An improved model calculating CO2 solubility in pure water and aqueous NaCl solutions from 273 to 533 K and from 0 to 2000 bar
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Effect of Greenhouse Gases Dissolved in SeawaterConstraints on the magnitude and rate of CO2 dissolution at Bravo Dome natural gas fieldStable carbon isotope fractionation data between H(2)CO(3)(*) and CO(2)(g) extended to 120 °C.Acidic ionic liquids as sustainable approach of cellulose and lignocellulosic biomass conversion without additional catalysts.Formulating formation mechanism of natural gas hydrates.Active chemisorption sites in functionalized ionic liquids for carbon capture.Geo-material microfluidics at reservoir conditions for subsurface energy resource applications.Effects of surface-active organic matter on carbon dioxide nucleation in atmospheric wet aerosols: a molecular dynamics study.Supramolecular assemblies of amphiphilic L-proline regulated by compressed CO2 as a recyclable organocatalyst for the asymmetric aldol reaction.A mechanistic understanding of plagioclase dissolution based on Al occupancy and T-O bond length: from geologic carbon sequestration to ambient conditions.CO2 production, dissolution and pressure dynamics during silage production: multi-sensor-based insight into parameter interactions.High temperatures and high pressures Brillouin scattering studies of liquid H(2)O+CO(2) mixtures.Effects of mineral spatial distribution on reaction rates in porous mediaStructural evolution of aqueous NaCl solutions dissolved in supercritical carbon dioxide under isobaric heating by mid and near infrared spectroscopyApplication of extreme learning machine for prediction of aqueous solubility of carbon dioxideThe environment of early Mars and the missing carbonatesInvestigating fossil hydrothermal systems by means of fluid inclusions and stable isotopes in banded travertine: an example from Castelnuovo dell’Abate (southern Tuscany, Italy)Preliminary geochemical modeling of water–rock–gas interactions controlling CO2 storage in the Badenian Aquifer within Czech Part of Vienna BasinAccelerated Carbonation of Steel Slag Compacts: Development of High-Strength Construction MaterialsQuantification of CO2 trapping and storage capacity in the subsurface: Uncertainty due to solubility modelsA Geochemical Model of Fluids and Mineral Interactions for Deep Hydrocarbon ReservoirsCoal seam gas distribution and hydrodynamics of the Sydney Basin, NSW, Australia
P2860
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P2860
An improved model calculating CO2 solubility in pure water and aqueous NaCl solutions from 273 to 533 K and from 0 to 2000 bar
description
article
@en
wetenschappelijk artikel
@nl
наукова стаття, опублікована в лютому 2003
@uk
ലേഖനം
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name
An improved model calculating ...... o 533 K and from 0 to 2000 bar
@en
An improved model calculating ...... o 533 K and from 0 to 2000 bar
@nl
type
label
An improved model calculating ...... o 533 K and from 0 to 2000 bar
@en
An improved model calculating ...... o 533 K and from 0 to 2000 bar
@nl
prefLabel
An improved model calculating ...... o 533 K and from 0 to 2000 bar
@en
An improved model calculating ...... o 533 K and from 0 to 2000 bar
@nl
P1433
P1476
An improved model calculating ...... o 533 K and from 0 to 2000 bar
@en
P2093
Zhenhao Duan
P304
P356
10.1016/S0009-2541(02)00263-2
P50
P577
2003-02-01T00:00:00Z