Complex assessment of drained groundwater of Yakovlevsky mine according to the results of hydrogeochemical monitoring
Authors:
About authors
- Postgraduate student G.V. Plekhanov Saint Petersburg Mining University
Abstract
Hydrogeochemical monitoring carried out in 2006-2007 allows estimation of the activity coefficient of overflowing and secondary humidifying of rich iron ores in the underground workings of the Yakovlevsky Mine. Ubiquitous manifestation of H2S of various geneses was revealed during the research. Regularities in H2S and Cl– content patterns were revealed. Zones of active water overflowing from law carboniferous limestones were mapped for the –425 and –370 m horizons. A tendency of decreasing in levels of lawcarbonic aquifer is established. Zones with various water inflows to the –425 m mine horizon were revealed.
Область исследования:
Geology
Funding:
None
Similar articles
Statistical processing of the results of microstructural analysis of ice cores from deep boreholes at Vostok station (Central Antarctica)
2007 E. V. Polyakova
Measurement and analysis of quality indicators of electric energy in networks of oil producing enterprises
2007 Yu. A. Sychev
Development of technology of processing of low-quality coal with the purpose of extraction of non-ferrous metals from it
2007 G. S. Roshchin
Causes and consequences of magneto-hydrodynamic instability in electrolysis processes for aluminum production
2007 M. A. Glushchenko