The temperature dependence of bytownite feldspar dissolution in neutral aqueous solutions of inorganic and organic ligands at low temperature (5-35°C)

Chemical Geology

Volumn 167, Issue 3-4, 2000, Pages 337-354

  Welch, Susan A ^a,b   Ullman, William J ^b  

^a UNIVERSITY OF WISCONSIN MADISON   (United States)

^b UNIVERSITY OF DELAWARE   (United States)

Author keywords

Bytownite feldspar dissolution; Ligands; Temperature dependence

Indexed keywords

AQUEOUS SOLUTION; DISSOLUTION; FELDSPAR; WEATHERING;

EID: 0034113449     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0009-2541(99)00238-7     Document Type: Article

References (75)

1. Afzal M., Hamdani K., Ahmad H. Thermodynamics of adsorption of organic acids from aqueous solutions on neutral alumina. Sci. Int. 2:1990;101-106.
2. Antweiler R.C., Drever J.I. The weathering of a late tertiary volcanic ash: importance of organic solutes. Geochim. Cosmochim. Acta. 47:1983;623-629.
3. Bennett P.C., Melcer M.E., Siegel D.I., Hassett J.P. The dissolution of quartz in dilute aqueous solutions of organic acids at 25°C. Geochim. Cosmochim. Acta. 52:1988;1521-1530.
4. 2 over Phanerozoic time. Am. J. Sci. 291:1991;339-376.
5. 2: importance of solar radiation and plant evolution. Science. 261:1993;68-70.
6. Berner R.A., Holdren G.R. Jr. Mechanism of feldspar weathering: II. Observations of feldspars from soils. Geochim. Cosmochim. Acta. 43:1979;1173-1186.
7. Berner R.A., Lasaga A.C., Garrels R.M. The carbon-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years. Am. J. Sci. 283:1983;641-683.
8. Bevan J., Savage D. The effect of organic acids on the dissolution of K-feldspar under conditions relevant to burial diagenesis. Mineral. Mag. 53:1989;415-425.
9. Blum A., Lasaga A.C. Role of surface speciation in the low temperature dissolution of minerals. Nature. 331:1988;431-433.
10. Bottari E., Ciavatta L. Studio potentiometrico dei complessi Al(III)-ossalato. Gazz. Chim. Ital. 98:1968;1004-1013.
11. 2. J. Geophys. Res. 96:1991;18101-18106.
12. Brady P.V., Dorn R.I., Brazel A.J., Clark J., Moore R.B., Glidewell T. Direct measurement of the combined effects of lichen, rainfall, and temperature on silicate weathering. Geochim. Cosmochim. Acta. 63:1999;3293-3300.
13. 2 and temperature on silicate weathering: possible implications for climate control. Geochim. Cosmochim. Acta. 58:1994;1853-1856.
14. Brady P.V., Walther J.V. Controls on silicate dissolution rates in neutral and basic pH solutions at 25°C. Geochim. Cosmochim. Acta. 53:1989;2823-2830.
15. Brady P.V., Walther J.V. Surface chemistry and silicate dissolution at elevated temperatures. Am. J. Sci. 292:1992;639-658.
16. Burch T.E., Nagy K.L., Lasaga A.C. Free energy dependence of albite dissolution kinetics at 80°C and pH 8.8. Chem. Geol. 105:1993;137-162.
17. Carroll S.A., Walther J.V. Kaolinite dissolution at 25°, 60°, and 80°C. Am. J. Sci. 290:1990;797-810.
18. Carroll-Webb S.A., Walther J.V. A surface complexation model for the pH dependence of corundum and kaolinite dissolution rates. Geochim. Cosmochim. Acta. 52:1988;2609-2623.
19. Casey W.H., Bunker B. Leaching of mineral and glass surfaces during dissolution. Hochella M.F., White A.F. Mineral-Water Interface Geochemistry. Rev. Mineral. 23:1990;397-426 Mineralogical Society of America.
20. Casey W.H., Sposito G. On the temperature dependence of mineral dissolution rates. Geochim. Cosochim. Acta. 56:1992;3825-3830.
21. Chen Y., Brantley S.L. Temperature and pH dependence of albite dissolution rate at acid pH. Chem. Geol. 135:1997;275-290.
22. Chen Y., Brantley S.L. Diopside and anthophyllite dissolution at 25° and 90°C and acid pH. Chem. Geol. 147:1998;233-248.
23. Chou L., Wollast R. Study of the weathering of albite at room temperature and pressure with a fluidized bed reactor. Geochim. Cosmochim. Acta. 48:1984;2205-2217.
24. Chou L., Wollast R. Steady-state kinetics and dissolution mechanisms of albite. Am. J. Sci. 285:1985;963-993.
25. Dorn R.I., Brady P.V. Rock-based measurement of temperature dependent plagioclase weathering. Geochim. Cosmochim. Acta. 59:1995;2847-2852.
26. Drever J.I., Vance G.F. Role of soil organic acids in mineral weathering processes. Pittman E.D., Lewan M.D. Organic Acids in Geological Processes. 1994;138-161 Springer, New York.
27. Eggleston C.M., Hochella M.F. Jr., Parks G.A. Sample preparation and aging effects on the dissolution rate and surface composition of diopside. Geochim. Cosmochim. Acta. 53:1989;797-804.
28. Fein J.B. Experimental study of aluminum-oxalate complexing at 80°C: implications for the formation of secondary porosity within sedimentary reservoirs. Geology. 19:1991;1037-1040.
29. Fein J.B., Brady P.V. Mineral surface controls on the diagenetic transport of oxalate and aluminum. Chem. Geol. 121:1995;11-18.
30. Fisher J.B. Distribution and occurrence of aliphatic acid anions in deep subsurface waters. Geochim. Cosmochim. Acta. 51:1987;2459-2468.
31. Fox T.R., Comerford N.B. Low-molecular-weight organics in selected forest soils of the southeastern USA. Soil Sci. Soc. Am. J. 54:1990;1139-1144.
32. Franklin S.P., Hajash A. Jr., Dewers T.A., Tieh T.T. The role of carboxylic acids in albite and quartz dissolution: an experimental study under diagenetic conditions. Geochim. Cosmochim. Acta. 58:1994;4259-4279.
33. Gordienko V.I., Mikhailyuk Y.I. Indicator amperometric method for determining instability constants of very simple complexes: Communication 1. Non-protonated complexes. Zh. Anal. Khim. 25:1970;2267.
34. Graustein W.C., Cromack K. Jr., Sollins P. Calcium oxalate: occurrence in soils and effect on nutrient and geochemical cycles. Science. 198:1977;1252-1254.
35. 2, and organic acidity on silicate weathering in the soil environment: formulation of a model and results. Global Biogeochem. Cycles. 8:1994;141-155.
36. Hellmann R. The albite-water system: Part I. The kinetics of dissolution as a function of pH at 100, 200, and 300°C. Geochim. Cosmochim. Acta. 58:1994;595-611.
37. Holdren G.R. Jr., Addams J.E. Parabolic dissolution kinetics of silicate minerals: an artifact of nonequilibrium precipitation processes? Geology. 10:1982;186-190.
38. 4. Can. J. Chem. 55:1977;3689-3699.
39. Johnston C.G., Vestal J.R. Biogeochemistry of oxalate in Antarctic cryptoendolithic lichen-dominated community. Microb. Ecol. 25:1993;305-319.
40. Knauss K.G., Wolery T.J. Dependence of albite dissolution kinetics on pH and time at 25°C and 70°C. Geochim. Cosmochim. Acta. 50:1986;2481-2498.
41. 3. J. Colloid Interface Sci. 75:1980;373-385.
42. Lasaga A.C., Soler J.M., Ganor J., Burch T., Nagy K.L. Chemical weathering rate laws and global geochemical cycles. Geochim. Cosmochim. Acta. 58:1994;2361-2386.
43. Lowell S., Shields J.E. Powder Surface Area and Porosity. 1984;Chapman & Hall, New York. 234 pp.
44. Manley E.P., Evans L.J. Dissolution of feldspars by low-molecular-weight aliphatic and aromatic acids. Soil Sci. 141:1986;106-112.
45. Masone M., Vicedomini M. Gluconate and lactate as ligands of calcium ion. Anal. Chem. (Rome). 71:1981;517-523.
46. Mast M.A., Drever J.I. The effect of oxalate on the dissolution rates of oligoclase and tremolite. Geochim. Cosmochim. Acta. 51:1987;2559-2568.
47. Motekaitis R.J., Martell A.E. Complexes of aluminum(III) with hydroxy carboxylic acids. Inorg. Chem. 23:1984;18-23.
48. Nagy K.L., Blum A.E., Lasaga A.C. Dissolution and precipitation kinetics of kaolinite at 80°C and pH 3: the dependence on solution saturation state. Am. J. Sci. 291:1991;649-686.
49. Nagy K.L., Lasaga A.C. Dissolution and precipitation kinetics of gibbsite at 80°C and pH 3: the dependence on solution saturation state. Geochim. Cosmochim. Acta. 56:1992;2903-3111.
50. Nordstrom D.K., May H.M. Aqueous equilibrium data for mononuclear aluminum species. Sposito G. The Environmental Chemistry of Aluminum. 2nd edn. 1996;39-80 Lewis Publishers, Boca Raton, FL.
51. Oelkers E.H., Schott J., Devidal J.L. The effect of aluminum, pH, and chemical affinity on the rates of alumino-silicate dissolution reactions. Geochim. Cosmochim. Acta. 58:1994;661-669.
52. Pačes T. Steady-state kinetics and equilibrium between ground water and granitic rock. Geochim. Cosmochim. Acta. 37:1973;2641-2663.
53. Palmer D.A., Bell J.L.S. Aluminum speciation and equilibria in aqueous solution: IV. A potentiometric study of aluminum acetate complexation in acidic NaCl brines to 150°C. Geochim. Cosmochim. Acta. 58:1994;651-659.
54. Parkhurst, D.L., 1995. User's Guide to PHREEQC - A Computer Program for Speciation, Reaction-Path, Advective-Transport, and Inverse Geochemical Calculations. Water-Resources Investigation Report 95-4227. US Geological Survey, Lakewood, CO, 143 pp.
55. Piatt J.J., Backhus D.A., Capel P.D., Eisenreich S.J. Temperature-dependent sorption of naphthalene, phenanthrene, and pyrene to low organic carbon aquifer sediments. Environ. Sci. Technol. 30:1996;751-760.
56. Schwartzenbach R.P., Gschwend P.M., Imboden D.M. Environmental Organic Chemistry. 1993;Wiley, New York. 681 pp.
57. Sjöberg S., Öhman L.-O. Equilibrium and structural studies of silicon (IV) and aluminum (III) in aqueous solution: XIII. A potentiometric and 27 Al nuclear magnetic resonance study of speciation and equilibria in the aluminum (III)-oxalic acid-hydroxide system. J. Chem. Soc., Dalton Trans. 1985;2665-2669.
58. Smith, R.M., Martell, A.E., 1993. NIST Critical Stability Constants of Metal Complexes Database (Version 1.0). National Institute of Standards and Technology, Gaithersburg, MD. (September 1993) (Electronic compilation).
59. Sokal R.R., Rohlf F.J. Biometry. 2nd edn. 1981;Freeman, New York. 859 pp.
60. Stillings L.L., Brantley S.L. Feldspar dissolution at 25°C and pH 3: reaction stoichiometry and the effect of cations. Geochim. Cosmochim. Acta. 59:1995;1483-1496.
61. Stillings L.L., Drever J.I., Brantley S.L., Sun Y., Oxburgh R. Rates of feldspar dissolution at pH 3-7 with 0-8 mM oxalic acid. Chem. Geol. 132:1996;79-89.
62. Surdam R.C., Boese S.W., Crossey L.J. The chemistry of secondary porosity. McDonald D.A., Surdam R.C. Clastic Diagenesis. Am. Assoc. Pet. Geol. Mem. 37:1984;127-149.
63. Tait C.D., Janecky D.R., Clark D.L., Bennett P.C. Oxalate complexation with aluminum (III) and iron (III) at moderately elevated temperatures. Kharaka Y.K., Maest A.S. Water-Rock Interaction Volume 1 Low Temperature Environments. Proceedings of the 7th International Symposium on Water-Rock Interaction, Park City, Utah, USA, 13-18 July:1992;349-352 A.A. Balkema, Rotterdam.
64. Thyne G.D., Harrison W.J., Alloway M.D. Experimental study of the stability of the Al-oxalate complexation at 100°C and calculations of the effects of complexation on clastic diagenesis. Kharaka Y.K., Maest A.S. Water-Rock Interaction Volume 1 Low Temperature Environments. Proceedings of the 7th International Symposium on Water-Rock Interaction, Park City, Utah, USA, 13-18 July:1992;353-357 A.A. Balkema, Rotterdam.
65. 4). Geochim. Cosmochim. Acta. 56:1986;845-850.
66. Ullman W.J., Kirchman D.L., Welch S.A., Vandevivere P. Laboratory evidence for the microbially mediated silicate mineral dissolution in nature. Chem. Geol. 132:1996;11-17.
67. Vandevivere P., Welch S.A., Ullman W.J., Kirchman D.L. Enhanced dissolution of silicate minerals by bacteria at near-neutral pH. Microb. Ecol. 27:1994;241-251.
68. 2 and global greenhouse warming? Geology. 21:1993;1059-1062.
69. 2 over the last 100 million years. Am. J. Sci. 287:1987;763-779.
70. Walker C.G., Hays P.B., Kasting J.F. A negative feedback mechanism for the long-term stabilization of Earth's surface temperature. J. Geophys. Res. 86:1981;9776-9782.
71. Welch, S.A., 1996. Effect of bacteria and microbial metabolites on bytownite feldspar dissolution at earth's surface temperature. PhD dissertation, Univ. of Delaware, 313 pp.
72. Welch S.A., Ullman W.J. The effect of organic acids on plagioclase dissolution rates and stoichiometry. Geochim. Cosmochim. Acta. 57:1993;2725-2736.
73. Welch S.A., Ullman W.J. Feldspar dissolution in acidic and organic solutions: compositional and pH dependence of dissolution rate. Geochim. Cosmochim. Acta. 60:1996;2939-2948.
74. Welch S.A., Ullman W.J. The effect of microbial glucose metabolism on bytownite feldspar dissolution rates between 5 and 35°C. Geochim. Cosmochim. Acta. 63:1999;3247-3259.
75. 2, and organic acids. Geochim. Cosmochim. Acta. 55:1991;943-954.