论文部分内容阅读
大多数陆架上近底流场的特征可以用叠加在准稳定平均水流上的波浪引起的摆动流(周期为3—20秒)来表示;这种准稳定平均水流可能是潮汐和/或风力躯动的。在这种流场中海底沉积物的再悬浮作用内有各种相互影响因素:有海底的粗糙程度、沉积物结构、密度分
The characteristics of the near-bottom flow field over most of the shelf can be represented by wobble waves (periods of 3-20 seconds) superimposed on waves of a quasi-steady average water flow; this quasi-steady mean flow may be a tidal and / or wind body moveable. Within this flow field there are various interdependent factors within the resuspension of seabed sediments: the roughness of the seabed, sediment structure, density