Будь ласка, використовуйте цей ідентифікатор, щоб цитувати або посилатися на цей матеріал: http://ir.nmu.org.ua/handle/123456789/161443
Назва: RESULTS OF DISPERSION AND SPATIAL ANALYSIS OF THE GERMANIUM DISTRIBUTION IN COAL SEAM C8B OF ZAHIDNO-DONBASKA MINE FIELD (UKRAINE)
Автори: Ishkov, Valerii
Kozii, Yevhen
Chernobuk, Oleksandr
Lozovyi, Andrii
Ключові слова: coal seam, mine field, germanium, dispersion analysis, cross-section
Дата публікації: 2022
Видавництво: International Science Group
Бібліографічний опис: Ishkov V.V., Kozii Ye.S., Chernobuk O.I., Lozovyi A.L. (2022). Results of dispersion and spatial analysis of the germanium distribution in coal seam c8в of Zahidno-Donbaska mine field (Ukraine). Proceedings of the ХХVIII International Scientific and Practical Conference. «Science and practice, actual problems, innovations», July 19 – 22, 2022, Milan, Italy, pp. 66-73. https://doi.org/10.46299/ISG.2022.1.28
Короткий огляд (реферат): The research actuality of studying the content of germanium in coal seams is due to the possibility of its industrial extraction and use as a valuable accompanying component. In coal, germanium belongs to the group of "small elements" or elements - coal impurities, which must be investigated in the process of prospecting geological works carried out in the coal deposits of Ukraine. For an objective geological and economic assessment of the possibility of simultaneous extraction of germanium from coal, waste and products of its processing and planning of the most effective organizational and technical measures in this regard, it is first of all necessary to have information about the character of the distribution and concentration level of this element in coal and coal-bearing rocks. In order to obtain such information, detailed studies of the distribution of germanium over the area and in the cross-section of the coal seam с8в of "Zakhidno-Donbaska" mine field were carried out.
Опис: The regional component of the total content of germanium increases in the south-northern direction. The content of germanium does not depend on the direction of fall, thickness and current depth of the coal seam, and its total sulfur in coal. Reverse relationship of the concentration of the studied element with the ash content of the formation, and therefore, its relationship with the organic component of coal.
URI (Уніфікований ідентифікатор ресурсу): http://ir.nmu.org.ua/handle/123456789/161443
ISBN: 979-8-88722-623-1
Розташовується у зібраннях:Кафедра геології та розвідки родовищ корисних копалин

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