Experimental determination of portlandite solubility in H sub 2 O and acetate solutions at 100-350C and 500 bars: Constraints on calcium hydroxide and calcium acetate complex stability
Journal Article
·
· Geochimica et Cosmochimica Acta; (United States)
- Univ. of Minnesota, Minneapolis (United States)
The solubility of portlandite was measured in H{sub 2}O and aqueous acetate solutions of varying concentration (1-10 mmolal) at temperatures from 100-350C and 500 bars pressure. Dissolved Ca concentrations increased with decreasing temperature and increasing dissolved acetate concentration. Using known thermodynamic data for portlandite, H{sup +}, OH{sup {minus}}, Ca{sup ++}, CH{sub 3}COO{sup {minus}}, CH{sub 3}COOH{sup 0}, and H{sub 2}O{sub (1)}, stability constants for CaOH{sup +} and CaCH{sub 3}COO{sup +} complexes were determined. These results indicate that the stabilities of CaOH{sup 1} and CaCH{sub 3}COO{sup 1} complex increase with increasing temperature. In the acetate-free experiments, CaOH{sup +} is the dominant form of dissolved Ca in equilibrium with portlandite at 100-350C and 500 bars, while in the acetate-rich experiments (10 mmolal acetate), Ca{sup ++} and CaOH{sup +} are the dominant forms of Ca in equilibrium with portlandite at low temperature (100-200C) and CaCH{sub 3}COO{sup +} and CaOH{sup +} are the dominant forms at relatively high temperature (200-350C). Metal-acetate complexing has long been suggested as an important mechanism for mobilizing base metals during the formation of ore deposits in organic-rich environments. Due to the stability of CaCH{sub 3}COO{sup +} complex in Ca-bearing fluids at elevated temperatures and pressures, however, the effectiveness of dissolved acetate to enhance base metal sulfide solubility is limited.
- OSTI ID:
- 6038861
- Journal Information:
- Geochimica et Cosmochimica Acta; (United States), Journal Name: Geochimica et Cosmochimica Acta; (United States) Vol. 55:3; ISSN GCACA; ISSN 0016-7037
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
58 GEOSCIENCES
580000 -- Geosciences
ACETATES
ALKALINE EARTH METAL COMPLEXES
ALKALINE EARTH METAL COMPOUNDS
AQUEOUS SOLUTIONS
BRINES
CALCIUM COMPLEXES
CALCIUM COMPOUNDS
CALCIUM HYDROXIDES
CARBOXYLIC ACID SALTS
CHALCOGENIDES
CHEMISTRY
COMPLEXES
DIAGENESIS
DISPERSIONS
GEOCHEMISTRY
GEOLOGIC DEPOSITS
HYDROGEN COMPOUNDS
HYDROTHERMAL ALTERATION
HYDROXIDES
INORGANIC PHOSPHORS
LEAD COMPOUNDS
LEAD SULFIDES
MINERAL RESOURCES
MINERALIZATION
MINERALS
MIXTURES
OIL WELLS
OXYGEN COMPOUNDS
PETROLEUM DEPOSITS
PHOSPHORS
PHYSICAL PROPERTIES
PRECIPITATION
PRESSURE EFFECTS
RESERVOIR ROCK
RESOURCES
SEPARATION PROCESSES
SOLUBILITY
SOLUTIONS
SULFIDE MINERALS
SULFIDES
SULFUR COMPOUNDS
TEMPERATURE EFFECTS
THERMODYNAMIC PROPERTIES
WELLS
ZINC COMPOUNDS
ZINC SULFIDES
020200* -- Petroleum-- Reserves
Geology
& Exploration
58 GEOSCIENCES
580000 -- Geosciences
ACETATES
ALKALINE EARTH METAL COMPLEXES
ALKALINE EARTH METAL COMPOUNDS
AQUEOUS SOLUTIONS
BRINES
CALCIUM COMPLEXES
CALCIUM COMPOUNDS
CALCIUM HYDROXIDES
CARBOXYLIC ACID SALTS
CHALCOGENIDES
CHEMISTRY
COMPLEXES
DIAGENESIS
DISPERSIONS
GEOCHEMISTRY
GEOLOGIC DEPOSITS
HYDROGEN COMPOUNDS
HYDROTHERMAL ALTERATION
HYDROXIDES
INORGANIC PHOSPHORS
LEAD COMPOUNDS
LEAD SULFIDES
MINERAL RESOURCES
MINERALIZATION
MINERALS
MIXTURES
OIL WELLS
OXYGEN COMPOUNDS
PETROLEUM DEPOSITS
PHOSPHORS
PHYSICAL PROPERTIES
PRECIPITATION
PRESSURE EFFECTS
RESERVOIR ROCK
RESOURCES
SEPARATION PROCESSES
SOLUBILITY
SOLUTIONS
SULFIDE MINERALS
SULFIDES
SULFUR COMPOUNDS
TEMPERATURE EFFECTS
THERMODYNAMIC PROPERTIES
WELLS
ZINC COMPOUNDS
ZINC SULFIDES