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Fu Qilong, Sha Qingan. Morphology Sedimentary Structural Characteristics and Genesis of The Changli Coastal Dunes,Hebei Province[J]. Acta Sedimentologica Sinica, 1994, 12(1): 98-105.
Citation: Fu Qilong, Sha Qingan. Morphology Sedimentary Structural Characteristics and Genesis of The Changli Coastal Dunes,Hebei Province[J]. Acta Sedimentologica Sinica, 1994, 12(1): 98-105.

Morphology Sedimentary Structural Characteristics and Genesis of The Changli Coastal Dunes,Hebei Province

  • Publish Date: 1994-03-10
  • The Changli coastal dunefield,situated on the southwestern shore of Liaodong Bay. is one of the largest coastal dunefields in China. The dunefield forms a strip 2一3 km wide and more than 30 km long. The dominant dune type in the studied area is transverse dunes,and these dunes have sqpaings of 80一600m with a height 5-38m. Most dune crests are oriented normal to the prevailing wind vector (NE一NEE)·There are close relationships between dune height,width and sapcing (r>0. 8). Eolian sand ripples,composed of well一sorted medium to fine一grained sand,occur mainly on the stoss sides of dunes,with their long axes parallel to the slope. Granule ripples form in the interdune lows of coarse lag deposits. They are form in the interdune lows of coarse lag deposits. They are usually asymmetrical and large,and move slowly than the sand ripples. In the m ain trenches,oriented at right angles to the dune crests,two types of stratifications were recongnized. Low一angle cross一strata sets occur on the surfacial parts of the stoss sides,they dip upwind (NE50一70),with angles less than 110. High一angle cross一strata sets are the dominant type of stratification in studied area,mostly they are tabular一planar,and measurements show the foreset strata with southwestern dips of 28°一31°. Sets of cross一strata in the beach are relatively thin and slightly dipping with angles less than 60. Sand dunes may occur where there is a协rge supply of sand,a wind to move it,and a place in which it can accumulate. Changli Coast,with wide and low一angle beach,is ideal location for these criteria to be met. The original sand source for the Changli coastal dunes is Luanhe River. The abundant fluvial sediments are transported north ward and deposited on the beach by the alongshore currents and waves. The onshore wind blows the well一sorted sand grains off the beach and transports them landward,then builds up large transverse dunes. At present time,the coastal dunes are still active.
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    2 任明达、李淑莺等.1988.渤海现代海进现象剖析,海洋学报,1期,67-75页。

    3 昊秀杰、田素珍等,1986,河北海岸带波浪状况分析,黄渤海海洋,3期,9-15页。

    4 昊正,1987,风沙地貌学,北京:科学出版社。

    5 高善明,1983.滦河口北岸海岸沙丘的形成时代,海洋湖沼通报,3期,30-32页。

    6 蔡爱智、蔡月娥,1983,中国海岸风沙沉积的形成与特征,中国沙漠.3期.1-10页。

    7 Bagnold R.A.,1941,The Physics of Blown Sand and Desert Dunes. Methuen&Co. Ltd.,London. p.56一183.

    Cooper W: S.,1958. Coastal Sand Dune of Gregon and Washington. Geol. Society of America Memoir 72, p. 169.

    8 Gornitz V.S.,1982. Global sea levee trend in the past century. Science, V. 215, p. 1161一1614.

    9 Hunter R. H. and Richmond B. M.,1988. Daily clycles in the coastal dunes. Sediment. Geol.,V.55, p.43一67.

    10 Pye K. and Bowman G. M.,1984, The Holocence marine transgression as a forcing function in episodic dune activity on eastern Australian coast. In:Thom B. G. (ed.),Coastal Geomorphology in Australia. Academics Press,Sydney.p. 179一186.

    11 Short A. D. and Hesp P. A.,1982. Wave, beach and dune interactions in Southeastern Australia. Marine Geol.,V.48. p.259一284.

    12 Wright L. D. et al.,1979. Morphodynamics of reflective and dissipative beach and inshore systems,Southeastern Australi-a. Marine Geol.,V. 32, p. 105一140.
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  • Published:  1994-03-10

Morphology Sedimentary Structural Characteristics and Genesis of The Changli Coastal Dunes,Hebei Province

Abstract: The Changli coastal dunefield,situated on the southwestern shore of Liaodong Bay. is one of the largest coastal dunefields in China. The dunefield forms a strip 2一3 km wide and more than 30 km long. The dominant dune type in the studied area is transverse dunes,and these dunes have sqpaings of 80一600m with a height 5-38m. Most dune crests are oriented normal to the prevailing wind vector (NE一NEE)·There are close relationships between dune height,width and sapcing (r>0. 8). Eolian sand ripples,composed of well一sorted medium to fine一grained sand,occur mainly on the stoss sides of dunes,with their long axes parallel to the slope. Granule ripples form in the interdune lows of coarse lag deposits. They are form in the interdune lows of coarse lag deposits. They are usually asymmetrical and large,and move slowly than the sand ripples. In the m ain trenches,oriented at right angles to the dune crests,two types of stratifications were recongnized. Low一angle cross一strata sets occur on the surfacial parts of the stoss sides,they dip upwind (NE50一70),with angles less than 110. High一angle cross一strata sets are the dominant type of stratification in studied area,mostly they are tabular一planar,and measurements show the foreset strata with southwestern dips of 28°一31°. Sets of cross一strata in the beach are relatively thin and slightly dipping with angles less than 60. Sand dunes may occur where there is a协rge supply of sand,a wind to move it,and a place in which it can accumulate. Changli Coast,with wide and low一angle beach,is ideal location for these criteria to be met. The original sand source for the Changli coastal dunes is Luanhe River. The abundant fluvial sediments are transported north ward and deposited on the beach by the alongshore currents and waves. The onshore wind blows the well一sorted sand grains off the beach and transports them landward,then builds up large transverse dunes. At present time,the coastal dunes are still active.

Fu Qilong, Sha Qingan. Morphology Sedimentary Structural Characteristics and Genesis of The Changli Coastal Dunes,Hebei Province[J]. Acta Sedimentologica Sinica, 1994, 12(1): 98-105.
Citation: Fu Qilong, Sha Qingan. Morphology Sedimentary Structural Characteristics and Genesis of The Changli Coastal Dunes,Hebei Province[J]. Acta Sedimentologica Sinica, 1994, 12(1): 98-105.
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