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Volume 40 Issue 7
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Article Navigation >  Haiyang Xuebao  > 2018  >  40(7): 1-21
Zhao Huanting. Cognitive development of characteristics of the Zhujiang River Estuary[J]. Haiyang Xuebao, 2018, 40(7): 1-21. doi: 10.3969/j.issn.0253-4193.2018.07.001
Citation: Zhao Huanting. Cognitive development of characteristics of the Zhujiang River Estuary[J]. Haiyang Xuebao, 2018, 40(7): 1-21. doi: 10.3969/j.issn.0253-4193.2018.07.001
shu

Cognitive development of characteristics of the Zhujiang River Estuary

doi: 10.3969/j.issn.0253-4193.2018.07.001

  • CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Collaborative Innovation Center for South China Sea Research, Nanjing University, Nanjing 210093, China

  • Received Date: 2017-07-08
  • Rev Recd Date: 2017-12-05
    Abstract
  • Foreign scientists firstly began to examine the delta of the estury of Zhujiang River along with the invasion of powers and the input of theory and technique of modern natural science into China. Then local scientists mastered and developed the associated knowledge and started the research of the natural entity. There are 6 leaps in the cognition of the Zhujiang River Estury. In 1915, W.Olivercrona wrote paper to call it "Guangzhou Delta" after field investigation and first proposed the concept of "Zhujiang River Delta", which is looked as the first leap. The second leap is made by Wu Shangshi, who discovered the geomorphology of sets of ancient sea cliff-sea cave-wave erosion platform and ancient sandbank-dried lagoon in the suburb of Guangzhou in 1937. In the academic debate of the presence of the Zhujiang River Delta, he supported the opinion that the seawater had been transgressioned into ancient estuary and developed delta. He wrote papers in 1941 and in 1947 to affirm the existence of the Zhujiang River Delta and determined its range. The third leap is created by Zeng Zhaoxuan, who proposed the development pattern of beading gap-cut deltas in 1980. He explained the special-time location of the the Zhujiang River Delta according to his creative study of historical morphology. The forth leap is in 1982, when Zhao Huanting revealed that the Zhujiang River Delta overlaid on old delta formed in the later period of later Pleistocene and modern delta forming in the middle Holocene, on the base of Wu Wenzhong's discovery about weathered granophyric ancient estuarine facies clay layer buried in the Zhujiang River Delta. New datum displayed the older delta formed in the middle period of later Pleistocene. The fifth leap is also marked by Zhao Huanting. In 1973-1982,he found the Zhujiang River Estury zone is distinct because river network in delta and residual estuary co-existed. He was one of the first scientists to study riverbed evolution of Zhujiang distributaries in the Shiziyang Distributary, estuary evolution in the Lingdingyang Estuary, and the distributaries mouth evolution in Modaomen distributary mouth. He used Simmons's concept of dominant flows and theory of estuary salt water wedge to study the morphological development and evolution of the distributary mouth and estuary. In 1990 he preliminarily summarized the evolution process of the Zhujiang River Estuary. The sixth leap is from Wu Chaoyu, who quantitatively reappeared the mosaic evolutionary process of the Zhujiang River Delta from 6 ka BP to 2.5 ka BP, according to the mutual confirmation of sedimentology, geomorphydynamics and his long-period mechanism model in 2006.
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