Interactive effects of conservation tillage on the aggregate stability and soil organic carbon
2022
Yang, Sha | Wang, Yaxin | Wang, Zhigang | Yan, Xiaobin | Feng, Meichen | Xiao, Lujie | Song, Xiaoyan | Zhang, Meijun | Li, Guangxin | Shafiq, Fahad | Yang, Wude | Wang, Chao
BACKGROUND: Soil carbon sequestration is of great significance to achieve carbon neutralization at an early date. AIMS: The present study was conducted in order to explore the interactive effects of conservation tillage on soil organic carbon (SOC) and aggregate stability, and to understand the response of soil organic carbon to aggregate structure and distribution characteristics. METHODS: Undisturbed soil from varying depths was collected from the conservation tillage demonstration base under differential tillage practices (NT, no‐tillage mulch; DT, deep‐tillage mulch; CT, conventional‐tillage mulch). SOC and stable‐aggregates of different particle sizes, their number, and structures were analyzed and the relationship between the stability of soil aggregates and SOC was presented. RESULTS: The SOC content was the highest under CT treatment (1.67 g kg–¹) and the lowest under NT treatment (1.31 g kg–¹). In surface soil, the number of macroaggregates (>0.25 mm, M) under NT treatment was the largest (89.1%), the mean weight diameter (MWD) and geometric mean diameter (GMD) of water stability and mechanical aggregates were the highest, and the fractal dimension (D) was the lowest. This indicated that the NT treatment could maintain the aggregate structure of surface soil well. In the short term, DT and CT could increase SOC content, while NT could decrease SOC content. There was a significant correlation between SOC content and MWD (R² = 0.40), GMD (R² = 0.38), and D (R² = 0.44). The more stable the aggregate structure, the higher the soil fixation and maintenance of SOC. CONCLUSIONS: SOC content and aggregate stability have a synergistic effect, and NT can promote the formation of soil aggregates, improve their stability, and balance the distribution of carbon in soil aggregates with different particle sizes.
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