摘要
对粤东后江岬间海岸1992和1993年7条重复地形剖面分析结果表明,当前各剖面年净冲淤变化很小,剖面分别与Bodge和Lee平衡剖面模式符合良好,拟合的平衡剖面截止水深反映了在海区波候条件作用下泥沙运动的临界水深.此外,根据底质净输运趋势模式对近岸区沉积物运动趋势作了统计分析.
This paper analyzes the variations and equilibrium states of seven coastal profiles measured in 1992 and 1993,respectively. The results show that the net erosion or siltation of the profiles is small.The shapes of every profiles fit well to the Bodges and Lees equilibrium profile models.The fitted closure water depthes of the profiles indicate the critical depthes of sediment motion under the wave climate of this waters. In addition, the sediment transport directions of the nearshore zone are statistically analyzed based on the model of net sediment transport trends.
出处
《中山大学学报(自然科学版)》
CAS
CSCD
北大核心
1998年第S2期9-14,共6页
Acta Scientiarum Naturalium Universitatis Sunyatseni
基金
国家自然科学基金
广东省自然科学基金
关键词
岬间海岸
剖面地形
平衡剖面模式
沉积物净输运趋势
coast between headlands, profile topography, equilibrium profile models, net sediment transport trends