Morphodynamic evolution of the Xiaoqing River mouth: a Huanghe River-derived mixed energy estuary
OriginalPaper|Updated:2023-05-16
|
Morphodynamic evolution of the Xiaoqing River mouth: a Huanghe River-derived mixed energy estuary
Morphodynamic evolution of the Xiaoqing River mouth: a Huanghe River-derived mixed energy estuary
海洋湖沼学报(英文)2012年30卷第5期 页码:889-904
Affiliations:
1. Key Laboratory of Marine Geology and Environment Institute of Oceanology Chinese Academy of Sciences
2. Nanjing University of Information and Technology
Author bio:
Funds:
Supported by the Knowledge Innovative Program of Chinese Academy of Sciences (No. KZCX2-EW-207), the National Natural Science Foundation of China (Nos. 41106041, 40706035, 40676037, 41076031), the Open Fund of the Key Laboratory of Marine Resources and Environmental Geology, SOA (No. MASEG200807), and the Marine Scientific Research and the Open Fund of the Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences (No. MGE2009KG04)
Morphodynamic evolution of the Xiaoqing River mouth: a Huanghe River-derived mixed energy estuary[J]. 海洋湖沼学报(英文), 2012,30(5):889-904.
Huang, H., Liu, Y. & Qiu, Z. Morphodynamic evolution of the Xiaoqing River mouth: a Huanghe River-derived mixed energy estuary., Chin. J. Ocean. Limnol. 30, 889–904 (2012). https://doi.org/10.1007/s00343-012-1295-4
Morphodynamic evolution of the Xiaoqing River mouth: a Huanghe River-derived mixed energy estuary[J]. 海洋湖沼学报(英文), 2012,30(5):889-904. DOI: 10.1007/s00343-012-1295-4.
Huang, H., Liu, Y. & Qiu, Z. Morphodynamic evolution of the Xiaoqing River mouth: a Huanghe River-derived mixed energy estuary., Chin. J. Ocean. Limnol. 30, 889–904 (2012). https://doi.org/10.1007/s00343-012-1295-4DOI:
Morphodynamic evolution of the Xiaoqing River mouth: a Huanghe River-derived mixed energy estuary
摘要
Abstract
In an estuary
tidal
wave and other marine powers interact with the coast in different ways and affect estuary morphology as well as its evolution. In the Huanghe (Yellow) River estuaries and nearby delta
there are many small sediment-affected estuaries with a unique morphology
such as the Xiaoqing River estuary. In this study
we investigated the special evolution and genetic mechanism of the Xiaoqing River estuary by analyzing graphic and image data with a numerical simulation method. The results show that NE and NE-E tide waves are the main driving force for sandbar formation. Sediment shoals have originated from huge amounts of sediment from the Huanghe River
with consequent deposition at the Xiaoqing River mouth. The lateral suspended sediments beyond the river mouth move landward. Siltation takes place on the northern shoreline near the river mouth whereas erosion occurs in the south. The deposits come mainly from scouring of the shallow seabed on the northern side of the estuary. Storm surges speed up deposition in the estuary. Development of the sediment shoals has occurred in two steps involving the processes of growth and further southward extension. Although the southward shift increases the river curvature and length
the general eastward orientation of the estuary is unlikely to change. Processes on the adjacent shorelines do not affect the development of the sediment shoals. The study presents a morphodynamic evolutionary model for the Xiaoqing River estuary
with a long-term series cycle
within which a relatively short cycle occurs.
关键词
Keywords
references
Blott S J, Pye K, van der Wal D, Neal A. 2006. Long-term morphological change and its causes in the Mersey Estuary, NW England. Geomorphology, 81(1–2): 185–206.
Blumberg A F, Mellor G L. 1983. Diagnostic and prognostic numerical circulation studies of the South Atlantic Bight. J. Geophysical Res., 88(NC8): 4 579–4 592.
Bumingham H, French J. 2006. Morphodynamics behaviour of a mixed sand-gravel ebb-tidal delta: Deben estuary, Suffolk, UK. Marine Geology, 225(1–4): 23–44.
Chen B, Huang H J, Yan L W, Mei B. 2009. Sediment movement and the effect of wind to sediment transport near Xiaoqing River Estuary. Acta Oceanologica Sinica, 31(2): 104–112. (in Chinese with English abstract)
Chen B A. 1982. Dynamic analysis of sediment in Xiaoqinghe River estuary and the adjacent regions. Marine Science Bulletin, 5: 57–70. (in Chinese with English abstract)
Edmonds D A, Slingerland R L. 2007. Mechanics of river mouth bar formation: implications for the morphodynamics of delta distributary networks. J. Geophys. Res.-Earth Surf., 112(F3): F02034.
Frazier P S, Page K J. 2000. Water body detection and delineation with Landsat TM data. Photogrammetric Engineering and Remote Sensing, 66(12): 1 461–1 467.
Huang H J, Li C Z. 1994. Application of Landsat images to the studies of the shoreline changes of the Huanghe River delta. Marine Geology & Quaternary Geology, 14(2): 29–37. (in Chinese with English abstract)
Huang H J, Short A D, Zeng T, Hanslow D. 2004. Impact of Brunswick River mouth training walls on adjacent beaches, Brunswick Heads, New South Wales, Australia. China Ocean Engineering, 18(2): 207–220.
Karunarathna H, Reeve D, Spivack M. 2008. Long-term morphodynamic evolution of estuaries: an inverse problem. Estuarine, Coastal and Shelf Science, 77(3): 385–395.
Li B C. 1999. Analysis of the influence of bed-load transport on the navigation channel deposition. Journal of Waterway and Harbor, 4: 29–34. (in Chinese with English abstract)
Li B C, Yang S S. 1999. Study of evolution regulation due to erosion and siltation at the Xiaoqinghe River mouth. Journal of Waterway and Harbor, 3: 27–32. (in Chinese with English abstract)
Ma S S, Xin F Y, Cui Y, Qiao X Y. 2004. Assessment of main pollution matter volume into the sea from Yellow River and Xiaoqing River. Marine Fisheries Research, 25(5): 47–51. (in Chinese with English abstract)
Maiti S, Bhattacharya A K. 2009. Shoreline change analysis and its application to prediction: a remote sensing and statistics based approach. Marine Geology, 257(1–4): 11–23.
Masselink G, Cointre L, Williams J, Gehrels R, Blake W. 2009. Tide-driven dune Migration and sediment transport on an intertidal shoal in a shallow estuary in Devon, UK. Marine Geology, 262(1–4): 82–95.
Moore R D, Wolf J, Souza A J, Flint S S. 2009. Morphological evolution of the Dee Estuary, eastern Irish Sea, UK: a tidal asymmetry approach. Geomorphology, 103(4): 588–596.
Oey L Y, Zhang Y H, Chen P. 1992. Simulation of the Norwegian coastal current in the vicinity of the Halten Bank: comparison with observations and process study of bank-induced meanders. Journal of Marine Systems, 3(4–5): 391–416.
Ryu J H, Won J S, Kyung D M. 2002. Waterline extraction from Landsat TM data in a tidal flat: a case study in Gomso Bay, Korea. Remote Sensing of Environment, 83(3): 442–456.
Saye S E, van der Wal, Pye K, Blott S J. 2005. Beach-dune morphological relationships and erosion/accretion: an investigation at five sites in England and Wales using LIDAR data. Geomorphology, 72(1–4): 128–155.
Sha L P. 1989. Sand transport patterns in the ebb-tidal delta off Texel inlet, Wadden Sea, the Netherlands. Marine Geology, 86: 137–154.
Van Rijn L C. 1984. Sediment transport, part II: suspended load transport. J. Hydr. Engr., 110(11): 1 613–1 638.
Wang X N. 1999. Storm surges along the coast of China. Impact of Science on Society, 2: 39–43. (in Chinese with English abstract)
Wang Y B. 2007. Statistical forecast model of storm surge on west coast of the Bohai Sea. Meteorological Monthly, 33(9): 40–46. (in Chinese with English abstract)
Xiong S L, Zeng J. 2008. Study on classification index and fluvial processes of tidal estuaries. J. Hydr. Engr., 39(12): 1 286–1 295. (in Chinese with English abstract)
Yang L H. 1998. Coastal storm surge in China. China Offshore Platform, 13(3): 25–27. (in Chinese with English abstract)
Yu C S, Wang Y L. 2002. Study on flood processes to middle-sized reservoirs in Xiaoqinghe River basin. Journal of Shandong University of Technology, 32(1): 62–66. (in Chinese with English abstract)
Zhang S P, Xu Z S, Wang J, Ding J L, Hou Q H. 2002. Study on extratropical storm surge forecasting in Laizhou Bay. Marine Forecasts, 19(1): 64–72. (in Chinese with English abstract)
The trial reading is over, you can activate your VIP account to continue reading.