Experimental metamorphism of NaCl-bearing aqueous solutions by reactions with silicates

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ID: 302792
1969
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Abstract
The starting materials, illite, glauconite, montmorillonite, and muscovite, were allowed to react with salt-solutions at 1 kb and 350 degrees , 450 degrees , and 550 degrees C, respectively. Na (super +) was fixed in Na-bearing aluminosilicates and K (super +) , Fe (super 3+) , Ca (super 2+) , and Mg (super 2+) entered the fluid phase. The fluid phase became acid, and the amount of NaCl consumed by the reactions increased with increasing temperatures as well as with increasing ionic strength. The K (super +) /Na (super +) ratio of the fluid phase increased with increasing temperature at fixed ionic strength and decreased in isothermal runs with increasing ionic strength. The Fe (super 2+) /Na (super +) ratio increased both with increasing temperature and salt concentration. At higher temperatures and ionic strengths, Fe (super 2+) became the most concentrated cation in the solution next to Na (super +) .
Reference Key
openalex_W2142305742 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors E. Althaus, Wilhelm Johannes
Journal american journal of science
Year 1969
DOI
10.2475/ajs.267.1.87
URL
Keywords Keywords not found

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