摘要
以神泉通道和乌坎通道的演变实例说明,河口型与河口湾型通道的形成和演变受径流量或潮流量的制约。而人为作用使径流量或潮流量减小,导致通道地形急剧演变和稳定程序变差。因此必须保持径流来量或纳潮量不变。但对不同类型的通道要作具体分析。
Illustracted by of Shenqucan Channle and Wukan Channel, the restrictions of formation of estuarine and bay channel and evolution by runoff and tide are studied. The human effect of reduction of runoff and tide has led to the fact change of channel geography and stability .
出处
《海洋科学》
CAS
CSCD
北大核心
1992年第6期54-57,共4页
Marine Sciences
