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Date submitted2021-01-18
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Date accepted2021-05-21
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Date published2021-09-20
Improving the efficiency of the technology and organization of the longwall face move during the intensive flat-lying coal seams mining at the Kuzbass mines
The reasons for the lag of the indicators of the leading Russian coal mines engaged in the longwall mining of the flat-lying coal seams from similar foreign mines are considered. The analysis of the efficiency of the longwall face move operations at the JSC SUEK-Kuzbass mines was carried out. A significant excess of the planned deadlines for the longwall face move during the thick flat-lying seams mining, the reasons for the low efficiency of disassembling operations and the main directions for improving the technology of disassembling operations are revealed. The directions of ensuring the operational condition of the recovery room formed by the longwall face are considered. The recommended scheme of converged coal seams mining and a three-dimensional model of a rock mass to justify its parameters are presented. Numerical studies using the finite element method are performed. The results of modeling the stress-strain state of a rock mass in the vicinity of a recovery room formed under conditions of increased stresses from the boundary part of a previously mined overlying seam are shown. The main factors determining the possibility of ensuring the operational condition of the recovery rooms are established. It is shown that it is necessary to take into account the influence of the increased stresses zone when choosing timbering standards and organizing disassembling operations at a interbed thickness of 60 m or less. A sufficient distance from the gob of above- or undermined seams was determined to ensure the operational condition of the recovery room of 50 m, for the set-up room – 30 m. Recommendations are given for improving technology and organization of the longwall face move operations at the mines applied longwall mining of flat-lying coal seams with the formation of a recovery room by the longwall face.
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Date submitted2009-10-21
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Date accepted2009-12-16
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Date published2010-09-22
Geomechanical foundations of the safe extraction in joint mining of rich, coppery and ore patches in deep ore mines at Тalnakh
- Authors:
- V. A. Zvezdkin
- A. A. Andreev
The paper deals with the specific formation of stress fields in ore-bearing intrusions at the Oktiabrsky and Talnakh ore deposits with due account of depth of occurrence and formation of tectonic disturbances. The authors have investigated the influence of mining works on stress state of ore-bearing portion of the intrusion. The relationships were obtained in terms of the formation of stress fields in the intrusion during its undermining, overmining and joint mining of several ore deposits. Some recommendations are given for mining of series of ore formations at the Oktiabrsky and Talnakh deposits.
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Date submitted1958-03-11
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Date accepted1958-05-28
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Date published1958-05-09
ТРАНСГРЕССИВНЫЕ И РЕГРЕССИВНЫЕ ЯВЛЕНИЯ В ЦИКЛАХ УГЛЕНОСНЫХ ФОРМАЦИЙ
- Authors:
- Unknown
Вопрос о трансгрессивных и регрессивных явлениях при накоплении осадков вступил в новую фазу. Это произошло благодаря изучению угленосных формаций с учетом цикличности их строения. В литологических работах по Кузнецкому, Карагандинскому и другим бассейнам, а особенно по Донецкому, выяснилось значение осадочных циклов, состоящих из регрессивных и трансгрессивных частей. В дальнейшем было установлено, что регрессия не повторяет в обратном порядке пород и фаций трансгрессивной части цикла. Она характеризуется рядом фаций с особыми признаками, если даже они развиваются на тех же глубинах и тех же расстояниях от берега, что и трансгрессивные фации. Соответственные признаки пород также несут на себе черты отличий, которые все более и более выявляются.
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Date submitted1958-03-20
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Date accepted1958-05-14
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Date published1958-05-09
О ВЕРХНЕМ ПАЛЕОЗОЕ ЮЖНОЙ КАЛБЫ (ВОСТОЧНЫЙ КАЗАХСТАН)
- Authors:
- Unknown
В 1933 г. нами в пределах Калбинского хребта выделены, а в 1934—1935 гг. изучены более детально верхнепалеозойские отложения. В дальнейшем, вопросом о верхнем палеозое Калбы занимался ряд исследователей, общим недостатком работ которых было слабое знание особенностей верхнепалеозойских отложений на всей площади их распространения в Калбе. В результате в представлениях о последовательности верхнепалеозойских свит, соотношении этих свит и их палеонтологической и литологической характеристике возникла некоторая путаница.
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Date submitted1951-08-26
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Date accepted1951-10-03
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Date published1952-04-24
Physical and mechanical properties of clays of the coal-bearing suite of the Lower Carboniferous of the Moscow Basin
- Authors:
- V. D. Lomtadze
In the Moscow Basin, clay deposits occupy a significant part of the section of the sandy-clayey coal-bearing suite of the Lower Carboniferous. This suite is almost continuously distributed throughout the basin (Fig. 1). Throughout its length, it is characterized by the inconsistency of the section in the vertical and horizontal directions. Along the southern wing of the basin, the coal beds are thicker, while to the north, along the western wing, the coal content of the suite gradually decreases, and already in the section of the Tikhvin region only black carbonaceous clays and occasionally thin coal interlayers are observed. At the same time, the saturation of the section with refractory clays is significantly reduced here, the place of which is occupied by bauxite deposits and red sandy clays. The variability of the section of the coal-bearing suite is explained by the coastal-marine and coastal-continental conditions of its accumulation. The change in the structure of the coal-bearing suite along the strike is the result of the facies replacement of coal by carbonaceous clays, and then carbonaceous clays by red sandy clays. A. E. Ulmer believes that the southern part of the western wing and the southern wing of the Moscow Basin are included in the facies zone of accumulation of continental and coastal-marine sediments, and the northern part of the western wing is included in the facies zone characterized by the predominance of continental erosion over accumulation.