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The influence of above-ground residue input and incorporation on GHG fluxes and stable SOM formation in a sandy soil

机译:地上残渣输入和掺入对沙质土壤GHG通量和稳定SOM形成的影响

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Carbon sequestration in agricultural soils has been promoted as a means to reduce atmospheric concentrations of greenhouse gases (GHG) whilst improving soil productivity. Although there is broad agreement on practices that increase carbon (C) stocks, there is a lack of understanding on the stability of these gains and how changes in soil organic carbon (SOC) pools can influence GHG fluxes. We tracked the fate of above-ground residues into functionally different SOC pools and GHG fluxes using isotopically labelled residues (C-13 and N-15) over 12 months in a pasture soil in sub-tropical Australia. Agricultural residue management was simulated by: (1) altering the rate of residue input and, (2) mixing residue with topsoil. GHG fluxes were significantly greater at high residue input levels due to the priming of existing SOC and elevated N2O losses, fuelled by a greater availability of labile substrate. There was evidence of an asymptotic relationship between C input and residue-derived C accumulation in stable soil C pools at higher input levels, indicating that the soil was reaching its protective capacity. Mixing of residues contributed to a 40% increase in GHG fluxes in comparison to surface applied treatment, most notably from residue-derived C and N. This can be attributed to (i) the physical disruption of soil, particularly that of aggregates, which changed the microenvironment stimulating microbial activity, and (ii) greater residue-soil contact. Greater residue-soil contact through mixing also contributed to a 2 fold increase in the residue-derived C recovered in the mineral soil with the majority (56%) in the active C pool. Over a 12 month period, C sequestration was outweighed by GHG fluxes at high rates of input and when residues were mixed with the topsoil. C sequestration policies and associated management approaches must be assessed holistically under a range of conditions and in the long-term to ensure that detrimental practices are not promoted. (C) 2016 Elsevier Ltd. All rights reserved.
机译:促进了农业土壤中的碳固存,以减少大气中温室气体的浓度,同时提高土壤生产力。尽管在增加碳(C)存量的做法上已达成广泛共识,但对这些收益的稳定性以及土壤有机碳(SOC)库的变化如何影响GHG通量缺乏了解。我们在亚热带澳大利亚的牧场土壤中,使用同位素标记的残留物(C-13和N-15)在12个月内追踪了地面残留物进入功能不同的SOC库和GHG通量的命运。通过以下方式模拟农业残余物管理:(1)改变残余物输入速率,(2)将残余物与表土混合。在高残留物输入水平下,GHG通量明显更大,这归因于现有SOC的引发和N2O损失的增加,而不稳定的底物则具有更大的可用性。有证据表明,在较高的输入水平下,稳定的土壤碳库中的碳输入与残留源碳积累之间存在渐近关系,表明土壤已达到其保护能力。与表面处理相比,残留物的混合使GHG通量增加了40%,最明显的是来自残留物的C和N。这可以归因于(i)土壤的物理破坏,尤其是骨料的物理破坏,这种破坏发生了变化刺激微生物活性的微环境,以及(ii)更大的残留物与土壤的接触。混合过程中残渣与土壤之间更大的接触也使矿物土壤中回收的残渣衍生碳增加了2倍,其中大部分(56%)位于活性碳库中。在12个月的时间里,高输入量下以及残留物与表层土混合时,GH气体通量使C的固存超过了。必须在一系列条件下以及长期内全面评估碳封存政策和相关的管理方法,以确保不提倡有害的做法。 (C)2016 Elsevier Ltd.保留所有权利。

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