摘要
元素含量分析表明东海北部近岸泥质区以低Sr、相对低Ca和最低的Sr/Ba为特征;中陆架砂质区低Ca、相对低Sr和相对低的Sr/Ba;中陆架泥质区高Ca、Sr、低Ba和高的Sr/Ba;外陆架砂质区具有最高的Ca、Sr和Sr/Ba。Ca、Sr、PIC三者关系密切,Ba与Ca、Sr、PIC的相关性均差。Ca、Sr具明显的亲自生性,主要赋存于海洋生源碳酸盐;Ba具明显的亲它生性,主要赋存于硅酸盐矿物。Ca、Sr、Ba的地球化学特征受研究区物源和水动力环境的强烈制约。海洋生物地球化学过程对Ca和Sr的地球化学特征有重要影响。中陆架泥质区是东海北部现代陆架Ca、Sr的“汇”
The element analyses of Ca, Sr, and Ba of 31 surface sediment samples taken from the middle continental shelf and its ambient areas of the East China Sea were carried out by using methods of AAS and ICPAES. The results show that the distribution pattern of the three elements is: low Sr, relatively low Ca and lowest ratios of Sr/Ba in the coastal mud area; low Ca, relatively low Sr and ratio of Sr/Ba in the middle continental shelf sand area; high Ca and Sr and ratio of Sr/Ba in the middle continental shelf mud area; highest Ca, Sr and ratio of Sr/Ba in the outer continental shelf sand area. The conentrations of Ca have a good relation to the concentrations of Sr and PIC (Particulate Inorganic Carbon). And the concentrations of Ba have little relation to the concentrations of Ca, Sr, and PIC. It is indicated that the geochemical characteristics of Ca, Sr and Ba are controlled by the sources of elements and dynamic environment in the study area. The interior influential factor affecting the geochemical characteristics of Ca, Sr and Ba is the ocurrence characters of the three elements. Also, the processes of marine geochemistry play an important role in the characteristics of Ca and Sr in the study area. It is supposed that the middle continental shelf mud area is the sink of the modern Ca and Sr in the Northern East China Sea.
基金
国家自然科学基金
关键词
东海
陆架
泥质区
周边底质
钙
锶
Ca, Sr and Ba
geochemical characteristic
influential factor
surface sediments
the East China Sea