中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid

Organic carbon mineralization pathways in the muddy sediments of the South Yellow Sea: Insights from steady-state modeling of porewater

文献类型:期刊论文

作者Ren, Jian-Hua2; Zhu, Mao-Xu2; Wang, De-Yan2; Tan, Ting-Ting2; Li, Tie2; Zhao, Miao1; Pan, Da-Wei1
刊名APPLIED GEOCHEMISTRY
出版日期2022-03-01
卷号138页码:12
ISSN号0883-2927
关键词China marginal Seas Organic carbon Marine sediments Diagenetic modeling Mineralization pathways Mineralization rate
DOI10.1016/j.apgeochem.2022.105237
通讯作者Zhu, Mao-Xu(zhumaoxu@ouc.edu.cn)
英文摘要In marine sediments, microbial mineralization of organic carbon (OC) proceeds through a cascade of pathways using different electron acceptors. Rates and relative importance of individual pathways can provide quantitative constraints on biogeochemical cycling of a number of elements, such as carbon, nitrogen, sulfur, iron, and manganese. However, such information is hitherto very scarce in the China marginal seas. To fill the gap, a multicomponent-coupled reaction-transport model CANDI was applied to quantify the rates and relative contributions of individual pathways of OC mineralization at three sites in the South Yellow Sea (SYS) sediments, based on which OC budgets were constructed. Model results at steady state generally well-reproduced the profiles of measured porewater solutes. The fast degrading OC pools G1 become exhausted over the upper 4 cm at the studied sites with the degradation rate constants k1 ranging between 0.6 and 1.65 yr(- 1), while the slow degrading OC pool G2 remains almost undegradable on the timescales of the studied depth (-25 cm) due to the low degradation rate constants k2 (10(- 5)-10(-4) yr(- 1)) The depth-integrated rates of OC mineralization at the studied sites are in the range of 5.1-18.3 mmol C m(- 2) d(- 1), and aerobic respiration stands out as the dominant pathway, with its average contribution of 62%, followed by sulfate reduction (22.6%), dissimilatory manganese/ iron reduction (8.4%), and denitrification (6.1%). Methanogenesis is a negligible process of OC mineralization within the studied depths. The contributions of aerobic respiration in the SYS sediments are much higher than the global average for marginal seas, but the contributions of sulfate reduction and iron dissimilatory reduction are much lower than their global averages, which could be ascribed to the low availability of degradable OC for anaerobic respiration. Budget of OC indicates that the mineralization and burial of OC in the muddy sediments account for 7.3 and 1.7%, respectively, of the total OC supplied to the sea, with the net OC accumulation efficiency of-19%.
WOS关键词EAST CHINA SEA ; ORGANIC-MATTER MINERALIZATION ; EARLY DIAGENETIC PROCESSES ; SURFACE SEDIMENTS ; MARINE-SEDIMENTS ; IRON REDUCTION ; SULFATE-REDUCTION ; PROVENANCE DISCRIMINATION ; CONTINENTAL SHELVES ; MARGIN SEDIMENTS
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000799846100002
资助机构National Natural Science Foundation of China ; National Key Research and Development Program of China
源URL[http://ir.yic.ac.cn/handle/133337/31174]  
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
烟台海岸带研究所_山东省海岸带环境工程技术研究中心
通讯作者Zhu, Mao-Xu
作者单位1.Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
2.Ocean Univ China, Coll Chem & Chem Engn, Key Lab Marine Chem Theory & Technol, Minist Educ, Qingdao 266100, Peoples R China
推荐引用方式
GB/T 7714
Ren, Jian-Hua,Zhu, Mao-Xu,Wang, De-Yan,et al.

Organic carbon mineralization pathways in the muddy sediments of the South Yellow Sea: Insights from steady-state modeling of porewater

[J]. APPLIED GEOCHEMISTRY,2022,138:12.
APA Ren, Jian-Hua.,Zhu, Mao-Xu.,Wang, De-Yan.,Tan, Ting-Ting.,Li, Tie.,...&Pan, Da-Wei.(2022).

Organic carbon mineralization pathways in the muddy sediments of the South Yellow Sea: Insights from steady-state modeling of porewater

.APPLIED GEOCHEMISTRY,138,12.
MLA Ren, Jian-Hua,et al."

Organic carbon mineralization pathways in the muddy sediments of the South Yellow Sea: Insights from steady-state modeling of porewater

".APPLIED GEOCHEMISTRY 138(2022):12.

入库方式: OAI收割

来源:烟台海岸带研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。