Research on the fluid dynamics interaction between submarine sand waves and seawater by seismic oceanography

被引:0
作者
Han, Tonggang [1 ]
Chen, Jiangxin [2 ,3 ]
He, Bingshou [1 ,3 ]
Azevedo, Leonardo [4 ]
机构
[1] Ocean Univ China, Key Lab Submarine Geosci & Prospecting Tech, Minist Educ, Qingdao, Peoples R China
[2] Qingdao Inst Marine Geol, Minist Nat Resources, Key Lab Gas Hydrate, Qingdao, Peoples R China
[3] Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao, Peoples R China
[4] Univ Lisbon, Inst Super Tecn, Lisbon, Portugal
基金
中国国家自然科学基金;
关键词
seismic oceanography; fluid dynamics; numerical simulation; hair-like reflection configuration; formation mechanism; INTERNAL SOLITARY WAVES; SEDIMENT; GULF; CLASSIFICATION; MORPHODYNAMICS; PROPAGATION; TRANSPORT; VELOCITY; LAYERS; MODEL;
D O I
10.3389/fmars.2023.1184787
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
IntroductionThe seafloor is an important interface between the lithosphere and the hydrosphere, where processes related to circulation and energy exchange happen along with various marine processes widely developed in the water column near the seafloor. These processes are still not yet completely understood as there are constraints of submarine detection technology and the interdisciplinary nature of these complex environments. Seismic reflection data have been a preferable tool to study and image these processes due to their characteristics in terms of spatial resolution. In seismic reflection data, submarine sand waves show hair-like reflection configurations with low continuity and wearing-hair style, appearing with an angle with the seafloor. Investigation of the relationship between the characteristics of submarine sand waves induced hair-like reflection configuration and hydrodynamics is crucial for understanding hair-like reflection configuration generation and spatiotemporal evolution. MethodsThis study combines fluid dynamics numerical simulation and seismic oceanography to discuss the seismic response characteristics and formation mechanisms of the hair-like reflection configuration. First, we create a seawater time-variant fluid-dynamical model followed by the numerical simulation of seismic oceanography data. This procedure results in seismic oceanography numerical simulation sections with hair-like reflection configurations for different constant flow conditions forced on the boundary. Optimal matching method is then applied to interpret field seismic reflection sections given the results obtained with the numerical experiments. Results and discussionAs consequence, the fluid dynamic explanation for the formation mechanism of the hair-like reflection configuration due to differences in seawater thermohaline is proposed. The study provides additional comprehension and further insights into the dynamic process of submarine sand waves induced hair-like reflection configuration using the seismic oceanography method.
引用
收藏
页数:16
相关论文
共 86 条
[1]   The formation and fate of internal waves in the South China Sea [J].
Alford, Matthew H. ;
Peacock, Thomas ;
MacKinnon, Jennifer A. ;
Nash, Jonathan D. ;
Buijsman, Maarten C. ;
Centuroni, Luca R. ;
Chao, Shenn-Yu ;
Chang, Ming-Huei ;
Farmer, David M. ;
Fringer, Oliver B. ;
Fu, Ke-Hsien ;
Gallacher, Patrick C. ;
Graber, Hans C. ;
Helfrich, Karl R. ;
Jachec, Steven M. ;
Jackson, Christopher R. ;
Klymak, Jody M. ;
Ko, Dong S. ;
Jan, Sen ;
Johnston, T. M. Shaun ;
Legg, Sonya ;
Lee, I-Huan ;
Lien, Ren-Chieh ;
Mercier, Matthieu J. ;
Moum, James N. ;
Musgrave, Ruth ;
Park, Jae-Hun ;
Pickering, Andrew I. ;
Pinkel, Robert ;
Rainville, Luc ;
Ramp, Steven R. ;
Rudnick, Daniel L. ;
Sarkar, Sutanu ;
Scotti, Alberto ;
Simmons, Harper L. ;
St Laurent, Louis C. ;
Venayagamoorthy, Subhas K. ;
Wang, Yu-Huai ;
Wang, Joe ;
Yang, Yiing J. ;
Paluszkiewicz, Theresa ;
Tang, Tswen-Yung .
NATURE, 2015, 521 (7550) :65-U381
[2]  
ASHLEY GM, 1990, J SEDIMENT PETROL, V60, P160
[3]   REVERSE TIME MIGRATION [J].
BAYSAL, E ;
KOSLOFF, DD ;
SHERWOOD, JWC .
GEOPHYSICS, 1983, 48 (11) :1514-1524
[4]   Three-dimensional seismic analysis of sediment waves and related geomorphological features on a carbonate shelf exposed to large amplitude internal waves, Browse Basin region, Australia [J].
Belde, Johannes ;
Back, Stefan ;
Reuning, Lars .
SEDIMENTOLOGY, 2015, 62 (01) :87-109
[5]   The morphodynamics of tidal sand waves:: A model overview [J].
Besio, G. ;
Blondeaux, P. ;
Brocchini, M. ;
Hulscher, S. J. M. H. ;
Idier, D. ;
Knaapen, M. A. F. ;
Nemeth, A. A. ;
Roos, P. C. ;
Vittori, G. .
COASTAL ENGINEERING, 2008, 55 (7-8) :657-670
[6]   Imaging meddy finestructure using multichannel seismic reflection data [J].
Biescas, B. ;
Sallares, V. ;
Pelegri, J. L. ;
Machin, F. ;
Carbonell, R. ;
Buffett, G. ;
Danobeitia, J. J. ;
Calahorrano, A. .
GEOPHYSICAL RESEARCH LETTERS, 2008, 35 (11)
[7]   The role of suspended load transport in the occurrence of tidal sand waves [J].
Borsje, B. W. ;
Kranenburg, W. M. ;
Roos, P. C. ;
Matthieu, J. ;
Hulscher, S. J. M. H. .
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 2014, 119 (04) :701-716
[8]   NEPHELOID LAYERS AND INTERNAL WAVES OVER CONTINENTAL SHELVES AND SLOPES [J].
CACCHIONE, DA ;
DRAKE, DE .
GEO-MARINE LETTERS, 1986, 6 (03) :147-152
[9]   Modeling the influence of storms on sand wave formation: A linear stability approach [J].
Campmans, G. H. P. ;
Roos, P. C. ;
de Vriend, H. J. ;
Hulscher, S. J. M. H. .
CONTINENTAL SHELF RESEARCH, 2017, 137 :103-116
[10]   Internal solitary wave-induced flow over a corrugated bed [J].
Carr, Magda ;
Stastna, Marek ;
Davies, Peter A. .
OCEAN DYNAMICS, 2010, 60 (04) :1007-1025