Directional movements of bed load in marine sediments are studied using a r
adioactive tracer, scandium, similar to the natural sediment in the area. S
candium glass prepared for this purpose was analyzed by atomic emission spe
ctrography for quality assurance purposes. A buffer composed of graphite wi
th 5% germanium oxide was used for accurate and reproducible analyses. The
role of this buffer in the excitation behavior of scandium and variations i
n spectral line intensity with respect to various influencing parameters ar
e reported. Volatilization of scandium was observed using the moving plate
technique, with a de-are as the excitation source. (C) 1999 Elsevier Scienc
e Ltd. All rights reserved.