Distributions and fluxes of 226^{226}Ra and 228^{228}Ra in the Irish Sea and in the English channel, in relation to hydrological conditions and sediment interactions

Abstract

International audienceDistribution of 226^{226}Ra activities and 228^{228}Ra/226^{226}Ra activity ratios were measured in the surface waters of the Irish Sea and in the English Channel. 226Ra activities vary from 0.001 Bq.l1^{−1} for the Atlantic water to 0.002 Bq.l1^{-1} for coastal waters, whereas 228^{228}Ra/226^{226}Ra activity ratios increase from 0.18 to 2.18. The coastal waters are clearly dominated by radium injection from nearshore sediments

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