强涌潮河口潮汐对盐水入侵的影响机制OA
Influence mechanism of tides on saltwater intrusion in macrotidal estuary
以钱塘江河口为例,采用平面二维涌潮盐度数学模型模拟了强涌潮河口的盐水入侵问题,通过改变模型下边界的潮位过程以反映外海潮汐变化,研究了高潮位、低潮位、潮差 3 个潮位特征值对河口区盐水入侵的影响机制.结果表明,外海潮汐变化主要通过高潮位变化影响河口的盐水入侵程度,低潮位变化影响甚微,故仅用潮差指标反映外海潮汐变化对河口盐水入侵的影响是不全面的;河口的盐水入侵对外海潮汐变化响应迅速,且可持续3 个潮周期以上.
Taking the Qiantang River Estuary as an example,this research employed a two-dimensional horizontal saltwater intrusion model capable of simulating tidal bore phenomena to investigate saltwater intrusion in a strong tidal bore estuary.By modifying the tidal level processes at the model's seaward boundary to represent variations in offshore tides,the study examined the influence mechanisms of three tidal characteristic parameters,high tidal level,low tidal level,and tidal range,on saltwater intrusion in the estuarine region.The results indicate that offshore tidal changes primarily affect the extent of saltwater intrusion through variations in high tidal levels,while changes in low tidal levels have minimal impact.Therefore,it is inadequate to only use the tidal range index to reflect the influence of offshore tidal variations on estuarine saltwater intrusion.In addition,estuarine saltwater intrusion responds rapidly to offshore tidal changes,with effects persisting for more than three tidal cycles.
李若华;张舒羽;胡立芳
浙江同济科技职业学院浙江同济科技职业学院中国计量大学能源环境与安全工程学院
盐水入侵潮位潮差数学模型钱塘江河口
saltwater intrusiontidal leveltidal rangemathematical modelthe Qiantang River Estuary
《水利水电科技进展》 2026 (1)
11-16,6
浙江省自然科学基金联合基金项目(LZJWY24E090002)
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