Knowledge Management System Of Guangzhou Institute of Energy Conversion, CAS
Experimental and Numerical Simulation of the Formation of Cold Seep Carbonates in Marine Sediments | |
Ye, Tao1,2,3,4,5; Jin, Guangrong1,2,3,4; Wu, Daidai1,2,3,4,6; Liu, Lihua1,2,3,4 | |
2019-04-02 | |
发表期刊 | INTERNATIONAL JOURNAL OF ENVIRONMENTAL RESEARCH AND PUBLIC HEALTH |
ISSN | 1660-4601 |
卷号 | 16期号:8页码:12 |
通讯作者 | Liu, Lihua(liulh@ms.giec.ac.cn) |
摘要 | Cold seep emissions of low temperature fluid from the marine sediment basins are mainly comprised of methane and other hydrocarbons. A series of biogeochemical processes related to methane lead to the formation of authigenic carbonate minerals. In this study, a self-built experimental device was used to study the formation process of carbonate minerals under cold seep conditions. The concentrations of pore water chemicals, HCO3- and Ca2+ at different heights of the reactor under flow conditions can be observed. According to the experimental results, the formation process of carbonate minerals under cold seep conditions was estimated, that 1 m carbonate growth needs 12,000 and 7000 years, respectively, under fast (5 mLmin(-1)) and slow emission (1 mLmin(-1)) conditions. Furthermore, TOUGHREACT was used to simulate the diagenesis process. A 1D unsteady react-transport model was developed, and the experimental data was used to constrain the simulation. The results of simulation show that the carbonates need 17,000 and 9700 years to grow 1 m under the condition of fast and slow flow scenarios, respectively. The results of this work will contribute to the study of foundation on the formation of authigenic minerals in cold seep areas, and for the physical properties of sedimentary media as well. |
关键词 | cold seeps authigenic carbonates experimental and numerical simulation diagenesis rate authigenic carbonate precipitation rate |
DOI | 10.3390/ijerph16081433 |
关键词[WOS] | HYDRATE-BEARING SEDIMENTS ; AUTHIGENIC CARBONATES ; SEA-FLOOR ; CALCITE PRECIPITATION ; FLUID-FLOW ; METHANE ; MARGIN ; TRANSPORT ; SYSTEM ; RATES |
收录类别 | SCI |
语种 | 英语 |
资助项目 | NSF of China[417760711] ; Institution of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences[ISEE2018YB03] ; Special Project for Marine Economy Development of Guangdong Province[GDME-2018D002] |
WOS研究方向 | Environmental Sciences & Ecology ; Public, Environmental & Occupational Health |
项目资助者 | NSF of China ; Institution of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences ; Special Project for Marine Economy Development of Guangdong Province |
WOS类目 | Environmental Sciences ; Public, Environmental & Occupational Health |
WOS记录号 | WOS:000467747100126 |
出版者 | MDPI |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.giec.ac.cn/handle/344007/25001 |
专题 | 中国科学院广州能源研究所 |
通讯作者 | Liu, Lihua |
作者单位 | 1.Chinese Acad Sci, Guangzhou Inst Energy Convers, Guangzhou 510640, Guangdong, Peoples R China 2.CAS Key Lab Gas Hydrate, Guangzhou 510640, Guangdong, Peoples R China 3.Guangdong Prov Key Lab New & Renewable Energy Res, Guangzhou 510640, Guangdong, Peoples R China 4.Chinese Acad Sci, Guangzhou Ctr Gas Hydrate Res, Guangzhou 510640, Guangdong, Peoples R China 5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 6.Chinese Acad Sci, Inst South China Sea Ecol & Environm Engn, Guangzhou 510640, Guangdong, Peoples R China |
第一作者单位 | 中国科学院广州能源研究所 |
推荐引用方式 GB/T 7714 | Ye, Tao,Jin, Guangrong,Wu, Daidai,et al. Experimental and Numerical Simulation of the Formation of Cold Seep Carbonates in Marine Sediments[J]. INTERNATIONAL JOURNAL OF ENVIRONMENTAL RESEARCH AND PUBLIC HEALTH,2019,16(8):12. |
APA | Ye, Tao,Jin, Guangrong,Wu, Daidai,&Liu, Lihua.(2019).Experimental and Numerical Simulation of the Formation of Cold Seep Carbonates in Marine Sediments.INTERNATIONAL JOURNAL OF ENVIRONMENTAL RESEARCH AND PUBLIC HEALTH,16(8),12. |
MLA | Ye, Tao,et al."Experimental and Numerical Simulation of the Formation of Cold Seep Carbonates in Marine Sediments".INTERNATIONAL JOURNAL OF ENVIRONMENTAL RESEARCH AND PUBLIC HEALTH 16.8(2019):12. |
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