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Changes in the biological “regulators” of organic carbon mineralization in silted soils of check dams as a result of wet‐dry cycles

Bibliographic Data

ID21647432
AuthorsXiaojun Liu (0000-0003-4672-8569, School of Agriculture Ningxia University Yinchuan People's Republic of China), Yi Zhang (0000-0002-7581-7061, Breeding Base for State Key Laboratory of Land Degradation and Ecological Restoration in Northwest China Ningxia University Yinchuan People's Republic of China, corresponding author), Peng Li (0000-0002-7138-430X, Key Laboratory of National Forestry Administration on Ecological Hydrology and Disaster Prevention in Arid Regions Xi'an University of Technology Xi'an People's Republic of China, corresponding author), Lie Xiao (0000-0002-0189-5841, Key Laboratory of National Forestry Administration on Ecological Hydrology and Disaster Prevention in Arid Regions Xi'an University of Technology Xi'an People's Republic of China)
Year2024
Volume35
Issue2
Pages705-716
Publication date2024-01-30
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.4946
OpenAlexW4387617032
LanguageEN
Citations received1
References cited42

Climate change is increasing the frequency of prolonged droughts and extreme rainfall events, with implications for ecosystem carbon (C) cycling and efforts to mitigate climate change. Exploring how wet and dry cycling events affect microbially mediated soil organic carbon (SOC) mineralization processes is critical for achieving global C neutrality targets. This study examines how drought, water stress, and wet‐dry cycles influence microorganisms and the SOC mineralization process. We found that wet‐dry cycles initially excited mineralization of SOC, but that soil mineralization gradually decreased as wet‐dry cycling continued. At the same time, the utilization of C sources by different microbial communities tended to change, from primarily carbohydrate, amines and acids to a single acid, esters, or alcohols. The limiting factors for SOC mineralization also varied when soils were exposed to drought, water stress, and wet‐dry cycles, and we quantified the direct and interactive contributions of each factor to SOC mineralization. The direct effects of the factors under drought and water stress were 0.70 and 0.74, while the interaction of the elements was only 0.29 and 0.24. The direct effects of the factors were only 0.30 under wet‐dry cycling conditions. Based on the results of this study, we propose a pathway for soil biological regulation of SOC mineralization during drought, water stress and wet‐dry cycles, in order to further clarify the microbial regulation mechanism related to SOC mineralization

Biology · Carbon cycle · Cycling · Ecosystem · Soil carbon · Soil water · Chemistry · Environmental Science · Gut microbiota and health · Microbial Community Ecology and Physiology · Soil Carbon and Nitrogen Dynamics · Ecology · Environmental Chemistry · Forestry · Soil Science

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Unique citing works1
Citations per year0,5
Citation span2024 - 2024 (1)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 1
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