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ULTRAFINE PARTICLES IN GROUND SULFIDE ORES: A COMPARISON OF FOUR CU-NI ORES FROM SIBERIA, RUSSIA
Автор | Михлин, Ю. Л. | |
Автор | Романченко, А. А. | |
Автор | Воробьев, С. А. | |
Автор | Карасев, С. В. | |
Автор | Волочаев, М. Н. | |
Автор | Каменский, Е. С. | |
Автор | Бурдакова, Е. А. | |
Дата внесения | 2019-07-01T07:28:39Z | |
Дата, когда ресурс стал доступен | 2019-07-01T07:28:39Z | |
Дата публикации | 2017-10 | |
Библиографическое описание | Михлин, Ю. Л. ULTRAFINE PARTICLES IN GROUND SULFIDE ORES: A COMPARISON OF FOUR CU-NI ORES FROM SIBERIA, RUSSIA [Текст] / Ю. Л. Михлин, А. А. Романченко, С. А. Воробьев, С. В. Карасев, М. Н. Волочаев, Е. С. Каменский, Е. А. Бурдакова // ORE GEOLOGY REVIEWS. — 2017. — Т. 81. — С. 1-9 | |
ISSN | 01691368 | |
URI (для ссылок/цитирований) | https://www.sciencedirect.com/science/article/pii/S0169136816304747?via%3Dihub | |
URI (для ссылок/цитирований) | https://elib.sfu-kras.ru/handle/2311/111202 | |
Описание | Текст статьи не публикуется в открытом доступе в соответствии с политикой журнала. | |
Аннотация | Nano-, submicro- and micrometer mineral particles may have an important role in beneficiation of metal ores and environmental impact, but their origin and characteristics are poorly understood. Here, we report data for the yield and the composition of fine fractions, and surfaces of several ground Cu-Ni sulfide ores studied using laser diffraction, scanning electron microscopy and energy dispersive X-ray analysis, X-ray photoelectron spectroscopy. Colloidal particles were characterized using dynamic light scattering, zeta-potential measurement, transmission electron microscopy and electron diffraction. The production of fines by dry milling was found to increase from about 0.01 vol.% to 0.2 vol.% for submicrometer particles and from ~0.5 vol.% to about 1.5 vol.% for particulate material less than 5 μm in the following order: Noril'sk disseminated low sulfide ore ≤ Noril'sk Cu-rich sulfide ore b Noril'sk valleriite ore b Kingash ore. For wet milling, the yield may be several times higher. Both surfaces of themilled ores and colloidswere enriched in O,Mg, Si (largely as serpentine slimes) and depleted in sulfur, basic metals and iron, but colloidal valleriite, chalcopyrite, and oxidized pyrrhotitewere found in the respective supernatants too. Typically, the colloidal particles formaggregateswith an average hydrodynamic diameter of about 1 μmand a smaller number of ~5 μmspecies, except for valleriite ore, which exhibits a single size distribution peak at 2.7 μm. Zeta-potential,which characterizes the electric charge of the particles and dispersion stability of colloids, changed from−25mVfor the lowsulfide ore to about 0mV for valleriite ore, and to+15mV for Kingash ore. Poor flotation recovery ofmetal fromKingash ore andNoril'sk valleriite ore is suggested to be due to both the large quantities and positive charge of hydrophilic ultrafine serpentine and/or magnesiumhydroxide minerals. Resistance to oxidation and hence stability against aggregation of copper-bearing sulfide colloids in waste waters is expected to result in a negative impact on the environment. | |
Тема | Cu-Ni sulfide ores | |
Тема | Ultrafine particles | |
Тема | Mineral surfaces | |
Тема | Colloids | |
Тема | Beneficiation | |
Тема | Environment | |
Название | ULTRAFINE PARTICLES IN GROUND SULFIDE ORES: A COMPARISON OF FOUR CU-NI ORES FROM SIBERIA, RUSSIA | |
Тип | Journal Article | |
Тип | Published Journal Article | |
Страницы | 1-9 | |
ГРНТИ | 52.45 | |
Дата обновления | 2019-07-01T07:28:39Z | |
DOI | 10.1016/j.oregeorev.2016.10.024 | |
Институт | Институт цветных металлов и материаловедения | |
Подразделение | Кафедра обогащения полезных ископаемых | |
Журнал | ORE GEOLOGY REVIEWS | |
Квартиль журнала в Scopus | Q1 | |
Квартиль журнала в Web of Science | Q1 |