FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4328106155> ?p ?o ?g. }

• W4328106155 endingPage "104388" @default.
• W4328106155 startingPage "104388" @default.
• W4328106155 abstract "Mud deposition is common on continental shelves worldwide, resulting from various dispersal behaviors of fine-grained sediments. The mud belt found in the East China Sea (ECS) is a product of a complex land-ocean sediment dispersal system, and has thus been the focus of oceanographic research for decades. However, its formation mechanisms, particularly the roles of different local currents on cross-shelf versus longshore transports, are still not clear. Therefore, we conducted a comprehensive review of the provenance and dynamical mechanism of the ECS mud belt, based on existing and new data from fields of geochemistry, sedimentology, and physical oceanography. Our results show that, during the summer, the Nearshore Kuroshio Branch Current (NKBC) intrusion onto the northwestern ECS shelf triggers the formation of transverse circulation and super rip current within the coastal area, facilitating the cross-shelf transport. Subsequently, the current displays a meandering trajectory off the southern Zhoushan Islands, leading to the formation of both cyclonic and anticyclonic eddies. During the winter, this northwards NKBC forms a coupled effect with the southwards Zhe-Min coastal current (ZMCC), enhancing the longshore transport. In winter,the Taiwan Warm Current (TWC) intrudes into the southwestern ECS and also forms a coupled effect with the southwards ZMCC. In summer, the ZMCC shifts northward and collides with the southward-directed Oujiang diluted water then forms a super rip current off the southern Oujiang River estuary. In the Taiwan Strait, we find there is a perennial Taiwan Coastal Current (TCC), which can transport Taiwan-derived sediments to the NKBC. These sediments are then carried further towards the northern ECS shelf. We conclude that the sources of the mud belt are mainly from the Yangtze River-derived sediments, and partially from Taiwan- and Minjiang River-derived sediments. The dispersion and sedimentation of Taiwan-derived sediments are controlled jointly by the TCC, NKBC, and anticyclonic eddy, and mainly occur in summer. The previously deposited Yangtze River-derived sediments in the coastal area are resuspended and then cross-shelf transported to form the depocenters during summertime. The diffusion and deposition of resuspended sediments from the Yangtze River estuary are dominated by the coupled effect of ZMCC, NKBC, and TWC in winter. Finally, with the Yangtze River sediment discharge decreasing, we predict that the ECS mud belt will increase in grain sizes in the coastal areas, and the contribution from small and medium-sized rivers will increase. On the other hand, the eastern portion of the mud belt, i.e. clinofrom's foreset, is expected to continue its gradual accumulation, the nearshore topset accumulation will slow down or experience erosion. These findings have scientific significance in enhancing our understanding of the fates of river-derived sediments to the sea, as well as the interactions between oceans and marginal seas." @default.
• W4328106155 created "2023-03-22" @default.
• W4328106155 creator A5000126673 @default.
• W4328106155 creator A5015050894 @default.
• W4328106155 creator A5053297508 @default.
• W4328106155 creator A5060165452 @default.
• W4328106155 creator A5072132888 @default.
• W4328106155 date "2023-05-01" @default.
• W4328106155 modified "2023-09-30" @default.
• W4328106155 title "Dispersal mechanism of fine-grained sediment in the modern mud belt of the East China Sea" @default.
• W4328106155 cites W1483835817 @default.
• W4328106155 cites W1507616995 @default.
• W4328106155 cites W1527749564 @default.
• W4328106155 cites W1605529503 @default.
• W4328106155 cites W1645950804 @default.
• W4328106155 cites W1663598123 @default.
• W4328106155 cites W1740170171 @default.
• W4328106155 cites W1770643654 @default.
• W4328106155 cites W1826264752 @default.
• W4328106155 cites W1947998206 @default.
• W4328106155 cites W1964135058 @default.
• W4328106155 cites W1967314147 @default.
• W4328106155 cites W1969646402 @default.
• W4328106155 cites W1969699502 @default.
• W4328106155 cites W1972211491 @default.
• W4328106155 cites W1973893814 @default.
• W4328106155 cites W1974270246 @default.
• W4328106155 cites W1974602078 @default.
• W4328106155 cites W1977608619 @default.
• W4328106155 cites W1978582186 @default.
• W4328106155 cites W1980633582 @default.
• W4328106155 cites W1981413656 @default.
• W4328106155 cites W1981751303 @default.
• W4328106155 cites W1982487268 @default.
• W4328106155 cites W1983267892 @default.
• W4328106155 cites W1983325553 @default.
• W4328106155 cites W1983697364 @default.
• W4328106155 cites W1995092177 @default.
• W4328106155 cites W1995163974 @default.
• W4328106155 cites W1997257433 @default.
• W4328106155 cites W2002836338 @default.
• W4328106155 cites W2005533603 @default.
• W4328106155 cites W2005582462 @default.
• W4328106155 cites W2008575755 @default.
• W4328106155 cites W2008904028 @default.
• W4328106155 cites W2008942529 @default.
• W4328106155 cites W2010152632 @default.
• W4328106155 cites W2012103907 @default.
• W4328106155 cites W2013261343 @default.
• W4328106155 cites W2015876559 @default.
• W4328106155 cites W2018606688 @default.
• W4328106155 cites W2021488718 @default.
• W4328106155 cites W2021653161 @default.
• W4328106155 cites W2023534137 @default.
• W4328106155 cites W2025733996 @default.
• W4328106155 cites W2028150759 @default.
• W4328106155 cites W2032843954 @default.
• W4328106155 cites W2036904527 @default.
• W4328106155 cites W2041786212 @default.
• W4328106155 cites W2044664427 @default.
• W4328106155 cites W2049103995 @default.
• W4328106155 cites W2050841105 @default.
• W4328106155 cites W2051604588 @default.
• W4328106155 cites W2054618755 @default.
• W4328106155 cites W2056636229 @default.
• W4328106155 cites W2057487548 @default.
• W4328106155 cites W2062748557 @default.
• W4328106155 cites W2063361150 @default.
• W4328106155 cites W2064210844 @default.
• W4328106155 cites W2069829590 @default.
• W4328106155 cites W2072573938 @default.
• W4328106155 cites W2076890521 @default.
• W4328106155 cites W2078241291 @default.
• W4328106155 cites W2078270931 @default.
• W4328106155 cites W2079840823 @default.
• W4328106155 cites W2079850063 @default.
• W4328106155 cites W2080378619 @default.
• W4328106155 cites W2080723971 @default.
• W4328106155 cites W2081132998 @default.
• W4328106155 cites W2082012545 @default.
• W4328106155 cites W2082889751 @default.
• W4328106155 cites W2083354894 @default.
• W4328106155 cites W2087210562 @default.
• W4328106155 cites W2087662765 @default.
• W4328106155 cites W2091349323 @default.
• W4328106155 cites W2092861444 @default.
• W4328106155 cites W2093278793 @default.
• W4328106155 cites W2094113712 @default.
• W4328106155 cites W2094756898 @default.
• W4328106155 cites W2095449834 @default.
• W4328106155 cites W2102736913 @default.
• W4328106155 cites W2103930806 @default.
• W4328106155 cites W2107356505 @default.
• W4328106155 cites W2108564379 @default.
• W4328106155 cites W2109063799 @default.
• W4328106155 cites W2130946534 @default.
• W4328106155 cites W2133377555 @default.
• W4328106155 cites W2135697520 @default.

• next