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Impact of reduced tillage on greenhouse gas emissions and soil carbon stocks in an organic grass-clover ley - winter wheat cropping sequence

机译:有机三叶草-冬小麦种植顺序中耕作减少对温室气体排放和土壤碳储量的影响

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摘要

Organic reduced tillage aims to combine the environmental benefits of organic farming and conservation tillage to increase sustainability and soil quality. In temperate climates, there is currently no knowledge about its impact on greenhouse gas emissions and only little information about soil organic carbon (SOC) stocks in these management systems. We therefore monitored nitrous oxide (N2O) and methane (CH4) fluxes besides SOC stocks for two years in a grass-clover ley – winter wheat – cover crop sequence. The monitoring was undertaken in an organically managed long-term tillage trial on a clay rich soil in Switzerland. Reduced tillage (RT) was compared with ploughing (conventional tillage, CT) in interaction with two fertilisation systems, cattle slurry alone (SL) versus cattle manure compost and slurry (MC). Median N2O and CH4 flux rates were 13 μg N2O-N m−2 h−1 and −2 μg CH4C m−2 h−1, respectively, with no treatment effects. N2O fluxes correlated positively with nitrate contents, soil temperature, water filled pore space and dissolved organic carbon and negatively with ammonium contents in soil. Pulse emissions after tillage operations and slurry application dominated cumulative gas emissions. N2O emissions after tillage operations correlated with SOC contents and collinearly to microbial biomass. There was no tillage system impact on cumulative N2O emissions in the grass-clover (0.8–0.9 kg N2O-N ha−1, 369 days) and winter wheat (2.1–3.0 kg N2O-N ha−1, 296 days) cropping seasons, with a tendency towards higher emissions in MC than SL in winter wheat. Including a tillage induced peak after wheat harvest, a full two year data set showed increased cumulative N2O emissions in RT than CT and in MC than SL. There was no clear treatment influence on cumulative CH4 uptake. Topsoil SOC accumulation (0–0.1 m) was still ongoing. SOC stocks were more stratified in RT than CT and in MC than SL. Total SOC stocks (0–0.5 m) were higher in RT than CT in SL and similar in MC. Maximum relative SOC stock difference accounted for +8.1 Mg C ha−1 in RT-MC compared to CT-SL after 13 years which dominated over the relative increase in greenhouse gas emissions. Under these site conditions, organic reduced tillage and manure compost application seems to be a viable greenhouse gas mitigation strategy as long as SOC is sequestered.
机译:减少有机耕作旨在将有机耕作和保护性耕作的环境效益结合起来,以提高可持续性和土壤质量。在温带气候下,目前尚不了解其对温室气体排放的影响,在这些管理系统中,关于土壤有机碳(SOC)储备的信息很少。因此,我们在草苜蓿(冬小麦)覆盖作物序列中监测了除了SOC存量以外的一氧化二氮(N2O)和甲烷(CH4)通量。该监测是在瑞士的富含粘土的土壤上进行的有机管理的长期耕作试验中进行的。在两个施肥系统(单独的牛粪(SL)与牛粪堆肥和粪便(MC))的相互作用下,将耕作减少(RT)与耕作(常规耕作,CT)进行了比较。 N2O和CH4的通量中位数速率分别为13μgN2O-N m-2 h-1和-2μgCH4C m-2 h-1,没有治疗效果。 N2O通量与硝酸盐含量,土壤温度,含水孔隙空间和溶解的有机碳呈正相关,与土壤中的铵含量呈负相关。耕作和施用泥浆后的脉冲排放量占累积气体排放量的大部分。耕作后的N2O排放与SOC含量相关,并与微生物生物量共线。在三叶草(0.8–0.9 kg N2O-N ha-1,369天)和冬小麦(2.1–3.0 kg N2O-N ha-1,296天)耕作季节中,耕作制度对累积N2O排放没有影响。 ,冬小麦的MC排放量要高于SL。包括两年小麦收割后的耕作诱导的高峰在内,整整两年的数据表明,RT上的累积N2O排放量比CT和MC上的累积N2O都高。累积的CH4摄取对治疗没有明显影响。表土的SOC累积(0-0.1 m)仍在进行中。相对于CT,在SOC中,SOC的股票层次比SL更明显。 RT上的总SOC储量(0-0.5 m)高于SL的CT和MC的相似。 13年后,RT-MC与CT-SL相比,最大相对SOC储量差异为+8.1 Mg C ha-1,占主导地位的是温室气体排放量的相对增加。在这些场所条件下,只要隔离SOC,减少有机耕作和肥料堆肥的施用似乎是可行的温室气体减排策略。

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