Citation: | LI Liang, HE Qijiang, LONG Genyuan, HE Chao, YANG Fan. SEDIMENT GRAIN SIZE DISTRIBUTION PATTERN AND TRANSPORTATION TREND IN THE XUANDE WATER, SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2017, 37(6): 140-148. doi: 10.16562/j.cnki.0256-1492.2017.06.015 |
Grain size analysis and parameter calculation have been carried out for 151 surface sediments collected from the Xuande Waters in the South China Sea. Results show that the surface sediments of the area are made of 8 types of sediments dominated by sand and gravel. Silt and clay contents are relatively small. Factor and Cluster analysis of grain size parameters is used to discriminate different depositional environments. The study area can be further divided into four subareas, The subareaⅠis mainly located in the middle of study area, the subarea Ⅱnear the reefs, the subarea Ⅲ located in the inner Xuande Atoll, and the subarea Ⅳ located in lateral edges of the reef atoll. Grain size trend analysis suggests that the sediment transport pattern is consistent with the hydrodynamic conditions of the study area, and a sediment depositional area is formed in the water next to the Tri Ton island.
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(a)Locantion of the stuady area and sampling positions(Red dots)and (b) Distribution of surface sediment types
Distribution map of gravel, sand, silt, and clay percentage of the surface sediments
Isoline map of grain size parameters of surface sediments
The grain-size factor loading map of surface sediments
Diagram of cluster analysis of surface sediments
Sedimentary environments of the study area (a) and sediment transport pattern by grain size trend analysis (b)
Velocity and direction of the Surface flow from typical sites in the study area