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长江口一、二维嵌套水流盐度数学模型
引用本文:谢作涛,罗景.长江口一、二维嵌套水流盐度数学模型[J].武汉大学学报(工学版),2007,40(2):7-11.
作者姓名:谢作涛  罗景
作者单位:1. 清华大学水利系,北京,100084;长江勘测规划设计研究院,湖北,武汉,430010
2. 武汉大学期刊社,湖北,武汉,430072
基金项目:国家重点基础研究发展计划(973计划);国家自然科学基金
摘    要:建立了长江大通至河口大范围的一、二维嵌套水流盐度数学模型,其中大通至江阴采用一维河网数学模型,江阴至口外段采用一般曲线坐标系平面二维数学模型.采用长江大通至江阴以及江阴至河口段的实测资料对建立的一、二维模型进行了较系统的率定,结果表明:数学模型计算与实测资料均吻合较好,验证了该数学模型运用于长江口水流盐度数值模拟的可靠性,为下一步进行长江口盐水入侵研究奠定了基础.

关 键 词:盐水入侵  一维河网模型  一般曲线坐标系  平面二维模型  长江口
文章编号:1671-8844(2007)02-0007-05
修稿时间:2006-01-20

Study on 1D and 2D coupling flow and salinity model for Yangtze River estuary
XIE Zuotao,LUO Jing.Study on 1D and 2D coupling flow and salinity model for Yangtze River estuary[J].Engineering Journal of Wuhan University,2007,40(2):7-11.
Authors:XIE Zuotao  LUO Jing
Affiliation:1. Department of Hydraulic Engineering, Tsinghua University, Beijing, 100084, China; 2. Changjiang Institute of Survey, Planning, Design and Research, Wuhan 430010,China; 3. Wuhan University Journals Press, Wuhan 430072 ,China
Abstract:1-D and 2-D coupling flow and salinity mathematical model is established,in which Datong to Jiangyin reach is simulated by 1-D model, and Jiangyin to estuary reach is simulated by 2-D model respectively.1-D river-net mathematical model and 2-D horizontal mathematical model in generalized curvilinear coordinate are established respectively; and then 1-D and 2-D models are coupled. The established 1-D and 2-D models are calibrated by field data from the Datong to Jiangyin reach and the Jiangyin to estuary reach.The calculated results are show that the established model is reliable;so that it can be used to simulate the rules of flow and salinity at the Yangtze River Estuary.
Keywords:1D river-net mode  generalized curvilinear coordinate  2D horizontal model  Yangtze River Estuary
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