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Changes in fertilizer-induced direct NO emissions from paddy fields during rice-growing season in China between 1950s and 1990s

机译:1950年代至1990年代中国水稻生长季肥料引起的稻田直接NO排放量的变化

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Nitrogen fertilizer-induced direct nitrous oxide (NO) emissions depend on water regimes in paddy fields, such as seasonal continuous flooding (F), flooding-midseason drainage-reflooding (F-D-F), and flooding-midseason drainage-reflooding-moist intermittent irrigation but without water logging (F-D-F-M). In order to estimate the changes in direct NO emission from paddy fields during the rice-growing season in Mainland of China between the 1950s and the 1990s, the country-specific emission factors ofNO-N under different water regimes combined with rice production data were adopted in the present study. Census statistics on rice production showed that water management and nitrogen input regimes have changed in rice paddies since the 1950s. During the 1950s-1970s, about 20-25% of the rice paddy was continuously waterlogged, and 75-80% under the water regime of F-D-F. Since the 1980s, about 12-16%, 77%, and 7-12% of paddy fields were under the water regimes of F, F-D-F, and F-D-F-M, respectively. Total nitrogen input during the rice-growing season has increased from 87.5 kg N hap# in the 1950s to 224.6 kg N hap# in the 1990s. The emission factors of NO-N were estimated to be 0.02%, 0.42%, and 0.73% for rice paddies under the F, F-D-F, and F-D-F-M water regimes, respectively. Seasonal NO emissions have increased from 9.6 Gg NO-N each year in the 1950s to 32.3 Gg NO-N in the 1990s, which is accompanied by the increase in rice yield over the period 1950s-1990s. The uncertainties in NO estimate were estimated to be 59.8% in the 1950s and 37.5% in the 1990s. In the 1990s, NO emissions during the rice-growing season accounted for 8-11% of the reported annual total of NO emissions from croplands in China, suggesting that paddy rice development could havecontributed to mitigating agricultural NO emissions in the past decades. However, seasonal NO emissions would be increased, given that saving-water irrigation and nitrogen inputs are increasingly adopted in rice paddies in China.
机译:氮肥导致的直接一氧化二氮(NO)排放取决于稻田的水情,例如季节性连续洪水(F),汛期中排水排水-FDF和汛期中排水排水-潮湿间歇灌溉无需注水(FDFM)。为了估算1950年代至1990年代中国大陆水稻生长季稻田直接NO排放的变化,采用了不同水分制度下特定国家的NO-N排放因子,并结合水稻生产数据在目前的研究中。稻米生产的普查统计数据表明,自1950年代以来,稻田的水分管理和氮素输入方式已发生变化。在1950年代至1970年代期间,大约20-25%的稻田被连续淹水,而在F-D-F的水域下则持续淹水75-80%。自1980年代以来,分别有F,F-D-F和F-D-F-M的水域下的稻田分别占12-16%,77%和7-12%。水稻生长期的总氮输入量从1950年代的87.5千克N hap#增加到1990年代的224.6千克N hap#。在F,F-D-F和F-D-F-M水分制度下,稻田的NO-N排放因子估计分别为0.02%,0.42%和0.73%。季节性NO排放量从1950年代的每年9.6 Gg NO-N增加到1990年代的32.3 Gg的NO-N,伴随着1950s-1990年代的稻米产量增加。 NO估计的不确定性在1950年代估计为59.8%,在1990年代估计为37.5%。在1990年代,水稻生长季节的一氧化氮排放量占中国农田每年报告的一氧化氮排放总量的8-11%,这表明在过去的几十年中,水稻的发展可能有助于减轻农业的一氧化氮排放。然而,鉴于中国稻田越来越多地采用节水灌溉和氮素输入,季节性NO排放量将增加。

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