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青藏高原多年冻土区沼泽草甸土壤CH_4产生速率研究
引用本文:赵拥华,杜二计,刘广岳,岳广阳.青藏高原多年冻土区沼泽草甸土壤CH_4产生速率研究[J].冰川冻土,2011,33(5):999-1005.
作者姓名:赵拥华  杜二计  刘广岳  岳广阳
作者单位:中国科学院青藏高原冰冻圈综合观测研究站,冰冻圈科学国家重点实验室,中国科学院寒区旱区环境与工程研究所,甘肃兰州730000;中国科学院青藏高原冰冻圈综合观测研究站,冰冻圈科学国家重点实验室,中国科学院寒区旱区环境与工程研究所,甘肃兰州730000;中国科学院青藏高原冰冻圈综合观测研究站,冰冻圈科学国家重点实验室,中国科学院寒区旱区环境与工程研究所,甘肃兰州730000;中国科学院青藏高原冰冻圈综合观测研究站,冰冻圈科学国家重点实验室,中国科学院寒区旱区环境与工程研究所,甘肃兰州730000
基金项目:国家重点基础研究发展计划项目(2010CB951402); 中国科学院冰冻圈科学国家重点实验室自主课题(SKLCS-ZZ-2008-01); 国家自然科学基金项目(40701033)资助
摘    要:用实验室培养法对青藏高原多年冻土区沼泽草甸土壤不同温度条件下的CH4产生速率进行了研究.结果表明:CH4产生速率与温度之间呈现显著的指数关系,整个土壤剖面平均CH4生成速率和CH4生成速率初始值随温度的变化具有显著的相似性,都表现出随温度的升高而增加规律,0℃、5℃、18℃时的CH4生成速率分别是-18℃时的5.7、1...

关 键 词:沼泽草甸  土壤  CH4产生速率  多年冻土  青藏高原

Study of Soil Methane Production Rate from Marsh Meadow in Permafrost Regions on Tibetan Plateau
ZHAO Yong-hua,DU Er-ji,LIU Guang-yue,YUE Guang-yang.Study of Soil Methane Production Rate from Marsh Meadow in Permafrost Regions on Tibetan Plateau[J].Journal of Glaciology and Geocryology,2011,33(5):999-1005.
Authors:ZHAO Yong-hua  DU Er-ji  LIU Guang-yue  YUE Guang-yang
Institution:ZHAO Yong-hua,DU Er-ji,LIU Guang-yue,YUE Guang-yang(Cryosphere Research Station on Qinghai-Tibet Plateau,State Key Laboratory of Cryospheric Sciences,Cold and Arid Regions Environment and Engineering Research Instute,Chinese Academy of Sciences,Lanzhou Gansu 730000,China)
Abstract:Soil methane production rate from marsh meadow in permafrost regions on the Tibetan Plateau at various temperatures were determined using an anaerobic incubation technique.The results show that there is a significant exponential correlation between methane production rate and temperature and the methane production rate averaged over all soil layers and the initial methane production rate have pronounced comparability(n=4,p<0.05),increasing with temperature.The methane production rate at 0 ℃,5 ℃,18 ℃ is 5.7,171.4 and 3 257 time more than that at-18 ℃.At 0 ℃,5 ℃,18 ℃,the vertical profile of methane production rates has "U" shape,with the higher rate at the ranges of 0~20 cm and 20~80 cm,and the lowest rate at the range of 20~80 cm.But at-18 ℃ there is no obvious changing tendency.The average methane production rates of various depths significantly correlate with incubation time at the incubation temperatures of-18 ℃,0 ℃,5 ℃,18 ℃(n=9,R+2=0.55;n=9,R+2=0.99;n=9,R+2=0.96;n=9,R+2=0.96).However,the ranges of the average methane production rates of various soil layers have obvious difference for all incubation temperatures with incubation time of 1~72 hour,for example,0.005~0.008,0.93~1.49 and 16.4~30.7 ng·g+-15h+-1 at-18 ℃,5 ℃,18 ℃,with the variation rate of 160%,160% and 187%.At 0 ℃ the range of methane production rate was 0.02~0.06 ng·g-15h-1,equivalent to a variation rate of 300%,which is the maximum.It is found that the methane production rate has no significant correlation with soil organic carbon,but the methane production rate of various soil layers has significant correlation with soil pH value at the incubation temperature of 0 ℃,5 ℃,18 ℃.At the same time,it is revealed that the methane production rate has significant correlation with soil mechanical composition.
Keywords:marsh meadow  soil  methane production rate  permafrost  Tibetan Plateau  
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