The depletion and regeneration of dissolution-active sites at the mineral-water interface: I. Fe, Al, and In sesquioxides

Geochimica et Cosmochimica Acta

Volumn 64, Issue 20, 2000, Pages 3471-3484

  Samson, Sherry D ^a   Stillings, Lisa L ^a   Eggleston, Carrick M ^a  

^a UNIVERSITY OF WYOMING   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

DISSOLUTION; LIGAND; MINERAL ALTERATION; WATER-ROCK INTERACTION;

EID: 0033708414     PISSN: 00167037     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0016-7037(00)00462-2     Document Type: Article

References (55)

1. Mossbauer study of ferric ions adsorbed at α-ferric oxide/aqueous solution interface
2. The growth of crystals and the equilibrium structure of their surfaces
3. A surface complex reaction model for the pH-dependence of corundum and kaolinite dissolution rates
4. On the relative dissolution rates of some oxide and orthosilicate minerals
5. What do dissolution experiments tell us about natural weathering?
6. Leaching of mineral and glass surfaces during dissolution
7. Silicate mineral dissolution as a ligand-exchange reaction
8. Control of dissolution rates of orthosilicate minerals by divalent metal-oxygen bonds
9. Study of the weathering of albite at room temperature and pressure with a fluidized bed reactor
10. Steady-state kinetics and dissolution mechanisms of albite
11. Water exchange between solvent and aquoamminenickel (II) complexes
12. Non-equilibrium water/rock interactions-I. Model for interface-controlled reactions
13. Uber die hydratation von nickeloxid
14. 3 and BeO
15. Kinetics of solvent water exchange on iron (III)
16. The albite-water system: Part II. The time-evolution of the stoichiometry of dissolution as a function of pH at 100, 200, and 300°C
17. Mechanism of feldspar weathering-I. Experimental studies
18. The chemistry of silica surfaces
19. 17O-NMR study of water exchange of hexaaquaaluminium(III)
20. The effect of coordinated ligands on the rate of replacement of bound water by ammonia in nickel (II) complexes
21. 2, temperature, and time
22. The dissolution kinetics of quartz as a function of pH and time at 70°C
23. 3+, and new experimental data
24. Influence of solution saturation state on the kinetics of ligand-controlled dissolution of oxide phases
25. Balance between surface complexation and surface phase transformation at the alumina/water interface
26. An FTIR spectral investigation of the structural species found on alumina surfaces
27. Substitution reactions of solvated metal ions
28. 3 (0001) surfaces: Synchrotron X-ray photoemission studies and thermodynamic calculations
29. Prediction of ligand-promoted dissolution rates from the reactivities of aqueous complexes
30. The effect of different functional groups on the ligand-promoted dissolution of NiO and other oxide minerals
31. Biotite dissolution at 25°C: The pH dependence of dissolution rate and stoichoimetry
32. Kinetics and mechanisms of complex formation and ligand exchange
33. The effect of oxalate on the dissolution rates of oligoclase and tremolite
34. Evolution of hematite surface microtopography upon dissolution by simple organic acids
35. 2+ (aq)
36. Aqueous equilibrium data for mononuclear aluminum species
37. Surface energy and adsorption at mineral-water interfaces: An introduction
38. Kinetics of dissolution of mechanically comminuted rock-forming oxides and silicates. I. Deformation and dissolution of quartz under laboratory conditions
39. Kinetics of dissolution of mechanically comminuted rock-forming oxides and silicates. II. Deformation and dissolution of oxides and silicates in the laboratory and at the earth's surface
40. 2O)(6-x)(3-x)(aq) complexes: Ligand-directed labilization of water as an analogue for ligand-induced dissolution of oxide minerals
41. Evaluation of internally consistent parameters for the triple-layer model by the systematic analysis of oxide surface titration data
42. Active sites and the non-steady-state dissolution of hematite
43. 3 at pH 3 and pH 6
44. Mechanism of pyroxene and amphibole weathering: I. Experimental studies of iron-free minerals
45. Crystallography of platelet-type hematite particles by electron microscopy
46. Kinetics and non-stoichiometry of labradorite dissolution
47. Factors controlling the solubility of aerosol trace metals in the atmosphere and on mixing into seawater
48. Ferrozine-a new spectrophotometric reagent for iron
49. Dissolution of oxide and silicate minerals: Rates depend on surface speciation
50. Characterization of hematite particles of different shapes
51. The dissolution kinetics of mixed-cation orthosilicate minerals
52. Dissolution kinetics of kaolinite in acidic aqueous solutions at 25°C
53. The coordination chemistry of weathering: III. A generalization on the dissolution rates of minerals