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Sökning: onr:"swepub:oai:DiVA.org:su-79777" > Effect of surface o...

Effect of surface orientation on dissolution rates and topography of caf2

Godinho, José R. A. (författare)
Stockholms universitet,Institutionen för geologiska vetenskaper
Piazolo, Sandra (författare)
Stockholms universitet,Institutionen för geologiska vetenskaper
Evins, L. Z. (författare)
 (creator_code:org_t)
Elsevier BV, 2012
2012
Engelska.
Ingår i: Geochimica et Cosmochimica Acta. - : Elsevier BV. - 0016-7037 .- 1872-9533. ; 86, s. 392-403
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • This paper reports how during dissolution differences in surface chemistry affect the evolution of topography of CaF2 pellets with a microstructure similar to UO2 spent nuclear fuel. 3D confocal profilometry and atomic force microscopy were used to quantify retreat rates and analyze topography changes on surfaces with different orientations as dissolution proceeds up to 468 h. A NaClO4 (0.05 M) solution with pH 3.6 which was far from equilibrium relative to CaF2 was used. Measured dissolution rates depend directly on the orientation of the exposed planes. The {111} is the most stable plane with a dissolution rate of (1.2 +/- 0.8) x 10(-9) mol m(-2) s(-1), and {112} the least stable plane with a dissolution rate 33 times faster that {111}. Surfaces that expose both Ca and F atoms in the same plane dissolve faster. Dissolution rates were found to be correlated to surface orientation which is characterized by a specific surface chemistry and therefore related to surface energy. It is proposed that every surface is characterized by the relative proportions of the three reference planes {111}, {100} and {110}, and by the high energy sites at their interceptions. Based on the different dissolution rates observed we propose a dissolution model to explain changes of topography during dissolution. Surfaces with slower dissolution rate, and inferred lower surface energy, tend to form while dissolution proceeds leading to an increase of roughness and surface area. This adjustment of the surface suggests that dissolution rates during early stages of dissolution are different from the later stages. The time-dependency of this dynamic system needs to be taken into consideration when predicting long-term dissolution rates.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geofysik (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geophysics (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)

Nyckelord

CRYSTALLOGRAPHIC PREFERRED ORIENTATION
MINERAL DISSOLUTION
PRECIPITATION CREEP
CAF2(111) SURFACE
ETCH PITS
KINETICS
MORPHOLOGY
GROWTH
FORCE
DISLOCATION

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Godinho, José R. ...
Piazolo, Sandra
Evins, L. Z.
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NATURVETENSKAP
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och Geovetenskap och ...
och Geofysik
NATURVETENSKAP
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och Geovetenskap och ...
och Geokemi
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Geochimica et Co ...
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Stockholms universitet

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