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题名

What determines the downstream evolution of turbidity currents?

作者
通讯作者Heerema,Catharina J.
发表日期
2020-02-15
DOI
发表期刊
ISSN
0012-821X
EISSN
1385-013X
卷号532
摘要
Seabed sediment flows called turbidity currents form some of the largest sediment accumulations, deepest canyons and longest channel systems on Earth. Only rivers transport comparable sediment volumes over such large areas; but there are far fewer measurements from turbidity currents, ensuring they are much more poorly understood. Turbidity currents differ fundamentally from rivers, as turbidity currents are driven by the sediment that they suspend. Fast turbidity currents can pick up sediment, and self-accelerate (ignite); whilst slow flows deposit sediment and dissipate. Self-acceleration cannot continue indefinitely, and flows might reach a near-uniform state (autosuspension). Here we show how turbidity currents evolve using the first detailed measurements from multiple locations along their pathway, which come from Monterey Canyon offshore California. All flows initially ignite. Typically, initially-faster flows then achieve near-uniform velocities (autosuspension), whilst slower flows dissipate. Fractional increases in initial velocity favour much longer runout, and a new model explains this bifurcating behaviour. However, the only flow during less-stormy summer months is anomalous as it self-accelerated, which is perhaps due to erosion of surficial-mud layer mid-canyon. Turbidity current evolution is therefore highly sensitive to both initial velocities and seabed character.
关键词
相关链接[Scopus记录]
收录类别
SCI ; EI
语种
英语
重要成果
NI期刊
学校署名
其他
资助项目
Ocean University of China[] ; Immune Tolerance Network[] ; [721403] ; U.S. Geological Survey[] ; [NE/R015953/1] ; David and Lucile Packard Foundation[NE/M007138/1] ; Leverhulme Trust[ECF-2018-267] ; U.S. Geological Survey[]
WOS研究方向
Geochemistry & Geophysics
WOS类目
Geochemistry & Geophysics
WOS记录号
WOS:000513291400007
出版者
EI入藏号
20195207902539
EI主题词
Energy dissipation ; Ignition ; Ocean currents ; Offshore oil well production ; Sediment transport
EI分类号
Seawater, Tides and Waves:471.4 ; Oil Field Production Operations:511.1 ; Fuel Combustion:521.1 ; Energy Losses (industrial and residential):525.4 ; Light/Optics:741.1
ESI学科分类
GEOSCIENCES
Scopus记录号
2-s2.0-85076752369
来源库
Scopus
引用统计
被引频次[WOS]:58
成果类型期刊论文
条目标识符http://sustech.caswiz.com/handle/2SGJ60CL/68909
专题南方科技大学
工学院_海洋科学与工程系
作者单位
1.Departments of Geography and Earth Sciences,Durham University,Durham,DH1 3LE,United Kingdom
2.Monterey Bay Aquarium Research Institute,Moss Landing,95039,United States
3.Ocean and Earth Science,University of Southampton,European Way,Southampton,SO14 3ZH,United Kingdom
4.National Oceanography Centre,University of Southampton Waterfront Campus,European Way,Southampton,SO14 3ZH,United Kingdom
5.Energy and Environment Institute,University of Hull,Hull,Cottingham Road,HU6 7RX,United Kingdom
6.Pacific Coastal and Marine Science Center,U.S. G.S.,Santa Cruz,95060,United States
7.National Institute of Water and Atmospheric Research,Wellington,New Zealand
8.Southern University of Science and Technology of China,Shenzhen,518055,China
9.Qingdao National Laboratory for Marine Science and Technology,Qingdao,266061,China
10.University of Plymouth,Plymouth,Drake Circus,PL4 8AA,United Kingdom
11.Antarctic Research Centre,Victoria University of Wellington,Wellington,New Zealand
12.
推荐引用方式
GB/T 7714
Heerema,Catharina J.,Talling,Peter J.,Cartigny,Matthieu J.,et al. What determines the downstream evolution of turbidity currents?[J]. EARTH AND PLANETARY SCIENCE LETTERS,2020,532.
APA
Heerema,Catharina J..,Talling,Peter J..,Cartigny,Matthieu J..,Paull,Charles K..,Bailey,Lewis.,...&Pope,Edward.(2020).What determines the downstream evolution of turbidity currents?.EARTH AND PLANETARY SCIENCE LETTERS,532.
MLA
Heerema,Catharina J.,et al."What determines the downstream evolution of turbidity currents?".EARTH AND PLANETARY SCIENCE LETTERS 532(2020).
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