Computer Science
Scientific paper
Mar 1981
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1981gecoa..45..431d&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 45, Issue 3, pp.431-437
Computer Science
7
Scientific paper
The partitioning of Ni between olivine and silicate melt has been investigated experimentally at atmospheric pressure in air. Beta track autoradiography using 63 Ni and direct microprobe analysis of polished run products were employed. At constant temperature and bulk composition, the olivine / liquid partition coefficient for Ni in the system Di 70 Fo 25 Qtz 5 remains independent of concentration from approximately 10 ppm to 40,000 ppm Ni in olivine. Similar experiments by (1979) in the system Jd 80 Fo 20 utilizing beta track autoradiography alone indicated that Henry's Law was followed only in the concentration interval of approx. 10-1000 ppm Ni in olivine. Above 1000 ppm, olivine/liquid partition coefficients decreased monotonically to about half of the value observed below 1000 ppm. We have performed experiments in the system Jd 80 Fo 20 , but are unable to replicate Mysen's results. While in agreement with Mysen below 1000 ppm Ni in olivine, we do not observe the decrease in partition coefficient value at higher concentrations. We conclude from our reversed experiments that, at constant temperature and bulk composition, the olivine / liquid partition coefficient for Ni in the system Jd 80 Fo 20 remains independent of concentration from approx. 10-60,000 ppm Ni in olivine. Attempts to resolve these differing conclusions by changing experimental techniques have been unsuccessful.
Drake Michael J.
Holloway John R.
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