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Xuehui Feng

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Articles 13
Citations 123
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Recent Articles
1.
Feng X, Wang Z, Wang Z, He C, Xun H, Chen Y, et al.
Front Digit Health . 2025 Jan; 6():1503831. PMID: 39834842
Introduction: The aim of this study is to compare the injury patterns of female water polo players before and after the implementation of the Male-Assisted Female Training (MAFT) program. The...
2.
Zhao J, Feng X, Hu J, He M, Wang S, Yang Y, et al.
Glob Chang Biol . 2024 Dec; 30(12):e70004. PMID: 39699571
A comprehensive understanding of the formation of mineral-associated organic matter (MAOM) is a prerequisite for the sustainable management of soil carbon (C) and the development of effective long-term strategies for...
3.
Hu J, Kang L, Li Z, Feng X, Liang C, Wu Z, et al.
Nat Commun . 2023 Jun; 14(1):3681. PMID: 37344478
Photochemical and biological degradation of dissolved organic carbon (DOC) and their interactions jointly contribute to the carbon dioxide released from surface waters in permafrost regions. However, the mechanisms that govern...
4.
He M, Li Q, Chen L, Qin S, Kuzyakov Y, Liu Y, et al.
Glob Chang Biol . 2023 Apr; 29(16):4638-4651. PMID: 37114938
Climate warming leads to widespread permafrost thaw with a fraction of the thawed permafrost carbon (C) being released as carbon dioxide (CO ), thus triggering a positive permafrost C-climate feedback....
5.
Feng X, Qin S, Zhang D, Chen P, Hu J, Wang G, et al.
Glob Chang Biol . 2022 Jun; 28(16):4845-4860. PMID: 35650709
Microbial growth and respiration are at the core of the soil carbon (C) cycle, as these microbial physiological performances ultimately determine the fate of soil C. Microbial C use efficiency...
6.
He M, Fang K, Chen L, Feng X, Qin S, Kou D, et al.
Glob Chang Biol . 2021 Nov; 28(3):936-949. PMID: 34726326
Microbial necromass carbon (C) has been considered an important contributor to persistent soil C pool. However, there still lacks large-scale systematic observations on microbial necromass C in different soil layers,...
7.
Song Y, Chen L, Kang L, Yang G, Qin S, Zhang Q, et al.
Environ Sci Technol . 2021 Jul; 55(16):11412-11423. PMID: 34310124
Permafrost thaw could increase methane (CH) emissions, which largely depends on CH production driven by methanogenic archaea. However, large-scale evidence regarding key methanogenic taxa and their relative importance to abiotic...
8.
Chen L, Fang K, Wei B, Qin S, Feng X, Hu T, et al.
Ecol Lett . 2021 Mar; 24(5):1018-1028. PMID: 33709557
Elucidating the processes underlying the persistence of soil organic matter (SOM) is a prerequisite for projecting soil carbon feedback to climate change. However, the potential role of plant carbon input...
9.
Kou D, Yang G, Li F, Feng X, Zhang D, Mao C, et al.
Nat Commun . 2020 Jul; 11(1):3331. PMID: 32620773
The ecosystem carbon (C) balance in permafrost regions, which has a global significance in understanding the terrestrial C-climate feedback, is significantly regulated by nitrogen (N) dynamics. However, our knowledge on...
10.
Zhang Q, Yang G, Song Y, Kou D, Wang G, Zhang D, et al.
Environ Sci Technol . 2019 Nov; 53(24):14243-14252. PMID: 31718180
Methane (CH) dynamics across permafrost regions is critical in determining the magnitude and direction of permafrost carbon (C)-climate feedback. However, current studies are mainly derived from the Arctic area, with...