NUMERICAL SIMULATION OF SEDIMENT DYNAMIC PROCESSES FOR MUD AREAS ON THE EAST CHINA SEA CONTINENTAL SHELVES: A REVIEW
-
摘要: 数值模拟技术可以突破时空限制，是研究沉积动力过程的重要手段。近几十年来，借助数值模式对我国陆架泥质区成因和演化进行了研究，包括泥质区形成的动力机制、沉积速率计算、沉积物的输运和堆积过程、古沉积环境反演等方面。在未来的研究中，仍需从地球系统科学的视角，在改进数值模型，提高沉积动力过程数值模拟技术的基础上，建立陆架大区域、多动力因素耦合数值模型，并开展古今沉积环境数值模拟，探索泥质区形成、演化的时空过程，并探讨陆架海沉积体系相互作用等。Abstract: Numerical simulation is one of the important methods to study sediment dynamic processes without limitation of time and space. In recent decades, numerical models have been widely applied to the study of some key problems concerning muddy deposits on continental shelves, for example, the genetic mechanism, deposition rate calculation, sediment transport and deposition, and ancient sedimentary environment interpretation, etc. In the future, further study will be focused on improving simulation models for the study of spatial and temporal evolution of muddy areas and their interactions with other depositional systems, from the viewpoint of whole continental shelf, which is influenced by various factors.
-
-
[1] 高抒. 浅海细颗粒沉积物通量与循环过程[J]. 世界科技研究与发展,2000,22(5):73-77. [GAO Shu. Fine-grained sediment fluxes and cycling on continental shelves[J]. World Sci-tech R&D,2000,22(5):73-77.]
[2] 高抒. 海洋沉积地质过程模拟:性质与问题及前景[J]. 海洋地质与第四纪地质,2011,31(5):1-6. [GAO Shu. Numerical modeling of marine sedimentary processes:The nature, scientific problems, and prospect.[J] Marine Geology and Quaternary Geology, 2011,31(5):1-6.]
[3] 远航,于定勇. 潮流与泥沙数值模拟回顾及进展[J]. 海洋科学进展,2004,22(1):97-106. [YUAN Hang, YU Dingyong. Review of and advances in numerical modeling of tidal current and sediment[J]. Advances in Marine Science,2004,22(1):97-106.]
[4] 李广雪,杨子赓, 刘勇. 中国东部海域海底沉积环境成因研究[M].北京:科学出版社,2005:65.[LI Guangxue, YANG Zigeng, LIU Yong. Study of Sedimentary Environment on the East China Sea[M]. Beijing:Science Press, 2005:65.] [5] Soulsby R. Dynamics of Marine Sands[M]. Thomas Telford, London, 1997:249.
[6] Wang X H. Tide-induced sediment resuspension and the bottom boundary layer in an idealized estuary[J]. Journal of Physical Oceanography,2002,32,3113-3131.
[7] 李华军,梁丙臣,李东永,等. 悬沙对Mellor-Yamada海洋边界层模型计算结果的影响[J]. 海洋科学,2004,28(1):27-32. [LI Huajun,LIANG Bingchen, LI Dongyong, et al. Influence of suspended sand on calculation of Mellor-Yamada ocean boundary layer model[J]. Marine Science,2004,28(1):27-32.]
[8] HydroQual, Inc. A Primer for ECOMSED[M]. Mahwah, USA. 2004:194.
[9] 高抒. 全球变化中的浅海沉积作用与物理环境演化——以渤、黄、东海区域为例[J]. 地学前缘,2002,9(2):329-335. [GAO Shu. Shallow marine sedimentation and physical environment evolution as a part of global change:an example from the Bohai, Yellow and East China Sea regions[J]. Earth Science Frontiers, 2002,9(2):329-335.]
[10] 石学法,刘升发,乔淑卿,等. 东海闽浙沿岸泥质区沉积特征与古环境记录[J]. 海洋地质与第四纪地质,2010,30(4):19-30. [SHI Xuefa, LIU Shengfa, QIAO Shuqing, et al. Depositional features and palaeoenvironmental records of the mud deposits in Min-Zhe coastal mud area, East China Sea[J]. Marine Geology and Quaternary Geology,2010,30(4):19-30.]
[11] Gao S,Park Y A,Zhao Y Y,et al. Transport and resuspension of Fine-grained sediments over the Southeastern Yellow Sea[C]//Proceeding of the Korea-China international seminar on Holocene and late Pleistocene environments in the Yellow Sea basin. Seoul National University,Seoul,1996:83-98.
[12] 高抒. 沉积物粒径趋势分析:原理与应用条件[J]. 沉积学报,2009,27(5):826-836. [GAO Shu. Grain size trend analysis:Principle and applicability[J]. Acta Sedimentologica Sinica, 2009,27(5):826-836.]
[13] 曹祖德,王桂芬. 波浪掀沙,潮流输沙的数值模拟[J].海洋学报,1993,15(1):107-118. [CAO Zude, WANG Guifen. Numerical simulation of sediment raised by waves and transported by tidal currents[J].Acta Oceanologica Sinica, 1993,15(1):107-118.]
[14] 江文胜,孙文心. 渤海悬浮颗粒物三维输运模式的研究[J]. 海洋与湖沼,2001,32(1):94-100. [JIANG Wensheng,SUN Wenxin. 3D suspended particulate matter transportation model in the Bohai Sea[J]. Oceanologia et Limnologia Sinica,2001,32(1):94-100.]
[15] 江文胜,苏健,杨华,等. 渤海悬浮物浓度分布和水动力特征的关系[J]. 海洋学报,2002(1):212-217.[JIANG Wensheng,SU Jian,YANG Hua, et al. The relationship between SPM concentration and hydrodynamic condition in the Bohai Sea[J]. Acta Oceanologica Sinica, 2002 (1):212-217.]
[16] Li G S,Wang H L,Liao H P. Numerical simulation on seasonal transport variations and mechanisms of suspended sediment discharged from the Yellow River to the Bohai Sea[J]. Journal of Geographical Science, 2010, 20(6):923-937.
[17] Lu J, Qiao F L, Wang X H,et al. A numerical study of transport dynamics and seasonal variability of the Yellow River sediment in the Bohai and Yellow seas[J]. Estuarine Coastal and Shelf Science, 2011, 95(1):39-51.
[18] 金亨植,李炎保,白玉川.黄海西朝鲜湾波浪潮流共同作用下二维潮流泥沙数值模拟与砂矿成矿分析[J].海洋技术,2005(2):75-79.[Kim Hyongsix, LI Yanbao, BAI Yuchuan. Research on the tide-sediment numerical model and placer mineralization by combined wave and tide action in Western Korean Bay of the Yellow Sea[J]. Ocean Technology,2005 (2):75-79.]
[19] Choi B H, Mun J Y,Ko J S. Wintertime suspended sediment simulation in the Huanghai and East China Seas[J]. Acta Oceanologica Sinica, 2005,25(1):46-59.
[20] Yanagi T,Inoue K I. A Numerical experiment on the sedimentation processes in the Yellow Sea and the East China Sea[J]. Journal of Oceanography, 1995(51):537-552.
[21] 雷坤.东海陆架悬浮体输送及其数值研究[D].中国海洋大学博士论文,2000:192.[LEI Kun. Transport and its numerical study of suspended sediment on the east China Sea continental shelf[D]. Doctor thesis of Ocean University of China, 2000:192.] [22] 王勇智,江文胜.渤、黄、东海悬浮物质量浓度冬、夏季变化的数值模拟[J].海洋科学进展,2007,1:28-33.[Numerical simulation of variations in winter and summer suspended material concentrations in the Bohai Sea, Yellow Sea and East China Sea[J]. Advances in Marine Science,2007 ,1:28-33.]
[23] Pang C G, YU W, YANG Y, et al. An improved method for evaluating the seasonal variability of total suspended sediment flux field in the Yellow and East China Seas[J]. International Journal of Sediment Research, 2011,26:1-14.
[24] Wang X H, Qiao F L, Lu J, et al. The turbidity maxima of the northern Jiangsu shoal-water in the Yellow Sea, China[J]. Estuarine Coastal and Shelf Science, 2011,93(3):202-211.
[25] Ono J, Guo X Y. Modeling of suspended Particulate Matter in the East China Sea[C]//Interdisciplinary Studies on Environmental Chemistry-Environmental Pollution and Ecotoxicology. 2012:311-319.
[26] 庞重光,王凡,白学志,等. 夏、冬两季长江口及邻近海域悬浮物的分布特征及其沉积量[J]. 海洋科学,2003,27(12):31-35. [PANG Chongguang,WANG Fan,BAI Xuezhi, et al. Distribution features oif suspended matter and amount of sediment at the Changjiang Estuary and adjacent area[J]. Marine Sciences, 2003,27(12):31-35.]
[27] Hu D X. Upwelling and Sedimentation dynamics I. The role of upwelling in sedimentation in the Huanghai Sea and East China Sea-A description of general features[J]. China J. Oceanol. Limnol.,1984,2(1):12-19.
[28] Qu T D, Hu D X. Upwelling and sedimentation dynamics:A simple model[J]. China J. Oceanol. Limnol.,1993,11(4):289-295.
[29] 朱玉荣. 近百年来渤、黄、东海陆架冲淤作用强度数值研究[J]. 海洋科学,2001a,25(6):35-38. [ZHU Yurong. Numerical study on modern erosion/sedimentation intensity on the continental shelves of the Bohai Sea, Yellow Sea and East China Sea[J]. Marine Science, 2001a,25(6):35-38.]
[30] 王伟,李安春,徐方建,等. 北黄海表层沉积物粒度分布特征及其沉积环境分析[J]. 海洋与湖沼,2009,5:525-531.[WANG Wei, LI Anchun, XU Fangjian, et al. Distribution of surface sediments and sedimentary environment in the North Yellow Sea[J]. Oceanologia et Limnologia Sinica, 2009 , 5:525-531.]
[31] Yang Z S,Milliman J D. Fine-grained sediments of the Changjiang and Huanghe rivers and sediment sources of the East China Sea[C]//Sedimentation on the Continental Shelf,with special Reference to the East China. Beijing:China Ocean Press,1983:436-446.
[32] Milliman J D,Beardsley R C,Yang Z S,et al. Modern Huanghe drived on the outer shelf of the East China Sea:identification and potential transport mechanism[J]. Continental Shelf Research,1985,4:175-188.
[33] 郭志刚,杨作升,胡敦欣,等. 春季东海北部海域悬浮体的分布结构与沉积效应[J]. 海洋与湖沼,1997,28(增刊):66-72.[GUO Zhigang, YANG Zuosheng, HU Dunxin, et al. Suspended particle matters distribution and deposition in the eastern East China Sea in spring[J]. Oceanologia et Limnologia Sinica,1997 , 28(supl.):66-72.]
[34] 肖尚斌. 东海内陆架泥质沉积的古环境记录[D]. 中国科学院研究生院博士论文,2004.[XIAO Shangbin. Postgraduate college of Chinese Academy of Sciences (Institute of oceanology), Doctor thesis,2004] [35] 肖尚斌,李安春,蒋富清,等. 近2 ka闽浙沿岸泥质沉积物物源分析[J]. 沉积学报,2005,23(2):268-274. [XIAO Shangbin, LI Anchun, JIANG Fuqing, et al. Provenance analysis of mud along the Min-Zhe Coast since 2 kaBP[J]. Acta Sedimentologica Sinica,2005, 23(2):268-274.]
[36] Liu J P, Li A C, Xu K H, et al. Sedimentary feature of hte Yangtze River-derived along-shelf clinoform deposit in the East China Sea[J]. Continental Shelf Research, 2006,26(17-18):2141-2156.
[37] Xu F, Li A, Li T, et al. Rare earth element geochemistry in the inner shelf of the East China Sea and its implication to sediment provenances[J]. Journal of Rare Earths,2011, 29(7):702-709.
[38] 肖尚斌,李安春,刘卫国,等. 闽浙沿岸泥质沉积的物源分析[J]. 自然科学进展,2009,19(2):185-191. [XIAO Shangbin, LI Anchun, LIU Weiguo, et al. Source of muddy sedimentation in the Min-zhe coast[J]. Progress in Natural Science,2009,19(2):185-191.]
[39] Zhu Y R, Chang R. Preliminary study of the dynamic origin of the distribution pattern of bottom sediments on the continental shelves of the Bohai Sea, Yellow Sea and East China Sea[J]. Estuarine, Coastal and Shelf Science, 2000, 51:663-680.
[40] 王永红,沈焕庭. 河口海岸环境沉积速率研究方法[J]. 海洋地质与第四纪地质,2002,22(2):115-120. [WANG Yonghong, SHEN Huanting. The study methods of sedimentation rates in the estuarine and coastal environments[J]. Marine Geology and Quaternary Geology, 2002,22(2):115-120.]
[41] 汪亚平,高抒. 胶州湾沉积动力学及相关领域研究进展[J]. 海洋科学,2001,25(2):26-28. [WANG Yaping, GAO Shu. Studies on sediment dynamics and related research fields of Jiaozhou Bay:A review[J]. Marine Sciences, 2001,25(2):26-28.]
[42] 杜瑞芝,刘国贤,杨松林,等. 渤海湾现代沉积速率和沉积过程[J]. 海洋地质与第四纪地质,1990,10(3):15-22. [DU Ruizhi,LIU Guoxian,YANG Songlin, et al. Modern sedimentation rate and sedimentation process in Bohai Bay[J]. Marine Geology and Quaternary Geology, 1990,10(3):15-22.]
[43] 赵一阳,李凤业,秦朝阳,等. 试论南黄海中部泥的物源及成因[J]. 地球化学,1991,2:112-117.[ZHAO Yiyang,LI Fengye,QIN Zhaoyang, et al. Source and genesis of mud in the central part of the South Yellow Sea in special reference to geochemical data[J]. Geochimica,1991 ,2:112-117.]
[44] 李凤业,高抒,贾建军,等. 黄、渤海泥质沉积区现代沉积速率[J]. 海洋与湖沼,2002,33(4):364-369. [LI Fengye, GAO Shu, JIA Jianjun, et al. Contemporary deposition rates of fine-grained sediment in the Bohai and Yellow Seas[J]. Oceanologia et Limnologia Sinica, 2002,33(4):364-369.]
[45] 蒋东辉,高抒,李凤业. 渤海海峡区域现代沉积速率分布的数值计算[J]. 海洋科学,2003,27(3):32-35. [JIANG Donghui, Gao Shu, LI Fengye. Numerical calculations of modern deposition rates for the Bohai Strait Region[J]. Marine Sciences, 2003,27(3):32-35.]
[46] 朱玉荣. 末次冰消期以来渤、黄、东海陆架潮汐、潮流演变过程模拟研究[J]. 青岛海洋大学学报,2002,32(2):279-286. [ZHU Yurong. A numerical simulation study on evolution process of the tide and tidal current on the continental shelves of the Bohai Sea, Yellow Sea and East China Sea Since the last deglaciation[J]. Journal of Ocean University of Qingdao, 2002,32(2):279-286]
[47] 朱玉荣. 潮流场对渤、黄、东海陆架底质分布的控制作用[J]. 海洋地质与第四纪地质,2001,21(2):7-13. [ZHU Yurong. The controlling role of tidal current regime in the distribution patterns of bottom sediments in the continental shelves of the Bohai Sea, Yellow Sea and East China Sea[J]. Marine Geology and Quaternary Geology, 2001,21(2):7-13.]
[48] Chen Q Q, Zhu Y R. Holocene evolution of bottom sediment distribution on the continental shelves of the Bohai Sea, Yellow Sea and East China Sea[J]. Sedimentary Geology,2012,273-274:58-72.
[49] 朱玉荣. 末次盛冰期以来渤、黄、东海陆架底质分布演变过程模拟研究[J]. 黄渤海海洋,2002,20(1):1-10. [ZHU Yurong. Simulation study on the evolution process of distribution pattern of bottom sediments on the continental shelves of the Bohai Sea, Yellow Sea and East China Sea Since the Last Glacial Maximum[J]. Journal of Oceanograpgy of Huanghai and Bohai Seas, 2002,20(1):1-10.]
[50] 朱玉荣. 全新世渤、黄、东海陆架泥沙输运演变过程模拟研究[J]. 黄渤海海洋,2001,19(2):25-38. [ZHU Yurong. Simulation Study on the evolution process of sediment transport on the continental shelves of the Bohai Sea, Yellow Sea and East China Sea During the Holocene[J]. Journal of Oceanograpgy of Huanghai and Bohai Seas, 2001,19(2):25-38.]
[51] 郑妍,郑洪波,王可. 末次冰期以来东海内陆架沉积反映的海平面变化[J]. 同济大学学报:自然科学版,2010,38(9):1381-1386. [ZHENG Yan, ZHENG Hongbo, WANG Ke. History of sea level change since Last Glacial:Reflected by sedimentology of core from East China Sea Inner Shelf[J]. Journal of Tongji University(Natural Science),2010,38(9):1381-1386.]
[52] Liu J,Li A,Chen M,et al. Sedimentary changes during the Holocene in the Bohai Sea and its paleoenvironmental implication[J]. Continent al Shelf Research,2008,28(10-11):1333-1339.
[53] 徐刚,刘健,孔祥淮,等. 南黄海中部泥质沉积成因和物源研究综述[J]. 海洋地质动态,2010,26(2):8-12. [XU Gang,LIU Jian,KONG Xianghuai, et al. Sedimentary origin and provenance of the muddy deposition in the central South Yellow Sea[J]. Marine Geology Letters, 2010,26(2):8-12.]
[54] 赵泉鸿,翦知湣,张在秀. 东海陆架泥质沉积区全新世有孔虫和介形虫及其古环境应用[J]. 微体古生物学报,2009,26(2):117-128. [ZHAO Quanhong, JIAN zhimin, ZHANG Zaixiu. Holocene Benthic foraminifera and ostracoda from the shelf mud area of the East China Sea and their paleoenvironmental implications[J]. Acta Micropalaeontologica Sinica, 2009,26(2):117-128.]
[55] Jian Z,Wang P,Sait o Y,et al. Holocene variability of the Kuroshio Current in the Okinaw a Trough,northwestern Pacific Ocean[J]. Earth and Planetary Science Letters,2000,184(1):305-319.
[56] 郭志刚,杨作升,范德江. 长江口泥质区的季节性沉积效应[J]. 地理学报,2003,58(4):591-597. [GUO Zhigang, YANG Zuosheng, FAN Dejiang. Seasonal sedimentary effect on the Changjiang Estuary Mud Area[J]. Acta Geographica Sinica, 2003,58(4):591-597.]
计量
- 文章访问数: 1772
- HTML全文浏览量: 172
- PDF下载量: 16
下载:
