О наличии гидрогеологической связи между горными выработками закрытых шахт в горнопромышленных районах на примере участка зоны водосбора р. Белая Перевальского района Луганской Народной Республики

Abstract

Работа посвящена выявлению гидрогеологической связи, возникающей при затоплении систем подземных выработок закрытых шахт, а также изучению особенностей водообмена между подземными и поверхностными водами в горнопромышленных районах на примере участка зоны водосбора р. Белая Перевальского района ЛНР, подработанного горными выработками закрытых шахт «Перевальская» и «Селезневская Восточная».

The paper is devoted to identifying the hydrogeological connection that occurs when the systems of underground workings of closed mines are flooded, as well as studying the features of water exchange between underground and surface waters in mining areas using the example of a site of the catchment area of the Belaya river in Perevalsky region of the LPR mined by mine workings of the closed mines “Perevalskaya ” and “Seleznevskaya Vostochnaya ”. The paper provides information on the flow rates (m /h) in the watercourses of self-flowing wel ls drilled into the mine workings of the closed mine “Seleznevskaya Vostochnaya ” and in the watercourse from the western ventilation block No. 1 of the “Perevalskaya ” mine along the k formation. The dependences of changes in the volumes of self-outflow of groundwater from the western connection No. 1 of the closed mine “Perevalskaya ” from plugged technical wells, and the levels of flooding of old mine workings of the closed mines of the TGC Artyom, atmospheric precipitation and runoff modules of the Belaya river at the site of the dam of the Isakovo storage lake.