The isotope ratios of Ni, Cu, Zn, Cd, and Pb are utilized
to trace
the origins and investigate the various processes affecting these
elements. In Part 1, we presented a method for the simultaneous analysis
of isotope ratios of dissolved trace metals in seawater using NOBIAS
PA1 chelate extraction and AG MP-1 M anion exchange. In Part 2, we
extend the applicability of this method to sediments, atmospheric
particles, and plankton. In the NOBIAS PA1 chelate extraction, an
NH4F solution was used to separate Ni, Cu, Zn, Cd, and
Pb from Al, Ti, Cr, Mn, Fe, Zr, and Sn, which are abundant in sediment
and atmospheric particles. Then, Ni, Cu, Zn, Cd, and Pb were separated
using anion exchange. The accuracy and precision were evaluated by
the repeated analysis of reference materials of marine sediments (PACS-3),
atmospheric particles (NIES-28), and river plankton (BCR-414). This
method has the following advantages over conventional methods: (1)
simultaneous analysis of isotope ratios of multiple elements from
a single sample in only two chemical separation steps, allowing for
high-throughput analysis; (2) clean and excellent chemical separation
providing highly precise data; and (3) high applicability to a wide
range of samples including marine sediments, plankton, and atmospheric
particles. The methods presented in Parts 1 and 2 are expected to
accelerate the multielemental isotope research of trace metals in
the ocean, atmosphere, and sediments.