冲绳海槽中南部及其邻近陆架悬浮体的分布、组成和影响因子分析
The distribution and composition of suspended matters and their influencing factors in the central-southern area of Okinawa Trough and its adjacent shelf sea
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摘要: 初夏冲绳海槽中南部海域悬浮体含量的分布特点为:表层水体中部海区高,南北海区低;中底层水体自南西至北东由低至高.从陆架到海槽断面的悬浮体含量分布为陆架最高值区、陆坡最低值区和海槽低值区.悬浮体组成包括矿物岩石碎屑、生物骨屑以及絮凝体.矿物岩石碎屑主要分布在陆架区中、下层水体,生物骨屑主要分布在海槽区(整个水层)和陆架区上层水体,絮凝体在研究区都有分布.海槽区与陆架区的悬浮体含量垂直分布和组分特征具有明显的差异.研究区悬浮体分布和组成主要受控于黑潮对陆架物质向冲绳海槽输送的阻隔、生物生产量以及地形、地理环境.Abstract: In early summer,concentration of total suspended matter(TSM) in the surface layer water in the middle area of the central-southern Okinawa Trough sea area is a relative higher than that in the north and south.While in the middle and bottom layers water,the concentration of TSM in the northeast of the central-southern Okinawa Trough is higher than that in the southwest.The sectional distribution of TSM from the shelf to the Okinawa Trough can be divided into three provinces,namely,the high TSM zone mainly corresponding to the shelf,the lowest TSM zone mainly corresponding to the continental slope,and the low TSM zone corresponding to the Okinawa Trough.The suspended matter chiefly consists of rock and mineral debris dominating in the middle-bottom layers water in the shelf,skeletal debris dominating in the whole water column in the Okinawa Trough and the upper water layer in the shelf,and aggregation distributing in the whole study area.The main factors controlling the distribution and composition of suspended matter are the obstruction of the Kuroshio Current which prevents the transport of terrigenous debris from shelf to the Okinawa Trough,marine organism production,and topographic and geographic environment.
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NINOH,EMERY K O.Sediments of shallow portions of East China Sea and South China Sea[J].The Geological Society of American Bulletin,1961,72:731~762. HONJO S,EMERY K O,YAMAMOTO S.Noncombustible suspended matter in surface waters off eastern Asia[J].Sedimentology,1974,21:555~575. QIN Y S,LI F.Study of influence of sediment loads discharge from Huanghe River on sedimentation in Bohai Sea and Huanghai Sea[A].Proceedings of International Symposium on Sedimentation on the Continental Shelf,with Special Reference to the East China Sea[C],Vol.1.Beijing:China Ocean Press,91~101. MILLIMANJ D,BEARDSLEY R C,YANG Z S,et al.Modern Huanghe derived on the outer shelf of the East China Sea:identification and potential mud transport mechanisms[J].Continental Shelf Research,1985,4:215~227. 谢钦春,叶银灿.东海陆架坡折地形和沉积作用过程[J].海洋学报,1984,6(1):61~71. 杨作升.黄河、长江、珠江沉积物中粘土矿物的组合、化学特征及其与物源区气候环境的关系[J].海洋与湖沼,1988,19(4):336~346. 杨作升,郭志刚,王兆祥,等.黄东海陆架悬浮体向东部深海区输送的宏观格局[J].海洋学报,1992,14(2):81~90. 杨作升,郭志刚,王兆祥,等.黄东海悬浮体中的有机包膜[J].海洋与湖沼,1992,23(2):217~227. 郭志刚,杨作升,王兆祥.黄、东海海域水团发育对底质沉积物分布的影响[J].青岛海洋大学学报,1995,25(1):75~84. 郭志刚,杨作升,胡敦欣,等.春季东海北部海域悬浮体的分布结构与沉积效应[J].海洋与湖沼,1997,28(增刊):66~72. YANG Zuo-sheng,GUO Zhi-gang,PANG Chon-guang,et al.Transport of suspended matter from the East China Sea to its eastern deeper waters[A].Proceedings of Japan-China Joint Symposium on Cooperative Study of Subtropical Circulation System[C].Seikai National Fisheries Research Institute,Fisheries Agency of Japan,1998.265~275. BEARDSLEY R C,LIMEBURNER R,YU H,et al.Discharge of the Changjiang(Yangtze River) into the East China Sea [J].Continental Shelf Research,1985,4:57~76. 管秉贤.东海黑潮变异研究的若干结果[J].海洋与湖沼,1979,10(4):297~305. 苏育嵩.黄东海地理环境概况、环流系统与中心渔场[J].山东海洋学院学报,1986,16(1):12~27. 王元培.1984年12月至1985年1月东海黑潮及其邻近海域的水文特征[A].黑潮调查研究论文集[C].北京:海洋出版社,1987.133~l48. -
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