海洋科学
海洋科學
해양과학
Marine Sciences
2015年
8期
70-77
,共8页
冯秀丽%魏飞%刘杰%刘潇%徐芳
馮秀麗%魏飛%劉傑%劉瀟%徐芳
풍수려%위비%류걸%류소%서방
粒度%黏土矿物%物源%渤海湾西部
粒度%黏土礦物%物源%渤海灣西部
립도%점토광물%물원%발해만서부
grain size%clay mineral%sediment source%the western Bohai Bay
对渤海湾西部海域和西岸入海河流中76个表层沉积物样品进行粒度及黏土矿物分析,研究表明该区有3种沉积物类型,黏土质粉砂分布于整个研究区,约占表层样的90%,是研究区最主要的沉积物类型;研究区黏土矿物以伊利石为主,黏土矿物组合为伊利石-高岭石-绿泥石-蒙皂石;渤海湾西部表层沉积物主要来源于海河等渤海湾西岸入海河流中的陆源碎屑物,滦河对研究区基本没有影响,黄河对研究区的影响变得比较小。对于研究渤海湾西岸的沉积特征及沉积物物源、了解陆地河流对于研究区海洋沉积环境的影响有着一定的科学意义。
對渤海灣西部海域和西岸入海河流中76箇錶層沉積物樣品進行粒度及黏土礦物分析,研究錶明該區有3種沉積物類型,黏土質粉砂分佈于整箇研究區,約佔錶層樣的90%,是研究區最主要的沉積物類型;研究區黏土礦物以伊利石為主,黏土礦物組閤為伊利石-高嶺石-綠泥石-矇皂石;渤海灣西部錶層沉積物主要來源于海河等渤海灣西岸入海河流中的陸源碎屑物,灤河對研究區基本沒有影響,黃河對研究區的影響變得比較小。對于研究渤海灣西岸的沉積特徵及沉積物物源、瞭解陸地河流對于研究區海洋沉積環境的影響有著一定的科學意義。
대발해만서부해역화서안입해하류중76개표층침적물양품진행립도급점토광물분석,연구표명해구유3충침적물류형,점토질분사분포우정개연구구,약점표층양적90%,시연구구최주요적침적물류형;연구구점토광물이이리석위주,점토광물조합위이리석-고령석-록니석-몽조석;발해만서부표층침적물주요래원우해하등발해만서안입해하류중적륙원쇄설물,란하대연구구기본몰유영향,황하대연구구적영향변득비교소。대우연구발해만서안적침적특정급침적물물원、료해륙지하류대우연구구해양침적배경적영향유착일정적과학의의。
This paper shows that there are 3 types of sediments in the study area according to analysis of 76 surface samples which were sampled from the western Bohai Bay waters and rivers that flow into the sea from the west coast. Clayey silt distributes throughout the study area, and is the most important type of sediments in the study area, accounting for about 90% of the surface samples. The sediment dynamic environmental characteristics of the sur-face sediments in the area were studied using the Flemming triangle graphic method and the results indicate that the sedimentary dynamics in the study area was relatively weak. The clay mineral analysis of 60 surface samples shows that the illite is the main clay mineral, and the clay mineral assemblage in the study area is illite - kaolinite - chlorite - smectite stone. The exploration of sediment source based on grain size and clay minerals shows that the surface sediments of the western Bohai Bay were mainly from the terrigenous detritus, which were carried by the rivers flowing into the sea in the western Bohai coast, such as the Haihe River, while the Luanhe River had nearly no effect on the surface sediments in the study. The influence of the Yellow River on the sea surface sediments was weak.