黄骅港海域泥沙运动的三维数学模拟
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摘要
黄骅港海岸属于粉沙淤泥质海岸,黄骅港自建港以来外航道屡次出现强淤和骤淤,研究黄骅港海域泥沙运动对于港口发展具有重要意义。为此,本文建立了综合考虑风、浪、流作用的三维水动力泥沙数学模型,并将其应用于黄骅港实际工程问题的研究,包括对黄骅港的滩面泥沙粗化问题和航道淤积问题进行分析。本文的具体工作和结论如下:
     首先,本文建立了SWAN风浪模型和EFDC水动力泥沙模型,将潮流、波浪、泥沙三者耦合,构成了考虑风、浪、流共同作用的三维多组分泥沙运动模型,并采用多重嵌套模型模拟黄骅港海域水动力、泥沙运动,模型得到黄骅港海域实测数据的验证。
     其次,将所建立的模型应用于黄骅港海区滩面泥沙粗化现象的模拟。计算结果表明,在6级和8级大风作用下,近岸处海滩床面均发生粗化现象,并且体现出了宏观上自南向北、自东向西滩面粒度由粗渐细的规律。而且风级较大时,底床颗粒的粗化更明显一些。
     最后,利用将所建立的模型对黄骅港在外航道整治工程前后航道淤积状况和回淤物的组成进行分析。结果表明,整治工程以后航道淤积量减小很多,且淤积物中细颗粒泥沙含量增大,整治效果明显。
Huanghua Port was built on silt-muddy coast. Since it was constructed, thesudden siltation occurred many times in Huanghua Port. So it is important for the portdevelopment to study the sediment transport around Huanghua Port. A 3D numericalmodel for multi-fraction sediment transport under the combined action of wind, waveand current was developed in the present thesis and was applied to study the practicalproblems of the Huanghua Port, such as the armoring of the beach and the channelsiltation problem. The main results are summarized as follows:
     Firstly, the SWAN wind wave model and the hydrodynamic and sedimenttransport model of EFDC were introduced. Then combining wind wave, current andthe sediment model together, the sediment transport model for multi-fraction sedimenttransport under the combined action of wind, wave and current was developed. Themodel was applied to simulate the hydrodynamics and sediment transport aroundHuanghua Port using nested simulation. The model was verified through the measureddata in site.
     Secondly, the model was applied to simulate the beach armoring phenomenonaround Huanghua Port. It is found that under the sixth and eighth grade wind loading,the sizes of sediment particles get coarser in the nearshore bed. The grain size becamefiner gradually from south to north and west to east. The armoring phenomenon of theparticles is more obvious with stronger wind.
     Finally, the channel siltation and the sediment composition deposited in thechannel before and after the regulation project was simulated using the model. It isshown that compared to the status before the regulation project, the siltation volumeof the channel decreased and the fine grain in sedimentation material increased. It isconcluded that the regulation project exerts an obvious effect of reducing siltation.
引文
[1]张庆河,张金凤,大尺度建筑物对近岸流场影响分析——以黄骅港为例,第八届全国海岸河口学术研讨会,上海:2004
    [2]曹永华,张庆河,闫澍旺,黄骅港海域二维流场分析,中国港湾建设,2005,(3):1-4
    [3]吴相忠,张庆河,张娜等,黄骅港海域三维流场数值模拟,水利水运工程学报,2005,(3):13-19
    [4]吴明阳,冯玉林,黄骅港沿堤流的研究,第十八届全国水动力学研讨会文集,2004
    [5]张庆河,张金凤,杨华等,黄骅港海域沿堤流现象遥感图像分析,中国港湾建设,2001,(1):29-31
    [6]白玉川,顾元棪,蒋昌波,潮流波流联合输沙及?渤逵傺荼涞睦砺厶逑涤?其数学模拟,海洋与湖沼,2000,31(2):186-196
    [7]邵守良,黄骅港一期工程设计波浪要素计算,港工技术,2004,(2):10-11
    [8]苗士勇,侯志强,黄骅港海域风浪场推算及波浪破碎位置分析,水道港口,2004,(4):41-43
    [9]王殿志,张庆河,时钟,渤海湾风浪场的数值模拟,海洋通报,2004,23(5):10-17
    [10]张宇,刘曙光,马钢峰,黄骅港港外波浪场分析,中国港口码头,2006,(3):12-18
    [11]夏波,张庆河,杨华,水动力时空变化对近岸风浪演化的影响——以渤海湾西南岸为例,海洋通报,2006,25(5):1-8
    [12]徐宏明,冯玉林,黄骅港工程泥沙问题研究,泥沙研究,1998,(1):20-29
    [13]张庆河,王崇贤,杨华等,黄骅港海域表层泥沙特性及其影响,中国港湾建设,2004,(4):14-17
    [14]阎新兴,黄骅港近海区沉积物组成与分布特征,水道港口,2005,26(3):144-148
    [15]张庆河,张娜,胡嵋,黄骅港泥沙静水沉降特性研究,港工技术,2005,(1):1-4
    [16]赵冲久,秦崇仁,黄明政,波流共同作用下近底高含沙水层的探讨,水道港口,2005,(1):12-16
    [17]张庆河,杨华,黄骅港泥沙运动遥感分析报告,交通部天津水运工程科学研究所,天津大学,2002
    [18]马芳,黄骅港周边海域悬浮泥沙运移和海底蚀淤变化规律研究:[博士学位论文],青岛:中国海洋大学,2007
    [19]严冰,粉沙质海岸泥沙运动及航道淤积机理研究:[博士学位论文],天津;天津大学,2008
    [20]高进,黄骅港外航道大风骤淤的机理及其整治,科技导报,2005,23(1):29-31
    [21]张庆河,吴相忠,杨华等,黄骅港外航道整治工程有关问题的探讨,水运工程,2007,(2):74-78
    [22]赵群,韩鸿胜,黄骅港骤淤机理的分析以及波浪作用下近岸含沙量场的三维特性,水道港口,2007,(28):77-80
    [23]曹祖德,我国海岸泥沙运动数值模拟,严恺主编,海岸工程,北京:海洋出版社,2001,665-666
    [24]曹祖德,焦桂英,赵冲久,粉沙质海岸泥沙运动和淤泥分析计算,海洋工程,2004,22(1):59-65
    [25]罗肇森,波、流共同作用下的近底泥沙输移及航道骤淤预报,泥沙研究,2004,(6):1-9
    [26]罗肇森,大风期黄骅港外航道的骤淤估算及防淤减淤措施探讨,水运工程,2004,(10):69-73
    [27]刘家驹,粉沙淤泥质海岸的航道淤积,水利水运工程学报,2004,(1):6-11
    [28]刘国亭,黄骅港海岸泥沙特性及防沙减淤工程措施的研究:[硕士学位论文],天津;天津大学,2005
    [29]白玉川,张彬,张胤祺等,波浪挟沙能力及航道骤淤机理的研究,2007,(6):646-653
    [30]孔令双,曹祖德,李炎保,利用“有效风能”预报航道淤积,水道港口,2004,25(4):209-212
    [31]丛锦松,开敞式航道粉沙骤淤的随机分析:[硕士学位论文],青岛;中国海洋大学,2006
    [32]张明霞,概率理论与随机数值模拟方法在海岸泥沙淤积预测中的应用:[硕士学位论文],青岛;中国海洋大学,2004
    [33]叶青,翁祖章,黄骅港建设中若干问题的探索,水运工程,2003,(4):25-37
    [34]李金亮,卓玉生,蒋国军,对黄骅港航道建设的看法,港工技术,2004,(3):19-23
    [35]张宗亮,多组分细颗粒泥沙输送的二维数值模型:[硕士学位论文],天津;天津大学,2005
    [36]张庆河,侯凤林,夏波等,黄骅港外航道淤积的二维数学模拟,中国港湾建设,2006,(5):6-9
    [37]赵群,基于SWAN和ECOMSED模式的大风作用下黄骅港波浪、潮流、泥沙的三维数值模拟,泥沙研究,2007,(4):17-26
    [38]申霞,基于POM的近海三维水质模型研究及其应用:[硕士学位论文],南京:河海大学,2006
    [39]张燕,海湾入海污染物总量控制方法与应用研究:[博士学位论文],青岛:中国海洋大学,2007
    [40]张娜,风浪作用下粘性泥沙运动的三维数值模拟:[硕士学位论文],天津;天津大学,2004
    [41] Frank Wolk, Three-dimensional lagrangian tracer modelling in Wadden Sea areas:[Diploma thesis], Hamburg; Carl-von-Ossietzky University Oldenburg, 2003
    [42]陈香珍,桩墩影响的二维水动力数值研究:[硕士学位论文],南京:河海大学,2006
    [43]彭靖,磨刀门咸潮上溯的数值模拟及其机理分析:[硕士学位论文],广州;中山大学,2007
    [44]陈秀华,朱良生,COHERENS模式在长江口赤潮源推测中的应用,海洋通报,2007,26(3):3-11
    [45]吴相忠,考虑垂向三维辐射应力的三维水流模型:[硕士学位论文],天津;天津大学,2005
    [46] Zhang Y, Baptista AM, A semi-implicit Eulerian-Lagrangian finite-element modelfor cross-scale ocean circulation, with hybrid vertical coordinates, InternationalJournal for Numerical Methods in Fluids, 2005, 21(3): 71-96
    [47] Zheng L, Chen C, Alber M, A modeling study of the Satilla River Estuary,Georgia, Estuaries, 2003, 26(3): 670-679
    [48]陈伟柏,淡水河口与近海三维水动力模式之模拟与应用:[学位论文],台湾;国立中央大学,2005
    [49]储鏖,Delft3D在天文潮与风暴潮耦合数值模拟中的应用,海洋预报,2004,21(3):29-36
    [50]陈凯麒,MIKE3软件在水温结构模拟中的应用研究:[硕士学位论文],北京:中国水利水电科学研究院,2004
    [51] Kopmann R, Markofsky M, Three-dimensional water quality modelling withTELEMAC-3D, Hydrological Processes, 2000, 14(13): 2279-2292
    [52]邹山,近岸水流和泥沙的数值模拟及其应用:[硕士学位论文],南京;南京水利科学研究院,2000
    [53]孔令双,河口、海岸波浪、潮流、泥沙数值模拟:[博士学位论文],天津;天津大学,2001
    [54]周杰,河口粘性泥沙输运数值模拟——以长江口为例:[博士学位论文],南京;河海大学,2005
    [55]李洪声,河口、海岸泥沙输移数值模拟:[硕士学位论文],大连;大连理工大学,2006
    [56] Tolman HL, A third generation model for wind waves on slowly varying unsteadyand inhomogeneous depths and currents. J Phys. Oceanogr, 1991, 21(6): 782-797
    [57] Ris RC, Holthuijsen LH, Booij N, A spectral model for waves in the near shorezone. Coastal Engineering, 1994, (1): 68-78
    [58] Booij N, Holthuijsen LH, Ris RC, The“SWAN”wave model for shallow water.Coastal Engineering, 1996, (1): 668-672
    [59] McAnally WH, Tomas W, A Two-and three-D modeling systems forsedimentation, Proc of the 3rd Int Symp on River Sedimentation. The Universityof Mississippi, 1986
    [60] Chen RF, Modeling of estuary hydrodynamics-A mixture of art and science.Proceedings of 3rd International Symp on River Sedimentation, USA, TheUniversity of Mississippi, 1986
    [61] Wang SY, Adeff SE, Three-dimensional modeling of river sedimentationprocesses, Proceedings of the third Int. symposium on river sedimentation, USA,The Univ. of Mississippi, 1986: 1594-1601
    [62] Van Rijn LC, Mathematical modeling of morphological processes in the case ofsuspended sediment transport, J Hydr Div, ASCE, 1987, 113(3): 981-994
    [63] Prinos P, Compound open flow with suspended sediments. Advance inHydro-science and Engineering, Part B, USA, The University of Mississippi,1993, (l): 1206~1214
    [64]窦国仁,潮汐水流中的悬沙运动及冲淤计算,水利学报,1963,(4):13-23
    [65]谢鉴衡,魏良瑛,河流泥沙模型的回顾与展望,泥沙研究,1987,(3):23-27
    [66]陈国祥,郁伟族,冲积河流模拟的进展,河海大学科技情报,1989,9(3):11-15
    [67]曹祖德,王运洪,水动力泥沙数值模拟,天津:天津大学出版社,1994
    [68]董壮,三维水流数值模拟研究进展,水利水运工程学报,2002,(3):66-73
    [69]陈国祥,陈界仁,沙捞?巴里,三维泥沙数学模型的研究进展,水利水电科技进展,1998,18(1):13-20
    [70]时钟,李世森,李艳红,近海与河口粘性泥沙输移过程——第六届INTERCOH2000综述,泥沙研究,2002,(3):74-80
    [71] Moffatt N, Hydrodynamic modeling tools and techniques, California StateCoastal Conservancy, 2005
    [72] Foreman MGG, Beauchemin L, Cherniawsky JY, A review of models in supportof oil and gas exploration off the North Coast of British Columbia. Institute ofOcean Sciences, 2005, 26(12): 57-63
    [73] Changsheng Chen, Haosheng Huang, Robert C, A finite volume numericalapproach for coastal coean circulation studies: Comparisons with finite differentmodels, Jourunal of Geophysical Research, 2007, (112): 1-34
    [74]王红,三维多组分泥沙数学模型及其应用:[硕士学位论文],天津;天津大学,2007
    [75] Hamrick JM, A three-dimensinal environmental fluid dynamics computer code:theorical and computational aspect, Special report No.317 in Applied MarineScience and Ocean Engineering, 1992
    [76]李瑞杰,诸裕良,郑金海,虎门太平水道航道整治工程潮流数值模拟计算,http://www.paper.edu.cn
    [77]陈景秋,赵万星,季振刚,重庆两江汇流水动力模型,水动力学研究与进展,2005,20(12):829-835
    [78]陈异晖,基于EFDC模型的滇池水质模拟,云南环境科学,2005,24(4):28-30
    [79]王建平,苏保林,贾海峰等,密云水库及其流域营养物集成模拟的模型体系研究,环境科学,2006,27(7):1286-1291
    [80] Paul M, Craig PE, User’s Manual for EFDC_Explorer: A Pre/Post Processor forthe Environmental Fluid Dynamics Code, 2004
    [81] Mellor GL, Yamada T, Development of a turbulence closure model forgeophysical fluid problems. Rev.Geophys.Space Phys., 1982, (20): 851-875
    [82] Garcia M, Parker G, Entrainment of bed sediment into suspension, J. HydraulicEngineering, 1991, (117): 414-435
    [83] Smith JD, Mclean SR, Spatially averaged flow over a wavy surface, J.Geophysical Research, 1977, (82): 1735-1746
    [84] Van Rijn LC, Sediment transport, partⅡ: Suspended load transport, Journal ofHydraulic Engineering, 1984, 110(11): 1613-1641
    [85] Van Rijn LC, Unified view of sediment transport by currents and waves:suspended transport, Journal of Hydraulic Engineering, 2007, 133(6): 668-689
    [86] Styles R, Glenn SM, Modeling stratified wave and current boundary layers on thecontinental shelf, J. Geophys. Res., 2000, 105(24): 119-24
    [87]韩鸿胜,破碎波作用下的粉沙悬沙浓度垂向分布计算方法的探讨:[硕士学位论文],天津;天津大学,2006
    [88]李孟国,郑敬云,中国海域潮汐预报软件Chinatide的应用,水道港口,2007,28(1):65-68
    [89]神华集团黄骅港建设指挥部,交通部天津水运工程科学研究所,1984~2003年黄骅港泥沙淤积研究资料汇编,2003
    [90] Teeter AM, Sediment Transport in Wind-Exposed Shallow: [Ph D. Dissertation],Vegetated Aquatic Systems, 2002
    [91]钱宁,万兆惠,泥沙运动力学,北京:科学出版社,2003
    [92]交通部天津水运工程科学研究所,神华黄骅港务有限责任公司,黄骅港外航道整治工程整治效果研究(报告材料),2006

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