THE CHEMICAL COMPOSITIONS OF MINERALS IN QINGZHEN METEORITE AND ITS GEOCHEMISTRY SIGNIFICANCE

The chemical compositions of silicate minerals, sulphide minerals and metal Fe-Ni in theQingzhen meteorite were measured by the microprobe analyses. Based upon these chemicalcompositions, the cosmochemical behaviour and characteristics of the existing forms of themajor elements in the Qinzhen meteorite have been discussed. These characteristics show thatunder the S-rich, O-poor, and strongly reducing conditions, the light metal elements, such asCa, Mg, K, Na may form sulphide, and metal Fe-Ni may contain Si and P. However, we con-sider that the light metal-sulphide can be stable in the lower mantle and there are some Siand P in the Fe-Ni core. Finally, an earth core-mantle model is established, where the Fe-Ni core contains some Si and P; the lower mantle is composed of Mg-rich silicate, SiO_2 andsulphide; the upper mantle, of silicate and oxide.     

Computer analysis of amino acid chromatograms and other linear elution spectra

A computer-aided method of evaluation of amino acid column chromatograms is proposed and compared with the usual synchronous peak-integration method. Spectra and their backgrounds are digitized separately by a curve digitizer; this allows a better estimate of the background time courses. A computer program then fits a set of superimposed Gaussian distributions to each corrected spectrum, thus circumventing the problems arising from incompletely separated peaks. Samples of known composition, run intermittently through the analyzer between the unknown spectra, allow a determination of the time dependence of the ratios of “peak areas over amounts of amino acids”; hence, the amounts of amino acids can automatically be corrected for aging effects of the analyzing system. A modified version of the computer program allows resolution of any spectrum to a sum of Gaussians, with least squares fitting of their amplitudes, widths and locations.