地球科学进展 ›› 2002, Vol. 17 ›› Issue (6): 864 -870. doi: 10.11867/j.issn.1001-8166.2002.06.0864

综述与评述 上一篇    下一篇

国内外河口悬沙通量研究进展
万新宁,李九发,何青,沈焕庭   
  1. 华东师范大学河口海岸国家重点实验室,上海 200062
  • 收稿日期:2002-01-14 修回日期:2002-05-27 出版日期:2002-12-20
  • 通讯作者: 万新宁(1977-),女,吉林人,硕士研究生,主要从事河口悬沙通量研究.E-mail:wanxinning@sina.com.cn E-mail:wanxinning@sina.com.cn
  • 基金资助:

    国家自然科学基金重点项目“长江河口物质通量” (编号: 49736220)资助.

REVIEW OF SUSPENDED SEDIMENT FLUX IN THE WORLD

WAN Xin-ning,LI Jiu-fa,HE Qing,SHEN Huan-ting   

  1. State Key Labortory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China
  • Received:2002-01-14 Revised:2002-05-27 Online:2002-12-20 Published:2002-12-01

系统地介绍了国内外河口悬沙通量研究的进展,目前对于河口悬沙通量主要采用模型研究、水文学方法、机制分解、仪器直接测量等方法从理论和实际相结合的角度来进行研究。目前物理模型的研究成果比较直观,但受到模型尺度和精度等的限制,数学模型研究具有快、准的优点,可以给出令人满意的定性结果,但未能达到定量预报的程度;传统的水文学方法可以用来研究河口地区悬移质泥沙在不同动力因子作用下的输移情况;机制分解法是比较成熟和可靠的方法,但该方法与河口动力机制和泥沙输移过程结合不够;使用先进仪器进行直接测量则受到仪器精度和取样点的布设等条件的限制。因此,关于河口悬沙通量的研究还有待于深入和细化。

The progress of the suspended sediment flux in the world is reviewed in this paper, the methods of researching in theory, simulation experiment, mathematical modeling, hydrological, mechanism analysis and field measurement with the advanced instruments have been adopted to study the suspended sediment flux. The transportation of the suspended sediment in the estuary mainly studied the vertical distribution of suspended sediment concentration and lopsided transportation. The physical models are intuitive, but limited by the scales and precisions of the models and lack of suspended sediment models. The mathematical models can provide qualitative products due to their speed and veracity. The transportation of the suspended sediment, especially the spatio-temporal distribution of the sediment, which can be studied with the traditional hydrological method under the different dynamic factors in the estuary. The mechanism analysis is a mature and credible method, but lacking in combing with the dynamical mechanism and the suspended sediment transportation in the estuary. The field measurement with the advanced instruments is affected by the precision of the instruments and the setting points. As a result, many things of suspended sediment flux need to be done thoroughly. 

中图分类号: 

[1]Holligan P M, de Boois H, eds. Land-Ocean Interactions in the Coastal Zone (LOICZ), Science Plan[R]. Global Change Report 25, 1993. 1-150.
[2]Pernetta J C, Milliman J D, eds. Land-Ocean Interactions in the Coastal Zone (LOICZ), Implementation Plan[R]. Global Change Report 33, 1995.1-125.
[3]Walling D E. Estimating the discharge of contaminants to coastal waters by rivers:some cautionary comments[J]. Marine Pollution Bulletin, 1985, 16: 488-492.
[4]David P. Tidal characteristics of suspended sediment concentrations[J]. Journal of Hydrological Engineering, 1997, 123 (4): 341-350.
[5]Shi Zhong. The processes of the fine sediment particles in the Changjiang estuary[J]. Journal of Sediment Research, 2000, 6: 72-78.[时钟.长江口细颗粒泥沙过程[J]. 泥沙研究, 2000, 6: 72-78.]
[6]Gelfenbaum G, Smith J D. Experimental evaluation of a generalized suspended-sediment transport theory[A].  In: Kinght R J, McLean J R, eds.  Shelf Sands and Sandstone[C]. Canada: Canadian Society of Petroleum Geologists, Memoir Ⅱ: 1986.133-144.
[7]Hill P S, Nowell A R M, Jumar P A. Flume evaluation of the relationship between suspended sediment concerntration and excess boundary shear stress[J]. Journal of Geophysical Research, 1988, 93: 12 499-12 509.
[8]Huang Sheng, Lu Qimiao. The Estuary Dynamic [M]. Beijing: Hydraulic and Electric Press, 1992. [黄胜, 卢启苗. 河口动力学 [M]. 北京:水利电力出版社, 1992.]
[9]Shi Zhong, Zhou Hongqiang. Numerical modeling of  concentration profiles of suspended sediment in the Changjiang estuary [J].  The Ocean Engineering,  2000, 18(3): 57-62. [时钟, 周洪强. 长江口北槽口外悬沙浓度垂线分布的数学模拟[J]. 海洋工程, 2000, 18(3): 57-62.]
[10]Kirby R, Parker W R. Distribution and behavior of fine sediment in the Severn Estuary and Inner Bristol Channel, VK[J]. Canadian Journal of Fishery and Aquatic Sciences, 1983, 40 (supp): 83-95.
[11]Ross M A, Mehta A J. The mechanics of lutoclines and fluid mud[J]. Journal of Coastal Research, 1989, (5): 51-61.
[12]Smith T J, Kirby R. Generation, stabilization and dissipation of layered fine sediment suspension[J]. Journal of Coastal Research, 1989, 5: 63-73.
[13]Wolanski E,  Asaede T,  Imberger J. Mixing across a lutocline[J].  Limnology and Oceanography, 1989, 34: 931-938.
[14]Dou Guoren. The transportation of suspended sediment and the calculation of erosion and deposition in the tides[J]. Journal of Hydraulic Engineering, 1963, 4:31-38. [窦国仁. 潮汐水流中的悬沙运动及冲淤计算[J]. 水利学报, 1963, 4:31-38.]
[15]Xiong Shaolong. The experimental research of the erosion and deposition in the deep channel of the north Hangzhou Bay[J]. Journal of Hydraulic Engineering, 1994, 10:54-60. [熊绍隆.杭州湾北岸深槽冲淤变化实验研究[J]. 水利学报, 1994, 10:54-60.]
[16]Yang Shusen. The Sediment Deposition in the Western Waterway and Local Moved-Bed Model in the Yingkou Habor[Z]. Tianjin Research Institute for Water Transport Engineering, 1990. [杨树森.营口港西水道泥沙淤积和局部动床模型试验研究[Z].交通部天津水运工程科学研究所, 1990.]
[17]Zhou Jifu, Wang Tao, Li Jiachun, et al. Influences of runoff and tide on sediment transport in the Changjiang estuary[J]. Journal of Hydrodynamics, 1999, 3: 90-100.  [周济福, 王涛, 李家春,等. 径流与潮流对长江口泥沙输运的影响[J]. 水动力学研究与进展, 1999, 3: 90-100.]
[18]Falconer R A, Owens P H. The numerical modeling of the suspended sediment flux in the estuary water area [J]. Journal of sediment Information, 1992, 6: 50-57. [Falconer R A, Owens  P H. 河口水域中悬沙通量的数值模拟[J]. 泥沙情报, 1992, 6: 50-57.]
[19]Clarke S, Elliott A J. Modelling suspended sediment concentrations in the firth of Forth[J]. Estuarine, Coastal and Shelf Science, 1998, 47(3): 235-250.
[20]Lin Bingnan, Han Zengcui, Sun Hongbin, et al. Two-D simulation of sediment transport and bed deformation by tides [J]. Journal of Sediment Research, 1988, 2: 1-8. [林秉南, 韩曾萃, 孙宏斌,等. 潮汐水流泥沙输移与河床变形的二维数学模型 [J]. 泥沙研究, 1988, 2: 1-8.]
[21]Zhao Dihua, Tan Renzhong, Tan Weiyan. Mathematical modeling the concentration of suspension in the south branch of Changjiang estuary [J]. Journal of Sediment Research, 1990, 2: 54-62.  [赵棣华,谭仁忠,谭维炎. 长江口南支河段悬移质含沙量计算模型 [J]. 泥沙研究, 1990, 2: 54-62.]
[22]Dou Guoren. Numerical modeling of the sediment in the estuary and coastal zones[J]. Science of China (A), 1995, 25 (9): 995-1 001.  [窦国仁. 河口海岸泥沙数学模型研究[J]. 中国科学(A辑), 1995, 25(9): 995-1 001.]
[23]Oey L Y.  A three-dimensional simulation of the Hudson-Raritan estuary, Part Ⅲ: Salt flux analysis[J]. Journal of Physical Oceanography, 1985, 15: 1 771-1 720.
[24]Sandrine A, Vincent R, Philippe F. Modelling of suspended sediment fluxes off the Rhone River Mouth [J].  Journal of Coastal Research, 1999, 15 (1): 61-73.
[25]Zhu Huifang, Zhou Jixiang. Mathematical simulation and prediction of the navigable channel-bar of the Changjiang estuary [J]. Oceanologia et Limnologia Sinica, 1993, 24(3): 293-303. [朱惠芳,周纪芗. 长江河口航道拦门沙冲淤变化的数学模拟和预测 [J]. 海洋与湖沼, 1993, 24(3): 293-303.]
[26]Xu Haigen, Gu Guochuan. Preliminary studies on dumping region of dredged material in Tongsha navigational channel of the Changjiang estuary [A]. In: Processes of Dynamics and Geomorphology of the Changjiang Estuary[C]. Shanghai: Shanghai Scientific and Technical Publishers, 1988. 237-252.  [徐海根,谷国传.长江口铜沙航道抛泥区初步研究 [A].见:长江河口动力过程与地貌演变 [C].上海:上海科学技术出版社,1988. 237-252.]
[27]Chen Zishen. Analysis on the  net transport of current and sediment in the tonggu waters of Lingding estuary [J]. The Ocean Engineering, 1999, 17 (1): 79-85.  [陈子燊. 伶仃河口湾铜鼓水域水沙净输运分析 [J]. 海洋工程, 1999, 17(1): 79-85.]
[28]Gu Guochuan. Distribution of suspended silt in an area off Changjiang estuary[J].  Donghai Marine Science, 1996, 4 (1): 12-20. [谷国传.长江口外水域悬沙分布特征 [J]. 东海海洋, 1996, 4(1): 12-20.]
[29]Fu Ningping, Bi Aohong. Investigation on some aspects of the movement of suspended sediment in Jiaojiang River [J]. Journal of sediment research, 1989, 9: 51-57. [符宁平,毕敖洪. 椒江悬沙运动若干问题的探讨[J]. 泥沙研究, 1989, 9:51-57.]
[30]Chen Shenliang, Gu Guochuan. Modeling suspended sediment concentrations in the mouth of  Hangzhou bay [J]. Journal of Sediment Research, 2000, 5: 45-50. [陈沈良, 谷国传. 杭州湾口悬沙浓度变化与模拟[J]. 泥沙研究, 2000, 5: 45-50.]
[31]Li Guangxue. The dispersion of the sediment to the sea from the Huanghe River and the river-ocean interaction[J]. Marine Geology & Quaternary Geology, 1999, 19(3): 1-10. [李广雪. 黄河入海泥沙扩散与河海相互作用[J]. 海洋地质与第四纪地质, 1999, 19(3): 1-10.]
[32]Walsh J P, Nittrouer C A. Observations of sediment flux to the Eel continental shelf, North California[J]. Marine Geology, 1999, 154: 55-68.
[33]Lund-Hansen L C, Valeur J, Pejrup M, et al. Sediment fluxes, re-suspension and accumulation rates at two wind-exposed coastal sites and in a sheltered bay[J]. Estuarine, Coastal and Shelf Science, 1997, 44 (5): 521-531.
[34]Jay D A, Geyer W R, Uncles R J, et al. A review of recent development in estuarine scalar flux estimation [J]. Estuaries, 1997, 20 (2): 262-280.
[35]Bowden K F. The mixing processes in a tidal estuary[J]. International Journal of Air and Water Pollution, 1965, 7: 343-356.
[36]Hansen D V. Current and mixing in the Columbia River estuary[Z]. Transactions of the Joint Conference on Ocean Science and Ocean Engineering, 1965. 943-955.
[37]Fisher H B. Mixing and dispersion in estuaries[J].  Annual Review of Fluid Mechanics, 1976, 8: 107-133.
[38]Dyer K R. The salt balance in stratified estuaries [J].  Estuarine and Coastal Marine Science, 1974, 2: 273-281.
[39]Dyer K R. The balance of suspended sediment in the Gironde and Thames estuaries[A]. In: Estuaries Transport Processes[C]. Giessen: Bruhlsche Universitatsdruckerst Publisher,1978. 135-145.
[40]Uncles R J, Elliott R C A, Weston S A. Dispersion of salt and suspended sediment in a partly mixed estuary[J]. Estuaries, 1985, 8: 256-269.
[41]Gerardo M E, Perillo M, Cintia Piccolo. Importance of grid-cell area in the estimation of estuarine residual fluxes[J]. Estuaries, 1998, 21 (1): 14-28.
[42]Gerardo M E, Perillo M, Cintia Piccolo. An interpolation method for estuarine and oceanographic data [J]. Computers & Geosciences, 1991, 17 (6): 813-820.
[43]Gerardo M E, Perillo M, Cintia Piccolo, et al. Algorithm to calculate equal-area grid cells in irregular estuarine cross-sections [J]. Computers & Geosciences, 1999, 25: 277-282.
[44]Wang Kangshan, Su Jilan. Analysis of the circulation and suspended sediment transportation in the South Channel of the Changjiang estuary [J]. The Ocean Science, 1987, 9: 627-637.  [王康缮,苏纪兰. 长江口南港环流及悬移质输运的计算分析[J]. 海洋科学, 1987, 9: 627-637.]
[45]Mario Pino Q, Gerardo M E,  Perillo, et al. Residual fluxes in a cross-section of the valdivia river estuary, Chile [J]. Estuarine, Coastal and Shelf Science, 1994, 38: 491-505.
[46]Shi Weirong. A phenomenological study on tidal variation of turbidity in the south passage of the Changjiang estuary[J]. Acta Geographica Sinica, 1993, 48(5): 412-420. [时伟荣. 长江口浑浊带含沙量的潮流变化及其成因分析[J]. 地理学报,1993,48(5):412-420.]
[47]Shi Weirong, Li Jiufa. Mud transport calculation in Yangtze estuary and analyses of formation of turbidity maximum [J]. Marine Science Bulletin, 1993, 12 (4): 69-76. [时伟荣,李九发. 长江河口南北槽输沙机制及浑浊带发育分析 [J]. 海洋通报, 1993, 12(4): 69-76.]
[48] Dyer K R.Fine Sediment Particle Transport in Estuaries [A].  In: Dronkers J, Leussen W van,eds. Physical Processes in Estuaries [C]. New York: Spring-Verlag, 1988, 295-310.
[49]Bjorn Kjerfve, Stevenson L Harold, Jeffrey A Proehl, et al. Estimation of material fluxes in an estuaries cross section: a critical analysis of spatial measurment density and errors [J].  Liminology and Oceanography, 1981, 26 (2): 325-335.
[50]Paker W R. Sediment mobility and erosion on a multibarred foreshore(Southwest Lanca shire,U K)[A].In: Hails J R, Carr A P, eds. Nearshore Sediment Dynamics and Sedimentation[C]. Chichester: John Wiley,1976.151-179.
[51]Lane A D, Prandle A J, Harrison P D, et al. Measuring fluxes in tidal estuaries: Sensitivity of instrumentation and associated data analyses[J]. Estuarine, Coastal and Shelf Science, 1997,(45): 433-451.
[52]Allen G P, Sauzay G, Castaing P, et al. Transport and deposition of suspended sediment in the Gironde estuary, France [A]. In:Wiley M, ed. Estuarine Processes [C]. New York: Academic Press, 1977,Ⅱ: 63-81.
[53]Schubel J D, Carter H H. Supended sediment budget for Chespeake bay[A]. In Wiley M, ed. Estuarine Processes[C]. New York: Academic Press, 1977,Ⅱ: 48-62.
[54]Krone R B. Sedimentation in the San Francisco Bay system[A]. In: Conomos T J, ed. San Francisco Bay: The Urbanized Estuary[C]. San Francisco: America Association for Science Pacific Divison, 1979. 85-96.
[55]Conimos T J, Peter D H. Suspended-particle transport and circulation in San Francisco Bay: an overview[A]. In: Wiley M, ed. Estuarine Processes[C]. New York: Academic Press, 1977,Ⅱ: 89-97.
[56]McCave I N. Discussion on net transport of sediment through the mouths of estuaries: seaward or landward [J].  Mem Inst Geol Bassin Aquitaine, 1974, 7: 207-213.
[57]Dyer K R. Velocity profiles over a rippled bed and the threshold of sand[J]. Estuarine Coastal Marine Science, 1980, 10: 181-199.
[58]Milliman J D, Shen Huanting. Transport and deposition of river sediment in the Changjiang estuary and adjacent shelf [J]. Continental Shelf Research, 1985,(4): 37-45.
[59]Shen Huanting, Zhang Chao, Mao Zhichang. Patterns of variations in the water and sediment fluxes from the Changjiang river to the estuary[J].  Oceanologia et Limnologia Sinica, 2000, 31(3): 288-294. [沈焕庭,张超,茅志昌. 长江入河口区水沙通量变化规律[J]. 海洋与湖沼, 2000, 31(3): 288-294.]
[60]Cai Deling, Chen F C. the origin and transportation of the organic carbon particles in the Amazon River and the estuary [J]. Journal of Ocean, 1989, 11(4): 458-469. [蔡德陵,陈 F C,艾德蒙德 J M. 亚马孙河及其河口区中颗粒有机碳的来源与运移[J]. 海洋学报, 1989, 11(4): 458-469.]
[61]Yun Caixing, Cai Mengyi. Analysis on the dispersion of the suspended sediment to the sea from the Changjiang River by the satellitic photos[J].   Oceanologia et Limnologia Sinica, 1981,12(5):391-401. [恽才兴,蔡孟裔. 应用卫星象片分析长江入海悬浮泥沙扩散问题[J]. 海洋与湖沼, 1981, 12(5): 391-401.]
[62]Chen Ming, Li Shihong, Liu Xiaojing. Disposing and analysis of the remote sensing information of the suspended sediment in the Changjiang estuary [J]. Journal of Hydraulic Engineering, 1991, 5: 47-51. [陈鸣, 李士鸿, 刘小靖. 长江口悬浮泥沙遥感信息处理和分析[J]. 水利学报, 1991, 5: 47-51.]
[63]He Qing, Yun Caixing, Shi Weirong. The remote sensing analysis of the suspended sediment concentration field in the surface layer of the Changjiang estuary[J]. Progrecess in Natural Science, 1999, 9(2): 160-165.[何青,恽才兴,时伟荣. 长江口表层水体悬沙浓度场遥感分析[J]. 自然科学进展, 1999, 9(2): 160-165.]
[64]Shi Zhong, Zhang Shuying, Hamilton L J. Observation of the acoustic dispersion of the fine suspended sediment transportation near the bed in the estuary [J]. Journal of Acoustics, 1998, 23 (3): 221-227. [时钟, 张叔英, Hamilton L J. 河口近底细颗粒悬沙运动的声散射观测 [J]. 声学学报, 1998, 23(3): 221-227.]
[65]Shi Zhong, Zhou Hongqiang. Vertical profiles of  suspension concentration at the north passage of the Changjiang estuary [J]. Journal of Shanghai Jiaotong University, 1997, 32(11): 132-138. [时钟, 周洪强. 长江口深水航道北槽口外悬沙浓度垂向分布 [J]. 上海交通大学学报, 1997, 32 (11): 132-138.]
[66]Shi Zhong, Ling Honglie. Vertical profiles of fine suspension concentration in the Changjiang estuary [J]. Journal of Sediment Research, 1999, 2: 59-64. [时钟, 凌鸿烈. 长江口细颗粒悬沙浓度垂向分布[J]. 泥沙研究, 1999, 2: 59-64.]

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