海洋学报(中文版)
海洋學報(中文版)
해양학보(중문판)
ACTA OCEANOLOGICA SINICA
2010年
1期
67-82
,共16页
周晓静%蒋富清%李安春%孟庆勇
週曉靜%蔣富清%李安春%孟慶勇
주효정%장부청%리안춘%맹경용
稀土元素%示踪标记%东海陆架%沉积物输运
稀土元素%示蹤標記%東海陸架%沉積物輸運
희토원소%시종표기%동해륙가%침적물수운
rare earth element%fingerprints%shelf of East China Sea%sediment transport
根据对长江等5条河流和东海陆架区总计146个沉积物样品的稀土元素和粒度分析结果,借助统计学方法,讨论了河流和东海近岸沉积物稀土元素分布格局的形成因素及其对沉积动力作用的响应,结果表明,各河流沉积物在稀土元素总量和轻重稀土分异等参数上有差异;在长江口沉积物中稀土元素在小于2和2~31 μm粒级中较富集,全岩稀土元素含量受物质组成占优的粒级控制;在东海陆架研究区稀土元素含量由岸向海有减小的趋势,在河口附近相对较高,轻重稀土分异自28°N向南有增大的趋势.
根據對長江等5條河流和東海陸架區總計146箇沉積物樣品的稀土元素和粒度分析結果,藉助統計學方法,討論瞭河流和東海近岸沉積物稀土元素分佈格跼的形成因素及其對沉積動力作用的響應,結果錶明,各河流沉積物在稀土元素總量和輕重稀土分異等參數上有差異;在長江口沉積物中稀土元素在小于2和2~31 μm粒級中較富集,全巖稀土元素含量受物質組成佔優的粒級控製;在東海陸架研究區稀土元素含量由岸嚮海有減小的趨勢,在河口附近相對較高,輕重稀土分異自28°N嚮南有增大的趨勢.
근거대장강등5조하류화동해륙가구총계146개침적물양품적희토원소화립도분석결과,차조통계학방법,토론료하류화동해근안침적물희토원소분포격국적형성인소급기대침적동력작용적향응,결과표명,각하류침적물재희토원소총량화경중희토분이등삼수상유차이;재장강구침적물중희토원소재소우2화2~31 μm립급중교부집,전암희토원소함량수물질조성점우적립급공제;재동해륙가연구구희토원소함량유안향해유감소적추세,재하구부근상대교고,경중희토분이자28°N향남유증대적추세.
Total of 146 sediment samples were collected from the shelf of the East China Sea and five rivers,including the Huanghe River,the Changjiang River,the Qiantang River,the Oujiang River and the Minjiang River.The sediment grain-size and the content of rare earth element (REE) were measured with a laser particle size analyzer and an ICP-MS respectively.Results show that the REE absolute content and the ratio of LREE (light REE) to HREE (heavy REE) content are different in the sediments between rivers.There are higher REE contents in being less than 2 μm and 2~31μm fractions in Changjiang Estuary surface sediments,and the bulk sediment REE contents are dominated by the corresponding values of those prevalent size-fractions.In the study area,the REE absolute contents of sediments are higher near the estuaries,and they trend downward in seaward direction on the inner shelf of the East China Sea.The ratio of LREE to HREE content has a tendency of increase southward from 28° N,whilst hydrodynamic conditions are dominated by the spacial distributions of the surficial sediment's REE parameters.In some cases,the current flows tend to remove the coarser light grains from initial populations,whilst deposit the finer heavy mineral grains.In most situations,the currents will change the ratio of sediment constituents,for example,between silts and clays.As a result,the various values of the REE absolute content or ratio of LREE to HREE content in different bulk sediments result from the change of size-fractions,rather than represent their different sources.Under the long-term stable hydrodynamic environment,i.e.,on the East China Sea shelf,a new sediment transport model based on the size and density gradation concept may help to understand the spatial distribution patterns of REE parameters.