摘要
对整个长江口研究区域洪季盐水入侵过程进行模拟.验证结果与实测资料基本一致,较好地模拟出地形变化对水流结构的影响,盐度的分布与实测资料所反映的情况相吻合,盐度纵向扩散梯度从外海向上游递减,北支盐度始终高于南支,再现了长江口地区水流特征和盐水入侵的基本规律.
The saltwater intrusion process at the periods of flood season was simulated in study area of Yangtze River. The salinity distribution of the area generally agreed with measured data. The gradient of salinity horizontal diffusion decreases upstream from the sea, and the salinity of north branch is always higher than that of south branch. The basic law of the saltwater intrusion in the Yangtze estuary was reproduced.
出处
《信阳师范学院学报（自然科学版）》
CAS
2009年第2期239-241,245,共4页
Journal of Xinyang Normal University(Natural Science Edition)
基金
国家自然科学基金项目(40476039)
教育部高等学校博士学科点基金项目(20050294009)
关键词
长江口
数值模拟
盐水入侵
Yangtze estuary
numerical simulation
saltwater intrusion
