- Geological Studies and Exploration
- Groundwater and Isotope Geochemistry
- Fluoride Effects and Removal
- Marine and environmental studies
- Hydrocarbon exploration and reservoir analysis
- Water Resources and Management
- Methane Hydrates and Related Phenomena
- Geotechnical and Geomechanical Engineering
- Geochemistry and Elemental Analysis
- Industrial Engineering and Technologies
- Engineering and Environmental Studies
- Aquatic and Environmental Studies
- Advanced Data Processing Techniques
- Geochemistry and Geologic Mapping
- Reservoir Engineering and Simulation Methods
- Food Industry and Aquatic Biology
- Oil and Gas Production Techniques
Tomsk Polytechnic University
2009-2018
National Research Tomsk State University
2011-2018
Chemical and microbiological composition of the Mid-Ob' its feeders' waters has been studied. Swampiness area is cause significant organic biogenic substance content in streams, it also responsible for a large variety organotrophic microflora. Microbiological studied streams characterizes them as contaminated. Settlements are main sources investigated water pollution.
The chemical composition of nitric thermal waters in Jiangxi Province, SE-China, is considered. It shown that the studied are characterized by low TDS (293-412 mg/l), but they always have alkaline or highly pH values. should be noted content Na+, Si, F-, HCO3-, CO32-, sometimes SO42- predominant, on other hand, Ca2+, Mg2+, Cl- low. has been established main factors responsible for concentrations some elements and high others continuous dissolution aluminosilicate minerals simultaneous...
Technique for the domestic wastewater treatment in small residential areas and oil gas facilities of natural man-made systems including a settling tank mechanical biological pond with peat substrate bog vegetation has been substantiated. parameters calculation similar developed. It was proven that effective can be performed Siberia all year round.
The paper presents calculation results of equilibrium groundwater in Kishenev with a variety secondary carbonate minerals. It is shown that the groundwater-rock system some minerals, such as calcite, magnesite, dolomite, siderite, but at same time not strontianite. indicates mineral precipitation possible. Specific nitrate chemical water type, which rarely observed nature and characterized by presence anthropogenic impact this territory, cases higher saturation compared to dolomite magnesite...
The calculation results of ground water equilibrium with the major water-bearing rock minerals (Moldova) are presented under condition anthropogenic impact. As a model HydroGeo software is used. It shown that both "ground water-rock" and "intermediate systems in number minerals.
The calculation modeling results of the nitric hydrotherms saturation in Baikal Rift Zone with calcite and dolomite are presented. make carbonate barrier to thermal waters equilibrium primary minerals igneous rocks. In research territory, there three main types geochemical which characterized by degree proportion precipitating phases. It has been established that waters-rock system these minerals, leads bonding migrated from rocks calcium magnesium secondary formed - dolomite.