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Geoscience ›› 2018, Vol. 32 ›› Issue (05): 1089-1096.DOI: 10.19657/j.geoscience.1000-8527.2018.05.22

• Applied Geochemistry • Previous Articles     Next Articles

Research on the Methane Emission and Carbon Isotope of Permafrost Wetland in Qinghai-Tibet Plateau

ZHANG Shunyao1,2,3(), YANG Fan2,3(), ZHANG Fugui2,3, SHI Zeming1, YANG Zhibin2,3, ZHOU Yalong2,3, WANG Huiyan2,3   

  1. 1. College of Earth Sciences, Chengdu University of Technology, Chengdu, Sichuan 610059, China
    2. Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang, Hebei 065000, China
    3. Key Laboratory of Geochemical Cycling of Carbon and Mercury in the Earth’s Critical Zone, Chinese Academy of Geological Sciences, Langfang, Hebei 065000, China
  • Received:2018-03-05 Revised:2018-07-12 Online:2018-10-10 Published:2018-11-04

Abstract:

As one of the most important wetland area component, carbon cycle in Qinghai-Tibet Plateau plays a critical role in the terrestrial ecosystem. For systematically studying the methane emission of permafrost wetland in Qinghai-Tibet Plateau, by using the chamber method, we made a field measurement on the methane carbon isotope. Furthermore, combining with the adsorbed gas chromatography result, we conducted the gas source discrimination. The results show that the soil methane emission is the highest and mainly on biogenic source in spring. In summer, methane of soil emission is mainly on mixed-genetic source. In autumn, the soil methane emission is the lowest and mainly on thermo genic gas. The biological action is the main influence factor of methane emission. Meanwhile, the gas escaped from the natural gas hydrate underground also influenced the atmospheric methane content to some extent.

Key words: Qinghai-Tibet Plateau, methane emission, methane carbon isotope, natural gas hydrate

CLC Number: