Leachability of Zircon as a Function of Alpha Dose
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		    Werner. Lutze, editor
 
 LEACHABILITY OF ZIRCON AS A FUNCTION OF ALPHA DOSE RODNEY C. EWING+, RICHARD F. HAAKER+ AND WERNER LUTZE+ +Department of Geology, University of New Mexico, Albuquerque, NM 87131 USA ++Hahn-Meitner Institute, Glienicker Strasse 100, 1000 Berlin 39, Federal Republic of Germany
 
 ABSTRACT The variation
 
 zircons
 
 the leachability of naturally occurring
 
 (ZrSiO4 )
 
 0
 
 an increase of one order
 
 the range of 1016 to 1018 alphas/gm there is
 
 doses in
 
 the weight percent of zircon that is
 
 of magnitude in in
 
 in
 
 a function of total alpha dose has been measured at 87 C. For calculated
 
 as
 
 dissolved and an increase
 
 leach rate of the zircon 2.9 x 10-8 to 2.3 x 10-7 gm/cm2 day.
 
 the
 
 metamict
 
 (dose >
 
 specimens 2
 
 10-6 gm/cm
 
 1019 alphas/gm)
 
 Totally
 
 have leach rates as high as 1.8 x
 
 day.
 
 INTRODUCTION The
 
 effect
 
 radiation damage on the leach rates of proposed high level
 
 of
 
 radioactive
 
 waste
 
 predictions
 
 of
 
 compositionally
 
 leaching
 
 a
 
 factor
 
 behavior
 
 can
 
 that be
 
 must made.
 
 it
 
 report the variations in metamict
 
 zircons
 
 Pb
 
 known
 
 natural
 
 Since
 
 isotopic
 
 zircon
 
 is
 
 a
 
 crystalline
 
 The purpose of this study is
 
 the leach rate of crystalline,
 
 for which age
 
 long term
 
 before
 
 a convenient model for which the effect of radiation
 
 is
 
 on leach rates can easily be measured.
 
 damage
 
 be
 
 simple and relatively conmion phase which occurs in
 
 and metamict forms,
 
 and
 
 is
 
 forms
 
 the alpha-dose
 
 determinations,
 
 or
 
 to
 
 partially metamict and
 
 has been calculated based on U,Th estimated
 
 on
 
 the
 
 basis
 
 of
 
 x-ray
 
 diffraction analysis and density determinations. There has been considerable discussion and controversy concerning radiation effects on the leachability of minerals and borosilicate glass and crystalline ceramic
 
 radioactive waste forms.
 
 altered,
 
 such phases
 
 that
 
 Ringwood8
 
 1,2,3,4,5 Since metamict minerals are often
 
 brittle and glassy, some mineralogists have assumed 6 7 less resistant than their crystalline counterparts. ,
 
 microfractured,
 
 citing
 
 are
 
 the work
 
 9
 
 of Pidgeon and others '
 
 1 0
 
 has
 
 suggested
 
 that
 
 in
 
 phases susceptible to radiation damage, such as zircon, actinides would remain "tightly bound" even in the metamict state. Further work has shown that naturally occurring Pb
 
 and that there is
 
 alpha in
 
 zirconolites only
 
 dose. 1112 Roy and Vance
 
 a crystalline
 
 have behaved
 
 a slight increase
 
 as closed systems for U, Th and in
 
 U leach rates with increased
 
 13 have maintained that the solubility changes
 
 phase due to radiation effects are likely to be quite small.
 
 390 14 In
 
 contrast,
 
 Fleischer
 
 mica,
 
 factor
 
 metamict
 
 of
 
 discordance
 
 that
 
 and
 
 the
 
 is
 
 documented
 
 of
 
 solubility of zircons in a mixture of 6 as a function of degree of metamictization.
 
 increased
 
 sulfuric acid
 
 and
 
 rates
 
 dissolution of altered and
 
 17
 
 hydrofluoric
 
 Increased
 
 ages.
 
 radiometric
 
 are substantiated by the differential
 
 zircon
 
 Also well
 
 Fleischer suggests
 
 and natural glass.
 
 quartz
 
 such as zircon,
 
 14
 
 the
 
 in
 
 dissolution
 
 have described the
 
 phases
 
 in
 
 loss of		
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