波浪海滩沙丘相互作用模式研究述评

摘要/Abstract

摘要： 波浪-海滩-沙丘相互作用模式是对海岸沙丘形成与演化机理的宏观解析，是了解和认识海岸沙丘形态、类型与规模等的区域差异的基本途径，与海岸沙丘表面风沙流过程研究一样是研究海岸风沙问题不可或缺的重要方面。在对20世纪80年代以来国内外关于波浪-海滩-沙丘间相互作用模式研究历程回顾的基础上，重点总结和概述了国外所提出的波浪-海滩-沙丘间相互作用模式，包括小尺度的波浪-海滩-沙丘相互作用模式、中尺度的波浪-海滩-沙丘相互作用模式等，并展望了未来我国波浪-海滩-沙丘相互作用模式研究的基本方向与主要内容。

关键词: 波浪, 海滩, 沙丘, 相互作用, 模式

Abstract: Comparing with the research on the aeolian process over coastal dune, research on the surfzone-beach-dune interaction models is the macroscopic explanation to the coastal dune origination and evolution mechanism, which is the base to understand the regional differences of coastal dune type and size and so on, and is one of the most important aspects of coastal aeolian research. The development process of research on the surfzone-beach-dune interaction model since 1980 was concluded. The surfzone-beach-dune interaction models proposed by some scientists in west countries were summarized and introduced, which included the surfzone-beach-dune interaction models with small scale and middle scale. At last, some suggestions to improve the research on the surfzone-beach-dune interaction models in China were put forward.

Key words: surfzone, beach, coastal dune, interaction, model

中图分类号:

P931.1

董玉祥. 波浪海滩沙丘相互作用模式研究述评[J]. 中国沙漠, 2010, 30(4): 796-800.

DONG Yu-xiang. Progress and Prospect of Research on the Surfzone-beach-dune Interaction Models[J]. JOURNAL OF DESERT RESEARCH, 2010, 30(4): 796-800.

参考文献

[1]Sherman D J,Bauer B O.Dynamics of beach-dune systems[J].Progress in physical geography,1993,17(4):413-447.
[2]Nordstorm K,Psuty N P,Carter B.Coastal dunes:form and process[M].Chichester:John Wiley & Sons,1990:1-387.
[3]Short A D,Hesp P A.Wave,beach and dune interactions in southeastern Australia[J].Marine Geology,1982,48:259-284.
[4]Sherman D J,Lyons W.Beach-state controls on Aeolian sand delivery to coastal dunes[J].Physical Geography,1994,15:381-395.
[5]Psuty N P.Principles of dune-beach interaction related to coastal management[J].Thalassas,1986,4:11-15.
[6]Hesp P.Surfzone,beach,and foredune interaction on the Australian southeast coast[J].Journal of Coastal Research,1988(special issue 3):15-25.
[7]Psuty N P.Dune/beach interaction[J].Journal of Coastal Research,1988(special issue 3):1-136.
[8]Mclachlan A.The exchange of material between beach and dune system[M]//Nordstorm K F,PsutyV P,Carter R W G.Coastal Dunes:Form and Process.Chichester:Wiley,1990:201-215.
[9]Psuty N P.Spatial variation in coastal foredune development[M]//Cater R W G,Curtis T G F,Sheehy-Skeffington M J.Coastal Dunes:Geomorphology,Ecology and Management for Conservation.Rotterdam:Balkema,1992:3-13.
[10]Psuty N P.Coastal foredune development and vertical displacement[J].Z Geomorph N F,1996(Suppl.-Bd):211-221.
[11]Pye K.Controls of fluid threshold velocity,rates of aeolian sand transport and dune grain size parameters along the Queensland coast[J].Memoirs,1986,8:483-509.
[12]Wal A,McManus J.Wind regime and sand transport on a coastal beach-dune complex,Tentsmuir,Eastern Scotland[M]//Pye K.The Dynamics and Environmental Context of Aeolian Sedimentary Systems (Geological Society Special Publication No.72).The Geological Society,1993:159-171.
[13]Pye K.Physical and human influence on coastal dune development between the Ribble and Mersey estuaries,northwest England[M]//Nordstrom K F,Psuty N P,Carter R W G.Coastal Dunes:Form and Process.Chichester:Wiley,1990:339-360.
[14]董玉祥.国外海岸沙丘形成与演化的研究[J].海洋地质与第四纪地质,2001,21(2):93-98.
[15]吴正,黄山,胡守真,等.华南海岸风沙地貌研究[M].北京:科学出版社,1995:1-146.
[16]董玉祥.中国海岸风沙研究:进展与展望[J].地理科学进展,2006,25（2）:26-35.
[17]王颖,朱大奎.海岸沙丘成因的探讨[J].中国沙漠,1987,7(3):30－40.
[18]李从先,陈刚,杨红君.福建海岸的风成沉积[J].中国沙漠,1989,9(4):8－18.
[19]傅启龙,沙庆安.昌黎海岸风成沙丘的形态与沉积构造特征及其成因初探[J].沉积学报,1994,12（1）:98-105.
[20]张文开,李祖光.福建长乐海岸沙丘形成发育及其区域分布特征[J].中国沙漠,1995,15（1）:31-36.
[21]陈方,蔡明理,李祖光,等.长乐东部沿海海岸风沙区域分异探讨[J].南京大学学报(自然科学版),1995,31(3):487－494.
[22]傅命佐,徐孝诗,徐小薇.黄、渤海海岸风沙地貌类型及其分布规律和发育模式[J].海洋与湖沼,1997,28(1):56-65.
[23]董玉祥.中国温带海岸沙丘分类系统初步探讨[J].中国沙漠,2000,20(2):159-165.
[24]祁兴芬,庄振业,韩德亮,等.秦皇岛市海岸风成沙丘的研究[J].中国海洋大学学报,2004,34(4):617－624.
[25]董玉祥.中国海岸风沙地貌的类型及其分布规律[J].海洋地质与第四纪地质,2006,26(4):99-104.
[26]董玉祥.国际海岸风沙研究的新进展[J].中国沙漠,2007,27（2）:347-348.
[27]董玉祥.人为干扰下海岸沙丘表面粒度分布变异实证研究[J].中国沙漠,2008,28（2）:202-207.
[28]董玉祥,Hesp P A,Namikas S L,等.海岸横向沙脊表面风沙流结构粒度响应的野外观测研究[J].中国沙漠,2008,28（6）:1022-1028.
[29]董玉祥,马骏,黄德全.河北昌黎黄金海岸横向沙脊表面的粒度分布模式[J].地理研究,2008,27（4）:725-733.
[30]董玉祥,Hesp P A,Namikas S L,等.海岸横向沙脊表面风沙流结构的野外观测研究[J].地理科学,2008,28（4）:507-512.
[31]Dong Yuxiang,Namikas S L,Hesp P A,et al.Field measurements of influence of sand transport rate on the structure of wind-sand flow over coastal transverse ridge[J].Chinese Geographical Science,2008,18(3):255-261.
[32]董玉祥,Namikas S L,Hesp P A.海岸风沙流中不同粒径组沙粒的垂向分布模式[J].地理研究,2009,28（5）:1179-1187.
[33]Bauer B O,Sherman D J.Coastal dune dynamics:Problems and prospects[M]//Goudie A S,Livingstone I,Stokes S.Aeolian Environments,Sediments and Landforms.Chichester:John Wiley and Sons,1999:71-104.