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Min Luo

Researcher at Fuzhou University

Publications -  35
Citations -  490

Min Luo is an academic researcher from Fuzhou University. The author has contributed to research in topics: Salinity & Chemistry. The author has an hindex of 8, co-authored 25 publications receiving 217 citations. Previous affiliations of Min Luo include Fujian Normal University.

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Impacts of increasing salinity and inundation on rates and pathways of organic carbon mineralization in tidal wetlands: a review

TL;DR: In this article, the authors review the existing literature on the likely effects of the increasing salinity and inundation on organic carbon mineralization in tidal wetlands and conclude that the changing electron acceptor pattern may result in microbial sulfate reduction predominating over other carbon metabolism pathways.
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A new insight into the strategy for methane production affected by conductive carbon cloth in wetland soil: Beneficial to acetoclastic methanogenesis instead of CO2 reduction

TL;DR: High-throughput sequencing showed that methane production may stem from the involvement of Methanosarcina for both treatments, suggesting that conductive carbon material can promote acetoclastic methanogenesis instead of CO2 reduction in a natural environment.
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Anaerobic organic carbon mineralization in tidal wetlands along a low-level salinity gradient of a subtropical estuary: Rates, pathways, and controls

TL;DR: In this paper, the authors examined how the rates and pathways of anaerobic organic carbon mineralization (AOCM) of tidal freshwater wetlands change with low-level increases in salinity, and investigated the rate and controls of microbial iron and sulfate reduction, methane production, and total AOCM in tidal wetlands along a freshwater to oligohaline (0.1-3.3) gradient in the Min River Estuary in southeastern China.
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Carbon nanotubes accelerate acetoclastic methanogenesis: From pure cultures to anaerobic soils

TL;DR: It is demonstrated that conducting CNTs favor methane production and that the mechanism involved is acetoclastic methanogenesis via acetate dismutation, at least partly, rather than classical CO2 reduction.
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A potential contribution of a Fe(III)-rich red clay horizon to methane release: Biogenetic magnetite-mediated methanogenesis

TL;DR: In this paper, soil samples with a depth profile were collected from a wetland in the Yellow River Delta (YRD), in which a special red clay horizon (RCH) widely exists.