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从某些文献中可以看出,现代热水中含锑量在o、n毫克/升的浓度时对锑的硫化物矿化就足够了。喀尔巴阡山某些构造带的碳酸水中锑的含量很高,达8—10毫克/升,也就是说,它们比已知的现代岩浆作用区热水中锑的含量要高一个数最级。碳酸水中的锑是用原子吸收法测定的,并用中子活化法进行了检验。说明这些水中锑含量值的确是毫克数量级。对喀尔巴阡山碳酸水中锑含量分布规律的反复研究表明这些水中锑的浓度随时间而变化。
It can be seen from some literature that it is sufficient to mineralize antimony sulfide in modern hot-water at concentrations of 0 and n mg / L. The antimony content of carbonated water in some of the Carpathian tectonic belts is high at 8-10 mg / L, meaning that they are the highest in the number of antimony in the hot water of the known modern magmatic zone . Antimony in carbonated water was determined by atomic absorption spectrometry and examined by neutron activation. This shows that the value of antimony in water is indeed milligram. Repeated studies of the distribution of antimony in Carbonic acid water show that the concentration of antimony in these water changes over time.