• Title/Summary/Keyword: Methanotrophic bacteria

Search Result 12, Processing Time 0.015 seconds

Biocatalytic Conversion of Methane to Methanol as a Key Step for Development of Methane-Based Biorefineries

  • Hwang, In Yeub;Lee, Seung Hwan;Choi, Yoo Seong;Park, Si Jae;Na, Jeong Geol;Chang, In Seop;Kim, Choongik;Kim, Hyun Cheol;Kim, Yong Hwan;Lee, Jin Won;Lee, Eun Yeol
    • Journal of Microbiology and Biotechnology
    • /
    • v.24 no.12
    • /
    • pp.1597-1605
    • /
    • 2014
  • Methane is considered as a next-generation carbon feedstock owing to the vast reserves of natural and shale gas. Methane can be converted to methanol by various methods, which in turn can be used as a starting chemical for the production of value-added chemicals using existing chemical conversion processes. Methane monooxygenase is the key enzyme that catalyzes the addition of oxygen to methane. Methanotrophic bacteria can transform methane to methanol by inhibiting methanol dehydrogenase. In this paper, we review the recent progress made on the biocatalytic conversion of methane to methanol as a key step for methane-based refinery systems and discuss future prospects for this technology.

Assessment of CH4 oxidation in macroinvertebrate burrows of tidal flats (갯벌의 무척추 동물 서식굴 내 메탄산화 평가)

  • Kang, J.;Kwon, K.;Woo, H.J.;Choi, J.U.
    • Journal of Wetlands Research
    • /
    • v.21 no.2
    • /
    • pp.95-101
    • /
    • 2019
  • In tidal flats that lack plants, methane ($CH_4$) fluxes are both positive (gas emission) and negative (gas "sinking") in nature. The levels of methanotroph populations significantly affect the extent of $CH_4$ sinking. This preliminary study examined $CH_4$ flux in tidal flats using a circular closed-chamber method to understand the effects of macroinvertebrate burrowing activity. The chamber was deployed over decapods (mud shrimp, Laomedia astacina and crab, Macrophthalmus japonicus) burrows for ~ 2 h, and the $CH_4$ and $CO_2$ concentrations were continuously monitored using a closed, diffuse $CH_4/CO_2$ flux meter. We found that Laomedia astacina burrow (which is relatively long) site afforded higher-level $CH_4$ production, likely due to diffusive emission of $CH_4$ in deep-layer sediments. In addition, the large methanotrophic bacteria population found in the burrow wall sediments has $CH_4$ oxidation (consumption) potential. Especially, nitrite-driven anaerobic oxidation of methane (AOM) may occur within burrows. The proposed $CH_4$-oxidation process was supported by the decrease in the ${\delta}^{13}C$ of headspace $CO_2$ during the chamber experiment. Therefore, macroinvertebrate burrows appear to be an important ecosystem environment for controlling atmospheric $CH_4$ over tidal flats.