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对43个无球粒陨石测试了硫的总丰度,二十个钙长辉长无球粒陨石总疏的范围为870μgS/g—3700μgS/g中值为118μgS/g。古铜钙长无球粒陨石的范围是:1490—32400μgS/g,硫的中值为2340μgS/g。奥长古铜无球粒陨石的范围是:130—3170μgS/g,中值为1280μgS/g,四个辉玻无球粒陨石的范围是740—2540μgS/g顽火无球粒陨石含有任何无球粒陨石族中大的硫丰度最范中值为1940μgS/g。 2450—8580μgS/g,中值为6020μgS/g。6020μgS/g一个单一的纯橄无球粒陨石其硫丰度为360μgS/g。无球粒陨石含硫量变化范围大反映出这些独特的地外物质的规模很小的非均质特征,其原因主要是硫化物矿物颗粒的分散所致。
The total abundance of sulfur was tested on 43 non-chondrites. The total sparse length of twenty calcium long chondrite-free chondrites was 870 μgS / g-3700 μgS / g with a median of 118 μgS / g. The range of bronze long non-chondrites is 1490-32400 μg S / g and the median sulfur is 2340 μg S / g. The scope of the Austrian long bronze non-chondrites is: 130-3170μgS / g, median 1280μgS / g, and the range of the four vitrinite non-chondrites is 740-2540μgS / g. The largest median abundance of chondrules was 1940 μgS / g. 2450-8580 μg S / g, median 6020 μg S / g. 6020μgS / g A single pure olive chondrule meteorite has a sulfur abundance of 360μgS / g. The wide range of sulfur content of non-chondrite meteorites reflects the small heterogeneity of these unique extra-terrestrial materials due to the dispersion of sulfide mineral particles.