https://scholars.lib.ntu.edu.tw/handle/123456789/315153
標題: | The carbon-sulfide-iron relationship and sulfate reduction rate in the East China Sea continental shelf sediments. | 作者: | HUANG, Kuo-MING LIN, SAULWOOD SAULWOOD LIN |
公開日期: | 1995 | 卷: | 29 | 期: | 5 | 起(迄)頁: | 301--315 | 來源出版物: | Geochemical Journal | 摘要: | Carbon/suifide/iron relationship and sulfate reduction rate were investigated in the East China Sea continental shelf sediments. The area is characterized by median to high sulfate reduction rate, and high concentrations of iron oxide minerals. Organic carbon was found to be the primary limiting factor for the pyrite formation. Sulfate reduction rate increased with increasing organic carbon concentration. C/S ratio displays a typical normal marine sediment ratio. Low DOP values and abundance of highly reactive iron oxide, ferrihydrite and lepidocrocite, indicate that iron is not limited in the East China Sea continental shelf. © 1995, GEOCHEMICAL SOCIETY OF JAPAN. All rights reserved. |
URI: | http://scholars.lib.ntu.edu.tw/handle/123456789/315153 | DOI: | 10.2343/geochemj.29.301 | SDG/關鍵字: | carbon/sulphide/iron; continental shelf; continental shelves; marine sediment; pyrite; sediment chemistry; sulphate reduction; East China Sea |
顯示於: | 海洋研究所 |
在 IR 系統中的文件,除了特別指名其著作權條款之外,均受到著作權保護,並且保留所有的權利。