海南四更沙海域沉积物分布及其受控机制

基于海南西部四更沙及其邻近海域185个底质的粒度数据,并结合研究区动力状况和水深地形特征,研究表层沉积物的组分和类型分布、粒度参数及其沉积环境分区。结果表明:①研究区沉积物类型多样,包括12种沉积类型,以砂质粉砂、粉砂、粉砂质砂和含砾砂为主,沉积物平均粒径变化范围较大(-0.70~7.13 φ),且大体呈现由北向南逐渐变细的分布趋势;②运用Fleming的三角图式,结合物源状况及地形地貌条件,对沉积环境进行划分,将研究区划分为四更沙岸外海滨沉积区、北黎湾中部沉积区和八所港近岸沉积区等3个沉积区;③研究区沉积物分布特征受沉积物来源和水动力及地形条件共同影响。横向分布上,西部主要受强潮流输沙影响,东部近岸则主要受波浪掀沙和搬运作用影响,表现为两侧粗,中间相对较细的特征。纵向上,四更沙岸外海滨沉积区,沉积物主要受昌化江影响,粒径粗,表现为河口沉积特征;北黎湾中部沉积区,沉积物粒径分布范围广,表现为较强的过渡区特性;八所港近岸沉积区,沉积物粒径最细,泥沙来源主要为外海带来的泥沙。

Sediment Distribution and Its Controlling Mechanism in the Littoral Zone of Sigengsha,Hainan, China

Owing to the interaction between land and ocean, littoral zones present unique sedimentation. Grain size, as a basic attribute of sediment, is an essential question of sediment dynamics. Grain size is controlled by sediment source and sink, and its parameters play a significant role in determining dynamic relationship between sediment and depositional environment. Sigensha littoral zone is located in the west of Hainan Island, the second largest island of China, extending from the Changhua River delta on the north to the Beili Bay on the south. This zone shows diverse sediment sources, complicated hydrodynamics and variable morphology, where special coastal evolution process is closely connected with its sedimentary environment. A field sampling was conducted in the study area on January 2013 with 185 surface samples collected. Mastersize 2000 laser particle sizer was applied to measure grain sizes all less than 2 mm and the sediments with sizes larger than 2 mm were tested by a comprehensive method, utilizing both sieve analysis and laser particle sizer. Sediment classification and nomenclature were based on Fork method and grain-size parameters were calculated including mean grain size M, standard deviation σ, skewness Sk and kurtosis K. The distribution of grain size parameters in the study area was then acquired by Kriging interpolation. Combined with sediment sources and bathymetric information, the sedimentary environment was divided by using the ternary diagram of Fleming. At last, the controlling mechanism of sediment distribution was investigated combined with hydrodynamic factors and morphology.The results suggest that the entire study area comprise 12 sediment types, mainly including sandy silt, silt, silty sand and gravel-bearing sand. Sandy silt, the mostly distributed sediment, mainly occurs in the central study area. Silt mainly distributed in the southern study area. Similar to sandy silt, silty sand is also distributed in the central study area. Gravel-bearing sand mostly distributed in the nearshore of the northern study area. Overall, the mean grain size of the study area ranges widely (-0.70 φ to 7.13 φ) and presents a fining trend from north to south. The standard deviation of sediment ranges from 0.30 to 2.73 with mean value of 1.75. It is characterized by a worse-worst-worse trend from north to south. The skewness changes from -0.77 to 0.73 with average of 0.09. The kurtosis range from 0.52 to 4.35 with average of 1.13 and shows mesokurtic to platykurtic pattern. Based on Fleming ternary diagram, combined with sediment sources, hydrodynamic and topographic condition, the study area was divided into three sedimentary districts: Sigengsha nearshore zone, middle Beili Bay zone and Basuo port nearshore zone. In the sediment distribution pattern, the western study area was mainly influenced by strong tidal currents. The nearshore was mostly impacted by wave winnowing and transport and was characterized by fine sediment distributed in the middle and coarse sediment in the two sides. Laterally, the Sigengsha nearshore zone is a high-energy coarse-grained sand area, where sand content is as large as 78.68%, mainly affected by sediments from Changhua River. The Beili Bay zone is a medium-energy transitional area of silty sand and sandy silt, where the grain sizes range widely. The Basuo port nearshore zone is a low-energy area, where silt content occupies 64.43%, and where the sediment is the finest and most likely comes from open sea.