Dissolution kinetics of a lunar glass simulant at 25 degrees C:  the effect of pH and organic acids.
The dissolution kinetics of a simulated lunar glass were examined at pH 3, 5, and 7.  Additionally, the pH 7 experiments were conducted in the presence of citric and oxalic acid at concentrations of 2 and 20 mM.  The organic acids were buffered at pH 7 to examine the effect of each molecule in their dissociated form.  At pH 3, 5, and 7, the dissolution of the synthetic lunar glass was observed to proceed via a two-stage process.  The first stage involved the parabolic release of Ca, Mg, Al, and Fe, and the linear release of Si.  Dissolution was incongruent, creating a leached layer rich in Si and Ti which was verified by transmission electron microscopy (TEM).  During the second stage the release of Ca, Mg, Al, and Fe was linear.  A coupled diffusion/surface dissolution model was proposed for dissolution of the simulated lunar glass at pH 3, 5, and 7.  During the first stage the initial release of mobile cations (i.e., Ca, Mg, Al, Fe) was limited by diffusion through the surface  leached layer of the glass (parabolic release), while Si release was controlled by the hydrolysis of the Si-O-Al bonds at the glass surface (linear release).  As dissolution continued, the mobile cations diffused from greater depths within the glass surface.  A steady-state was then reached where the diffusion rate across the increased path lengths equalled the Si release rate from the surface.  In the presence of the organic acids, the dissolution of the synthetic lunar glass proceeded by a one stage process.  The release of Ca, Mg, Al, and Fe followed a parabolic relationship, while the release of Si was linear.  The relative reactivity of the organic acids used in the experiments was citrate > oxalate.  A thinner leached layer rich in Si/Ti, as compared to the pH experiments, was observed using TEM.  Rate data suggest that the chemisorption of the organic anion to the surface silanol groups was responsible for enhanced dissolution in the presence of the organic acids.  It is proposed that the increased rate of Si release is responsible for the one stage parabolic release of mobile cations and the relatively thin leached layer compared to experiments at pH 3 and 5.
Eick
M J
MJ
Department of Plant and Soil Sciences, University of Delaware, Newark 19717-1303, USA.
Grossl
P R
PR
Golden
D C
DC
Sparks
D L
DL
Ming
D W
DW
D000383:Agriculture / Q000379:methods; D000535:Aluminum / Q000737:chemistry; D019343:Citric Acid / Q000737:chemistry; D005898:Glass / Q000737:chemistry*; D006863:Hydrogen-Ion Concentration; D007700:Kinetics; D008854:Microscopy, Electron; D008903:Minerals / Q000737:chemistry*; D016081:Moon; D010070:Oxalates / Q000737:chemistry; D019815:Oxalic Acid; D012825:Silicon / Q000737:chemistry; D012987:Soil / Q000032:analysis*; D014025:Titanium / Q000737:chemistry
D008903:Minerals; D010070:Oxalates; D012987:Soil; D019343:Citric Acid; D019815:Oxalic Acid; D000535:Aluminum; D014025:Titanium; D012825:Silicon