Qu Junfeng, Jiang Nan, Dai Yuting, Yang Ying, Ning Yang, Wang Kun, Chen Fuyao, Huang Jiu, Tan Min
School of Public Policy and Management, China University of Mining and Technology, Xuzhou, 221116, Jiangsu, China.
Carbon Neutral Research Institute, China University of Mining and Technology, Xuzhou, 221116, Jiangsu, China.
Sci Rep. 2025 Jul 1;15(1):21344. doi: 10.1038/s41598-025-08409-0.
Under the background of ecological restoration and soil structure improvement in coal mining subsidence areas, understanding the impact of land use on soil organic carbon pools and aggregate characteristics is of great significance to evaluate the quality change and ecological effect of reclaimed soil and guide the improvement of reclaimed soil. Although the dynamics of soil organic carbon under land use changes have been studied, the mechanism of aggregate carbon protection in reclaimed mining soil is still unclear. Taking the reclaimed soils of farmland, woodland, and wasteland in the Dongtan mining area of Zoucheng City in Shandong Province as the research object, by comparing the particle size composition of soil aggregates, the distribution characteristics of organic carbon in 0-20 cm and 20-40 cm soil layers, and analyzing the differences of different organic carbon components, it was found that the organic carbon content of aggregates in the 0-20 cm soil layer was higher than that in the 20-40 cm soil layer; In topsoil, the contribution of fine aggregates to total organic carbon was the largest; the contents of free light fraction (free LF) organic carbon in fine aggregates, micro-aggregates, and total free light fraction organic carbon in forest soil were significantly higher than those in farmland and wasteland. These results suggest that fine aggregates may serve as primary carriers of reclaimed soil organic carbon. The study on the surface soil aggregate organic carbon helps reveal the transformation and accumulation process of reclaimed soil organic carbon. The study found that woodland reclamation may enhance microbial-driven soil organic carbon storage, suggesting that targeted land-use strategies have the potential to maximize the carbon sequestration capacity in degraded ecosystems. Findings are specific to the 7-year reclamation period and Dongtan mining area, requiring long-term regional validation.
在煤矿塌陷区生态修复和土壤结构改良的背景下,了解土地利用对土壤有机碳库和团聚体特征的影响,对于评估复垦土壤的质量变化和生态效应以及指导复垦土壤改良具有重要意义。尽管已对土地利用变化下土壤有机碳的动态进行了研究,但复垦矿土中团聚体碳保护机制仍不明确。以山东省邹城市东滩矿区农田、林地和荒地的复垦土壤为研究对象,通过比较土壤团聚体的粒径组成、0 - 20厘米和20 - 40厘米土层中有机碳的分布特征,并分析不同有机碳组分的差异,发现0 - 20厘米土层中团聚体的有机碳含量高于20 - 40厘米土层;在表层土壤中,细团聚体对总有机碳的贡献最大;森林土壤中细团聚体、微团聚体的游离轻组(free LF)有机碳含量及总游离轻组有机碳含量显著高于农田和荒地。这些结果表明,细团聚体可能是复垦土壤有机碳的主要载体。对表层土壤团聚体有机碳的研究有助于揭示复垦土壤有机碳的转化和积累过程。研究发现,林地复垦可能增强微生物驱动的土壤有机碳储存,这表明有针对性的土地利用策略有潜力使退化生态系统中的碳固存能力最大化。研究结果特定于7年的复垦期和东滩矿区,需要长期的区域验证。