The Fluid Mechanics of Deep-Sea Mining

被引:27
|
作者
Peacock, Thomas [1 ]
Ouillon, Raphael [1 ]
机构
[1] MIT, Dept Mech Engn, Cambridge, MA 02139 USA
基金
美国国家科学基金会;
关键词
sediment transport; sediment plumes; physical oceanography; turbidity currents; settling; flocculation; GRAVITY CURRENTS; TURBIDITY CURRENTS; HYDROTHERMAL PLUMES; TROPICAL PACIFIC; SCALE TRANSPORT; TURBULENT JETS; MANGANESE; ENTRAINMENT; PROPAGATION; SEDIMENT;
D O I
10.1146/annurev-fluid-031822-010257
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Fluid mechanics lies at the heart of many of the physical processes associated with the nascent deep-sea mining industry. The evolution and fate of sediment plumes that would be produced by seabed mining activities, which are central to the assessment of the environmental impact, are entirely determined by transport processes. These processes, which include advection, turbulent mixing, buoyancy, differential particle settling, and flocculation, operate at a multitude of spatiotemporal scales. A combination of historical and recent efforts that combine theory, numerical modeling, laboratory experiments, and field trials has yielded significant progress, including assessing the role of environmental and operational parameters in setting the extent of sediment plumes, but more fundamental and applied fluid mechanics research is needed before models can accurately predict commercial-scale scenarios. Furthermore, fluid mechanics underpins the design and operation of proposed mining technologies, for which there are currently no established best practices.
引用
收藏
页码:403 / 430
页数:28
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