,SOC增加率越高,但SOC固存率越低。此外,偏相关分析和结构方程模型表明,秸秆总碳投入是全国SOC增加率的关键驱动因素,而秸秆还田持续时间是SOC固存率的主要限制因素。气候条件是东北-西北-华北地区SOC增加率和华东-华中地区SOC固存率的潜在限制因素。从SOC固存的角度来看,建议在中国北方地区(东北-西北-华北)的旱地更大力推荐大量施用秸秆还田,特别是在开始阶段施用秸秆。