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Reference material for radionuclides in sediment IAEA-384 (Fangataufa Lagoon sediment)

✍ Scribed by P. P. Povinec; M. K. Pham; J. A. Sanchez-Cabeza; G. Barci-Funel; R. Bojanowski; T. Boshkova; W. C. Burnett; F. Carvalho; B. Chapeyron; I. L. Cunha; H. Dahlgaard; N. Galabov; L. K. Fifield; J. Gastaud; J. -J. Geering; I. F. Gomez; N. Green; T. Hamilton; F. L. Ibanez; M. Ibn Majah; M. John; G. Kanisch; T. C. Kenna; M. Kloster; M. Korun; L. Liong Wee Kwong; J. La Rosa; S. -H. Lee; I. Levy-Palomo; M. Malatova; Y. Maruo; P. Mitchell; I. V. Murciano; R. Nelson; A. Nouredine; J. -S. Oh; B. Oregioni; G. Le Petit; H. B. L. Pettersson; A. Reineking; P. A. Smedley; A. Suckow; T. D. B. van der Struijs; P. I. Voors; K. Yoshimizu; E. Wyse


Publisher
Springer
Year
2007
Tongue
English
Weight
174 KB
Volume
273
Category
Article
ISSN
1588-2780

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✍ S. Caroli; O. Senofonte; S. Caimi; P. Robouch; J. Pauwels; G.N. Kramer πŸ“‚ Article πŸ“… 1998 πŸ› Elsevier Science 🌐 English βš– 68 KB

The final product turned out to contain mostly particles smaller than 90 m (97% of total mass); particles larger than 150 m were practically absent. The fraction between 90 and 150 m comprised mainly organic material homogeneously distributed over the sediment. Five hundred two brown glass bottles (