Analytical Chemistry Chemical Cytometry Quantitates Superoxide
Analytical Chemistry Chemical Cytometry Quantitates Superoxide
Analytical Chemistry Chemical Cytometry Quantitates Superoxide
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contamination of the substances of interest (e.g., trace metals).<br />
When this strategy is used, the time needed to complete γ<br />
spectrometry before further analyses can be performed also<br />
needs to be taken into consideration.<br />
In many laboratories, the total 210 Pb concentration is determined<br />
by R spectrometry, through its daughter radionuclide<br />
210 Po in equilibrium. The technique is simple, rapid, reliable<br />
(recoveries >95%), and shows good precision. 10,11 Furthermore,<br />
although the technique is destructive, only ca. 250 mg of dry<br />
sediment is needed, and because laboratories usually have several<br />
R detectors (they are much cheaper than Ge detectors), sample<br />
throughput is much larger than with γ spectrometry. Typical<br />
counting times range from 1 to 7 days, depending on sample<br />
activity and desired uncertainty. An experimented analyst might<br />
produce a full total 210 Pb profile within a month after sample<br />
receipt (ca. 40 samples). When R spectrometry is used, the<br />
base 210 Pb can only be indirectly determined by assuming that<br />
the 226 Ra concentration is constant along the profile and<br />
therefore estimated as the average of concentrations in the<br />
profile bottom sections, as equilibrium should have been<br />
reached. 12 However, as 226 Ra may vary along the profile, this<br />
may lead to inaccurate 210 Pbex values. It is not uncommon that,<br />
once the total 210 Pb profile is known, γ spectrometry is carried<br />
out in selected sections, thus optimizing the use of this limiting<br />
resource, although because of sample size requirements this<br />
might be impracticable for many laboratories. As γ spectrometry<br />
is carried out on the untreated sample and 210 Po on a<br />
digestate, these techniques sometimes yield results which are<br />
not fully consistent.<br />
Liquid scintillation counting (LSC), mostly used for the<br />
determination of � emitters, 13,14 has also been extensively used<br />
to quantify R emitters, such as 226 Ra, in environmental samples<br />
(mainly waters). 15,16 Some of the reported methods include direct<br />
R LSC after water sample concentration, 17 226 Ra extraction from<br />
water samples with specific scintillation cocktails such as<br />
Radaex, 18 or generation of a radium-barium sulfate coprecipitate<br />
that is transformed into a soluble chloride or nitrate. 19,20<br />
Villa et al. 21 opted for this approach for sediment: the sediment<br />
is digested, and after the elimination of actinides as hydroxides,<br />
radium is recovered as Ra-Ba-SO4, dissolved in EDTA 0.2 M<br />
ammonia solution, and counted. However, most of these<br />
methods cannot be directly used with sediment digestates and/<br />
or are excessively resource-consuming.<br />
(10) Sanchez-Cabeza, J. A.; Masqué, P.; Ani-Ragolta, I. J. Radioanal. Nucl. Chem.<br />
1998, 227, 19–22.<br />
(11) Vesterbacka, P.; Ikaheimonen, T. K. Anal. Chim. Acta 2005, 545, 252–<br />
261.<br />
(12) Binford, M. W. J. Paleolimnol. 1990, 3, 253–268.<br />
(13) Pujol, L.; Sanchez-Cabeza, J. A. J. Radioanal. Nucl. Chem. 1999, 2, 391–<br />
398.<br />
(14) Liong Wee Kwong, L.; LaRosa, J. J.; Lee, S. H.; Povinec, P. P. J. Radioanal.<br />
Nucl. Chem. 2000, 248, 751–755.<br />
(15) Salonen, L. Sci. Total Environ. 1993, 130-131, 23–35.<br />
(16) Salonen, L.; Hukkanen, H. J. Radioanal. Nucl. Chem. 1997, 226, 67–74.<br />
(17) Sanchez-Cabeza, J. A.; Pujol, L. Analyst 1998, 123, 399–403.<br />
(18) Aupiais, J. Anal. Chim. Acta 2005, 532, 199–207.<br />
(19) Repinc, U.; Benedik, L. J. Radioanal. Nucl. Chem. 2002, 254, 181–185.<br />
(20) Galan-Lopez, M.; Martin-Sanchez, A.; Tosheva, Z.; Kies, A. In LSC 2005<br />
Advances in Liquid Scintillation Spectrometry; Chalupnik, S., Schoenhofer,<br />
F., Noakes, J., Eds.; Radiocarbon: Tucson, AZ, 2006; pp 165-170.<br />
(21) Villa, M.; Moreno, H. P.; Manjón, G. Radiat. Meas. 2005, 39, 543–550.<br />
6848 <strong>Analytical</strong> <strong>Chemistry</strong>, Vol. 82, No. 16, August 15, 2010<br />
After 210 Po analysis for R spectrometry, 226 Ra remains in<br />
solution. In this work, we propose, develop, and validate a new<br />
method to determine 226 Ra by 222 Rn emanation to a scintillation<br />
cocktail, which eliminates the need to perform any further<br />
purification, and counting with an ultralow background liquid<br />
scintillation system.<br />
EXPERIMENTAL SECTION<br />
Equipment. An ultralow background liquid scintillation system,<br />
Quantulus 1220 TM (Wallac, Turku, Finland), was used to<br />
carry out this work. In this system, background is reduced by<br />
an optimized combination of active and passive shields. A pulseshape<br />
analysis (PSA) circuit permits the discrimination of<br />
pulses produced by R and � radiation by comparing the area<br />
of the pulse tail after 50 ns from the start with its total area.<br />
Pulse-shape discrimination is accomplished using a software<br />
adjustable parameter (PSA parameter) which can vary between<br />
1 and 256. 16,22 Quenching (sample extinction) was quantified with<br />
the standard quenching parameter (SQP(E)) which is used to<br />
determine the counting efficiency for each sample through<br />
calibration curves. 23,24 Counting was performed with Wallac<br />
OptiScint HiSafe III, a diisopropyl naphthalene based aqueous<br />
immiscible cocktail, and low-diffusion PE counting vials (Packard<br />
BioScience).<br />
Counting Solutions. The tracer solutions were prepared by<br />
gravimetrically spiking 226 Ra/2 M HNO3 (NIST, SRM4967,<br />
U.S.A.) into known amounts of deionized water contained in<br />
20 mL low-diffusion PE counting vials. OptiScint HiSafe was<br />
then added to reach a total admixture volume of 20 mL. These<br />
were stored for 3 weeks in a dark temperature-controlled area<br />
to allow in-growth and equilibrium of the radioactive progenies.<br />
The background solutions, used for calibration purposes, were<br />
prepared with 10 mL of deionized water, acidified to match<br />
the standard solutions, to which 10 mL of the scintillation<br />
cocktail was added. In all cases, quenching was changed by<br />
adding different amounts of CCl 4, ranging from 0 to 200 µL.<br />
All reagents used in the experiments were of analytical grade<br />
(Fisher Scientific).<br />
RESULTS<br />
When counting a 226 Ra aqueous solution with an immiscible<br />
scintillant (such as OptiScint Hisafe), the R emitter 226 Ra decays<br />
to the R emitter 222 Rn (T1/2 ) 3.8332 ± 0.0008 days). Radon is<br />
highly soluble in oil-based scintillators and is selectively<br />
extracted in the cocktail, suffering some decay while this<br />
process takes place. Once solubilized in the organic phase,<br />
222 Rn decays to the R emitter 218 Po (T1/2 ) 3.094 ± 0.006 min),<br />
this mainly decays to the � emitter 214 Pb (T1/2 ) 26.8 ± 9 min),<br />
which decays to the � emitter 214 Bi (T1/2 ) 19.9 ± 0.4 min),<br />
which mainly decays to the R emitter 214 Po (T1/2 ) 162.3 ± 1.2<br />
µs), and this one to 210 Pb (T1/2 ) 22.23 ± 0.12 years). Therefore,<br />
in the scintillant, and after an appropriate equilibration time<br />
(usually set to about 3 weeks), the R emitters 222 Rn, 218 Pb, and<br />
214 Pb are in secular equilibrium (Figure 1). As the probability<br />
of these R decays is in all cases close to one, the maximum<br />
(22) Kaihola, L. J. Radioanal. Nucl. Chem. 2000, 243, 313–317.<br />
(23) Villa, M.; Manjon, G.; Garcia-Leon, M. Nucl. Instrum. Methods Phys. Res.,<br />
Sect. A 2003, 496 (2-3), 413–424.<br />
(24) Sanchez-Cabeza, J. A.; Pujol, L. Health Phys. 1995, 68 (5), 674–82.