Watercolumn total Th-234, Palmer Station, 2012-2013
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Total watercolumn Th-234 was determined at Stations E and B near Palmer Station from Nov 2012 - Mar 2013. Th-234 can be used as a tracer for particle cycling in the upper water column. To compute carbon export from this Th-234 data please see the C:Th-234 ratios that can be derived from contemporaneous sediment trap deployments. For more details, please see Stukel et al. (in review, Global Biogeochemical Cycles).
创建时间：
2019-04-11
