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Seabed sediment classification in the northern South China Sea using inversion method
[Zheng, Hong-bo; Yan, Pin; Wang, Yan-lin] S China Sea Inst Oceanol, CAS Key Lab Marginal Sea Geol, Guangzhou, Guangdong, Peoples R China; [Zheng, Hong-bo] Chinese Acad Sci, State Key Lab Acoust, Beijing, Peoples R China; [Chen, Jing] SOA, S China Sea Marine Engn Surveying Ctr, Guangzhou, Guangdong, Peoples R China; hongbozheng@126.com
2013
Source PublicationAPPLIED OCEAN RESEARCH
ISSN0141-1187
Volume39Pages:131-136
AbstractSub-bottom profile data can be used not only for the interpretation of the seabed strata structure and formation, but also for seabed sediments classification using inversion method. In the present paper, sub-bottom profile data from a survey line located on the continental slope of the northern South China Sea were processed. The data collected were used to calculate seabed reflection coefficient and attenuation rolloff, while sediment acoustic characteristics parameters, including porosity and permeability, were defined based on the Blot model that calculates wave propagation in sediment fluid mixtures. Finally, the mean grain sizes and corresponding sediment classification were quantitatively estimated. By comparing the inversion result with sediment description of gravity piston cores which were acquired near the survey line, we found that the results from inversion method accord with the particle size analysis of sediment cores. However, the inversion method is only suitable for the soft seabed sediments such as mud or sand. The petrous sediment in the survey is classified by Gardner formula and we concluded the petrous seabed sediments are carbonate crusts which are generated from leaky gas hydrate. (C) 2012 Elsevier Ltd. All rights reserved.
Department海洋地质
KeywordContinental Slope Of The norThern South China Sea Sub-bottom Profile Data Seabed Sediment Sediment Classification Inversion Method
Subject AreaEngineering, Ocean ; Oceanography
Funding OrganizationThis project is supported by State Key Laboratory of Acoustics, Chinese Academy of Sciences (no. SKLOA201106) and National Natural Science Young Foundation of China (no. 41106056). The authors also sincerely appreciate the two anonymous reviewers for invaluable critical comments. ; This project is supported by State Key Laboratory of Acoustics, Chinese Academy of Sciences (no. SKLOA201106) and National Natural Science Young Foundation of China (no. 41106056). The authors also sincerely appreciate the two anonymous reviewers for invaluable critical comments. ; This project is supported by State Key Laboratory of Acoustics, Chinese Academy of Sciences (no. SKLOA201106) and National Natural Science Young Foundation of China (no. 41106056). The authors also sincerely appreciate the two anonymous reviewers for invaluable critical comments. ; This project is supported by State Key Laboratory of Acoustics, Chinese Academy of Sciences (no. SKLOA201106) and National Natural Science Young Foundation of China (no. 41106056). The authors also sincerely appreciate the two anonymous reviewers for invaluable critical comments.
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Language英语
Funding OrganizationThis project is supported by State Key Laboratory of Acoustics, Chinese Academy of Sciences (no. SKLOA201106) and National Natural Science Young Foundation of China (no. 41106056). The authors also sincerely appreciate the two anonymous reviewers for invaluable critical comments. ; This project is supported by State Key Laboratory of Acoustics, Chinese Academy of Sciences (no. SKLOA201106) and National Natural Science Young Foundation of China (no. 41106056). The authors also sincerely appreciate the two anonymous reviewers for invaluable critical comments. ; This project is supported by State Key Laboratory of Acoustics, Chinese Academy of Sciences (no. SKLOA201106) and National Natural Science Young Foundation of China (no. 41106056). The authors also sincerely appreciate the two anonymous reviewers for invaluable critical comments. ; This project is supported by State Key Laboratory of Acoustics, Chinese Academy of Sciences (no. SKLOA201106) and National Natural Science Young Foundation of China (no. 41106056). The authors also sincerely appreciate the two anonymous reviewers for invaluable critical comments.
WOS IDWOS:000315077300014
Citation statistics
Cited Times:2[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.scsio.ac.cn/handle/344004/11142
Collection中科院边缘海地质重点实验室
Corresponding Authorhongbozheng@126.com
Recommended Citation
GB/T 7714
[Zheng, Hong-bo,Yan, Pin,Wang, Yan-lin] S China Sea Inst Oceanol, CAS Key Lab Marginal Sea Geol, Guangzhou, Guangdong, Peoples R China,et al. Seabed sediment classification in the northern South China Sea using inversion method[J]. APPLIED OCEAN RESEARCH,2013,39:131-136.
APA [Zheng, Hong-bo,Yan, Pin,Wang, Yan-lin] S China Sea Inst Oceanol, CAS Key Lab Marginal Sea Geol, Guangzhou, Guangdong, Peoples R China,[Zheng, Hong-bo] Chinese Acad Sci, State Key Lab Acoust, Beijing, Peoples R China,[Chen, Jing] SOA, S China Sea Marine Engn Surveying Ctr, Guangzhou, Guangdong, Peoples R China,&hongbozheng@126.com.(2013).Seabed sediment classification in the northern South China Sea using inversion method.APPLIED OCEAN RESEARCH,39,131-136.
MLA [Zheng, Hong-bo,et al."Seabed sediment classification in the northern South China Sea using inversion method".APPLIED OCEAN RESEARCH 39(2013):131-136.
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