How to use nucfilms Ra adsorbing sheets
Warning
: The method described is recommended only for untreated waters having drinking
water quality. For waste waters, for acid leachates and also for some
intercomparison samples (barium spiked)
the method may be used, but requires special precaution.
Nucfilms Ra adsorbing sheets are polyamide sheets covered on both sides
with a thin MnO
2
film.
Sampling
There is no need to acidify waters having drinking water quality. Simply avoid
glass containers.
Use polyethylene bottles and fill them completely. If you are scared about
precipitation, you may
add up to 1g Na
2
-EDTA(Titriplex III) / liter.
Exposition to the water sample
Fill 100 ml of your untreated water sample into a 100 ml FEP beaker. Don't use
glass beakers.
FEP (Fluor-Ethylene-Propylene) showed negligible adsorption. If your sample has
been acidified
rise pH with NaOH to to 5 to 7. Below pH 4.5 adsorption efficiency sharply
decreases.
To highly mineralised (g/liter) or sparkling samples add some 30 mg Na
2
-EDTA (Titriplex III) / 80 ml to avoid precipitation during exposition.
Up to 100 mg Na
2
-EDTA / 80 ml showed
no noticeable effect on adsorption efficiency. For waters having a very low
mineralization (conductivity below 100 micro-Siemens/cm) it is recommended to
add NaHCO
3
to complex the uranyl ion (300 mg HCO
3
/l). If not you risk to have uncomplexed uranyl cations adsorbing on the MnO
2
films.
Rinse the sheet with distilled or deionized water and carefully wipe it dry
with a soft paper (e.g. Cleenex).
Fix the sheet with a stainless steel clamp in your sample as shown
in the
figure
. Stir at approx. 200 rpm using a teflon covered stirring rod.
After 6 h remove the sheet
from your sample, rinse it with distilled or deionized water and dry it with
not too hot air (hair drier).
For some samples containing high CO
2
concentrations
gas bubbles may form on the film surface. In this case just lift the sheet
shortly out of the sample and put it back.
This removes the bubbles. This prodcedure may be necessary several times during
the first hour of exposition.
It is not known if these bubbles have an effect on adsorption.
Any data are welcome
.
Measurement
It is recommended to measure both sides of the sheet. In general the side that
has been exposed towards
the flow ("upstream") holds some 20% more activity than the
"downstream" side.
With the sheet at a distance of about 10 mm from the surface of a 900 mm
2
alpha detector you have a detection efficiency around 20% .
Summing up the counts from both sides and assuming a 100% adsorption efficiency
1 count/1000s thus corresponds to around 65 mBq/l in your sample.
Adsorption efficiency and calibration
Barium at mg/l concentrations, Sr at some 10 mg/l and U at Bq/l levels are
known to reduce adsorption
efficiency for radium considerably. Apart from U in some mineral waters these
levels are not found in
drinking waters. For drinking waters you thus can expect to have adsorption
efficiencies > 80% for
20 mm x 20 mm sheets exposed as given above. To verify adsorption efficiency
you can expose successively
several sheets in the same 80 ml sample. Assuming that every sheet takes up the
same fraction of the radium
that remained in the sample, adsorption efficiency will be 1- (Ra activity on
sheet n+1)/(Ra activity on sheet n).
Radium standard solutions have to be essentially free from barium (<<
1mg/l). NPL (GB) sells a radium
standard having very low barium. A 1 Bq/l solution prepared from the original
200 Bq/ml acid solution by simply
diluting it (in 3 steps) with deionized water showed a 93% to 95% adsorption
efficiency.
I
nterferences from
234
U
MnO
2
generally adsorbs radium considerably
stronger than uranium. In drinking waters having a pH above 6 uranium
adsorption showed to be at least
an order of magnitude lower than radium adsorption. However in some initially
strongly acid uranium ore
leachates (with the pH risen by NaOH to around 4.5 for the measurement) radium
adsorption may be very
low, even below 10%, with a uranium adsorption of the same order of magnitude.
In most cases energy resolution will not be sufficient to distinguish between
226
Ra
lines and
234
U lines. This may lead to an overestimate
of the
226
Ra concentration. To solve this problem one
can assume as a first approximation that
238
U
and
234
U are in equilibrium. The amount
of
238
U adsorbed can be determined without
interference problems and then be used to correct for the
234
U contribution. However
238
U and
234
U are rarely in perfect equilibrium in natural water samples.
Although
234
U/
238
U ratios mostly are in the range of 0.8 to 1.3 values up to 3 have been
reported. In some cases it thus may be necessary to determine the
2
34
U/
238
U ratio by a
different method, e.g. by liquid scintillation alpha spectrometry (PERALS) or
by adsorption on U-selective thin films.
Bad samples
Unfortunately some organisers of intercomparison exercises only feel good if
their samples are acidified
down to pH 1 and they like to use barium rich radium standards.These samples
are hard to bring to a pH of 5 without
precipitation. Adding some
g/l Na
2
EDTA may help, but radium adsorption efficiency
is generally bad, even below 10%. In this case it does not help much to expose
several sheets. The only
solution is to add some barium-free radium tracer after the first exposition
and then to expose a second sheet.
From the counts difference between the first and the second sheet and the known
added activity one then can
calculate the efficiency.
October 15, 2004 Heinz Surbeck