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Dissolution of quartz in aqueous basic solution, 106-236 degree C: Surface kinetics of perfect crystallographic faces

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
; ;  [1]
  1. Univ. of California, Los Angeles (USA)

Past work on dissolution kinetics of minerals has focused on particulates and the total transfer of material to solution. The authors look instead at local topography of single crystals. Etching of quartz in alkali hydroxide solutions produces four types of features: flat-bottomed negative crystals with facets for walls, believed to nucleate on microfractures; jumbo pits, giant etch pits cored by dislocations and often with hollow cores; small pits, also believed to be dislocation-cored; and etch tunnels extending from some jumbo pits. A transition from selective etching to nonselective etching occurs as a function of ionic strength, with small pits forming only at ionic strengths below {approximately}0.005 m. This transition is attributed to the decrease in Debye-Hueckel length with increasing solution strength. The authors introduce the negative crystal method, whereby dissolution rates of nominally perfect crystal faces are obtained by measuring the size of individual negative crystals during a sequence of dissolution steps. Rates are obtained to {approximately}4% accuracy, with temperature control of {plus minus} 1.25{degree}C. Using this method, they find apparent activation energies for dissolution of the prism and for an average of the rhombs to be 86.39 and 90.19 kJ/mol, respectively, with corresponding pre-exponential factors of 2.99 {times} 10{sup 9} and 1.43 {times} 10{sup 10} {mu}m/h.

OSTI ID:
6262080
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Journal Name: Geochimica et Cosmochimica Acta; (USA) Vol. 54:11; ISSN GCACA; ISSN 0016-7037
Country of Publication:
United States
Language:
English

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