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Stable Isotope Geochemistry

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Subject:
rate for H2O + D2O --> 2HDO
From:
Jeff Turner <[log in to unmask]>
Reply To:
Stable Isotope Geochemistry <[log in to unmask]>
Date:
Mon, 22 Jun 1998 16:25:10 +0800
Content-Type:
TEXT/PLAIN
Parts/Attachments:
TEXT/PLAIN (34 lines)
On 19 June, David L. Dettman wrote:

...   Does anyone have thoughts on how long the mixed waters should sit
aroundbefore use in order to allow H2O + D2O to go to 2HDO? What is the rate of
diffusion / exchange? Is there a catalyst we could use to speed this up (if
it is slow)?

Proton mobilities in water are very high and can be represented by
reactions such as:

  H20 + H3O+ = H3O+ + H2O  (k1 = 10.6 +/- 4 x 10**9 litre mol(-1) sec(-1))

thus the half life of the proton transfer reaction for this second order
exchange is about 2 x 10-12 sec.  There will be an isotope effect for
deuterium (deuton?) exchange that would decrease the exchange rate
constant, but in practical terms the deuterium exchange reaction would
still be instantaneous.

So the short answer is that the exchange is practically instantaneous. In
artificially prepared tracer water, say up to +1000 per mille, the
contribution of D2O to mass 4 is vanishingly small.

Jeffrey Turner

 =============================================================================
   Dr Jeffrey Turner
   Centre for Groundwater Studies
   CSIRO Land and Water           Phone:  +61 (0)8 9 333 6314 (International:
   Private Bag                    Fax:    +61 (0)8 9 387 8211   Delete 0)
   PO Wembley WA 6014             E-mail:  [log in to unmask]
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