Hi Georges and Pier,
 
My previous email was to mainly answer the question: "WHY do we need to add
P2O5 to the 85 % orthophosphoric  acid??" by millionh@yahoo,com . The words,
"100%" H3PO4 or water-free I used, is kind of oral language. Of course,
theoretically all the water can become phosphoric acid by the reaction of
P2O5 + 3H2O = 2H3PO4 under the correct reactive conditions, but practically
it's not the case as Pier pointed out. But whether the acid is completely
water-free or not, it doesn't matter regarding the carbonate isotope
analyses as long as the portion of the remaining water in the acid is
relatively insignificant and you have the carbonate standards (I would say
at least two), such as NBS19, run along with your carbonate samples in the
same batch analysis by using the same batch of the acid because the
systematic errors during the sample preparation processes can be subtracted
out (or significantly eliminated) via the solid carbonate standard
calibration.
 
Wenbo


-----Original Message-----
From: Stable Isotope Geochemistry [mailto:[log in to unmask]] On Behalf
Of Georges L. Paradis
Sent: Monday, September 18, 2006 9:37 AM
To: [log in to unmask]
Subject: Re: [ISOGEOCHEM] preparing 100% phosphoric acid


Dear Pier and Wembo,
 
Thanks for the clear demystification of the "Phosphoric acid folklore".  I
refer to it as folklore because I found that if you ask 7 labs how they
prepare their acid, you'll get 7 different answers.  Some of those will
inevitably describe the acid as anhydrous or water-free, which as Pier
plainly pointed out, there is no such state of phosphoric acid.  Since there
seems to be much variation in acid prep technique (even though we'll all
continue to cite Coplen, 1983, Thanks Ty!), we are probably all using
slightly different reaction conditions.  If that is true, then our isotopic
fractionation factors must be inaccurate.  If that is true, then isn't our
(the isotope community) data comparable by using a good calibration
traceable to NBS19? 
 
Much thanks,
Georges
 
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
Georges L. Paradis
ICPMS Lab Manager
Department of Earth Science, Marine Science Institute
University of California Santa Barbara
Santa Barbara, CA 93106
805-893-7182
[log in to unmask]
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~

----- Original Message ----- 
From: Pier de Groot <mailto:[log in to unmask]>  
To: [log in to unmask] 
Sent: Monday, September 18, 2006 1:32 AM
Subject: Re: [ISOGEOCHEM] preparing 100% phosphoric acid

Wembo and others,

Just a note on the phosphoric acid discussion. What Wembo states, to have
100 percent-water free acid is not completely true. By extracting water
(either by heating or by adding P2O5) the acid polymerizes and liberates
water - and with polymerization viscosity increases. Even if getting more
than 100 percent acid (some name the acid with 1.93 density 103 percent
acid) by continued polymerization water is formed.
By adding water in priciple the acid de-polymerize. Probably a reason why
the concentrated acid is highly hygroscopic.
In fact phosphoric acid has different 'forms', such as orthophosphoric acid
(H3PO4), pyrophosphoric acid (H4P2O7), and polyphopsphoric acid (chain and
ring shaped polymerized acid; highly concentrated acid may crystallize).

One also can gently heat the acid while connected to a low-vacuum line. No
back-hydration of the acid by air-humidity can occur then (if simply heated
in open-air) and also eventual dissolved gases are better removed.
But the original procedure (McCrea, 1950), as part of the calibration of the
carbonate acid digestion method and of the isotopic fractionation(s) related
to this method, was by adding P2O5, a spatula-tip of CrO3 (acid turns yellow
and after heating into green) and about 3 ml of H2O2 is added after a 7
hours heating.
The CrO3-H2O2 procedure was included because the phosphoric acid in older
days probably contained some traces of organic matter (was less pure as it
is nowadays).
Using lower density acid in automates (for viscosity reasons) has a risk to
deviate from the original McCrea (1950) calibration and related isotopic
fractionations, and thus from the proper scale. In any case, the less dense
acid contains more water, increasing possibilities of isotopic exchange with
the oxygen in the produced CO2.
Wasn't it Harmon Craig in the early days of existence of the isogeochem list
who warned against deviating from the original calibrated procedure...(must
still be in the archives...)?


Some thoughts.
Best wishes,
Pier.
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From: Wenbo Yang <[log in to unmask]>
Reply-To: Stable Isotope Geochemistry <[log in to unmask]>
Date: Sun, 17 Sep 2006 17:29:38 -0700
To: <[log in to unmask]>
Subject: Re: [ISOGEOCHEM] preparing 100% phosphoric acid

Yes,  the easiest way to make "100%" H3PO4 is to just simply heat the 85%
H3PO4 on a hot plate to remove (or evaporate) the 15% H2O in fume hood. But
the alternative way is by chemical reaction: P2O5 + 3H2O = 2H3PO4, so that
you can get the "100%" H3PO4 or the water-free H3PO4 acid, too. 



 
-----Original Message-----
From: Stable Isotope  Geochemistry [mailto:[log in to unmask]] On
Behalf Of  millionh@yahoo,com
Sent: Sunday, September 17, 2006 9:56  AM
To: [log in to unmask]
Subject: [ISOGEOCHEM]  preparing 100% phosphoric acid


I know this topic have been on this site few months ago. I have some
questions and suggestion on the topic, how to make 100 % phosphoric acid. I
have been following the same procedure Pier described on this site, that is
following Bowen's (1966) and Coplen et al. (1983). (i.e., adding P2O5 to 85%
orthophosphoric acid and heating at 200 oC)
 
 
 
But, the On-line lab manual for Stanford by Mucciarone uses very  simple
method for his Kiel device.  Just heat the ACS grade 85%  commercial
Phosphoric acid to get ride of the 15% water out of it. Does anyone  see any
problem with this method?  The specific gravity he is using is  1.89 to 1.90
which is similar to the method most are using.
 
 
 
WHY do we need to add P2O5 to the 85 % orthophosphoric  acid?? 
 
 
 
Thanks
 
 
 

 

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