Increasing the pH of tropical peat can enhance methane production and methanogenic growth under anoxic conditions

• CH 4 production from tropical peat was examined by incubation at varying pH. • Increasing pH of originally acidic tropical peat enhanced CH 4 production. • Increasing pH of tropical peat increased the relative abundance of methanogens. Methane (CH 4 ), the second-most-potent greenhouse gas, is produced by methanogens under anaerobic conditions. Tropical peat swamp forests, which are widely distributed in Southeast Asia, have recently been subjected to large-scale deforestation and conversion to agricultural land. The pH of low-pH (acidic) tropical peat soils on agricultural lands is generally controlled to promote plant growth. Unintended waterlogged conditions in agricultural lands during the wet season can create an anaerobic environment in which methanogens are active. In this study, surface peat soil collected from a tropical peat swamp forest in Central Kalimantan, Indonesia, was examined to clarify the effect of increasing pH on CH 4 production. Soil samples were prepared at varying pH (3.4, 4.7, 6.6, and 7.7) by adding calcium hydroxide and incubated under anoxic conditions. Soil remained under dark and cool conditions for years before incubation. CH 4 production increased with incubation time at all pH levels. Overall, soils at higher pH showed significantly greater CH 4 production compared with peat at pH 3.4 (control) at most measurement points during a 76-day incubation. Analysis of the phylogenetic composition of archaeal and bacterial communities in peat after a 76-day incubation showed that the relative abundance of Euryarchaeota (Methanobacteria + Methanomicrobia), organisms that produce CH 4 , increased from pH 3.4 (∼0%) to pH 4.7 (5.3 %), pH 6.6 (8.7 %), and pH 7.7 (8.7 %). This suggests that increasing the pH of tropical peat enhances CH 4 production by increasing the proportion of methanogens. It should also be noted that the anaerobic microbe populations in tropical peat can survive and recover after long-term cold storage.

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Publication Details

Journal
CATENA
Published
2025-02-03
DOI
https://doi.org/10.1016/j.catena.2025.108791
Citations
7
Primary Topic
Methane Hydrates and Related Phenomena
Type
article
Field-Weighted Citation Impact
6.02

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article

Increasing the pH of tropical peat can enhance methane production and methanogenic growth under anoxic conditions

Masayuki Itoh, Kitso Kusin, Adi Jaya, Takashi Hirano et al.
7 citations
CATENA
Methane Hydrates and Related Phenomena
6.02
article

Increasing the pH of tropical peat can enhance methane production and methanogenic growth under anoxic conditions

Masayuki Itoh, Kitso Kusin, Adi Jaya, Takashi Hirano, Takeshi Tokida, Hideyuki Doi, Kensuke Ogawa
article en
7 citations

Abstract

• CH 4 production from tropical peat was examined by incubation at varying pH. • Increasing pH of originally acidic tropical peat enhanced CH 4 production. • Increasing pH of tropical peat increased the relative abundance of methanogens. Methane (CH 4 ), the second-most-potent greenhouse gas, is produced by methanogens under anaerobic conditions. Tropical peat swamp forests, which are widely distributed in Southeast Asia, have recently been subjected to large-scale deforestation and conversion to agricultural land. The pH of low-pH (acidic) tropical peat soils on agricultural lands is generally controlled to promote plant growth. Unintended waterlogged conditions in agricultural lands during the wet season can create an anaerobic environment in which methanogens are active. In this study, surface peat soil collected from a tropical peat swamp forest in Central Kalimantan, Indonesia, was examined to clarify the effect of increasing pH on CH 4 production. Soil samples were prepared at varying pH (3.4, 4.7, 6.6, and 7.7) by adding calcium hydroxide and incubated under anoxic conditions. Soil remained under dark and cool conditions for years before incubation. CH 4 production increased with incubation time at all pH levels. Overall, soils at higher pH showed significantly greater CH 4 production compared with peat at pH 3.4 (control) at most measurement points during a 76-day incubation. Analysis of the phylogenetic composition of archaeal and bacterial communities in peat after a 76-day incubation showed that the relative abundance of Euryarchaeota (Methanobacteria + Methanomicrobia), organisms that produce CH 4 , increased from pH 3.4 (∼0%) to pH 4.7 (5.3 %), pH 6.6 (8.7 %), and pH 7.7 (8.7 %). This suggests that increasing the pH of tropical peat enhances CH 4 production by increasing the proportion of methanogens. It should also be noted that the anaerobic microbe populations in tropical peat can survive and recover after long-term cold storage.

CATENAVol. 250
University of Palangka Raya (ID), National Agriculture and Food Research Organization (JP), University of Hyogo (JP), Hokkaido University (JP), Kyoto University (JP), Kyoto College of Graduate Studies for Informatics (JP), Advanced Analysis Center (JP)
Research Institute for Humanity and Nature, Japan Society for the Promotion of Science
Zero hunger
Openalex Percentile: Top 4%
Methane Hydrates and Related Phenomena
6.02
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