A5031270910- Hydrocarbon exploration and reservoir analysis
- Methane Hydrates and Related Phenomena
- Geological Studies and Exploration
- Groundwater and Isotope Geochemistry
- Geochemistry and Geologic Mapping
- Fluoride Effects and Removal
- Advanced Data Processing Techniques
- Geological and Geophysical Studies
- Geochemistry and Elemental Analysis
- Geotechnical and Geomechanical Engineering
- Marine and environmental studies
- Geothermal Energy Systems and Applications
- Water Resources and Management
- Coal and Coke Industries Research
- Karst Systems and Hydrogeology
- Aquatic and Environmental Studies
- Industrial Engineering and Technologies
- CO2 Sequestration and Geologic Interactions
- Oil and Gas Production Techniques
- Geological and Geochemical Analysis
- Reservoir Engineering and Simulation Methods
Institute of Petroleum Geology and Geophysics
2018-2021
Far East Geological Institute
2019-2021
National Research Tomsk State University
2015-2020
Tomsk Polytechnic University
2015-2020
Milieux environnementaux, transferts et interactions dans les hydrosystèmes et les sols
2020
Sorbonne Université
2020
Low-enthalpy thermal waters (30–70 °C) with nitrogen as a dominant associated gas are spread within the active continental margin of Russian Far East (east and north Okhotsk Sea Coast) traditionally great importance for recreation balneology facilities. The chemically classified into three groups: (i) Na–HCO3(SO4) type, low TDS (0.2 g/L) lowest temperature (<50 high pH (9.1–9.3), (ii) Na–SO4 type (~1 g/L), highest (70 weak alkaline (8.7) (iii) Ca–Na–Cl (15 moderate T (59 neutral (7.5)....
The chemical and isotopic compositions of Jiangxi Province thermal waters are considered. It is shown, carbon dioxide more mineralized (TDS=0.3–3.9 g/l) than nitric (TDS=0.3-0.4 g/l), in addition, the waters, general, weak acid neutral (pH=5.70-7.77), – alkaline (pH=8.5-9.25). should be noted, content Na+, Si, HCO3-, CO32-, sometimes SO42− Ca2+ K+ predominant F-, HCO3− predominant, but concentrations Ca2+, Mg2+, Cl− quite low waters. has been identified that have meteoric origin....
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...
The chemical and isotopic compositions of waters associated gases in the Republic Buryatia are investigated this report. Results show thermal predominantly enriched N 2 . They alkaline, low salinity have high concentrations HCO 3 - , SO 4 2- F, Si but values for Ca 2+ Mg K + According to composition, meteoric origin. Despite salinity, equilibrium with calcite, magnesite, fluorite, albite, laumontite other minerals not respect primary aluminosilicates. This indicates that water-bearing rocks...
Восточный Китайский технологический университет, Наньчан, провинция Цзянси В работе представлены результаты расчетов глубинных температур азотных термальных вод провинции Цзянси.Показано, что азотные термальные воды являются пресными, минерализация меньше 0,5 г/л
АННОТАЦИЯ: В статье рассмотрен характер равновесия термальных вод провинции Цзянси с минералами водовмещающих пород.Показано, что азотные и углекислые термальные воды имеют разную степень насыщенности к минералам, образуя при этом равновесно-неравновесную систему воды-горные породы.Установлено, представляют собой определенный этап геологической
In world practice, groundwater is the main raw material for iodine production. current geopolitical conditions, a significant part of traditional areas production located outside Russian Federation. As biogenic by its origin, it associates with oil and petroleum water. Therefore, produced waters deposits Western Siberia acquire leading role as raw-material base
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.
ТЕРМАЛЬНЫЕ ВОДЫ БАЙКАЛЬСКОЙ СКЛАДЧАТОЙ ОБЛАСТИ КАК ЭТАП ГЕОЛОГИЧЕСКОЙ ЭВОЛЮЦИИ СИСТЕМЫ «ВОДА -ПОРОДА» 1 Зиппа Е.В., 2 Пургина Д.В., 1,2 Дребот В.В. Томский филиал Института нефтегазовой геологии и геофизики им.А.А.Трофимука СО РАН, Томск, e-mail:
Chemical composition and saturation degree of the Annenskiy thermal waters to minerals water-bearing rock have been considered in manuscript. It is shown that are low mineralized, alkaline belong HCO 3 -Na type. The waters-rock system equilibrium-nonequilibrium. means dissolve primary continuously, never reaching (anorthite, K-field spar etc.), form new secondary mineral phases simultaneously, (gibbsite, montmorillonite, albite etc.). Besides, peculiarities equilibrium with rocks for surface...