加热时巴库油田相成分变化

Q3 Materials Science
O. Y. Sheshukov, M. A. Mikheenkov, E. A. Vyaznikova, A. S. Bykov, L. B. Vedmid
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引用次数: 0

摘要

本文介绍了在惰性氧化气氛中对不同氧化铁含量的Bakal矿床的菱铁矿进行加热,研究了镁铁氧体的形成机理。结果表明,在惰性气氛中烧制时,高铁含量菱铁矿的分解温度较低,分解焓较小。这种影响可以用样品相组成的不同来解释。氧化烧成条件下形成的主要相为赤铁矿和镁铁氧体。不同氧化铁含量的试样在氧化气氛下烧制时产生的赤铁矿和镁铁氧体的量不同。氧化铁含量高的菱铁矿烧成产物中含有较多的赤铁矿,氧化铁含量低的菱铁矿烧成产物中含有较多的镁铁氧体。氧化镁铁氧体是在氧化烧制条件下形成的固溶体,铁和镁离子的取代程度不同。氧化铁含量高的菱铁矿中,镁离子被铁离子取代的程度大于氧化铁含量低的菱铁矿。由于Bakal矿床的菱铁矿为贫矿,在焙烧过程中形成了大量的镁铁氧体,使得传统的富集方法难以分离硅酸盐和氧化铁的焙烧产物。氧化烧成产物中的浮士体是检测不到的,因为在这些条件下,它处于亚稳态,在弱氧化气氛的存在下转化为磁铁矿。科学的新颖性在于对菱铁矿分解机理的解释和对分解产物的描述。对Bakal矿床菱铁矿分解机理的认识,为开发有利于其产物分离的还原焙烧菱铁矿技术提供了可能,其关键在于调控还原焙烧硅酸盐产物的相组成,保证镁铁氧体的崩解和氧化铁的分离。所开发的技术可为巴加尔矿床提供高质量的菱铁矿富集。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Изменение фазового состава сидеритов Бакальского месторождения при нагреве
The article presents the results of a study of formation mechanism of magnesia-ferrite when heated siderites of the Bakal deposit with different iron oxide content in an inert and oxidizing atmosphere. It was established that in the case of firing in an inert atmosphere, the decomposition of siderite with high iron content begins at a lower temperature and the enthalpy of such decomposition is less. This effect can be explained by the different phase composition of the samples. The main phases formed under conditions of oxidative firing are hematite and magnesia-ferrite. The amount of hematite and magnesia-ferrite produced in the samples with different iron oxide content during firing in an oxidizing atmosphere is different. Siderite with high content of iron oxides contains more hematite in the firing products than magnesia-ferrite, and siderite with a low content of iron oxides contains more magnesia-ferrite in the firing products than hematite. Formed under conditions of oxidative firing magnesia-ferrites are solid solutions and differ in the degree of substitution of iron and magnesium ions. In siderites with high content of iron oxides, the degree of substitution of magnesium ions with iron ions is greater than in samples with a low content of iron oxides. Since the siderites of the Bakal deposit are poor ore formations, the considerable amount of magnesia-ferrite formed in them during firing makes it difficult to separate silicate and iron-oxide firing products by traditional enrichment methods. Wustite in the products of oxidative firing is not detected, because under these conditions it is in a metastable state and in the presence of a weakly oxidizing atmosphere is converted into magnetite. The scientific novelty is the explanation of the mechanism of siderite decomposition and the description of products of such decomposition. Understanding of the mechanism of decomposition of siderite from the Bakal deposit made it possible to develop the technology of reductive firing of siderite to facilitate separation of its products, and which consists in the regulation of the phase composition of silicate products of reductive firing, ensuring the collapse of magnesia-ferrite and output of iron oxide in a separate phase. The developed technology can be used to provide high-quality enrichment of siderite from the Bakal deposit.
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来源期刊
Izvestiya Vysshikh Uchebnykh Zavedenij. Chernaya Metallurgiya
Izvestiya Vysshikh Uchebnykh Zavedenij. Chernaya Metallurgiya Materials Science-Materials Science (miscellaneous)
CiteScore
0.90
自引率
0.00%
发文量
81
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