应用生态学报2017，Vol.28Issue(7)：2269-2276,8.DOI:10.13287/j.1001-9332.201707.026
不同灌溉量对华北平原菜地N2O排放及其来源的影响
Effects of soil water condition on N2O emission and its sources in vegetable farmland of North China Plain
摘要
Abstract
To understand the mechanisms of agricultural N2 O emission,we investigated the N2 O emission dynamics,the N2O isotope signatures,and the site preference value under different soil water conditions in the vegetable farmland of North China,by using the stable isotope technique and the acetylene inhibition method.The results demonstrated that N2O emission was significantly affected by the water condition,and N2 O emissions from soil with water-filled pore space (WFPS) of 70％ were significantly higher than that with 50％ WFPS.N2O emission occurred mostly in the early stage of fertilization,and decreased rapidly in the later stage of fertilization.At 50％ WFPS,nitrification was the major process generating N2O during the early fertilization stage,accounting for approximately 90％ of the N2O emission.However,the contribution of nitrification decreased sharply,whereas denitrification became the dominant process,accounting for 80％ of the N2O emission 7 days after the fertilization.On the other hand,at 70％ WFPS,denitrification was the main process releasing N2O during the early fertilization stage,decreasing from 70％ to 40％ and then gradually increasing to 80％ 10 days after the fertilization.Overall,N2O emission was mainly dominated by the denitrification.The effect of different water treatments on soil nitrification and denitrification took place mainly in the early stage of fertilization,and N2O emission was gradually dominated by the denitrification at the later stage.These results suggested we could reduce N2O emission by appropriately reducing the amount of irrigation in the vegetable farmland of North China.关键词
N2O/稳定同位素/SP值/硝化作用/反硝化作用/灌溉Key words
N2O/stable isotope/site preference value/nitrification/denitrification/irrigation引用本文复制引用
丁军军,张薇,李玉中,林伟,徐春英,李巧珍..不同灌溉量对华北平原菜地N2O排放及其来源的影响[J].应用生态学报,2017,28(7):2269-2276,8.基金项目
本文由国家自然科学基金项目(41473004,41501318,41301553)资助 This work was supported by the National Natural Science Foundation of China (41473004,41501318,41301553). （41473004,41501318,41301553）
