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Impacts of Cropping Systems on Aggregates Associated Organic Carbon and Nitrogen in a Semiarid Highland Agroecosystem

机译:耕作制度对半干旱高原农业生态系统中聚集体相关有机碳和氮的影响

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摘要

The effect of cropping system on the distribution of organic carbon (OC) and nitrogen (N) in soil aggregates has not been well addressed, which is important for understanding the sequestration of OC and N in agricultural soils. We analyzed the distribution of OC and N associated with soil aggregates in three unfertilized cropping systems in a 27-year field experiment: continuously cropped alfalfa, continuously cropped wheat and a legume-grain rotation. The objectives were to understand the effect of cropping system on the distribution of OC and N in aggregates and to examine the relationships between the changes in OC and N stocks in total soils and in aggregates. The cropping systems increased the stocks of OC and N in total soils (0–40 cm) at mean rates of 15.6 g OC m-2 yr-1 and 1.2 g N m-2 yr-1 relative to a fallow control. The continuous cropping of alfalfa produced the largest increases at the 0–20 cm depth. The OC and N stocks in total soils were significantly correlated with the changes in the >0.053 mm aggregates. 27-year of cropping increased OC stocks in the >0.053 mm size class of aggregates and N stocks in the >0.25 mm size class but decreased OC stocks in the <0.053 mm size class and N stocks in the <0.25 mm size class. The increases in OC and N stocks in these aggregates accounted for 99.5 and 98.7% of the total increases, respectively, in the continuous alfalfa system. The increases in the OC and N stocks associated with the >0.25 mm aggregate size class accounted for more than 97% of the total increases in the continuous wheat and the legume-grain rotation systems. These results suggested that long-term cropping has the potential to sequester OC and N in soils and that the increases in soil OC and N stocks were mainly due to increases associated with aggregates >0.053 mm.
机译:耕作制度对土壤团聚体中有机碳(OC)和氮(N)分布的影响尚未得到很好的解决,这对于了解农业土壤中OC和N的固存具有重要意义。在一项为期27年的田间试验中,我们分析了三种未施肥的耕作系统中与土壤团聚体相关的OC和N分布:连续种植苜蓿,连续种植小麦和豆科作物轮作。目的是了解耕作制度对骨料中OC和N分布的影响,并研究总土壤和骨料中OC和N储量变化之间的关系。种植系统以05.6 cm OC m -2 yr -1 和1.2 g N的平均速率增加了总土壤(0–40 cm)中OC和N的储量m -2 yr -1 相对于休闲控件。苜蓿的连作在0–20 cm深度产生最大的增幅。总土壤中的OC和N储量与> 0.053 mm团聚体的变化显着相关。播种27年后,骨料> 0.053毫米级别的OC种群增加,> 0.25毫米大小级别的N种种群增加,但<0.053毫米大小的类别的OC种群减少,<0.25mm大小的类别的N种群减少。在连续苜蓿系统中,这些骨料中OC和N量的增加分别占总增加量的99.5和98.7%。与> 0.25 mm的总大小相关的OC和N储量的增加占连续小麦和豆类-谷物轮作系统总增加量的97%以上。这些结果表明,长期种植有可能隔离土壤中的OC和N,而土壤OC和N储量的增加主要归因于聚集体> 0.053 mm的增加。

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