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Greenhouse Gas Flux and Crop Productivity after 10 Years of Reduced and No Tillage in a Wheat-Maize Cropping System

机译:减少10年的小麦玉米耕作后的耕作减少和免耕后的温室气体通量和作物生产率

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摘要

Appropriate tillage plays an important role in mitigating the emissions of greenhouse gases (GHG) in regions with higher crop yields, but the emission situations of some reduced tillage systems such as subsoiling, harrow tillage and rotary tillage are not comprehensively studied. The objective of this study was to evaluate the emission characteristics of GHG (CH4 and N2O) under four reduced tillage systems from October 2007 to August 2009 based on a 10-yr tillage experiment in the North China Plain, which included no-tillage (NT) and three reduced tillage systems of subsoil tillage (ST), harrow tillage (HT) and rotary tillage (RT), with the conventional tillage (CT) as the control. The soil under the five tillage systems was an absorption sink for CH4 and an emission source for N2O. The soil temperature positive impacted on the CH4 absorption by the soils of different tillage systems, while a significant negative correlation was observed between the absorption and soil moisture. The main driving factor for increased N2O emission was not the soil temperature but the soil moisture and the content of nitrate. In the two rotation cycle of wheat-maize system (10/2007–10/2008 and 10/2008–10/2009), averaged cumulative uptake fluxes of CH4 under CT, ST, HT, RT and NT systems were approximately 1.67, 1.72, 1.63, 1.77 and 1.17 t ha−1 year−1, respectively, and meanwhile, approximately 4.43, 4.38, 4.47, 4.30 and 4.61 t ha−1 year−1 of N2O were emitted from soil of these systems, respectively. Moreover, they also gained 33.73, 34.63, 32.62, 34.56 and 27.54 t ha−1 yields during two crop-rotation periods, respectively. Based on these comparisons, the rotary tillage and subsoiling mitigated the emissions of CH4 and N2O as well as improving crop productivity of a wheat-maize cropping system.
机译:适当的耕作在减轻作物高产地区的温室气体排放方面起着重要的作用,但是对一些耕作减少的耕作系统(例如深耕,耙耕和旋耕)的排放情况尚未进行全面研究。这项研究的目的是基于华北平原的10年耕作试验,其中包括免耕(NT),评估2007年10月至2009年8月四种减耕系统下温室气体(CH4和N2O)的排放特征。 ),并以常规耕作(CT)为对照,对三种耕作方式进行了分耕作法,分别为:土壤耕作(ST),耙耕(HT)和旋耕(RT)。五种耕作制度下的土壤是CH4的吸收池和N2O的排放源。土壤温度对不同耕作制度土壤对CH4的吸收有正向影响,而吸收与土壤水分之间存在显着的负相关关系。 N2O排放增加的主要驱动因素不是土壤温度,而是土壤水分和硝酸盐含量。在小麦-玉米系统的两个旋转周期中(10 / 2007-10 / 2008和10 / 2008-10 / 2009),CT,ST,HT,RT和NT系统下CH4的平均累积吸收通量分别约为1.67、1.72 ,分别为1.63、1.77和1.17 t ha -1 -1 ,同时大约为4.43、4.38、4.47、4.30和4.61 t ha -1这些系统的土壤分别排放出 year −1 。此外,他们还分别在两个轮作期分别获得了33.73、34.63、32.62、34.56和27.54 t ha 的产量。基于这些比较,旋转耕作和深松减少了CH4和N2O的排放,并提高了小麦玉米种植系统的作物生产力。

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