Preliminary studies on methane fluxes in Hainan mangrove communities

Lu Chang-yi; Wong Yuk-shan; Tam Nora F. Y.; Ye Yong; Cui Sheng-hui; Lin Peng

doi:10.1007/BF02848219

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Preliminary studies on methane fluxes in Hainan mangrove communities

OriginalPaper | Updated：2023-05-16

- Preliminary studies on methane fluxes in Hainan mangrove communities
- Preliminary studies on methane fluxes in Hainan mangrove communities
- 海洋湖沼学报（英文） 1998年16卷第1期页码：64-71
- Affiliations：
  
  1. Research Laboratory of SEDC of Marine Ecological Environment
  2. Research Centre/Biology Department
  3. Department of Biology and Chemistry
  4. Department of Biology
- Author bio：
- Funds：
  
  Project 49676298 supported by NSFC and this work also funded by Hong Kong University of Science & Technology.
- DOI：10.1007/BF02848219
  中图分类号：
- 纸质出版：1998
- Accepted：
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Preliminary studies on methane fluxes in Hainan mangrove communities[J]. 海洋湖沼学报（英文）, 1998,16(1):64-71.

Chang-yi, L., Yuk-shan, W., Nora F. Y., T. et al. Preliminary studies on methane fluxes in Hainan mangrove communities., Chin. J. Ocean. Limnol. 16, 64–71 (1998). https://doi.org/10.1007/BF02848219
Preliminary studies on methane fluxes in Hainan mangrove communities[J]. 海洋湖沼学报（英文）, 1998,16(1):64-71. DOI： 10.1007/BF02848219.

Chang-yi, L., Yuk-shan, W., Nora F. Y., T. et al. Preliminary studies on methane fluxes in Hainan mangrove communities., Chin. J. Ocean. Limnol. 16, 64–71 (1998). https://doi.org/10.1007/BF02848219 DOI：

摘要

Abstract

In this work

a static chamber technique was used to measure methane fluxes from sediments of six mangrove communities and polyethylene bags were used to measure methane fluxes across plant leaves of six mangrove species. Methane fluxes from mangrove sediments at the disturbed Ta—Shi (TS) site were higher than those at the other sites

indicating that organic matter in soil is an important source of methane fluxes from sediments. Tidal condition is more important than air and soil temperature in affecting diurnal variations of methane fluxes from mangrove sediments. The spatial differences of methane fluxes from sediments in three mudflat zones may be due to the differences of soil moisture. Methane fluxes across mangrove leaves may be negative or positive during different observation periods and mangrove leaves generally absorb atmospheric methane as an overall effect. Plant leaves of mangrove with pneumatophores absorb more atmospheric methane than those without pneumatophores.

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references

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