Isotope ratios of dissolved trace metals in seawater
are useful
for understanding marine biogeochemical cycles; however, the analysis
requires considerable time and effort to concentrate trace metals
from seawater and remove high concentrations of alkali and alkaline
earth metals. This paper introduces a novel method for the simultaneous
analysis of isotope ratios for Fe, Ni, Cu, Zn, Cd, and Pb in seawater
using solid-phase chelate extraction and anion exchange. The process
involves chelate extraction with a NOBIAS Chelate PA1 resin column
to concentrate Fe, Ni, Cu, Zn, Cd, and Pb while removing alkali metals,
alkaline earth metals, and Mo. Subsequent anion exchange using an
AG MP-1 M column separated Fe, Ni, Cu, Zn, Cd, and Pb from each other.
The recoveries for Fe, Ni, Cu, Zn, Cd, and Pb during the entire chemical
separation process exceed 94%, and the total procedure blanks are
only 4 pmol/kg for Fe, 0.3 pmol/kg for Ni, 1.3 pmol/kg for Cu, 0.9
pmol/kg for Zn, 0.03 pmol/kg for Cd, and 0.01 pmol/kg for Pb. Seawater
samples from Suruga Bay, Japan are analyzed to evaluate the accuracy
and precision of isotopic analysis for Fe, Ni, Cu, Zn, Cd, and Pb.
Using this method, isotope ratios of Fe, Ni, Cu, Zn, Cd, and Pb were
determined in reference seawater materials (GSC, NASS-7, and CASS-6)
and seawater samples that were collected at a station in the North
Pacific. Despite involving only two chemical separation steps, this
method accurately analyzes the isotope ratios from a single seawater
sample, significantly reducing the processing time, labor, reagents,
and seawater samples required for analysis.