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冬作季节土地管理对水稻土CH4排放季节变化的影响
引用本文:徐华,蔡祖聪,李小平,鹤田治雄.冬作季节土地管理对水稻土CH4排放季节变化的影响[J].应用生态学报,2000,11(2):215-218.
作者姓名:徐华  蔡祖聪  李小平  鹤田治雄
作者单位:1. 中国科学院南京土壤研究所,南京,210008
2. 日本国立农业环境技术研究所,筑波,305
基金项目:中国科学院资助项目,中国科学院实验室基金 
摘    要:通过温室盆栽试验对水稻土CH4排放的生节变化及冬作季节土地管理的影响进行了研究,结果表明,冬作季节种植紫云英、淹水休闲及干燥休闲但泡水前施用稻草处理泡水后30dCH4排放量分别高达133d观测期总排放量的675%、35.5%及33.3%,且在泡水后第13天及水稻移栽后第7、40、91天分别出现4个CH4排放高峰;而种植小麦和干燥休闲但冬作前施用稻草处理泡水后55dCH4排放量才占观测期总排放量的6

关 键 词:甲烷  排放通量  季节变化  冬季  土地管理  稻田
修稿时间:1998-08-10

Effect of land management in winter crop season on seasonal variations of CH4 emissions from rice paddy soils
XU Hua,CAI Zucong,LI Xiaoping,Haruo Tsuruta.Effect of land management in winter crop season on seasonal variations of CH4 emissions from rice paddy soils[J].Chinese Journal of Applied Ecology,2000,11(2):215-218.
Authors:XU Hua  CAI Zucong  LI Xiaoping  Haruo Tsuruta
Institution:Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008.
Abstract:A pot experiment in greenhouse was carried out to study seasonal variations of CH4 fluxes from rice paddy soils and the effect of land management in winter crop season on the seasonal variations. The results showed that four emission peaks occurred respectively 13 days after flooding and 7, 40, 91 days after rice transplanting, and CH4 emission amounts during the first 30 days after flooding accounted for as high as 67.5%, 35.5% and 33.3% of the total emission amounts during the observing period of 133 days for treatments with dry fallow but rice straw being applied just before flooding, alfalfa, and flooded fallow in winter crop season. However, for treatments with dry fallow but rice straw being applied before winter crop cultivating and winter wheat in winter crop season, CH4 emission amounts during the first 50 days after flooding just accounted for 0.27% and 6.74 of the total emission amounts during the observing period, and CH4 fluxes thereafter were also very small. Difference in the seasonal variation patterns of soil Eh due to land management in winter crop season was the main reason why seasonal variation patterns of CH4 fluxes from different treatments were different.
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