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种稻盆钵土壤甲烷排放通量变化的研究
引用本文:徐华,蔡祖聪.种稻盆钵土壤甲烷排放通量变化的研究[J].生态与农村环境学报,1999(1).
作者姓名:徐华  蔡祖聪
作者单位:中国科学院南京土壤研究所
摘    要:通过温室盆栽试验,研究了不同冬作处理时后茬水稻生长期甲烷排放通量及土壤温度、土壤Eh的日变化规律。结果表明:连续晴天甲烷排放通量和土壤温度存在明显的昼夜变化,最大值出现在下午4时左右,最小值出现在凌晨4时左右,符合余弦函数变化规律;连续阴雨天甲烷排放通量有逐日降低的趋势,但其昼夜变化缺乏规律性。种稻盆钵土壤甲烷排放通量昼夜变化主要受0~10cm深土壤温度的影响,而与土壤氧化还原电位无关。

关 键 词:甲烷  排放通量  土壤温度  土壤氧化还原电位

Study on Diurnal Variations of CH 4 Fluxes from Rice Soils in Pots.
Xu Hua,et al.Study on Diurnal Variations of CH 4 Fluxes from Rice Soils in Pots.[J].Journal of Ecology and Rural Environment,1999(1).
Authors:Xu Hua
Abstract:A pot culture experiment of rice in greenhouse was carried out to investigate the diurnal variations of CH 4 fluxes,soil temperatures and soil Eh during rice growing period with different treatments applied in the former winter cropping season.The results showed that there existed obvious diurnal variations of CH 4 fluxes and soil temperatures in continuous fine days.The maximum fluxes occurred at 4 pm while the minimum fluxes at about 4 am,and the variation patterns of CH 4 fluxes and soil temperatures were in conformity with cosine function of time t as a variable.Methane fluxes in continuous overcast and rainy days had a decreasing tendency day by day,and its diurnal variations could not be fitted with a cosine functional curve of time t .Diurnal variations of CH 4 fluxes were mainly influenced by soil temperature at 0 10 cm soil depth.And there is no influence of soil Eh on diurnal variations of CH 4 fluxes.
Keywords:CH  4      emission flux  soil temperature  soil Eh  
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