ECOLOGICAL-HYDRO-GEOMECHANICAL CONSEQUENCES OF THE FILTRATION STRUCTURE REFORMING IN THE ROCK MASSIF OF THE WESTERN DONBAS

N. Diachenko
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Abstract

A study was carried out to assess the ecological-hydro-geomechanical consequences of the filtration structure reformation of the rock massif during underground coal mining, using as an example the territories of Western and Central Donbas regions. A complex of problems of the geological environment transformation during mining has been determined. They are associated with: compaction of sedimentary deposits caused by groundwater pumping out; effect of unauthorized formation of suffusion channels system with a different order and differentiated permeability that occurred in the space above the mine workings, which complicates the filtration conditions of the coal-bearing massif natural structure; increase in rock mass fracturing under the influence of horizontal alternating deformations with multiple stage-by-stage substitution of compression zones with extension zones and vice versa (in the process of mining) and generating a quasi-regular network of vertically oriented man-made reservoirs. It has been established that as a result of the groundwater intensive exploitation in the course of mine drainage and water intake activities, both single depression surfaces as well as local depression craters and water rise in various water-bearing horizons were formed. Their general changes and sizes have practically not changed in recent years, which indicates a quasi-stationary regime of groundwater and that water intake in a large area is practically compensated by natural resources. It has been reported that during the long-term period of the depression funnel formation, the groundwater contour was pulled up from the north (the area of the Orel River). Thus, in the conditions of coal mining in the mines of Western Donbass, the river does not receive feeding from the catchment area and becomes shallow. On the other hand, the "wet conservation" of mines will further reduce the revenue side of the river's water balance, since most of the water will be used for flooding. Problems with shallowing are not only experienced by Orel River but also by Samara River. In the zone of local depression fall villages Braginovka and Petropavlovka, and Shevchenko farm. It is concluded that there is a need for comprehensive monitoring of geomechanical, hydrogeological, geochemical and environmental processes both at the completion of the coal mines development and during the mine workings flooding. Such monitoring will make it possible to assess in a timely manner the nature and scale of changes of the geofiltrational and geomechanical characteristics in the rock mass, disturbed by operational work for a long time.   
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西部顿巴斯岩体过滤结构改造的生态-水文-地质力学后果
以顿巴斯西部和中部地区为例,进行了一项研究,以评估地下煤矿开采期间岩体过滤结构改造的生态-水文-地质力学后果。确定了开采过程中地质环境改造的一系列问题。它们与以下因素有关:地下水抽出造成的沉积物压实;矿井工作面上方空间内无序形成不同阶序、不同渗透率的渗透通道系统,使含煤块状自然构造的过滤条件复杂化;水平交替变形作用下岩体破裂增加,开采过程中压缩区与延伸区多次阶段性交替,形成拟规则的垂向人工储层网络。在矿井排水和取水活动过程中,由于地下水的集约开采,既形成了单一的洼地面,也形成了局部洼地坑和各个含水层的积水。它们的一般变化和大小近年来几乎没有变化,这表明地下水的准稳定状态,并且大面积的取水实际上是由自然资源补偿的。据报道,在凹陷漏斗形成的长期过程中,地下水等值线从北部(奥廖尔河地区)向上拉升。因此,在顿巴斯西部矿区的煤矿开采条件下,河流没有从集水区获得补给,变得很浅。另一方面,矿井的“保湿”将进一步减少河流水平衡的收益,因为大部分水将被用于洪水。不仅奥廖尔河,萨马拉河也有浅水问题。在当地的萧条地带,布拉吉诺夫卡村、彼得罗巴甫洛夫卡村和舍甫琴科农场都倒下了。结论认为,在煤矿开发完成和矿井采空区淹水过程中,都需要对地质力学、水文地质、地球化学和环境过程进行综合监测。这种监测将能够及时评估长期受到作业干扰的岩体的地质滤过性和地质力学特征变化的性质和规模。
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PECULIARITIES OF RELATIONSHIP BETWEEN COBALT AND GERMANIUM CONCENTRATIONS IN COAL SEAM С₈Н OF DNIPROVSKA MINE OF WESTERN DONBAS THE HISTORY OF THE CREATION OF THE MUSEUM OF PRECIOUS AND DECORATIVE STONES. HISTORICAL AND SCIENTIFIC ASPECTS OF THE SCIENTIFIC AND PRACTICAL CONFERENCE «MINERAL AND RAW MATERIAL WEALTH OF UKRAINE: WAYS OF OPTIMUM USE» RESTORING OF THE BASIN STATUS OF SIVERSKY DONETS-ZAPURUKA, SOLUTION OF THE MAIN ENVIRONMENTAL PROBLEMS OF DONBAS ASSESSMENT OF ENVIRONMENTAL IMPACT FACTORS OF COAL MINING BY MEANS OF CORRELATION-REGRESSION ANALYSIS NANDANA GEM & MUSEUM, SRI LANKA
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