引用本文:	杨治家,林国军,吴龙生,蒋孟荣,岳海东.防城港拦门沙航道浚深—7.5m后的泥沙冲淤的研究[J].海洋科学,1988,12(1):9-14.

【打印本页】【HTML】【下载PDF全文】【查看/发表评论】【下载PDF阅读器】【关闭】

过刊浏览高级检索

本文已被：浏览 1390次下载 1371次	码上扫一扫！
分享到：微信更多字体:加大+\|默认\|缩小-
防城港拦门沙航道浚深—7.5m后的泥沙冲淤的研究
杨治家¹, 林国军¹, 吴龙生¹, 蒋孟荣¹, 岳海东¹
中国科学院海洋研究所

摘要:

防城湾比较隐蔽、浪小。航通流速大且落潮流速大于涨潮流速。拦门沙形成于全新世中期,目前处于相对稳定时期,但季节变化明显。泥沙补给少,航道浚深—7.5m后淤积量小,呈现出冬季冲刷为主、夏季淤积为主的特点。虽经台风袭击,但航道并未造成聚淤现象。

关键词:

DOI：

分类号:

基金项目:

THE SILT ALLUVIAL AT FANGCHENG HARBOUR BAR CHANNEL AFTER DREDGING FOR-7.5m

Abstract:

The silt accumulated at Fangcheng harbour bar channel has been less than 40000 m³ since the channel was dredged for-7.5 m in December 1983. The channel is now being scoured in winter and silted up in summer. Sudden silting up has not been witnessed even after the attack of typhoon.

Key words: