GEOCHEMICAL JOURNAL
Online ISSN : 1880-5973
Print ISSN : 0016-7002
ISSN-L : 0016-7002
Spatial variations of 226Ra, 228Ra, and 228Th activities in seawater from the eastern East China Sea
MUTSUO INOUEKEISUKE YOSHIDAMASAYUKI MINAKAWAYOKO KIYOMOTOHISAKI KOFUJISEIYA NAGAOYASUNORI HAMAJIMAMASAYOSHI YAMAMOTO
Author information
JOURNAL FREE ACCESS

2012 Volume 46 Issue 5 Pages 429-441

Details
Abstract
A total of 74 surface and subsurface water samples at depths shallower than 200 m were collected in the eastern East China Sea (ECS), and spatial and seasonal variations in 226Ra, 228Ra, and 228Th activities were examined by low-background γ-spectrometry. The 228Ra and 228Th activities (as well as 228Ra/226Ra and 228Th/228Ra activity ratios) on the surface exhibited notable seasonal and lateral variations (228Ra/226Ra = 0.2-3.4; 228Th/228Ra = 0.1-0.4). From the 228Ra activity (0.2-6 mBq/L) and salinity (27.2-34.5), fractions of the Kuroshio, shelf, and Yangtze River waters on the surface of the ECS were estimated to be 50-95%, 3-50%, and 2-8% in July, and 95-100%, 1-5%, and 0-1% in April, respectively, exhibiting a lower fraction of shelf water in winter-spring and on the Japan side of the ECS. While the surface waters had high 228Th activity (~0.1-0.6 mBq/L) in July, resulting from the high activity of the parent 228Ra, their 228Th/228Ra ratio (~0.1) was lower compared with that of waters in February-April (0.15-0.35). 228Th is considered to be preferentially removed from the surface in summer, reflecting a high flux of biogenic particles.
Content from these authors
© 2012 by The Geochemical Society of Japan
Previous article Next article
feedback
Top