Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Weiyan Xin"'
Publikováno v:
Water, Vol 15, Iss 11, p 2047 (2023)
In China’s Yangtze River Basin, systematic waterway improvement and dredging maintenance have increased the waterway water depth compared with that before the implementation of the Three Gorges Project. Although the water depth of the middle sectio
Externí odkaz:
https://doaj.org/article/a0f9a0d4067f43fd99c48102e52878f7
Publikováno v:
Water, Vol 14, Iss 16, p 2522 (2022)
Sediment is carried by flows into lake during the formation of lacustrine deltas. The subsequent movement of sediment-laden flow is maintained by the initial momentum at the early stage of delta growth. A theoretical model of the plane jet boundary l
Externí odkaz:
https://doaj.org/article/2f51da0dcc69411da3772e0cb30208e8
Autor:
Wanli Liu, Weiyan Xin
Publikováno v:
Lecture Notes in Civil Engineering ISBN: 9789811961373
The rule of flow distribution in the diversion region at the head of sandbar of bifurcated reach is studied. The results show that there are diversion points and stagnation points in the diversion area at the head of sandbar in straight-bifurcated re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef63c80ea1e1ab0b9df4de5be2266901
https://doi.org/10.1007/978-981-19-6138-0_19
https://doi.org/10.1007/978-981-19-6138-0_19
Publikováno v:
Geomorphology. 303:210-228
A new river discriminant system is presented based on resistance law. A parameter characterizing river morphology and indicators reflecting activity of bed and bank are derived. They are defined as river morphology parameter and river activity indica
Publikováno v:
Applied Ocean Research. 117:102955
The top-tensioned risers have been widely used in the field of ocean engineering. They are usually used to transport fluid flows from seabed wells to surface platforms. Under the action of ocean currents, these risers are often subjected to vortex-in
Publikováno v:
CATENA. 182:104125
In the process of delta evolution, the flow regime and sediment transport change with the development of topography. Flow is the dynamic factor of shaping topography, while sediment scouring and silting is the direct cause of topography formation, an