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Tillage effects on N2O emissions as influenced by a winter cover crop

机译:冬季覆盖作物对耕作对N2O排放的影响

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Conservation tillage practices are widely used to protect against soil erosion and soil C losses, whereas winter cover crops are used mainly to protect against N losses during autumn and winter. For the greenhouse gas balance of a cropping system the effect of reduced tillage and cover crops on N2O emissions may be more important than the effect on soil C. This study monitored emissions of N2O between September 2008 and May 2009 in three tillage treatments, i.e., conventional tillage (CT), reduced tillage (RI) and direct drilling (DD), all with (+CC) or without (-CC) fodder radish as a winter cover crop. Cover crop growth, soil mineral N dynamics, and other soil characteristics were recorded. Furthermore, soil concentrations of N2O were determined eight times during the monitoring period using permanently installed needles. There was little evidence for effects of the cover crop on soil mineral N. Following spring tillage and slurry application soil mineral N was dominated by the input from slurry. Nitrous oxide emissions during autumn, winter and early spring remained low, although higher emissions from +CC treatments were indicated after freezing events. Following spring tillage and slurry application by direct injection N2O emissions were stimulated in all tillage treatments, reaching 250-400 mu g N m(-2) h(-1) except in the CT + CC treatment, where emissions peaked at 900 mu g N M-2 h(-1). Accumulated emissions ranged from 1.6 to 3.9 kg N2O ha(-1). A strong positive interaction between cover crop and tillage was observed. Soil concentration profiles of N2O showed a significant accumulation of N2O in CT relative to RI and DD treatments after spring tillage and slurry application, and a positive interaction between slurry and cover crop residues. A comparison in early May of N2O emissions with flux estimates based on soil concentration profiles indicated that much of the N2O emitted was produced near the soil surface
机译:保护性耕作实践被广泛用于防止土壤侵蚀和土壤碳损失,而冬季覆盖作物主要用于防止秋冬季节的氮素损失。对于耕作系统的温室气体平衡而言,耕作和覆盖作物减少对N2O排放的影响可能比对土壤C的影响更为重要。这项研究在2008年9月至2009年5月之间通过三种耕作处理监测了N2O的排放,即常规耕作(CT),减耕(RI)和直接钻探(DD),全部使用(+ CC)或不使用(-CC)饲料萝卜作为冬季覆盖作物。记录了覆盖作物的生长,土壤矿质氮的动力学以及其他土壤特征。此外,在监测期间,使用永久安装的针头测定了N2O的土壤浓度八次。几乎没有证据表明覆盖作物对土壤矿质N的影响。春季耕作和施用泥浆后,土壤矿质N以泥浆的投入为主导。秋季,冬季和早春期间的一氧化二氮排放量仍然较低,尽管在冰冻事件后表明+ CC处理的排放量较高。在春季耕作和通过直接注入施用泥浆后,在所有耕作处理中均会刺激N2O排放,达到250-400μgN m(-2)h(-1),但CT + CC处理除外,后者的排放峰值为900μg N M-2 h(-1)。累积排放量为1.6至3.9 kg N2O ha(-1)。观察到覆盖作物和耕作之间有很强的正向相互作用。在春季耕作和施用泥浆后,相对于RI和DD处理,N2O的土壤浓度剖面显示出CT中N2O的大量积累,并且泥浆和农作物残留之间存在正向相互作用。 5月初,N2O排放量与基于土壤浓度曲线的通量估算值进行了比较,结果表明,大量N2O排放量产生于土壤表面附近

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