Rasmussen R A, Khalil M A K.Atmospheric methane:trends and seasonal cycles. J Geophys Res, 1981, 86:9826～9832
[2]
Crutzen P J. Methane\'s sinks and source. Nature,1991, 350:380～381
[3]
Dickinson R E, Cicerone R J. Future global warming from atmospheric trace gasesNature, 1986, 319:109～115
[4]
叶笃正．中国的全球变化预研究．北京：气象出版社，1991
[5]
Khalil M A K, Rasmussen R A. Sources, sinks, and seasonal cycles of atmosphericmethane. J Geophys. Res, 1983, 88(9):5 131～5 144
[6]
Cicerone R J, Oremland R S. Biogeochemical aspects of atmospheric methane. GlobalBiogeochem Cycles, 1988, 2:299～327
[7]
Whiting G J, Chanton J P. Primary production control of methane emission fromwetlands. Nature, 1993, 364(26): 794～795
[8]
Seiler W, Holzpfel-Pschorn A, Conrad R, et al. Methane emission from rice paddies,JAtmos Chem,1984
[9]
Holzapfel-Pschorn A, Conrad R, Seiler W. Eftects of vegetation on the emission ofmethane by submerged paddy soil PlantSoil, 1986, 92:223～233
[10]
Cicerone R J, Shetter J D, Delwiehe C C. Seasonal variation of methane flux from aCalifornia rice paddy. J Geophys Res,1983. 88(C): 11 022～11 024
[11]
上官行健,王明星,沈壬兴.稻田CH4的排放规律.地球科学进展,1953,8(5):23～36
[12]
Kelley C A, Martens C S, Ussler W Ⅲ. Methane dynamics across a tidally floodedriverbank margin. Limnol Oceanogr,1995, 40(6): 1 112～1 129
[13]
Harriss R C, Ebacher D I, Bartlett K B. Et al. Sources of atmospheric methane inthe South Florida environment.Global Bio-geochem Cycle, 1988, 2(3): 231～243
[14]
Bartlett D S, Bartlett K B, Hartman J M, et al. Methane emissions from the Floridaeverglades:patterns of variability in a re-gional wetland ecosystem. Global BiogeochemCycles, 1989, 3:363～374
[15]
Sotomayor D, CorredorJ E, Morell J M. Methane flux from mangrove sediments alongthe southwestern coast of Puerto Ri-co.Estuaries, 1994, 17(1B): 140～147
[16]
Alford D P, DeLaune R D, Lindau C W. Methane flux from Mississipi River deltaicplain wetlands.Biogeochem, 1997, 37(3): 227～236
[17]
Bartlett KB, Harriss R C, Sobachar D Ⅰ. Methane flux from coastal salt marshes.JGeophys Res, 1985, 90(D3): 5710～5 720
