海岸带海底地下水排放估算
review of approaches to submarine groundwater discharge flux
地下水入海通量是海陆相互作用的重要组成部分,也是全球水循环的重要环节,相关研究表明地下水向海排泄是陆地污染物质和营养盐排放入海的重要通道,对海水系统物质和能量的输入会产生重要影响,同时对近岸的海域环境也有一定的影响。 地下水入海通量的研究在国外尤其是美国、日本等国家受到相当的重视,而这方面的研究在我国还处于空白阶段。文中介绍了地下水入海通量估算的三类方法:示踪技术、物理测定法和模型方法。其中模型方法又主要介绍了断面法、水量平衡法、水文分割法和数值模拟法,且探讨了地下水入海通量各种方法的发展趋势。
Submarine groundwater discharge (SGD) is an important part of interactions between sea and land. Also it is an important section of the worldwide water circulation. Relative research reveals that it serves as a significant pathway for land nutrients and pollutants to the coastal ocean. So it can severely influence material and energy inputs to the ocean system, and nearshoreneritic maritime space environment. American, Japan and many other countries attach more and more attention to the study on SGD. But in our country, relative research in this field is still blankness, we seldom examine submarine groundwater discharge. This paper provides three basic approaches to the SGD flux, including tracer techniques, direct measurements and modeling techniques. There about modeling techniques, this paper concentrate on four approaches: Darcy’s Law and Dupuit-Ghyben-Herzberg formula, water balance approaches, hydrograph separation techniques and numerical simulations. This paper also present their tendency in detail.
胡星、陶大伟
海洋学环境科学理论环境科学技术现状
地下水入海通量示踪技术数值模拟法
Submarine groundwater discharge fluxtracer techniquesmodeling techniques
胡星,陶大伟.海岸带海底地下水排放估算[EB/OL].(2009-01-19)[2025-08-16].http://www.paper.edu.cn/releasepaper/content/200901-854.点此复制
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