- 责任者：Huang Lu (Research Institute of Environmental Fluid ; Anhui University of Technology ; Maanshan 243032 ; China) ; Zhang Jianian
- 刊名：Acta Sedimentologica Sinica
- 出版年：2013
- 卷期：31(6)
- 关键词：海底峡谷 ; submarine canyons ; 浊积岩 ; turbidite
- 页码：p.1001-1007
- 图表：7 illus., 1 table, 28 refs.
- 分类号：0803
- issnNo：ISSN1000-0550
- isbnNo：CN62-1038/P
The characteristics of the flow and deposition of turbidity currents in deep-sea is a focus of present re search. A three-dimensional computational model based on Reynolds-averaged Navier-Stokes equation and buoyancy modified turbulence k-E model is used to study the flow and deposition of turbidity currents in a sinuous submarine canyon with arc cross-section. The findings are： （1） subaqueous turbidity current generally increases its thickness on its way downstream due to the entrainment of environmental fluid and spills over the bank as soon as its thickness ex ceeds the height of the canyon, resulting in mass and momentum losses; （2） at channel bend apex, much current strips out due to centrifugal force ; the largest local stripping occurs just downstream the outer bank of the bend apex, excess density of the stripped current reaches as much as 37.5% that of inflow; （3） the secondary flow at canyon bend apex is river-like, i.e. directed from outer bank to the inner bank near the bed for the arc-shaped channel simu lated; （4） in the canyon simulated, deposition occurs around canyon center and downstream the inner bank of bend apex, while erosion occurs downstream the outer bank of bend apex. Those features may assist us in reconstructing the ancient environments in exploring the submarine hydrocarbon reservoirs by observing the turbidites.