口外海滨

1

长江口口外海滨盐度扩散的分层数学模型

A Stratification Model For Salinity Diffusion In The Offshore Region Of The Changjiang Estuary
2

长江口外海滨悬浮体的粒度特征及其与锋面的关系

The Grain Size Characteristics of the Suspended Matters in the Offshore Region of the Changjiang Estuary and the Relation with the Front Information
3

具体为：河口围填后相当于河流近口段、河口段、口外海滨段相应地向海延伸，必然会引起河口体系的自动调整并形成新的动态平衡；

After reclamation , the mouth of river extends towards sea , causing the system of estuary adjustment automatically and reaching a new balance .
4

本文根据1988～1991年河口锋区现场调查资料分析的基础上，论述长江口外海滨悬浮体的粒度组成、分布及其与锋面的关系。

This paper intends to describe the composition , distribution of the suspended matters in the offshore region of the Changjiang Estuary and the relation with the front .