摘要
国内外对沙坝 泻湖海岸的研究主要采取动力地貌学的方法 ,本文评述了近一个半世纪以来在这一领域所取得的重要成果 .波浪、潮汐、径流等特殊的动力场决定了泥沙输运的方式和路径 ,从而形成了与其相应的沙坝、泻湖。
It is mostly by means of dynamical geomorphology to research on barrier lagoon coast at home and abroad. The review made in this paper is focused on those important results obtained in one and a half centuries. The sediment transported modes and paths are controlled by the special dynamical field such as wave, tide and fluvial flow, which correspondingly lead to the geomorphologic system constituted by barriers, lagoons and tidal inlets.
出处
《台湾海峡》
CAS
CSCD
2001年第4期565-572,共8页
Journal of Oceanography In Taiwan Strait
