首页> 外文期刊>Agriculture, Ecosystems & Environment: An International Journal for Scientific Research on the Relationship of Agriculture and Food Production to the Biosphere >Projected changes in soil organic carbon stocks of China's croplands under different agricultural managements, 2011-2050.
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Projected changes in soil organic carbon stocks of China's croplands under different agricultural managements, 2011-2050.

机译:2011-2050年,不同农业经营方式下中国农田土壤有机碳储量的预测变化。

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The timing, magnitude, and regional distribution of soil organic carbon (SOC) changes are uncertain when factoring in climate change and agricultural management practices. The goal of this study is to analyze the implications of changes in climate and agricultural management for Chinese soil carbon sequestration over the next 40 years. We used the Agro-C model to simulate climate and agricultural management scenarios to investigate the combined impacts of climate change and management on future SOC stocks in China's croplands. The model was run for croplands on mineral soils in China, which make up a total of 130 M ha of cropland. The model used climate data (years 2011-2050) from the FGOALS and PRECIS climate models based on four Intergovernmental Panel on Climate Change (IPCC) emissions scenarios. Three equidistant agricultural management scenarios were used. S0 was a current scenario, and S2 was an optimal scenario. Under the S2 scenario, crop yields increased annually by 1%, the proportion of crop residue retained in the field reached 90% by 2050, and the area of no-tillage increased to 50% of the cultivated area by 2050. The S1 scenario applied half of the increased rates in crop yields, residue retention and no-tillage area values that were used in the S2 scenario. Across all croplands in China, the results suggest that SOC will increase under all combinations of climate and management and that the effect of climate change is much smaller than the effect of changes in agricultural management. Most croplands in China show a significant increase in SOC stocks, while very few zones (mainly in northeastern China) show a decrease. Rice paddy soils under the intensive farming management scenario show higher rates of carbon sequestration than dry-land soils. The maximum carbon sequestration potential of the croplands of China is estimated to be 2.39 Pg C under S2. Annual increases in SOC stocks could offset a maximum of 2.9% of the CO2 emissions from fossil-fuel combustion in 2009. These results suggest that China's croplands, especially rice paddies, may play an important role in C sequestration and future climate change mitigation.
机译:当考虑到气候变化和农业管理实践时,土壤有机碳(SOC)变化的时间,幅度和区域分布是不确定的。这项研究的目的是分析气候和农业管理的变化对未来40年中国土壤固碳的影响。我们使用Agro-C模型来模拟气候和农业管理情景,以调查气候变化和管理对中国农田未来SOC存量的综合影响。该模型是针对中国矿质土壤上的农田(总共占1.3亿公顷农田)运行的。该模型使用了来自FGOALS和PRECIS气候模型的气候数据(2011-2050年),该气候模型基于四个政府间气候变化专门委员会(IPCC)排放情景。使用了三种等距的农业管理方案。 S0是当前方案,S2是最佳方案。在S2情景下,到2050年,农作物的产量每年增加1%,保留在田间的农作物残渣的比例达到90%,到2050年免耕面积增加到耕地的50%。 S2情景中使用的作物单产,残retention留率和免耕面积增加率的一半。结果表明,在中国所有耕地中,在气候和管理的所有组合下,SOC都会增加,而且气候变化的影响远小于农业管理变化的影响。中国大部分耕地的SOC存量均显着增加,而极少的区域(主要在中国东北)则有所下降。在集约化耕作管理方案下,稻田土壤的固碳率比旱地土壤高。在S2下,中国农田的最大固碳潜力估计为2.39 PgC。 SOC的年度增加量最多可以抵消2009年化石燃料燃烧产生的CO 2 排放量的2.9%。这些结果表明,中国的耕地,尤其是稻田,可能在碳中起重要作用。隔离和未来减缓气候变化。

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