Dj. Lindstrom et Jh. Jones, NEUTRON-ACTIVATION ANALYSIS OF MULTIPLE 10-100 MU-G GLASS SAMPLES FROM SIDEROPHILE ELEMENT PARTITIONING EXPERIMENTS, Geochimica et cosmochimica acta, 60(7), 1996, pp. 1195-1203
Experimental studies of the metal/silicate partitioning of Ir have pro
duced two sets of results differing by a factor of 10(6) (Jones and Dr
ake, 1986; O'Neill et al., 1995). In an attempt to understand this dis
crepancy, we have performed instrumental neutron activation analyses o
f multiple glass chips from these siderophile element partitioning exp
eriments. From seven to ten individual chips (similar to 10-100 mu g e
ach) were analyzed from each experimental glass. The major target was
Ir, which was detected at concentrations ranging from 690 ppb (ng/g) t
o less than 1 ppb. Detection limits are less than 10(-13) grams Ir. Al
most all of the run products appear to be homogeneous with respect to
lithophile elements, but most vary considerably in their Ir concentrat
ions. It appears that most of the experiments analyzed so far contain
small amounts of metal in the glass separates. One experiment from Jon
es and Drake (1983) appears to be homogeneous, but in fact may not be.
More recent experiments are definitely not homogeneous, and require t
he existence of a metallic phase distinctly different from the bulk so
lid metal or liquid metal/sulfide phases also present in the charges.
Iridium contents of the glass in the stirred crucible experiment studi
ed (O'Neill et al., 1996) decreased continuously over a period of seve
ral months, even as the oxygen fugacity was increasing, suggesting tha
t the experiment never achieved equilibrium. Iridium contents in multi
ple samples of the glasses varied over factors of 2 to 3x. Further sub
division of one low-Lr glass did not result in a reduction in the vari
ation of Ir between aliquots. Thus, the variation in Ir concentration
appears to remain fairly constant, irrespective of the scale of the sa
mpling.