Carbon and Nitrogen Analyses, Leg 42A

Abstract

Samples were dried at 40°C, ground and mixed to a homogeneous powder. Subsequently, samples were divided in several parts for different determinations. One part was analyzed for its total carbon content. A second one was treated with hydrochloric acid and analyzed for residual "organic" carbon. The difference between total and organic carbon, called here "inorganic" carbon, was used for carbonate calculation (Müller, this volume). Carbon determinations were made using a LECO Carbon Analyzer. Procedure and precision of this method is described in detail by Boyce and Bode (1972). Relative error of own measurements is calculated to about ± 1%. Nitrogen was determined by the standard micro-Kjeldahl method. Mostly sapropel(ic) sediments were analyzed (Sigl et al., this volume). Due to the small amounts of sample material available, the values reported here have a precision of ±3% only. In sediments with low nitrogen content (<0.1%), the relative analytical error may increase to ±6%. By the Kjeldahl method, the content of total nitrogen is measured. This includes organic nitrogen and so-called fixed and ex-changeable ammonia nitrogen (Bremner, 1965). Data are presented in Table 1. ACKNOWLEDGMENT This study is a part of the sedimentological survey of Leg 42A samples financed by the Deutsche Forschungsgemeinschaft. I am indebted to C. Lutz, A. Schneider, and W. Schuster for laboratory work and performance of analyses.