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                <gco:CharacterString>&amp;lt;pre&amp;gt;
   &amp;lt;b&amp;gt;PI:&amp;lt;/b&amp;gt;              Bob Anderson
   &amp;lt;b&amp;gt;of:&amp;lt;/b&amp;gt;              Lamont-Doherty Earth Observatory
   &amp;lt;b&amp;gt;dataset:&amp;lt;/b&amp;gt;         Radionuclides, moored sediment trap samples

 &amp;lt;/pre&amp;gt;</gco:CharacterString>
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                <gco:CharacterString>from Deployment: EqPac-Array January 8, 2002
Bob Anderson
Lamont-Doherty Earth Observatory

It was necessary to composite individual time-series sediment trap samples
to obtain sufficient material for radionuclide analysis.  In the
spreadsheet we indicate the cup numbers, as presented by Honjo et al.,
1995, used to prepare each composite sample.  The EqPac sediment trap
samples were analyzed by isotope dilution alpha spectrometry for the U- and
Th-series.  The Th-232 content of the trap samples was so low that we were
unable to resolve the Th-232 peak above the tail of the Th-230 peak, so no
Th-232 data are reported.  Be-10 was measured by accelerator mass
spectrometry.

The reference that best described the methods followed for measuring Th, Pa
and 10Be in sediment trap samples is:

Y. Lao, R.F. Anderson, W.S. Broecker, H.J. Hofmann and W. Wolfli,
Particulate fluxes of 230Th, 231Pa, and 10Be in the Northeastern Pacific
Ocean, Geochimica Cosmochimica Acta 57(1), 205-217, 1993.

The reference that best described the method followed for measuring Pb-210
in sediment trap samples is:

Anderson, R. F., S. L. Schiff and R. H. Hesslein (1987).  Determining
sediment accumulation and mixing rates using 210Pb, 137Cs, and other
tracers: problems due to post depositional mobility or coring artifacts.
Can. J. Fish. Aquat. Sci., Vol. 44, Supplement No. 1: 231-250.</gco:CharacterString>
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