中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Inundation depth modulates wetland soil organic carbon stability by altering microbial biomass and mineral protection

文献类型:期刊论文

作者Zhao, Mingliang4,5; Wang, Lianjing3; Xiao, Leilei4,5; Ma, Tian4,5; Li, Yuan4,5; Paytan, Adina2; Lichtfouse, Eric1; Song, Weimin4,5; Wang, Xiaojie4,5; Chu, Xiaojing4,5
刊名GEODERMA
出版日期2026-05-01
卷号469页码:12
关键词Carbon sequestration Microbial necromass Mineral property Hydrological regime Yellow River Delta
ISSN号0016-7061
DOI10.1016/j.geoderma.2026.117798
通讯作者Han, Guangxuan(gxhan@yic.ac.cn)
英文摘要Wetlands are essential carbon (C) reservoirs, crucial for climate change mitigation, but their hydrological regimes are increasingly threatened by climate change. Inundation depth, a key hydrological factor in wetlands, influences Soil Organic Carbon (SOC) storage and stability, yet its effects on SOC fractions and stability, especially in subsoils, remain critically underexplored. This study investigated the impact of inundation depth on SOC in the topsoil (0-20 cm) and subsoil (20-40 cm) over a 6-year field experiment. As the inundation depth increased from 0 cm to 40 cm, SOC content increased significantly by 62% in the topsoil and by 222% in the subsoil. Particulate Organic C (POC) and Mineral-Associated Organic C (MAOC) responded differently across soil layers, with topsoil POC driven by plant inputs and MAOC by microbial turnover, while subsoil POC and MAOC were influenced by nutrient availability and mineral protection, respectively. Inundation depth increased the subsoil SOC stability but did not affect topsoil stability, where key mineral protection capacity (i.e., clay and free/amorphous Fe/Al oxides) remained unaltered. In the subsoil, both microbial biomass and mineral protection jointly enhanced SOC stability. We identified 20 cm inundation depth as an operational benchmark where SOC accumulation reaches a saturation plateau. This suggests that, within hydrologically managed restoration settings in the Yellow River Delta, maintaining moderate inundation around this depth may help maximize SOC storage, whereas deeper inundation did not provide additional SOC gains. Collectively, these findings advance our mechanistic understanding of depth-dependent carbon dynamics and provide a practical reference for sitelevel hydrological regulation, although the applicability of this threshold to other wetlands requires further validation.
WOS关键词NITROGEN ; MATTER
WOS研究方向Agriculture
语种英语
WOS记录号WOS:001742352700001
资助机构National Key Research and Development Program of China ; Natural Science Foundation of China
源URL[http://ir.yic.ac.cn/handle/133337/42396]  
专题烟台海岸带研究所_中科院海岸带环境过程与生态修复重点实验室
通讯作者Han, Guangxuan
作者单位1.Xi An Jiao Tong Univ, State Key Lab Multiphase Flow Power Engn, Xian 710049, Shaanxi, Peoples R China
2.Univ Calif Santa Cruz, Inst Marine Sci, Santa Cruz, CA USA
3.Fudan Univ, State Key Lab Wetland Conservat & Restorat,Minist, Natl Observat & Res Stn Wetland Ecosyst Yangtze Es, Key Lab Biodivers Sci & Ecol Engn,Sch Life Sci,Min, Shanghai 200438, Peoples R China
4.Chinese Acad Sci, Yellow River Delta Field Observat & Res Stn Coasta, Dongying 257500, Shandong, Peoples R China
5.Chinese Acad Sci, CAS Key Lab Coastal Environm Proc & Ecol Remediat, Yantai Inst Coastal Zone Res, Yantai 264003, Shandong, Peoples R China
推荐引用方式
GB/T 7714
Zhao, Mingliang,Wang, Lianjing,Xiao, Leilei,et al. Inundation depth modulates wetland soil organic carbon stability by altering microbial biomass and mineral protection[J]. GEODERMA,2026,469:12.
APA Zhao, Mingliang.,Wang, Lianjing.,Xiao, Leilei.,Ma, Tian.,Li, Yuan.,...&Han, Guangxuan.(2026).Inundation depth modulates wetland soil organic carbon stability by altering microbial biomass and mineral protection.GEODERMA,469,12.
MLA Zhao, Mingliang,et al."Inundation depth modulates wetland soil organic carbon stability by altering microbial biomass and mineral protection".GEODERMA 469(2026):12.

入库方式: OAI收割

来源:烟台海岸带研究所

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