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Wang Wenjie. SEDIMENTATION AND SEDIMENTARY FACIES OF THE ZHUJIANG (PEARL RIVER)MOUTH[J]. Acta Sedimentologica Sinica, 1985, 3(2): 129-140.
Citation: Wang Wenjie. SEDIMENTATION AND SEDIMENTARY FACIES OF THE ZHUJIANG (PEARL RIVER)MOUTH[J]. Acta Sedimentologica Sinica, 1985, 3(2): 129-140.

SEDIMENTATION AND SEDIMENTARY FACIES OF THE ZHUJIANG (PEARL RIVER)MOUTH

  • Received Date: 1982-12-03
  • Publish Date: 1985-06-10
  • The Zhujiang river mouth is a drainage basin of Zhujiang river system. The amount of yearly average runoff is totally 341.2xl08m3, and the amount of annual suspended silt is 83.36 million tons, 80% of which enters into the Zhujiang river mouth area. A large area of silt-clay or sandy deposits has been formed under the coaction of the river and the sea. Dynamic and environmental features at the Zhujiang mouth are as follows: 1 The discharges of runoff and suspended silt mainly occur during the flood season, and respectively account for 80% and 81--95% of the annul amounts; 2 Water mass of the South China Sea is a constant influence on the river mouthj 3 River flow and tidal current at each river mouth or estuary are different from one another in intensity) 4 Water currents flowing at river mouths or estuaries are to-and-fro currents, but outside they are rotative currents; 5 The nearshore current mainly flows southwe-stward; 6 A large amount of organic matters and chemical elements is carried into the estuary. According to the dynamic and environmental condintions,three types of sedim- entation can be classified at the Zhujiang mouth: 1 Distributary mouths(including Jiaomen,Honggili,Hengmen,Medaomen,Jitimen,Hutiaomen),at which runoff affection is dominent and tidal affection is weaker; 2 Esturies(river mouths are mainly affected by tide), such as, Lingdinyang(Humen) and Huangmaohai(Yamen). Their yearly runoff is far smaller than the tidal current and varies a lot. At estuaries, salt water is mixed with fresh water and a sharp variation occurs because of the flood season and low-water season; 3 Shelf shallow sea, which is not only affected by tidal, sea and inshore currents, but also affected by river fresh water. However, its sedimentary environment is dominated by sea factors. Its main sedimentary facies are river-mouth sand bar, forelandaccretion bed, alluvial-river bed, subaerial or subaquatic levees, interdistributary bay, flood-tide trough, predelta, tidal channel, tidal sand bar, tidal flat and shelf shallow sea.
  • [1] (1)吴文中等,1976,珠江三角洲的沉积相与肥水的分布规律,《南海海岸地貌学论文集》第3集,南海海洋研究所。

    (2)范信平,1982,试论伶仃洋射流结构和沉积类型的关系《热带地理》,1期。

    (3)王文介,1982,伶仃洋近期淤积演变间题《热带地理》,2期。

    (4)A"J斯科特和W"J·费希尔,1969,三角洲体系和三角洲沉积作用《三角洲沉积与油气勘探》,(陈景山、陈昌明译1981 ) 1 -34,石油工业出版社。

    (5)J"M·科尔曼和L"D赖特,1975,现代河流三角洲:作用和砂体的可变性《三角洲沉积与油气勘探》(陈景山、陈昌明译,1981 ) 43-81石油工业出版社。

    (6)L"D"赖特,河口的沉积搬运和沉积作用《河口海岸研究》,1980年7期(唐钧蓓译),华东师范大学河口海岸研究所。

    (7)Prithard.D.W.1955, Estuarine circulation patterns proc.Amer.Soc. Civil Eng 81 No 717.

    (8)Chau.Y.K.and Wong.C.K.1960, Oceanographical investigations in the Northern shelf region of the South China sea off Hong Kong, Hong Kong Union Fish J.(3)1 -25.
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  • Received:  1982-12-03
  • Published:  1985-06-10

SEDIMENTATION AND SEDIMENTARY FACIES OF THE ZHUJIANG (PEARL RIVER)MOUTH

Abstract: The Zhujiang river mouth is a drainage basin of Zhujiang river system. The amount of yearly average runoff is totally 341.2xl08m3, and the amount of annual suspended silt is 83.36 million tons, 80% of which enters into the Zhujiang river mouth area. A large area of silt-clay or sandy deposits has been formed under the coaction of the river and the sea. Dynamic and environmental features at the Zhujiang mouth are as follows: 1 The discharges of runoff and suspended silt mainly occur during the flood season, and respectively account for 80% and 81--95% of the annul amounts; 2 Water mass of the South China Sea is a constant influence on the river mouthj 3 River flow and tidal current at each river mouth or estuary are different from one another in intensity) 4 Water currents flowing at river mouths or estuaries are to-and-fro currents, but outside they are rotative currents; 5 The nearshore current mainly flows southwe-stward; 6 A large amount of organic matters and chemical elements is carried into the estuary. According to the dynamic and environmental condintions,three types of sedim- entation can be classified at the Zhujiang mouth: 1 Distributary mouths(including Jiaomen,Honggili,Hengmen,Medaomen,Jitimen,Hutiaomen),at which runoff affection is dominent and tidal affection is weaker; 2 Esturies(river mouths are mainly affected by tide), such as, Lingdinyang(Humen) and Huangmaohai(Yamen). Their yearly runoff is far smaller than the tidal current and varies a lot. At estuaries, salt water is mixed with fresh water and a sharp variation occurs because of the flood season and low-water season; 3 Shelf shallow sea, which is not only affected by tidal, sea and inshore currents, but also affected by river fresh water. However, its sedimentary environment is dominated by sea factors. Its main sedimentary facies are river-mouth sand bar, forelandaccretion bed, alluvial-river bed, subaerial or subaquatic levees, interdistributary bay, flood-tide trough, predelta, tidal channel, tidal sand bar, tidal flat and shelf shallow sea.

Wang Wenjie. SEDIMENTATION AND SEDIMENTARY FACIES OF THE ZHUJIANG (PEARL RIVER)MOUTH[J]. Acta Sedimentologica Sinica, 1985, 3(2): 129-140.
Citation: Wang Wenjie. SEDIMENTATION AND SEDIMENTARY FACIES OF THE ZHUJIANG (PEARL RIVER)MOUTH[J]. Acta Sedimentologica Sinica, 1985, 3(2): 129-140.
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