FRONT SYSTEMS AND SUSPENDED SEDIMENT DYNAMICS OF LINGDINGYANG BAY IN THE SUMMER, PEARL RIVER ESTUARY, SOUTH CHINA
Author(s) -
Hongkai Wei
Publication year - 2019
Publication title -
applied ecology and environmental research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.234
H-Index - 32
eISSN - 1785-0037
pISSN - 1589-1623
DOI - 10.15666/aeer/1704_84658484
Subject(s) - estuary , pearl , bay , oceanography , sediment , china , front (military) , environmental science , fishery , hydrology (agriculture) , geography , geology , biology , geomorphology , archaeology , geotechnical engineering
Lingdingyang (LDY) is an important navigation waterway for the Pearl River delta (PRD), and an important passage for fresh water and sediments entering the sea. The data and hydrological information, including SSC, current, water level, and bed sediment was collected on July 6-7, 2005 to analyze its characteristics, and sediment transport. The data was entered into a hydrodynamic simulation model used to characterize the processes of sedimentation and morphological evolution of the Pearl River estuary (PRE). LDY was divided into three sub-areas dominated by (1) west shoal area, (2) jet flow area, and (3) saline water area. Navigation engineering and other human activities result in an increase of deposition rate. These characteristics can be greatly accelerated by human activities. Field data and model results indicate that the front system, composed of the shear front and tide incursion front, has an important impact on sedimentation.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom