Prediction of the thermodynamic properties of aqueous metal complexes to 1000 degrees C and 5 kb.
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Thermodynamic Simulation of Carbonate Cements-Water-Carbon Dioxide Equilibrium in Sandstone for Prediction of Precipitation/Dissolution of Carbonate CementsBiosphere frontiers of subsurface life in the sedimented hydrothermal system of Guaymas Basin.Sphalerite is a geochemical catalyst for carbon-hydrogen bond activation.Potential for biogeochemical cycling of sulfur, iron and carbon within massive sulfide deposits below the seafloor.Chemolithotrophy in the continental deep subsurface: Sanford Underground Research Facility (SURF), USA.The energetics of organic synthesis inside and outside the cell.Activity and phylogenetic diversity of sulfate-reducing microorganisms in low-temperature subsurface fluids within the upper oceanic crustThermodynamic modeling of poorly complexing metals in concentrated electrolyte solutions: an X-ray absorption and UV-Vis spectroscopic study of Ni(II) in the NiCl2-MgCl2-H2O system.High-temperature water-rock interactions and hydrothermal environments in the chondrite-like core of EnceladusPower limits for microbial life.Sulfur radical species form gold deposits on Earth.Zn/Cd ratios and cadmium isotope evidence for the classification of lead-zinc depositsBioelectric Field Enhancement: The Influence on Membrane Potential and Cell Migration In Vitro.The energetics of anabolism in natural settings.Energetics of Amino Acid Synthesis in Alkaline Hydrothermal Environments.Sulfur oxidation genes in diverse deep-sea viruses.Transport of Pb and Zn by carboxylate complexes in basinal ore fluids and related petroleum-field brines at 100°C: the influence of pH and oxygen fugacity.Speciation and fate of trace metals in estuarine sediments under reduced and oxidized conditions, Seaplane Lagoon, Alameda Naval Air Station (USA).In situ electrochemical enrichment and isolation of a magnetite-reducing bacterium from a high pH serpentinizing spring.Implications for metal and volatile cycles from the pH of subduction zone fluids.Ion-pair formation in aqueous strontium chloride and strontium hydroxide solutions under hydrothermal conditions by AC conductivity measurements.Microbial iron uptake as a mechanism for dispersing iron from deep-sea hydrothermal vents.Rational Development of Neutral Aqueous Electrolytes for Zinc-Air Batteries.Changes in Microbial Energy Metabolism Measured by Nanocalorimetry during Growth Phase Transitions.Laying out ground rules for protein-aided nanofabrication: ZnO synthesis at 70°C as a case study.The mechanisms of crystal growth inhibition by organic and inorganic inhibitors.Uranium transport in acidic brines under reducing conditions.AB INITIO MOLECULAR DYNAMICS STUDY OF DISSOLVED SiO2 IN SUPERCRITICAL WATERA New View on the Petrogenesis of the Oman Ophiolite Chromitites from Microanalyses of Chromite-hosted InclusionsFluid Evolution of the Monte Mattoni Mafic Complex, Adamello Batholith, Northern Italy: Insights from Fluid Inclusion Analysis and Thermodynamic ModelingChemical evolution of metamorphic fluids in the Central Alps, Switzerland: insight from LA-ICPMS analysis of fluid inclusionsMass transfer and fluid evolution in late-metamorphic veins, Rhenish Massif (Germany): insight from alteration geochemistry and fluid-mineral equilibria modelingNumerical Simulation of Reactive Fluid Flow on Unstructured MeshesPhase equilibria controls on the chemistry of vent fluids from hydrothermal systems on slow spreading ridges: Reactivity of plagioclase and olivine solid solutions and the pH-silica connectionDissolved carbon species in associated diffuse and focused flow hydrothermal vents at the Main Endeavour Field, Juan de Fuca Ridge: Phase equilibria and kinetic constraintsThe Chemistry of Diffuse-Flow Vent Fluids on the Galapagos Rift (86°W)° Temporal Variability and Subseafloor Phase Equilibria ControlsFerroan Dolomitization by Seawater Interaction with Mafic Igneous Dikes and Carbonate Host Rock at the Latemar Platform, Dolomites, Italy: Numerical Modeling of Spatial, Temporal, and Temperature Data
P2860
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P2860
Prediction of the thermodynamic properties of aqueous metal complexes to 1000 degrees C and 5 kb.
description
1997 nî lūn-bûn
@nan
1997 թուականի Ապրիլին հրատարակուած գիտական յօդուած
@hyw
1997 թվականի ապրիլին հրատարակված գիտական հոդված
@hy
1997年の論文
@ja
1997年論文
@yue
1997年論文
@zh-hant
1997年論文
@zh-hk
1997年論文
@zh-mo
1997年論文
@zh-tw
1997年论文
@wuu
name
Prediction of the thermodynami ...... es to 1000 degrees C and 5 kb.
@ast
Prediction of the thermodynami ...... es to 1000 degrees C and 5 kb.
@en
type
label
Prediction of the thermodynami ...... es to 1000 degrees C and 5 kb.
@ast
Prediction of the thermodynami ...... es to 1000 degrees C and 5 kb.
@en
prefLabel
Prediction of the thermodynami ...... es to 1000 degrees C and 5 kb.
@ast
Prediction of the thermodynami ...... es to 1000 degrees C and 5 kb.
@en
P2093
P1476
Prediction of the thermodynami ...... es to 1000 degrees C and 5 kb.
@en
P2093
Helgeson HC
Sverjensky DA
P304
P356
10.1016/S0016-7037(97)00009-4
P577
1997-04-01T00:00:00Z