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珠江三角洲沉积体与河网干流河道的形成发育

韦惺 吴超羽

韦惺, 吴超羽. 珠江三角洲沉积体与河网干流河道的形成发育[J]. 海洋学报, 2018, 40(7): 66-78. doi: 10.3969/j.issn.0253-4193.2018.07.006
引用本文: 韦惺, 吴超羽. 珠江三角洲沉积体与河网干流河道的形成发育[J]. 海洋学报, 2018, 40(7): 66-78. doi: 10.3969/j.issn.0253-4193.2018.07.006
Wei Xing, Wu Chaoyu. The formation and development of the deposition bodies and main channels in the Zhujiang River Delta[J]. Haiyang Xuebao, 2018, 40(7): 66-78. doi: 10.3969/j.issn.0253-4193.2018.07.006
Citation: Wei Xing, Wu Chaoyu. The formation and development of the deposition bodies and main channels in the Zhujiang River Delta[J]. Haiyang Xuebao, 2018, 40(7): 66-78. doi: 10.3969/j.issn.0253-4193.2018.07.006

珠江三角洲沉积体与河网干流河道的形成发育

doi: 10.3969/j.issn.0253-4193.2018.07.006
基金项目: 广州市科技计划项目(201607020042)。

The formation and development of the deposition bodies and main channels in the Zhujiang River Delta

  • 摘要: 应用PRD-LTMM长周期"动力-沉积-形态"模型和非线性动力学拉格朗日拟序结构理论对全新世海侵盛期以来珠江三角洲以及河网干道的形成演变进行了地貌动力学分析,结果显示:受曲折岸线和复杂地形的影响,海侵盛期古珠江河口湾的水动力随时空高度变化,形成了7个具有不同运动特性的条带区域,并产生了许多不同尺度且相对独立的沉积动力结构,形成了众多的沉积体。这些沉积体成为了三角洲发育演变的基本建构单元。三角洲的主体沉积可概括为受原始地形分隔的若干相对独立的充填过程,干流河道的形成和发育往往是若干相邻沉积体发育和延伸的结果,而三角洲河网干道的总体分布格局则受这些动力区域所控制。
  • 吴尚时, 曾昭暶. 珠江三角洲[J]. 岭南学报, 1946(1):47-53. Wu Shangshi, Zeng Zhaoxuan. The Pearl River Delta[J]. Lingnan Journal of Chinese Studies, 1946(1):47-53.
    黄镇国, 李平日, 张仲英, 等. 珠江三角洲形成发育演变[M]. 广州:科学普及出版社广州分社, 1982. Huang Zhenguo, Li Pingri, Zhang Zhongying, et al. The Formation and Evolution of the Pearl River Delta[M]. Guangzhou:Guangzhou Branch of Science Popularization Press, 1982.
    曾昭璇, 黄少敏. 珠江三角洲历史地貌学研究[M]. 广州:广东高等教育出版社, 1987:201. Zeng Zhaoxuan, Huang Shaomin. Historical Geomorphology of the Pearl River Delta[M]. Guangdong:Guangdong Higher Education Press, 1987:201.
    李春初. 中国南方河口过程与演变规律[M]. 北京:科学出版社, 2004:248. Li Chunchu. Estuary Process and Evolution in the South China[M]. Beijing:Science Press, 2004:248.
    张虎男. 断块型三角洲[J]. 地理学报, 1980, 35(1):58-67. Zhang Hunan. The fault delta[J]. Acta Geographica Sinica, 1980, 35(1):58-67.
    黄玉昆, 夏法, 陈国能. 断裂构造对珠江三角洲形成和发展的控制作用[J]. 海洋学报, 1983, 5(3):316-327. Huang Yukun, Xia Fa, Chen Guoneng. The impact of fault structure on the formation and development of the Pearl River Delta[J]. Haiyang Xuebao, 1983, 5(3):316-327.
    李平日, 乔彭年. 珠江三角洲六千年来的发展模式[J]. 泥沙研究, 1982(3):33-42. Li Pingri, Qiao Pengnian. The model of evolution of the Pearl River Delta during last 6000 years[J]. Journal of Sediment Research, 1982(3):33-42.
    乔彭年. 珠江三角洲河网发育的成因分析[J]. 人民珠江, 1981, 2:31-40. Qiao Pengnian. Evolution of the river networks in the Pearl River Delta[J]. Pearl River, 1981, 2:31-40.
    Wu Chaoyu, Bao Yun, Ren Jie, et al. A study on the Pearl River Delta in the last 6000 years:A long-term modeling approach[C]//International Conference on Tidal Dynamics and Environment (TIDAL ITE 2002). Hangzhou, 2002.
    任杰. 末次海进盛期以来珠江三角洲演变的长周期动力地形模型及应用[D]. 广州:中山大学, 2003. Ren Jie. The long-term dynamic terrain model and its application in the evolution of the Pearl River Delta since the Last Great Ocean Expansion[D]. Guangzhou:Sun Yat-sen University, 2003.
    吴超羽, 包芸, 任杰, 等. 珠江三角洲及河网形成演变的数值模拟和地貌动力学分析:距今6000~2500 a[J]. 海洋学报, 2006, 28(4):64-80. Wu Chaoyu, Bao Yun, Ren Jie, et al. A numerical simulation and mophodynamic analysis on the evolution of the Zhujiang River Delta:6000-2500 a BP[J]. Haiyang Xuebao, 2006, 28(4):64-80.
    韦惺, 吴超羽, 任杰, 等. 6 ka以来广州溺谷湾形成演变的数值模拟和地貌动力学分析[J]. 中国科学D辑:地球科学, 2008, 38(11):1384-1395. Wei Xing, Wu Chaoyu, Ren Jie, et al. A numerical simulation and mophodynamic analysis on the evolution of the drowned valley of Guangzhou since 6000 yrBP[J]. Science China Earth Sciences, 2008, 38(11):1384-1395.
    Wei Xing, Wu Chaoyu. Long-term process-based morphodynamic modeling of the Pearl River Delta[J]. Ocean Dynamics, 2014, 64(12):1753-1765.
    何志刚. 珠江三角洲大鳌平原形成与古磨刀门动力演变的互动机制研究[D]. 广州:中山大学, 2006. He Zhigang. Research on the interaction mechanism between the formation of the Daban Plain in the Pearl River Delta and the dynamic evolution of ancient Modaomen[D]. Guangzhou:Sun Yat-sen University, 2006.
    韦惺. 全新世以来珠江三角洲的沉积演变模式研究[D]. 广州:中山大学, 2010. Wei Xing. A study of the Holocene sedimentary evolution pattern of the Pearl River Delta[D]. Guangzhou:Sun Yat-sen University, 2010.
    李平日, 乔彭年, 郑洪汉, 等. 珠江三角洲一万年来环境演变[M]. 北京:海洋出版社, 1991:154. Li Pingri, Qiao Pengnian, Zheng Honghan. Environmental Changes of the Pearl River Delta in the Last 10000 Years[M]. Beijing:China Ocean Press, 1991:154.
    Wei Xing, Wu Chaoyu. Holocene delta evolution and sequence stratigraphy of the Pearl River Delta in South China[J]. Science China Earth Sciences, 2011, 54:1523-1541.
    韦惺, 莫文渊, 吴超羽. 珠江三角洲地区全新世以来的沉积速率与沉积环境分析[J]. 沉积学报, 2011, 29(2):328-335. Wei Xing, Mo Wenyuan, Wu Chaoyu. Analysis on the sedimentation rates and depositional environment of the Pearl River Delta since Holocene[J]. Acta Sedimentologica Sinica, 2011, 29(2):328-335.
    Haller G, Yuan G. Lagrangian coherent structures and mixing in two dimensional turbulence[J]. Physica D, 2000, 147:352-370.
    Haller G. Lagrangian coherent structures from approximate velocity data[J]. Physics of Fluids, 2002, 14(6):1851-1861.
    Shadden S C, Lekien F, Marsden J E. Definition and properties of Lagrangian coherent structures from finite-time Lapunov exponents in two-dimensional a periodic flows[J]. Physica D, 2005, 212(3/4):271-304.
    Lekien F, Coulliette C. Chaotic stirring in quasi-turbulent flows[J]. Philosophical Transactions of the Royal Society A, 2007, 365:3061-3084.
    Shadden S C, Lekien F, Paduan J D, et al. Thecorrelation between surface drifters and coherent structures based on high frequencyradar data in Monterey Bay[J]. Deep-Sea Research Ⅱ, 2009, 56:161-172.
    Wu C, Wei X, Ren J, et al. Morphodynamics of the rock-bound outlets of the Pearl River estuary, South China-A preliminary study[J]. Journal of Marine Systems, 2010, 82:S17-S27.
    吴超羽, 何志刚, 任杰, 等. 珠江三角洲中部子平原形成演变机理研究——以大鳌平原为例[J]. 第四纪研究, 2007, 27(5):814-827. Wu Chaoyu, He Zhigang, Ren Jie, et al. Physical study on the evolution of the sub-deltaic plains in the mid Zhujiang River Delta:a case study of da'ao sub-delta[J]. Quaternary Sciences, 2007, 27(5):814-827.
    莫文渊. 珠江三角洲顺德平原和番禺平原的形成及其动力机制研究[D]. 广州:中山大学, 2010. Mo Wenyuan. Formation and dynamic mechanism of Shunde Plain and Panyu Plain in the Pearl River Delta[D]. Guangzhou:Sun Yat-sen University, 2010.
    Zong Y, Huang G, Switzer A D, et al. An evolutionarymodel for the Holocene formation of the Pearl River delta, China[J].The Holocene, 2009, 19(1):129-142.
    蒋陈娟. 珠江三角洲网河潮汐空间特征[J]. 中山大学研究生学刊:自然科学、医学版, 2007, 28(3):78-90. Jiang Chenjuan. The tidal spatial character of the pearl river delta[J]. Journal of the Graduates Sun Yat-Sen University:Natural Sciences, Medicine, 2007, 28(3):78-90.
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出版历程
  • 收稿日期:  2018-05-30
  • 修回日期:  2018-06-15

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