The distributions of major-to-ultratrace elements into natural salt from coastal seawater in a salt-preparation process were investigated by ICP-AES(inductively coupled plasma atomic emission spectrometry) and ICP-MS(inductively coupled plasma mass spectrometry) with preconcentration using a chelating resin. The coastal seawater samples were collected off-shore near to the Nie coast, where Agehama-made salt is produced by a classical Agehama method. Natural salt was produced from original coastal seawater in the laboratory in a similar manner to the Agehama method. First, the seawater samples were filtered with a membrane filter(pore size of 0.45μm), and the elements in the dissolved fraction(filtrate) and in the particulate fraction(particulate on the filter) were determined by ICP-AES and ICP-MS. The analytical results for seawater indicate that alkali elements, alkaline earth elements, and oxoanion-forming elements (V, Mo, W, U) were dominantly in the dissolved fraction, while other elements such as Al, Fe, Pb and rare earth elements were mostly in the particulate fraction. The elements in laboratory-made salt and Agehama-made salt were also determined by ICP-AES and ICP-MS after dissolving them in a 0.1M HNO
3 solution. Although the concentrations of trace elements in laboratory-made salt and Agehama-made salt were almost at the same levels for 27 elements among 34 elements within a factor between ca.1/5 and 5, Ba, Mn, Cd and Pb in Agehama-made salt were much higher (8-30 fold) in concentration than those in the laboratory-made salt. Based on the experimental results mentioned above, the distributions of major-to-ultratrace elements into natural salt from seawater were discussed, taking into consideration the preparation process of natural salt.
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