首页> 外文期刊>Geoderma: An International Journal of Soil Science >Methane and nitrous oxide emissions from flooded rice fields as affected by water and straw management between rice crops
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Methane and nitrous oxide emissions from flooded rice fields as affected by water and straw management between rice crops

机译:稻田间水和稻草管理对稻田中甲烷和一氧化二氮排放的影响

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摘要

Rice fields in the tropics can vary in water regime before production of rice on flooded soil, but relatively little is known about the effects of soil water regime and crop residue management between rice crops (i.e., fallow period) on methane (CH4) and nitrous oxide (N2O) emissions during a subsequent rice crop. We measured CH4 and N2O emissions during two cropping seasons in the Philippines from field plots exposed to contrasting treatments during the fallow before land preparation for rice cultivation. The fallow treatments were continuous soil flooding (flooded), soil drying with exclusion of rainfall (dry), soil drying with dry tillage (dry + tillage), and a control with soil drying and wetting from rainfall (dry and wet). All plots were subdivided into removal of all aboveground rice residues from the previous crop (without residue) and retention of standing biomass after harvest of the previous rice crop (with residue). Emitted gas was collected weekly using chambers. Fallow treatments greatly influenced greenhouse gas (GHG) emissions during rice growth. Methane emissions and global warming potential (GWP) in both cropping seasons were highest following the flooded fallow, intermediate following the dry and wet fallow, and lowest following dry and dry + tillage fallows. The GWP was higher with than without residue across all fallow treatments. Nitrous oxide emissions were small during the season, and CH4 emissions contributed more than 90% of the cumulative GWP during the rice crop regardless of fallow and residue management. Soil drying between rice crops in the tropics can reduce CH4 emissions and GWP during the subsequent rice crop
机译:热带地区的稻田在淹没土壤上生产水稻之前,水分状况可能会有所不同,但是人们对土壤水分状况和水稻作物之间的作物残留管理(即休耕期)对甲烷(CH4)和亚硝酸盐的影响知之甚少随后的稻谷作物中的氧化物(N2O)排放。我们测量了菲律宾两个作物种植季节的甲烷和一氧化二氮排放量,这些土地是在水稻耕地整地前在休耕期间接受对比处理的田间田地。休耕处理包括连续的土壤淹水(淹水),不包括降雨的土壤干燥(干燥),采用干耕的土壤干燥(干+耕作)和采用降雨干燥和湿润的土壤对照(干湿)。所有地块都细分为从上一茬作物中清除所有地上稻米残留物(无残留),并在收获前一稻作物后(残留物)保留剩余生物量。使用隔室每周收集一次排放的气体。休耕处理极大地影响了水稻生长期间的温室气体排放。在两个农作物季节中,甲烷的排放量和全球变暖潜能值在洪涝休耕后最高,在干湿休耕后居中,而在干湿休耕后最低。在所有休养期治疗中,GWP均高于无残留。在本季节中,一氧化二氮排放量很小,无论休耕和残留管理如何,CH4排放量占稻谷作物累积GWP的90%以上。热带地区水稻作物之间的土壤干燥可以减少随后的水稻作物中的CH4排放量和GWP

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