A TER. Observation of Xe with the PNNL ARSA System PNNL UC-7 13

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PNNL-11654 UC-7 13 135 Observation of Xe with the PNNL ARSA System P.L. Reeder, T.W. Bowyer, K.H. Abel, C.W. Hubbard, M.E. Panisko, R.C. Thompson, R.A. Warner August 1997 Prepared for the US. Department of Energy Under Contract DE-ACO6-76RLO 1830 Pacific Northwest National Laboratory Richland, Washington 99352 A TER

DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, mommendktion, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof.

DISC LA1 M ER Portions of this document may be illegible electronic image products. Images are produced from the best available original document.

SUMMARY The automated radioxenon sampler-analyzer (ARSA) developed by PNNL and with funding and support form the DOE NN-20 CTBT research and development program, observed 9.1-hr 135Xe in a sample of New York City air obtained on April 4th, 1997. The report below briefly describes the ARSA system and the first ever reported measurement of the short-lived 135Xe isotope fiom an automated radioxenon system. a... 111

Contents SUMMARY... Introduction... *. Beta-Gamma Comcidence Data... References........ 111 1 1.5 Figures Figure 1. Xe sample obtained fiom New York City air on April 2,1997 showing '35Xe peak (channel 304) in addition to '33Xepeaks (channels 39 and 102). Top curve is ungated spectrum. Bottom curve is beta-gated spectrum. Both curves are sum of left and right NaI crystals... 4 Figure 2. Background spectra (sum of both gamma detectors) or cell 3. Top curve is ungated spectrum. Bottom curve is beta-gated spectrum. Note residual peaks from prior samples of '33Xeand absence of '35Xepeak in beta-gated spectrum... 4 iv

Introduction The ARSA system is an autonomous radioxenon sampler-analyzer capable of measuring the radioxenon content of the air several times per day, storing the sample, and automatically sending the data to an appropriate data center'. Currently, the ARSA is undergoing field-testing at the Environmental Measurements Laboratory (EML) for fbture use as part of an International Monitoring System (IMS) for the Comprehensive Nuclear test Ban Treaty (CTBT). The ARSA automatically samples air continuously and measures the radioxenon component of the gas very soon after the sample has been purified. The rapid collection and analysis (nuclear counting begins about 10 hrs after the sample has been collected) of the samples allows for measurement of the shorter-lived radioxenon species that may be present in measurable levels near nuclear power plants or after a nuclear detonation. The nuclear counting system employed in the ARSA is a beta-gamma coincidence spectrometer developed at PWNL and is described in detail elsewhere*. Even though '33Xeand 135Xeactivity levels near our testing site in New York City are expected3to be detectable, '35Xeactivity levels from an automated xenon sampleranalyzer have never been reported. This may be due to the fact the short half-life of the isotope previously made it impossible for either automated or manual systems to collect and start analysis of the sample quickly enough to measure it. Also, other than the ARSA, there are no operating fully automated xenon samplers reported in the open literature. During routine testing of the ARSA at EML, located in New York City, we observed a detectable signal from '35Xe. Beta-Gamma Coincidence Data The beta-gamma coincidence spectrometer used in the ARSA2produces a pair of beta-gated gamma-ray energy spectra'three times per day from its dual crystal NaI(T1)based spectrometer. Gamma spectra for the sum of the left and right NaI crystals for this sample are shown in figure 1 for April 4" 1997. The beta-gated gamma spectrum clearly shows the expected two peaks from '33Xeat 31 kev and 81 kev. The peak centered at channel 304 corresponds to an energy of 25W3 kev in close agreement with the known peak from '35Xeat 249.8 kev. The ARSA system allows gamma spectra to be gated by a window on lowamplitude beta pulses as well as by all beta pulses. The spectra gated by the lowamplitude beta pulses are enhanced in '33Xerelative to background events which tend to have large amplitude beta pulses. The beta spectrum associated with the 249.8 kev peak has an endpoint energy of 900 kev which is much greater than the endpoint energy of 346 kev for the beta spectrum from 133Xe.The relative abundance of the 250-keV peak in the spectrum gated by low-amplitude betas was compared to its relative abundance in 1

the spectrum gated by all betas. The 250-keV peak was found to be enhanced in the spectrum gated by high-amplitude beta pulses which is consistent with its assignment to 13%e. The concentrations of '33Xeand '35Xewere calculated based on the current best estimates of various efficiency factors. The counts in a given peak were determined as the net area under a peak after correcting for tails above and below the peak in the betagated spectra for the sum of the two NaI crystals. The concentrationswere calculated by dividing the net counts by the following factors and are reported in units of millibecquerels per cubic meter of air (mbq/m3). For the 31-ke V ueak (assumed to be entirelv due to 133Xe): = 5504 Net counts Counting time Beta efficiency (3 1) Gamma eff. (31) Abundance (3 1) Chemical yield Vol. of air sample = 0.75 = 0.64 = 0.4894 Concentration '33Xe = 32.1 = 58,560 s = 0.5 (estimate) = 25 m3 mbq/m3 For the 8I -kev Deak - 133Xe: Net counts = 3487 = 58,560 s Counting time Beta efficiency (81) = 0.50 Gamma eff. (81) = 0.80 Abundance (8 1) = 0.37 Chemical yield = 0.5 (estimate) = 25 m3 Vol. of air sample Concentration '33Xe = 32.2 mbq/m3 For the 250-keV ueak - 135Xe: Net counts = 459 = 58,560 s Counting time Beta efficiency (250) = 0.75 (estimate) = 0.80 (estimate) Gamma eff. (250) = 0.90 Abundance (250) = 0.5 (estimate) Chemical yield = 25 m3 Vol. of air sample (Concentration 13'Xe = 1.16 mbq/m3) 2

Because of the 9.1 -hr half-life '35Xe, the concentration of 135Xe must be corrected for decay during the 16.3-hr counting time. Dividing by the correction factor, (l-e-)'3/ht = 0.573, gives 2.03 mbq/m3 at the beginning of the counting period. An additional correction (e-" = 0.543) is needed for decay of the sample between the end of collection and the beginning of the count (8 hr). At the end of the sample collection, the concentration of '35Xe was 3.7 mbq/m3. The equivalent decay corrections for 133Xe are much smaller (~5%) and have not been applied here. If the observed Xe fission products are produced by leaks fiom an operating nuclear reactor, one might expect that the relative amounts of '33Xe and '35Xe are given by their respective cumulative fission yields, but due mainly to burnup of '35Xe, one would expect4 the '35Xe level to be somewhat lower. Assuming a thermal or fission spectrum neutron fission of 235U, the cumulative fission yields, and normal burn-up of '35Xe in a pressurized water reactor (PWR) in equilibrium, the expected ratio '35Xe/'33Xe at t=o is 0.37. The experimentally observed ratio of 135Xe/'33Xe = 3.7/32 = 0.12 implies that the '35Xe has decayed by about 1.4 half-lives while traveling from the source to the sampling station. Other complications such as hold-up at the source after release or variable concentrations during the 8-hr sampling period were not considered here. Figure 2 is an example of background gamma spectra taken during the 24 hours prior to the sample shown in figure 1. Note that the background does show some residual 133Xe fiom previous samples in the cell. Tests at PNNL have shown that about 5% of a Xe sample remains in the cell after pumping the cell to remove the sample. However, note that there is no evidence of a background peak in the vicinity of the 250-keV peak fiom '35Xe. 3

Left+Right Nal"0403970025.sarn-4.CG 10000 1000 E? 5 0 100 0 10 I 0 50 100 150 200 250 300 350 400 450 500 Channel Number Figure 1. Xe sample obtained from New York City air on April 2,1997 showing I3'Xe peak (channel 304) in addition to '33Xepeaks (channels 39 and 102). Top curve is ungated spectrum. Bottom curve is beta-gated spectrum. Both curves are sum of left and right NaI crystals. Left + Right Nal"O402970001.BKG-XCG" 10000 1000 100 10 1 I 0 50 100 150 200 250 300 350 400 450 500 Channel No. Figure 2. Background spectra (sum of both gamma detectors) for cell 3. Top curve is ungated spectrum. Bottom curve is beta-gated spectrum. Note residual peaks from prior samples of '33Xeand absence of 13'Xe peak in beta-gated spectrum. 4

References Automatic Radioxenon Analyzer for CTBT Monitoring, T.W Bowyer, K.H Abel, W.K. Hensley, C.W. Hubbard, A.D. McKinnon, M.E. Panisko, R.W. Perkins, P.L. Reeder, R.C. Thompson, RA. Warner, PNNL-11424, December, 1996. Beta-Gamma Counting System for Xe Fission Products, P.L. Reeder, T.W Bowyer, R.W. Perkins, Int. Conf. Meth. and Appl. Of Radioanal. Chem., Kailua-Kona, HI, April 6-1 1,1997, to be published in J. Radioanal. Chem. Ambient 33XeLevels in the Northeast U.S.,T.W Bowyer, K.H Abel, W.K. Hensley, M.E. Panisko, R.W. Perkins, PNNL-SA-27197, 1996, and in print, J. of Enivron. Radioac. Fission and Activation Products in Nuclear Reactor Fuels and Nuclear Explosion Debris, RW Perkins, U.P Jenquin, PNNL- 11554, April 1997. 5