Message Board

Respected readers, authors and reviewers, you can add comments to this page on any questions about the contribution, review, editing and publication of this journal. We will give you an answer as soon as possible. Thank you for your support!

Full name
E-mail
Phone number
Title
Message
Verification Code
He Yanyu, Liu Jianhui, Cai Feng, Li Bailiang, Wang Lihui, Zhou Changmao. Several characteristics of beach aeolian sand transport influenced by tide: A case study in the Yuandangao Beach, Pingtan Island, Fujian Province[J]. Haiyang Xuebao, 2018, 40(9): 90-102. doi: 10.3969/j.issn.0253-4193.2018.09.008
Citation: He Yanyu, Liu Jianhui, Cai Feng, Li Bailiang, Wang Lihui, Zhou Changmao. Several characteristics of beach aeolian sand transport influenced by tide: A case study in the Yuandangao Beach, Pingtan Island, Fujian Province[J]. Haiyang Xuebao, 2018, 40(9): 90-102. doi: 10.3969/j.issn.0253-4193.2018.09.008

Several characteristics of beach aeolian sand transport influenced by tide: A case study in the Yuandangao Beach, Pingtan Island, Fujian Province

doi: 10.3969/j.issn.0253-4193.2018.09.008
  • Received Date: 2017-09-05
  • Rev Recd Date: 2018-04-03
  • Coastal aeolian is a typical product of sea, land and air interaction. Based on a comprehensive observation of beach aeolian sand in the Yuandangao beach of Pingtan Island, Fujian Province, this paper aims to explore and summarize the vertical distribution, entrainment and transport characteristics of beach aeolian sand influenced by tide. The main conclusions are as follows:(1) The vertical distribution of wind-sand flow in intertidal zone is almost entirely(98.9%) in the range of 0-30 cm, and the specific distribution function varies with different particle size; (2) The threshold velocity of beach aeolian sand is significantly higher than that of inland desert, and the changing process of it in the tidal circulation mainly reflects the interaction between average surface moisture and fetch length; (3) The wind-blown sand flux of intertidal zone involves the interaction of average surface moisture, fetch length and wind speed, and the dominant factors of its changing process vary in different stages of ebb and flow; (4) Entrainment of sand from a dry source and transport across a moist surface is one of the typical beach aeolian sand transport mode, with a short delivered distance at a time, and a highly relayed way of overall transport.
  • loading
  • 吴正, 吴克刚. 中国海岸风沙研究的进展和问题[J]. 地理科学, 1990, 10(3):230-236. Wu Zheng, Wu Kegang. Progress and problem on research of coastal aeolian erosion in China[J]. Scientia Geographica Sinica, 1990, 10(3):230-236.
    吴正. 风沙地貌学[M]. 北京:科学出版社, 1987. Wu Zheng. Aeolian Landforms[M]. Beijing:Science Press, 1987.
    陈方. 海坛岛海岸风沙特征及其发育[J]. 海洋科学, 1994, 18(6):46-50. Chen Fang. Coastal aeolian characteristics and development of Haitan Island, Fujian[J]. Marine Science, 1994, 18(6):46-50.
    王颖, 朱大奎. 海岸沙丘成因的讨论[J]. 中国沙漠, 1987, 7(3):29-40. Wang Ying, Zhu Dakui. An approach on the formation causes of coastal sand dunes[J]. Journal of Desert Research, 1987, 7(3):29-40.
    刘建辉, 郭占荣, 雷怀彦,等. 福建长乐东部海岸沙丘风蚀坑研究[J]. 应用海洋学学报, 2008, 27(2):230-236. Liu Jianhui, Guo Zhanrong, Lei Huaiyan, et al. A study on coastal dune blowouts in east coast of Changle[J]. Journal of Applied Oceanography, 2008, 27(2):230-236.
    吴正,等. 华南海岸风沙地貌研究[M]. 北京:科学出版社, 1995. Wu Zheng, et al. Research on the Landforms of the Wind-drift Sand in South China Coast[M]. Beijing:Science Press, 1995.
    陈方, 朱大奎. 闽江口海岸沙丘的形成与演化[J]. 中国沙漠, 1996, 16(3):227-233. Chen Fang, Zhu Dakui. Dune formation and evolution along the south coast of Minjiang estuary[J]. Journal of Desert Research, 1996, 16(3):227-233.
    陈方, 贺辉扬. 海岸沙丘沙运动特征若干问题的研究——以闽江口南岸为例[J]. 中国沙漠, 1997, 17(4):355-361. Chen Fang, He Huiyang. Research of several problems on movement characteristics of coastal dune sand-an example from the south coast of Minjiang estuary[J]. Journal of Desert Research, 1997, 17(4):355-361.
    刘建辉. 长乐东部海岸沙丘的沉积与移动特征研究[D]. 厦门:厦门大学, 2007. Liu Jianhui. A study on sedimentary and moving characteristics of sandy dunes in the eastern coast, Changle, Fujian[D]. Xiamen:Xiamen University, 2007.
    董玉祥, 马骏. 风速对海岸风沙流中不同粒径沙粒垂向分布的影响[J]. 中山大学学报:自然科学版, 2008, 47(5):98-103. Dong Yuxiang, Ma Jun. Influence of wind velocity on the vertical distribution of different grain size sands in the wind-sand flow on the coastal dune[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 2008, 47(5):98-103.
    董玉祥, 马骏. 输沙量对海岸沙丘表面风沙流中不同粒径沙粒垂向分布的影响[J]. 中山大学学报:自然科学版, 2009, 48(3):102-108. Dong Yuxiang, Ma Jun. Influence of total sand transport rates on the vertical distribution of different sand grain sizes in wind-sand flow on the coastal dune[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 2009, 48(3):102-108.
    董玉祥, 黄德全, 马骏. 海岸沙丘表面不同部位风沙流中不同粒径沙粒垂向分布的变化[J]. 地理科学, 2010, 15(3):391-397. Dong Yuxiang, Huang Dequan, Ma Jun. Change of vertical distribution of different sand grain sizes in wind-sand flow at different sites over coastal dune[J]. Scientia Geographica Sinica, 2010, 15(3):391-397.
    董玉祥. 海岸现代风成砂粒度参数特征的研究——以中国温带海岸为例[J]. 沉积学报, 2002, 20(4):656-662. Dong Yuxiang. Characteristics of grain size parameters of modern coastal aeolian sands in temperate coastal region in China[J]. Acta Sedimentologica Sinica, 2002, 20(4):656-662.
    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 Yuxiang. Progress and prospect of research on the surfzone-beach-dune interaction models[J]. Journal of Desert Research, 2010, 30(4):796-800.
    董玉祥, 黄德全, 张雪琴. 海岸爬坡沙丘形态对台风响应——以2014年"麦德姆"台风为例[J]. 中国沙漠, 2016, 36(4):865-870. Dong Yuxiang, Huang Dequan, Zhang Xueqin. Observation of morphological responses of a coastal climbing dune to typhoon[J]. Journal of Desert Research, 2016, 36(4):865-870.
    Jackson N L, Nordstrom K F. Effects of time-dependent moisture content of surface sediments on aeolian transport rates across a beach, wildwood, New Jersey, U.S.A.[J]. Earth Surface Processes & Landforms, 1997, 22(7):611-621.
    Wiggs G F S, Baird A J, Atherton R J. The dynamic effects of moisture on the entrainment and transport of sand by wind[J]. Geomorphology, 2004, 59(1/4):13-30.
    Bauer B O, Davidson-Arnott R G D. A general framework for modeling sediment supply to coastal dunes including wind angle, beach geometry, and fetch effects[J]. Geomorphology, 2002, 49(1):89-108.
    Lynch K, Jackson D, Cooper A. The fetch effect on aeolian sediment transport on a sandy beach:a case study from Magilligan Strand, Northern Ireland[J]. Earth Surface Processes & Landforms, 2016, 41(8):1129-1135.
    Reginato R J. Sampling soil-water distribution in the surface centimeter of a field soil[J]. Soil Science, 1975, 120(4):292-294.
    Sherman D J, Swann C, Barron J D. A high-efficiency, low-cost aeolian sand trap[J]. Aeolian Research, 2014, 13(13):31-34.
    吴正, 等. 风沙地貌与治沙工程学[M]. 北京:科学出版社, 2003:61-62. Wu Zheng, et al. Aeolian Landforms and Wind-sand Engineering[M]. Beijing:Science Press, 2003:61-62.
    Van Dijk P M, Stroosnijder L, De Lima J L M P. The influence of rainfall on transport of beach sand by wind[J]. Earth Surface Processes and Landforms, 1996, 21:341-352.
    Neuman M K, Scott M M. A wind tunnel study of the influence of pore water on aeolian sediment transport[J]. Journal of Arid Environments, 1998, 39(3):403-419.
    韩庆杰, 屈建军, 廖空太,等. 海岸湿沙表面风沙传输特征的风洞实验研究[J]. 中国沙漠, 2012, 32(6):1512-1521. Han Qingjie, Qu Jianjun, Liao Kongtai, et al. A wind tunnel experiment of aeolian sand transport over wetted coastal sand surface[J]. Journal of Desert Research, 2012, 32(6):1512-1521.
    Williams G P. Some aspects of the Aeolian saltation load[J]. Sedimentology, 1964, 3(4):257-287.
    White B R. Two-phase measurements of saltating turbulent boundary layer flow[J]. International Journal of Multiphase Flow, 1982, 8(5):459-473.
    Sørensen M. Estimation of some aeolian saltation transport parameters from transport rate profiles[M]//Barndorff Nielsen O E, Mller J T, Rasmussen K R, et al. International Workshop on the Physics of Blown Sand. Denmark:Aarhus University, 1985:141-190.
    Sharp R P. Wind-driven sand in Coachella Valley, California[J]. Geological Society of America Bulletin, 1964, 75(9):785-803.
    Nickling W G. Grain-size characteristics of sediment transported during dust storms[J]. Journal of Sedimentary Petrology, 1983, 53(3):1011-1024.
    Rasmussen K R, Srensen M, Willetts B B. Measurement of saltation and wind strength on beaches[M]//Barndorff Nielsen O E, M ller J T, Rasmussen K R, et al. Proceedings of International Workshop on the Physics of Blown Sand. Denmark:Aarhus University, 1985:301-325.
    Butterfield G R. Near-bed mass flux profiles in aeolian sand transport:high-resolution measurements in a wind tunnel[J]. Earth Surface Processes & Landforms, 1999, 24(5):393-412.
    Stout J E, Zobeck T M. Establishing the threshold condition for soil movement in wind-eroding fields[C]//Proceedings of the International Conference on Air Pollution from Agricultural Operations. MWPS C-3, Kansas City,1996:65-71.
    吴正, 等. 风沙地貌与治沙工程学[M]. 北京:科学出版社, 2003:37-38. Wu Zheng, et al. Aeolian Landforms and Wind-sand Engineering[M]. Beijing:Science Press, 2003:37-38.
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Article views (821) PDF downloads(395) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return