College of Resources and Environmental Engineering, Guizhou University, Guiyang, 550025, Guizhou, China.
College of Resources and Environmental Engineering, Guizhou University, Guiyang, 550025, Guizhou, China; Key Laboratory of Karst Georesources and Environment, Ministry of Education, Guizhou University, Guiyang, 550025, China; Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang, 550025, China.
Environ Res. 2024 Nov 1;260:119623. doi: 10.1016/j.envres.2024.119623. Epub 2024 Jul 15.
Carbon storage and the aboveground biomass of farmland provide practical significance for understanding global changes and ensuring food production and quality. Based on soil carbon storage, aboveground biomass, climate, geochemistry, and other data from 19 farmland ecological stations in China, we analysed the distribution characteristics of farmland carbon storage in topsoil and aboveground biomass. We notably revealed the response direction and degree of climate and geochemical factors to farmland carbon storage in topsoil and aboveground biomass. The results indicated that the average carbon stocks of farmland in different regions ranged from 0.28 to 7.91 kg m, the average fresh weight of the aboveground biomass (FAB) ranged from 1370.64 to 5997.28 g m, and the average dry weight of the aboveground biomass (DAB) ranged from 119.95 to 852.35 g m. The least angle regression (LARS) and the best subsection selection regression (BSS) showed that evapotranspiration and extreme low temperatures were significant climatic factors affecting carbon sequestration and aboveground biomass on long-time scales. The linear mixed-effects model (LMM) further showed that AN and AP had significant long-term effects on carbon sequestration and aboveground biomass (p < 0.05), with AN having the highest contribution to SOC FAB, and DAB. The structural equation model (SEM) showed that carbon sequestration and aboveground biomass in agricultural fields were significantly positively correlated (p < 0.05). Moreover, the climate had a less direct contribution to carbon sequestration and above-ground biomass compared to geochemistry (PC < 0.1<PC), and its effect was more indirect. When the geochemical variables were removed, the correlation between climate and carbon and aboveground biomass variables decreased significantly. We conclude that it is possible that extremes climate and geochemistry control carbon sequestration and above-ground biomass in long-term cropland through interactions in the context of global change, which provides new insights into the evolution of soil organic carbon in long-term cropland and the scientific formulation of policies to increase food production and preserve quality.
农田土壤碳储量和地上生物量对理解全球变化、保障粮食生产和品质具有重要意义。本研究基于中国 19 个农田生态站的土壤碳储量、地上生物量、气候、地球化学等数据,分析了农田土壤碳储量和地上生物量的分布特征,揭示了气候和地球化学因子对农田土壤碳储量和地上生物量的响应方向和程度。结果表明,不同区域农田土壤碳储量平均为 0.28-7.91 kg·m-2,地上生物量鲜重平均为 1370.64-5997.28 g·m-2,地上生物量干重平均为 119.95-852.35 g·m-2。最小角回归(LARS)和最佳分段回归(BSS)分析表明,蒸散和极端低温是影响农田土壤碳固存和地上生物量的重要气候因子。线性混合效应模型(LMM)进一步表明,土壤全氮(AN)和有效磷(AP)对农田土壤碳固存和地上生物量有显著的长期影响(p<0.05),AN 对 SOC、FAB 和 DAB 的贡献最大。结构方程模型(SEM)表明,农田土壤碳储量和地上生物量呈显著正相关(p<0.05)。此外,与地球化学相比,气候对农田土壤碳固存和地上生物量的直接贡献较小(PC<0.1<PC),其作用更间接。去除地球化学变量后,气候与碳和地上生物量变量之间的相关性显著降低。综上,在全球变化背景下,极端气候和地球化学通过相互作用可能控制长期农田土壤碳固存和地上生物量,为深入理解长期农田土壤有机碳演变和制定增加粮食生产和保持品质的政策提供了新的视角。