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Effects of Different Tillage and Straw Return on Soil Organic Carbon in a Rice-Wheat Rotation System

机译:稻麦轮作体系中不同耕作方式和秸秆还田对土壤有机碳的影响

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摘要

Soil management practices, such as tillage method or straw return, could alter soil organic carbon (C) contents. However, the effects of tillage method or straw return on soil organic C (SOC) have showed inconsistent results in different soil/climate/cropping systems. The Yangtze River Delta of China is the main production region of rice and wheat, and rice-wheat rotation is the most important cropping system in this region. However, few studies in this region have been conducted to assess the effects of different tillage methods combined with straw return on soil labile C fractions in the rice-wheat rotation system. In this study, a field experiment was used to evaluate the effects of different tillage methods, straw return and their interaction on soil total organic C (TOC) and labile organic C fractions at three soil depths (0–7, 7–14 and 14–21 cm) for a rice-wheat rotation in Yangzhong of the Yangtze River Delta of China. Soil TOC, easily oxidizable C (EOC), dissolved organic C (DOC) and microbial biomass C (MBC) contents were measured in this study. Soil TOC and labile organic C fractions contents were significantly affected by straw returns, and were higher under straw return treatments than non-straw return at three depths. At 0–7 cm depth, soil MBC was significantly higher under plowing tillage than rotary tillage, but EOC was just opposite. Rotary tillage had significantly higher soil TOC than plowing tillage at 7–14 cm depth. However, at 14–21 cm depth, TOC, DOC and MBC were significantly higher under plowing tillage than rotary tillage except for EOC. Consequently, under short-term condition, rice and wheat straw both return in rice-wheat rotation system could increase SOC content and improve soil quality in the Yangtze River Delta.
机译:土壤管理实践(例如耕作方法或秸秆还田)可能会改变土壤有机碳(C)的含量。但是,耕作方法或秸秆还田对土壤有机碳(SOC)的影响在不同的土壤/气候/作物系统中均显示出不一致的结果。中国的长江三角洲是稻米和小麦的主要产区,稻麦轮作是该地区最重要的耕作制度。但是,在该地区进行的研究很少,以评估不同耕作方法与秸秆还田对稻麦轮作系统中土壤不稳定碳组分的影响。在这项研究中,通过田间试验评估了三种耕作深度(0–7、7–14和14)下不同耕作方法,秸秆还田及其相互作用对土壤总有机碳(TOC)和不稳定有机碳组分的影响。 – 21厘米)在中国长江三角洲扬中的稻麦轮作。本研究测量了土壤TOC,易氧化碳(EOC),溶解有机碳(DOC)和微生物生物量碳(MBC)的含量。秸秆还田对土壤有机碳和不稳定有机碳组分的含量有显着影响,并且在秸秆还田处理下,土壤有机碳和有机碳组分含量在三个深度均高于非秸秆还田。在0–7 cm的深度下,耕作下的土壤MBC显着高于旋耕,但EOC恰好相反。旋耕比7–14 cm耕作耕作的土壤总有机碳含量高得多。但是,在14–21 cm的深度下,除EOC外,耕作下的TOC,DOC和MBC显着高于旋耕。因此,在短期条件下,稻麦轮作体系中的稻麦秸秆均返回,可以增加长三角的SOC含量并改​​善土壤质量。

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