Abstract

Purpose: Measurement of carbon in cores of undisturbed sediments may provide valuable information on historical trends in sea primary production and carbonate precipitation which can be related to climate changes. Since core sediments are usually subjected to a different analysis, it is important to preserve the sample. A non-destructive technique for carbon measurement in sediments based on fast neutron activation analysis (FNAA) has been developed, which might replace the loss-on-ignition (LOI) as a conventional method for carbon analysis.

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