北海道産マンガン土の加熱放出ガスによる研究;北海道産マンガン土の加熱放出ガスによる研究;Gas analysis of manganese wad from Hokkaido.

H. Miura, Yu Hariya
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Abstract

This paper describes released gas analysis of manganese wad from Akan, Kogane and Niimi. The samples were heated by the infrared image furnace in He gas condition, and mass spectra of released gas phase were measured by Q-mass spectrometer. Experimental results show that(a) the detected phases on heating are H2O, N2, O2 and CO2, (b) the volume of CO2 mainly depends on the species of manganese mineral, and(c) O/Mn ratio of manganese wad was varied widely and there is a negative correlation between O/Mn ratio and crystallinity. The above features are mostly depend on the amorphous part of the managanese wad. As X-ray diffraction method is insufficient for amorphous phase, gas analysis can provides an important data for study of manganese wad. Manganese wad from Akan (Akan-2) shows unique charactaristics.(a) Akan-2 does not release O2 gas on heating in He gas condition.(b) The structure deforms on heating at 42°C.(c) The DTA data shows a exothermic peak at 300°C.
北海道产锰土的加热释放气体研究;北海道产锰土的加热释放气体研究;Gas analysis of manganese wad from Hokkaido。
本文介绍了阿干、小原和尼米锰团的释放气体分析。样品在He气条件下用红外成像炉加热,用q -质谱仪测定其释放气相的质谱。实验结果表明:(a)加热时检测到的相有H2O、N2、O2和CO2, (b) CO2的体积主要取决于锰矿物的种类,(c)锰团的O/Mn比变化很大,O/Mn比与结晶度呈负相关。上述特征主要取决于锰团的非晶态部分。由于x射线衍射法对非晶相的分析不足,气相分析可以为锰团的研究提供重要的数据。Akan (Akan-2)锰团在He气条件下加热时不释放O2气体,在42℃加热时结构变形,在300℃时差热分析数据显示出放热峰。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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