台湾海峡
檯灣海峽
태만해협
JOURNAL OF OCEANOGRAPHY IN TAIWAN STRAIT
2010年
1期
58-65
,共8页
官宝聪%雷怀彦%林炳煌%柳浩然%史跃中%林建宁
官寶聰%雷懷彥%林炳煌%柳浩然%史躍中%林建寧
관보총%뢰부언%림병황%류호연%사약중%림건저
海洋地球化学%表层沉积物%化学成分%分布特征%泉州湾
海洋地毬化學%錶層沉積物%化學成分%分佈特徵%泉州灣
해양지구화학%표층침적물%화학성분%분포특정%천주만
marine geochemistry%surface sediments%chemical composition%distribution characteristic%Quanzhou Bay
根据2008年泉州湾调查采集的样品,测定了泉州湾表层沉积物中常量元素和微量元素的含量,采用相关分析和因子分析进行元素组合特征的研究,讨论了它们的分布趋势、相互关系和主要来源,并探讨了其地球化学意义.元素相关分析结果表明,泉州湾表层沉积物常量元素与微量元素含量的相关性明显,表层沉积物成分以SiO_2和Al_2O_3为主,其含量的最高值分别达78.39%和22.02%(m/m),其中SiO_2与大部分常量元素、微量元素的含量呈负相关,而Fe_2O_3、MgO、Cu、Co、Ni、Rb、Pb与Al_2O_3含量之间呈强正相关.元素因子分析表明,泉州湾表层沉积物的物质来源主要有陆源和生物源2种,以陆源的为主.
根據2008年泉州灣調查採集的樣品,測定瞭泉州灣錶層沉積物中常量元素和微量元素的含量,採用相關分析和因子分析進行元素組閤特徵的研究,討論瞭它們的分佈趨勢、相互關繫和主要來源,併探討瞭其地毬化學意義.元素相關分析結果錶明,泉州灣錶層沉積物常量元素與微量元素含量的相關性明顯,錶層沉積物成分以SiO_2和Al_2O_3為主,其含量的最高值分彆達78.39%和22.02%(m/m),其中SiO_2與大部分常量元素、微量元素的含量呈負相關,而Fe_2O_3、MgO、Cu、Co、Ni、Rb、Pb與Al_2O_3含量之間呈彊正相關.元素因子分析錶明,泉州灣錶層沉積物的物質來源主要有陸源和生物源2種,以陸源的為主.
근거2008년천주만조사채집적양품,측정료천주만표층침적물중상량원소화미량원소적함량,채용상관분석화인자분석진행원소조합특정적연구,토론료타문적분포추세、상호관계화주요래원,병탐토료기지구화학의의.원소상관분석결과표명,천주만표층침적물상량원소여미량원소함량적상관성명현,표층침적물성분이SiO_2화Al_2O_3위주,기함량적최고치분별체78.39%화22.02%(m/m),기중SiO_2여대부분상량원소、미량원소적함량정부상관,이Fe_2O_3、MgO、Cu、Co、Ni、Rb、Pb여Al_2O_3함량지간정강정상관.원소인자분석표명,천주만표층침적물적물질래원주요유륙원화생물원2충,이륙원적위주.
By carrying out the elemental analysis on the surface sediments of Quanzhou Bay,the combination characteristics of important elements and the significance of geochemistry are studied using correlation analysis and factor analysis.The result shows that the surface sediments from Quanzhou Bay have obvious correlation between main and trace element,and the SiO_2 and Al_2O_3 are the most dominant components at the surface sediments with maximum value of 78.39% and 22.02%(m/m),respectively.SiO2 showed a negative correlation between most important elements and trace element,while Fe_2O_3,MgO,Cu,Co,Ni,Rb and Pb shows strong positive correlation with Al_2O_3.Factor analysis shows that surface sediments in this area aremostly composed of continental and biological origin.However,the former are themost important.