SAIC, contractor to US Geological Survey (USGS) Center for Earth Resources Observation and Science, Sioux Falls, SD 57198, USA.
Carbon Balance Manag. 2007 Jul 24;2:7. doi: 10.1186/1750-0680-2-7.
Tillage practices greatly affect carbon (C) stocks in agricultural soils. Quantification of the impacts of tillage on C stocks at a regional scale has been challenging because of the spatial heterogeneity of soil, climate, and management conditions. We evaluated the effects of tillage management on the dynamics of soil organic carbon (SOC) in croplands of the Northwest Great Plains ecoregion of the United States using the General Ensemble biogeochemical Modeling System (GEMS). Tillage management scenarios included actual tillage management (ATM), conventional tillage (CT), and no-till (NT).
Model simulations show that the average amount of C (kg C ha-1yr-1) released from croplands between 1972 and 2000 was 246 with ATM, 261 with CT, and 210 with NT. The reduction in the rate of C emissions with conversion of CT to NT at the ecoregion scale is much smaller than those reported at plot scale and simulated for other regions. Results indicate that the response of SOC to tillage practices depends significantly on baseline SOC levels: the conversion of CT to NT had less influence on SOC stocks in soils having lower baseline SOC levels but would lead to higher potentials to mitigate C release from soils having higher baseline SOC levels.
For assessing the potential of agricultural soils to mitigate C emissions with conservation tillage practices, it is critical to consider both the crop rotations being used at a local scale and the composition of all cropping systems at a regional scale.
耕作方式极大地影响了农业土壤中的碳(C)储量。由于土壤、气候和管理条件的空间异质性,量化耕作对 C 储量的影响一直具有挑战性。我们使用通用集合生物地球化学建模系统(GEMS)评估了耕作管理对美国西北大平原生态区农田土壤有机碳(SOC)动态的影响。耕作管理方案包括实际耕作管理(ATM)、常规耕作(CT)和免耕(NT)。
模型模拟表明,1972 年至 2000 年间农田每年释放的 C 量(kg C ha-1yr-1)平均为 246 用 ATM,261 用 CT,210 用 NT。与在其他地区模拟的小块土地规模报告的相比,在生态区规模上从 CT 转为 NT 可大大减少 C 排放率的降低。结果表明,SOC 对耕作实践的响应在很大程度上取决于基线 SOC 水平:CT 转为 NT 对基线 SOC 水平较低的土壤中的 SOC 储量影响较小,但对基线 SOC 水平较高的土壤中减少 C 释放的潜力更大。
为了评估保护性耕作实践对农业土壤减少 C 排放的潜力,必须考虑当地使用的作物轮作以及区域范围内所有耕作系统的组成。