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青藏高原开阔湿地甲烷排放的年际变化:一项为期三年的研究。

Inter-annual variations of methane emission from an open fen on the Qinghai-Tibetan Plateau: a three-year study.

机构信息

Chengdu Institute of Biology, Chinese Academy of Sciences, Chengdu, China.

出版信息

PLoS One. 2013;8(1):e53878. doi: 10.1371/journal.pone.0053878. Epub 2013 Jan 14.

Abstract

The study aimed to understand the inter-annual variations of methane (CH(4)) emissions from an open fen on the Qinghai-Tibetan Plateau (QTP) from 2005 to 2007. The weighted mean CH(4) emission rate was 8.37±11.32 mg CH(4) m(-2 )h(-1) during the summers from 2005 to 2007, falling in the range of CH(4) fluxes reported by other studies, with significant inter-annual and spatial variations. The CH(4) emissions of the year of 2006 (2.11±3.48 mg CH(4) m(-2 )h(-1)) were 82% lower than the mean value of the years 2005 and 2007 (13.91±17.80 mg CH(4) m(-2 )h(-1) and 9.44±14.32 mg CH(4) m(-2 )h(-1), respectively), responding to the inter-annual changes of standing water depths during the growing season of the three years. Significant drawdown of standing water depth is believed to cause such significant reduction in CH(4) emissions from wetlands in the year 2006, probably through changing the methanogen composition and decreasing its community size as well as activating methanotrophs to enhance CH(4) oxidation. Our results are helpful to understand the inter-annual variations of CH(4) emission and provide a more reasonable regional budget of CH(4) emission from wetlands on the QTP and even for world-wide natural wetlands under climate change.

摘要

本研究旨在了解青藏高原(QTP)开阔湿地 2005-2007 年甲烷(CH(4))排放的年际变化。2005-2007 年夏季加权平均 CH(4)排放率为 8.37±11.32 mg CH(4) m(-2 )h(-1),与其他研究报道的 CH(4)通量范围相当,具有显著的年际和空间变化。2006 年(2.11±3.48 mg CH(4) m(-2 )h(-1))的 CH(4)排放量比 2005 年和 2007 年的平均值低 82%(分别为 13.91±17.80 mg CH(4) m(-2 )h(-1)和 9.44±14.32 mg CH(4) m(-2 )h(-1)),这与三年生长季期间积水深度的年际变化相对应。积水深度的显著下降被认为是导致 2006 年湿地 CH(4)排放量显著减少的原因,这可能是通过改变产甲烷菌的组成、减少其群落大小以及激活甲烷氧化菌来增强 CH(4)氧化作用所致。我们的研究结果有助于了解 CH(4)排放的年际变化,并为青藏高原湿地乃至全球自然湿地在气候变化下的 CH(4)排放提供更合理的区域估算。

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