Chemical composition of natural waters and brines as a result of hydrogeochemical processes in water-rock-gas systems

Geochemistry International

Volumn 50, Issue 13, 2012, Pages 1101-1150

  Ryzhenko, B N ^a   Cherkasova, E V ^a  

^a VERNADSKY INSTITUTE OF GEOCHEMISTRY AND ANALYTICAL CHEMISTRY   (Russian Federation)

Author keywords

geochemical types of groundwater; open closed system; petrochemical type of rocks; thermodynamic modeling; volatile components; water rock

Indexed keywords

ACID BASE; ALKALINE WATER; AQUEOUS PHASE; CARBONATE FIELDS; CHEMICAL COMPOSITIONS; CLOSED SYSTEMS; COMPUTER MODELING; DEEP HORIZON; DISSOLUTION RATES; EVAPORATIVE CONCENTRATION; GEOCHEMICAL EVOLUTION; HYDROGEOCHEMICAL; HYDROGEOCHEMICAL PROCESS; HYDROGEOLOGIC ENVIRONMENT; MASS RATIO; MINERAL COMPOSITION; NATURAL WATERS; OPEN-CLOSED SYSTEM; PHYSICOCHEMICAL CONDITIONS; REDOX STATE; SEAWATER CONCENTRATION; SURFACE CONDITIONS; TEMPERATURE INCREASE; TEMPERATURE-PRESSURE CONDITIONS; THERMODYNAMIC MODELING; VOLATILE COMPONENTS; WATER EXCHANGE; WATER ROCKS;

ALKALINITY; BIOGEOCHEMISTRY; BIOLOGICAL MATERIALS; BOUNDARY CONDITIONS; CARBON DIOXIDE; CHLORINE; GROUNDWATER; HYDROCHEMISTRY; HYDROGEOLOGY; ION EXCHANGE; ORGANIC COMPOUNDS; PETROCHEMICALS; PROCESS CONTROL; ROCKS; SEAWATER EFFECTS; SODIUM;

MINERALS;

ALKALINE WATER; BOUNDARY CONDITION; BRINE; CARBON DIOXIDE; CHEMICAL COMPOSITION; COMPUTER SIMULATION; CONCENTRATION (COMPOSITION); CRYSTALLINE ROCK; DISSOLUTION; GROUNDWATER; HYDROGEOCHEMISTRY; NUMERICAL MODEL; REDOX CONDITIONS; THERMODYNAMICS; WATER-ROCK INTERACTION;

EID: 84870738687     PISSN: 00167029     EISSN: 15561968     Source Type: Journal    
DOI: 10.1134/S0016702912130058     Document Type: Article

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