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Gross mineralization, nitrification and N2O emission under different tillage in the North China Plain

机译:华北平原不同耕作方式下的总矿化,硝化和N2O排放

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摘要

No-tillage cropping can increase soil carbon (C) stocks and aggregation, and subsequently impact the internal nitrogen (N) cycle and gas loss. The 15N pool dilution method was used to study gross N transformations, and relative proportions of nitrous oxide (N2O) emissions derived from denitrification versus nitrification-related processes under long-term tillage systems (no-tillage, rotary tillage and conventional tillage) in the North China Plain. In-field incubation experiments were repeated in successive growing seasons during April-November in 2007. Gross mineralization rates for rotary and mouldboard plough tillage (3.6+or-0.3-10.6+or-1.5 mg N kg-1 days-1) were significantly higher than for no-tillage (1.7+or-0.8-6.8+or-1.1 mg N kg-1 days-1). Gross mineralization was positively correlated with soil moisture and temperature, as well as with microbial biomass N and C. However, there was no consistent tillage effect on gross nitrification, and gross nitrification was positively correlated with soil moisture, but not with gross mineralization and microbial biomass. N2O emissions were higher in no-tillage (NT) than for conventional tillage (CT) during May-August. The 15N labelling indicated that 26-92% of the N2O was directly derived from the soil ammonium (NH4+) pool. Emission rates of N2O from both nitrification and denitrification were positively correlated with NH4+ supply as expressed by gross mineralization, but not correlated with supply of nitrate as expressed by gross nitrification. The fraction of nitrified N emitted as N2O was positively correlated with changes in soil moisture and varied within 0.01-2.51 per mil. Our results showed that the tillage management impact on gross N transformation was not consistent with N2O emission, and more detailed information on the controls over N2O formation needs to be sought.
机译:免耕种植会增加土壤碳(C)的存量和聚集,进而影响内部氮(N)循环和气体损失。 15 N池稀释法用于研究总氮转化率以及长期反硝化与硝化相关过程产生的一氧化二氮(N 2 O)排放的相对比例华北平原长期耕作制度(免耕,轮耕和常规耕作)。在2007年4月至11月的连续生长季节中重复进行了田间孵化试验。旋耕机和犁板耕作的总矿化率(3.6 +或-0.3-10.6 +或-1.5 mg N kg -1 天 -1 )明显高于免耕(1.7 + or-0.8-6.8 +或-1.1 mg N kg -1 days -1 )。总矿化与土壤水分和温度以及微生物生物量氮和碳呈正相关。但是,耕作对总硝化没有持续的影响,总硝化与土壤水分呈正相关,但与总矿化和微生物无正相关。生物质。免耕(NT)的N 2 O排放量高于常规耕作(CT)的5-8月。 15 N标记表明N 2 O的26-92%直接来自土壤铵盐(NH 4 + )池。硝化和反硝化过程中N 2 O的排放速率与总矿化所表达的NH 4 + 供给呈正相关,但与总硝化表示的硝酸盐供应。 N 2 O排放的硝化氮分数与土壤水分变化呈正相关,且在0.01-2.51 / mil之间变化。我们的研究结果表明,耕作管理对总氮转化的影响与N 2 O的排放不一致,因此需要更详细的控制N 2 O形成的信息。寻求。

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