Can abundance of methanogen be a good indicator for CH4 flux in soil ecosystems?

Jinhyun Kim, Seung Hoon Lee, Inyoung Jang, Sang Seom Jeong, Hojeong Kang

Research output: Contribution to journalArticle

4 Citations (Scopus)

Abstract

Methane, which is produced by methanogenic archaea, is the second most abundant carbon compound in the atmosphere. Due to its strong radiative forcing, many studies have been conducted to determine its sources, budget, and dynamics. However, a mechanistic model of methane flux has not been developed thus far. In this study, we attempt to examine the relevance of the abundance of methanogen as a biological indicator of methane flux in three different types of soil ecosystems: permafrost, rice paddy, and mountainous wetland. We measured the annual average methane flux and abundance of methanogen in the soil ecosystems in situ. The correlation between methane flux and the abundance of methanogen exists only under a specific biogeochemical conditions such as SOM of higher than 60 %, pH of 5.6–6.4, and water-saturated. Except for these conditions, significant correlations were absent. Therefore, microbial abundance information can be applied to a methane flux model selectively depending on the biogeochemical properties of the soil ecosystem.

Original languageEnglish
Pages (from-to)1007-1015
Number of pages9
JournalEnvironmental Geochemistry and Health
Volume37
Issue number6
DOIs
Publication statusPublished - 2015 Dec 1

Fingerprint

Methanogens
soil ecosystem
Methane
Ecosystems
methane
Fluxes
Soils
Permafrost
Wetlands
radiative forcing
bioindicator
permafrost
indicator
Carbon
rice
wetland
Water
atmosphere
carbon

All Science Journal Classification (ASJC) codes

  • Environmental Engineering
  • Environmental Chemistry
  • Water Science and Technology
  • Environmental Science(all)
  • Geochemistry and Petrology

Cite this

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title = "Can abundance of methanogen be a good indicator for CH4 flux in soil ecosystems?",
abstract = "Methane, which is produced by methanogenic archaea, is the second most abundant carbon compound in the atmosphere. Due to its strong radiative forcing, many studies have been conducted to determine its sources, budget, and dynamics. However, a mechanistic model of methane flux has not been developed thus far. In this study, we attempt to examine the relevance of the abundance of methanogen as a biological indicator of methane flux in three different types of soil ecosystems: permafrost, rice paddy, and mountainous wetland. We measured the annual average methane flux and abundance of methanogen in the soil ecosystems in situ. The correlation between methane flux and the abundance of methanogen exists only under a specific biogeochemical conditions such as SOM of higher than 60 {\%}, pH of 5.6–6.4, and water-saturated. Except for these conditions, significant correlations were absent. Therefore, microbial abundance information can be applied to a methane flux model selectively depending on the biogeochemical properties of the soil ecosystem.",
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Can abundance of methanogen be a good indicator for CH4 flux in soil ecosystems? / Kim, Jinhyun; Lee, Seung Hoon; Jang, Inyoung; Jeong, Sang Seom; Kang, Hojeong.

In: Environmental Geochemistry and Health, Vol. 37, No. 6, 01.12.2015, p. 1007-1015.

Research output: Contribution to journalArticle

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T1 - Can abundance of methanogen be a good indicator for CH4 flux in soil ecosystems?

AU - Kim, Jinhyun

AU - Lee, Seung Hoon

AU - Jang, Inyoung

AU - Jeong, Sang Seom

AU - Kang, Hojeong

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AB - Methane, which is produced by methanogenic archaea, is the second most abundant carbon compound in the atmosphere. Due to its strong radiative forcing, many studies have been conducted to determine its sources, budget, and dynamics. However, a mechanistic model of methane flux has not been developed thus far. In this study, we attempt to examine the relevance of the abundance of methanogen as a biological indicator of methane flux in three different types of soil ecosystems: permafrost, rice paddy, and mountainous wetland. We measured the annual average methane flux and abundance of methanogen in the soil ecosystems in situ. The correlation between methane flux and the abundance of methanogen exists only under a specific biogeochemical conditions such as SOM of higher than 60 %, pH of 5.6–6.4, and water-saturated. Except for these conditions, significant correlations were absent. Therefore, microbial abundance information can be applied to a methane flux model selectively depending on the biogeochemical properties of the soil ecosystem.

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