Temporal and spatial variations of abundance of phycocyanin- and phycoerythrin-rich Synechococcus in Pearl River Estuary and adjacent coastal area

2016 ◽  
Vol 15 (5) ◽  
pp. 897-904 ◽  
Author(s):  
Tao Jiang ◽  
Chao Chai ◽  
Jifang Wang ◽  
Ling Zhang ◽  
Jingyi Cen ◽  
...  
Keyword(s):  
Coastal Area ◽  
River Estuary ◽  
Pearl River Estuary ◽  
Spatial Variations ◽  
Pearl River ◽  
Temporal And Spatial Variations ◽  
Temporal And Spatial ◽  
Adjacent Coastal Area

scholarly journals Temporal and Spatial Variations of Hypoxic Water and Suspended Substances around Tama River Estuary in Tokyo Bay, Japan

2007 ◽  
Vol 54 ◽  
pp. 1036-1040 ◽  
Author(s):  
Hiroshi YAGI ◽  
Nobuaki EZURE ◽  
Hajime ISE ◽  
Kazuo NADAOKA ◽  
Kazunobu MOROHOSHI ◽  
...  
Keyword(s):  
River Estuary ◽  
Spatial Variations ◽  
Tokyo Bay ◽  
Temporal And Spatial Variations ◽  
Suspended Substances ◽  
Hypoxic Water ◽  
Temporal And Spatial

Study on the Characteristics of Temporal and Spatial Variation of Suspended Sediment in the Pearl River Estuary

2009 ◽  
Author(s):  
Wei Zhang ◽  
Mingyuan Yang ◽  
Xiaolin Zhang ◽  
Peipei Dong
Keyword(s):  
Spatial Variation ◽  
Suspended Sediment ◽  
Large Scale ◽  
Research Result ◽  
River Estuary ◽  
Pearl River Estuary ◽  
Tidal Range ◽  
Pearl River ◽  
Temporal And Spatial Variation ◽  
Temporal And Spatial

The Lingding Estuary is one of the main parts of the whole Pearl River Delta, which lies in the South Sea, China. It is about 60 km wide from Hong Kong in the east to Macao in the west and the water areas are approximately 2110 km2. The process of suspended sediment movement is influenced by many factors, such as the estuarine geometry, tidal range and ravine flows etc.. In this paper, large scale hydrological observations in the Lingding Estuary have been respectively carried out in July, 2003. Based on these data, characteristics of temporal and spatial variation of suspended sediment concentration (SSC) in the Lingding Estuary are studied. The research result shows that SSC changes with the variation of tide current and runoff, the sediment re-suspension is often occurred 1–2 hour following the flood or ebb tide. The maximum turbidity appears near the gauging station V3. In the flood dominant stage, the sediments move towards the mainland, while during the ebb sediments move down.

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