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海盗号X射线荧光实验的初步结果:来自火星克里斯平原的首个样本。

Preliminary Results from the Viking X-ray Fluorescence Experiment: The First Sample from Chryse Planitia, Mars.

作者信息

Toulmin P, Clark B C, Baird A K, Keil K, Rose H J

出版信息

Science. 1976 Oct 1;194(4260):81-4. doi: 10.1126/science.194.4260.81.

Abstract

Iron, calcium, aluminum, silicon, and sulfur are major elements in the first surface sample of Mars that has been analyzed by the Viking x-ray fluorescence spectrometer. Titanium is present in minor quantities. This is consistent with the sample being a mixture of fine silicate and oxide mineral grains, with a significant proportion of sulfates, possibly hydrated. Ferric oxide is regarded as the red pigmenting agent on the martian surface, but if it coats silicate grains, the coatings must be very thin (</= 2 micrometers) or discontinuous. A high abundance of Fe, relatively low abundances of Al, Rb, Sr, and Zr, and a high Ca/K ratio are distinctive features of the spectra. Preliminary determinations indicate the following abundances (as percentages by weight): Fe, 14 +/- 2; Ti < 1; S, 2 to 5; the Ca/K ratio by weight is greater than 5.

摘要

铁、钙、铝、硅和硫是火星首个表面样本中的主要元素,该样本已由海盗号X射线荧光光谱仪进行了分析。钛含量较少。这与该样本是细硅酸盐和氧化物矿物颗粒的混合物相符,其中含有相当比例的硫酸盐,可能是水合硫酸盐。氧化铁被视为火星表面的红色色素,但如果它覆盖在硅酸盐颗粒上,涂层必定非常薄(≤2微米)或不连续。高丰度的铁、相对低丰度的铝、铷、锶和锆,以及高钙钾比是光谱的显著特征。初步测定表明以下丰度(以重量百分比计):铁,14±2;钛<1;硫,2至5;钙钾重量比大于5。

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