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Stable Isotope Geochemistry

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Date:
Thu, 6 Jun 1996 18:12:40 -0400
From:
"Tyler B Coplen II, Research Chemist, Reston, VA "<[log in to unmask]> (Tyler Coplen)
Subject:
H/D ring test
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Dear Participants to Willi Brand's H2 Ring Test,

In an attempt to study linerity of hydrogen 
isotope-ratio mass spectrometers and improve the 
comparibility of hydrogen isotopic data among 
laboratories, Willi proposed that gaseous 
hydrogen reference materials be prepared and 
distributed to interested laboratories.  He 
encouraged Messer Griesheim, a gas manufacturer 
in Germany, to support this program, and about 
50 laboratories have agreed to participate.

Before these reference materials are distributed 
it is important to determine that they are 
isotopically homogeneous.  I agreed to perform 
this task.  We received 7 each of the three 
different gases on May 24.  Below are the results 
of the investigation.

The isotopic composition of the gases are 
approximately:
   Gas A     0 per mill
   Gas B  -400 per mill
   Gas C  -700 per mill
The label says that the Gas Range is 0 (or 
-400 or -700) v.s.SMOW  (I would have chosen VSMOW, 
but that's a discussion for another day).  Please 
note that the key word here is "Range."  These 
values are only approximate and should be 
determined by the 50 laboratories to the best of 
their ability.  Forms are provided with the gases 
for reporting isotopic results to Willi.

Each gas is provided in a light weight, thin-walled 
aluminum tank with a volume of 1 liter.  One valve 
is provided for three tanks.  Gas pressure is about 
12 bars.

The aluminum tanks and valve were easy to use.  
Users should be advised that there is no need to
purge the valve as suggested on the side of each
tank if one conscientiously evacuates the dead 
volume prior to sampling.

Users are advised to place a valve as close as 
possible to the valve on the tank in order to 
minimize the amount of gas that is extracted from 
a tank and expanded into their mass spectrometer.  
To help minimize the amount of hydrogen extracted, 
I put solid glass rod inside of my 1/4 inch tubing 
to minimize internal volume.  I replaced the 1/4 
inch Swaglok stainless steel front ferrule on the 
valve outlet with a Teflon ferrule.  Teflon provides 
leaktight service for repeated connections.

We have checked each tank for contamination by 
comparing the ion gauge reading of the sample 
with that of the working standard.  We have seen
no measureable contamination--detection level is
about 2 percent.

We recorded the pressure of the gas taken from 
each tank.  To my surprise, they are not the 
same.  At least two of the tanks I received were 
leaking hydrogen through the tank closure device 
(similar to the top of a conventional spray can).  
One of these (Gas A, tank 2) had dropped in 
pressure from about 12 bars initially to 9 bars 
by the time we analyzed it on May 30.  Gas C, 
tank 1, was leaking slightly when I received it, 
but the leak was not sufficient to affect its 
isotopic composition (see results below).

Users can identify tanks that have (or are) 
leaking in two ways.  The first is by measuring 
the pressure of gas in the tank when the tank 
arrives by using the gauge on the valve 
provided.  If the pressure is less than 10 bars, 
then the tank may have leaked and the user might 
want to consider obtaining a replacement.  Second, 
it will be impossible to obtain an excellent 
vacuum when pumping on a leaking tank.

The isotopic results follow.

Tank Pressure   Delta H-2 (relative to mean)
 #    bars      standard deviations are 1 sigma
              
Gas A
 1    12.2    +0.1 ± 0.3  6 analyses on 3 aliquots
 2     9.0    +0.8 ± 0.4  4 analyses on 2 aliquots
 3    11.8    +0.1 ± 0.4  4 analyses on 2 aliquots
 4    10.9    -0.2 ± 0.4  4 analyses on 2 aliquots
 5    12.5     0.0 ± 0.4  4 analyses on 2 aliquots
 6    13.1    +0.2 ± 0.3  8 analyses on 2 aliquots
 7    13.1    -0.2 ± 0.3  4 analyses on 2 aliquots
Mean (excluding Tank 2)  0.0


Tank Pressure   Delta H-2 (relative to mean)
 #    bars      standard deviations are 1 sigma

Gas B
 1    12.9    +0.1 ± 0.6  5 analyses on 3 aliquots
 2    12.1    -0.4 ± 0.4  4 analyses on 2 aliquots
 3    12.1    -0.1 ± 0.5  4 analyses on 2 aliquots
 4    12.9    +0.3 ± 0.7  4 analyses on 2 aliquots
 5    12.7    -0.4 ± 0.6  4 analyses on 2 aliquots
 6    12.6    -0.4 ± 0.6  3 analyses on 2 aliquots
 7    13.1    +0.6 ± 0.3  5 analyses on 2 aliquots
Mean (of all 7 tanks)   0.0 


Tank Pressure   Delta H-2 (relative to mean)
 #    bars      standard deviations are 1 sigma

Gas C
 1    13.0    +0.1 ± 0.7  10 analyses on 3 aliquots
 2    13.0    -0.1 ± 0.4  4 analyses on 2 aliquots
 3    12.2    +0.2 ± 0.9  4 analyses on 2 aliquots
 4    13.2    +0.2 ± 0.9  4 analyses on 2 aliquots
 5    13.2    -0.3 ± 0.5  4 analyses on 2 aliquots
 6    13.2     0.0 ± 0.9  4 analyses on 2 aliquots
 7    13.2    +0.1 ± 0.2  4 analyses on 2 aliquots
Mean (of all 7 tanks)   0.0 

Of the tanks of Gas A hydrogen, Tank 2 is the most 
enriched in H-2 and is statistically different than 
the other 6--it lies outside (but just barely) the 
mean plus 2 sigma standard deviation.  Evidently 
H-1 leaks out faster than H-2, even though the 
pressure is relativey high.  The remaining 6 tanks 
of Gas A are statistically identical.

All 7 tanks of Gases B are statistically 
identical within our measurement accuracy.

All 7 tanks of Gases C are statistically 
identical within our measurement accuracy.

>From these results my conclusion is that Messer 
Griesheim has succeeded in producing three very 
useful and desirable isotopically homogeneous 
gaseous reference materials.  I suspect that 
these gases will be extremely useful over time 
to the laboratories that have or are able to 
purchase them.

When analyzing these gases, you may want to confirm 
that your H3+ contribution coefficient is correct in 
your software.  An easy way to do this is employ a 
working standard and sample with greatly different 
isotopic composition.  For example, you might analyze 
Gas C versus Gas A.  Measure the delta valve with 
sample and standard voltages matched.  Next, increase 
the sample voltage by 50%.  Analyze again. The delta 
values should be identical within experimental error.  
If not, see Isotope Geoscience, v. 72, p. 293-297, 
1988, (Equation 18), for an algorithm to calculate 
the "correct" delta value.

Good Luck with your measurements,

Tyler B. Coplen
U.S. Geological Survey
431 National Center
Reston, VA  22092
Tel:  703-648-5862
Fax:  703-648-5274
E-mail: [log in to unmask]


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