Congruent and incongruent dissolution of labradorite in dilute, acidic salt solutionsReport as inadecuate




Congruent and incongruent dissolution of labradorite in dilute, acidic salt solutions - Download this document for free, or read online. Document in PDF available to download.

Kinetics, Surface-chemistry, Mechanism, Room-temperature, Minerals, Feldspar, Albite, Coordination chemistry, Element, Reactor

Additional contributors:

Subject-Keyword: Kinetics Surface-chemistry Mechanism Room-temperature Minerals Feldspar Albite Coordination chemistry Element Reactor

Type of item: Journal Article Published

Language: English

Place:

Time:

Description: Abstract: Polished 001 cleavage faces of Nain Labradorite An almost-equal-to 56 were leached at 20-degrees-C +- 2-degrees for 72 days in distilled water pH almost-equal-to 5.6, in HCl solution pH almost-equal-to 4.05 and in four other HCl solutions containing 1 mg-l or less of Na, K, Ca, Alaq, and SiO2aq pH of all four solutions almost-equal-to 4.05. Analysis of the cleavage faces by Secondary Ion Mass Spectrometry SIMS revealed no residual surface layer on faces leached by distilled water. By contrast, thick Si-rich residual layers 1500 angstrom formed on surfaces leached by pure HCl solutions. Much thinner residual layers 700 angstrom were observed on labradorite leached by HCl solutions containing 1 mg-l of Na, Ca, and K, whereas leached layers < 75 angstrom thick formed on faces leached by solutions containing 1 mg-l each of Na, K, Ca, Alaq and Siaq; consequently incongruent dissolution of feldspars occurs in HCl solution, but congruent dissolution of feldspars occurs in mixed electrolyte solutions in which dissolved cations are more abundant than H3O+ hydronium or proton. Of the cations studied, Alaq most affects formation of the leached layers, SiO2aq, however, does not noticeably affect thickness of the residual layer. Affinity of cations for surface functional groups affects the rate of formation of the leached layer diffusion, and the rate of surface dissolution from the Si-rich surface layer, by controlling the concentration of H3O+ surface complexes on the surface of the leached layer. Diffusion through the leached layer apparently proceeds via lattice diffusion and line defects. A \-competitive adsorption model\- is proposed to explain the SIMS results and experimental leaching results of others. An important prediction of the model is that Si-rich residual layers generally do not form on feldspars of most soil and weathering profiles. If the residues form, they generally will be thin, with the thickness controlled by the composition of the soil solution.

Date created: 1991

DOI: doi:10.7939-R3DF6K988

License information:

Rights: © 1991 University of Chicago Press. This version of this article is open access and can be downloaded and shared. The original authors and source must be cited.





Author: Nesbitt, H. W. MacRae, N. D. Shotyk, W.

Source: https://era.library.ualberta.ca/



DOWNLOAD PDF




Related documents