首页    期刊浏览 2024年12月03日 星期二
登录注册

文章基本信息

  • 标题:Effect of microtopography on isotopic composition of methane in porewater and efflux at a boreal peatland
  • 本地全文:下载
  • 作者:Maxim Dorodnikov ; Maija Marushchak ; Christina Biasi
  • 期刊名称:Boreal Environment Research
  • 印刷版ISSN:1239-6095
  • 出版年度:2013
  • 卷号:18
  • 期号:3-4
  • 页码:269-279
  • 语种:English
  • 出版社:Finnish Limnological Society
  • 摘要:The application of stable isotopes is an approach to identify pathways of methanogenesis, methane (CH4) oxidation and transport in peatlands. We measured the stable C isotopic characteristics (δ13C) of CH4 in peat profiles below hummocks, lawns and hollows of a Finnish mire to study the patterns of CH4 turnover. Porewater CH4 concentrations ([CH4]; at 0.5–2 m) increased with depth below all microforms. Emissions of CH4 from hummocks were the lowest, and increased with the increasing water-saturated zone, being ~10 times higher from hollows. Thus, the microtopography of the peatland did not affect the porewater [CH4] in the water-saturated part of the peat profile, but the CH4 emissions were affected due to differences in the oxidative potential of the microforms. There was a decrease in δ13C-CH4 with depth below all microforms indicating dominance of CO2- reduction over acetate cleavage pathway of methanogenesis at deep peat layers. However, estimated potential portions of transported CH4 comprised 50%–70% of the δ13C-CH4 enrichment on microforms at the 0.5-m depth, hereby masking the acetate cleavage pathway of methanogenesis. Stable C composition (δ13C) of CH4 proved to be a suitable (but not sufficient) tool to differentiate between types of methanogenesis in continuously watersaturated layers below microforms of a peatland. Combined flux-based and multi-isotopic approaches are needed to better understand the CH4 turnover process.
国家哲学社会科学文献中心版权所有