Department of Soil and Crop Sciences, Colorado State University, Fort Collins, Colorado, 80523, USA.
Graduate Degree Program in Ecology, Colorado State University, Fort Collins, Colorado, 80523, USA.
Ecol Appl. 2021 Apr;31(3):e02278. doi: 10.1002/eap.2278. Epub 2021 Mar 3.
Increasing the quantity and quality of plant biomass production in space and time can improve the capacity of agroecosystems to capture and store atmospheric carbon (C) in the soil. Cover cropping is a key practice to increase system net primary productivity (NPP) and increase the quantity of high-quality plant residues available for integration into soil organic matter (SOM). Cover crop management and local environmental conditions, however, influence the magnitude of soil C stock change. Here, we used a comprehensive meta-analysis approach to quantify the effect of cover crops on soil C stocks from the 0-30 cm soil depth in temperate climates and to identify key management and ecological factors that impact variation in this response. A total of 40 publications with 181 observations were included in the meta-analysis representing six countries across three different continents. Overall, cover crops had a strong positive effect on soil C stocks (P < 0.0001) leading to a 12% increase, averaging 1.11 Mg C/ha more soil C relative to a no cover crop control. The strongest predictors of SOC response to cover cropping were planting and termination date (i.e., growing window), annual cover crop biomass production, and soil clay content. Cover crops planted as continuous cover or autumn planted and terminated led to 20-30% greater total soil C stocks relative to other cover crop growing windows. Likewise, high annual cover crop biomass production (>7 Mg·ha ·yr ) resulted in 30% higher total soil C stocks than lower levels of biomass production. Managing for greater NPP by improving synchronization in cover crop growing windows and climate will enhance the capacity of this practice to drawdown carbon dioxide (CO ) from the atmosphere across agroecosystems. The integration of growing window (potentially as a proxy for biomass growth), climate, and soil factors in decision-support tools are relevant for improving the quantification of soil C stock change under cover crops, particularly with the expansion of terrestrial soil C markets.
增加植物生物量在时空上的数量和质量可以提高农业生态系统在土壤中捕获和储存大气碳 (C) 的能力。间作是增加系统净初级生产力 (NPP) 和增加可整合到土壤有机质 (SOM) 中的高质量植物残体数量的关键措施。然而,间作管理和当地环境条件会影响土壤碳储量变化的幅度。在这里,我们使用综合荟萃分析方法来量化间作对温带气候下 0-30 厘米土壤深度土壤碳储量的影响,并确定影响这种响应变化的关键管理和生态因素。共有 40 篇文献,包含 181 个观测值,代表了来自三个不同大陆的六个国家。总的来说,间作对土壤碳储量有很强的正效应 (P < 0.0001),平均使土壤碳增加 1.11 Mg C/ha,相对于不间作对照。对 SOC 响应间作的最强预测因子是种植和终止日期(即生长窗口)、年度间作生物量产量和土壤粘粒含量。作为连续覆盖或秋季种植和终止的间作导致总土壤碳储量比其他间作生长窗口增加 20-30%。同样,高年度间作生物量产量 (>7 Mg·ha·yr )比低生物量产量导致总土壤碳储量增加 30%。通过改善间作生长窗口和气候的同步性来提高 NPP,可以增强这种做法从大气中吸收二氧化碳 (CO ) 的能力。在决策支持工具中整合生长窗口(可能作为生物量生长的代理)、气候和土壤因素与扩大陆地土壤 C 市场相关,有助于提高间作下土壤碳储量变化的量化。