3
Radioactivity 6- Radiochemistry The Counting Room: SpecialEdition Robert C. McFarland Analytics, Inc. programs. 1General coincidence summingproblems and specific coincidence summing problems encoun- teredwhen measuring these two radionuclides on fil- ter papers werediscussed in the lastissue? In order to perform accurate measurements of 134CS and 60Co in liquid samples usingMarinelli beakers, coin- cidence summing effects shouldbe investigated. Liquid samples of 134Cs and 60Co were prepared in Marinelli beakers and measured by germanium gamma-ray spectroscopy using the efficiency curve from the coincidence-free standards. The measured activity of 134Cs using the 605-keV gamma raywas only 85% of the knownvalue. Obviously, coinci- dence summing correction factorsmustbe known in orderto accurately determine the activity of 134CS in unknownliquid samples in Marinelli beakers. As with the filter-papergeometry discussed in the last issue, coincidence summingcorrection factorswill probably be differentfor each detector. The measured activityof 6° Co in the Marinelli- beaker sample was 96%of the knownvaluewhenus- ing the 1173-keVgamma ray. The 1332-keVgamma raywasnot used because it would have requiredan extrapolation of 220 keYpast the highest energy point on the coincidence-free efficiency curve. Turning from the measurement process to the calibration process, the coincidence-free standards described above sufferfrom two major deficiencies. First,the energy range is restricted by the highest en- ergy gamma ray (1115.5 keY). Second, someof the components have relatively shorthalf-lives. Several remedies to these deficiencies have been used but nis article discusses some of the coincidence summing problems encountered when measuring aqueous samples in Marinelli beakers using germanium gamma-ray spec- troscopy. Determination of the coincident gamma- ray radionuclides 134CS and 60Co is discussed. Cali- brations with the coincident gamma-ray radio- nuclides 88y,60Co,133Ba,152Eu, and 154Eu are com- pared to essentiallycoincidence-free calibrations. For these measurements,standards were pre- pared by adding 500:t 2 mL ofa liquid of known ra- dionuclide concentration to 500-mL, plastic Ma- rinelli beakersof the type described in ANSI/IEEE Std 680-1978. Gamma-ray measurementswere per- formed using a 19.4%, 84-cm3, p-type, closed coax- ial, intrinsic germanium detector. Essentiallycoinci- dence-free standards for this particular detector/ geometry combination were prepared using 241 Am (59.5 keV), 109Cd (88 keV), 57CO (122 keV), 139Ce (165.9 keV), 203Hg (279.2 keV), 113Sn (391.7 keV), 137Cs (661.6 keV), 58CO (810 keV), 54Mn (834.8 keV), and 65Zn(1115.5 keV). Decay data used in this work was obtained from NIST or NCRP Report 58. The counting efficiency vs gamma-ray-energy data was fit to a 5th order polynomial with a maximum devia- tion of 3%. This curve fit was considered adequate for demonstrating the magnitude of the coincidence summing effects in measurements with Marinelli beakers. Two coincident gamma-ray radionuclides, 134Cs and 60Co, are environmentally important as well as convenient for use in interlaboratory, cross-check 72 Reprint of "From the Counting Room", Vol. 2, No.3, 1991

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Radioactivity 6- Radiochemistry

The Counting Room: Special Edition

Robert C. McFarlandAnalytics, Inc.

programs. 1 General coincidence summing problems

and specific coincidence summing problems encoun-tered when measuring these two radionuclides on fil-ter papers were discussed in the last issue? In orderto perform accurate measurements of 134CS and60Co in liquid samples using Marinelli beakers, coin-cidence summing effects should be investigated.

Liquid samples of 134Cs and 60Co were preparedin Marinelli beakers and measured by germaniumgamma-ray spectroscopy using the efficiency curvefrom the coincidence-free standards. The measuredactivity of 134Cs using the 605-keV gamma ray wasonly 85% of the known value. Obviously, coinci-dence summing correction factors must be known inorder to accurately determine the activity of 134CS inunknown liquid samples in Marinelli beakers. Aswith the filter-paper geometry discussed in the lastissue, coincidence summing correction factors willprobably be different for each detector.

The measured activity of 6° Co in the Marinelli-

beaker sample was 96% of the known value when us-ing the 1173-keVgamma ray. The 1332-keVgammaray was not used because it would have required anextrapolation of 220 keY past the highest energypoint on the coincidence-free efficiency curve.

Turning from the measurement process to thecalibration process, the coincidence-free standardsdescribed above suffer from two major deficiencies.First, the energy range is restricted by the highest en-ergy gamma ray (1115.5 keY). Second, some of thecomponents have relatively short half-lives. Severalremedies to these deficiencies have been used but

nis article discusses some of the coincidencesumming problems encountered whenmeasuring aqueous samples in Marinellibeakers using germanium gamma-ray spec-

troscopy. Determination of the coincident gamma-ray radionuclides 134CS and 60Co is discussed. Cali-brations with the coincident gamma-ray radio-nuclides 88y, 60Co, 133Ba,152Eu, and 154Eu are com-pared to essentially coincidence-free calibrations.

For these measurements, standards were pre-pared by adding 500:t 2 mL ofa liquid of known ra-dionuclide concentration to 500-mL, plastic Ma-rinelli beakers of the type described in ANSI/IEEEStd 680-1978. Gamma-ray measurements were per-formed using a 19.4%, 84-cm3, p-type, closed coax-ial, intrinsic germanium detector. Essentially coinci-dence-free standards for this particular detector/geometry combination were prepared using 241 Am

(59.5 keV), 109Cd (88 keV), 57CO (122 keV), 139Ce(165.9 keV), 203Hg (279.2 keV), 113Sn (391.7 keV),137Cs (661.6 keV), 58CO (810 keV), 54Mn (834.8 keV),and 65Zn (1115.5 keV). Decay data used in this workwas obtained from NIST or NCRP Report 58. Thecounting efficiency vs gamma-ray-energy data wasfit to a 5th order polynomial with a maximum devia-tion of 3%. This curve fit was considered adequatefor demonstrating the magnitude of the coincidencesumming effects in measurements with Marinellibeakers.

Two coincident gamma-ray radionuclides, 134Csand 60Co, are environmentally important as well asconvenient for use in interlaboratory, cross-check

72 Reprint of "From the Counting Room", Vol. 2, No.3, 1991

"Coincidence Summing Considerations When Using Marinelli-Beaker Geometries in Germanium Gamma-Ray Spectroscopy"

Robert C. McFarland

~rc-"c,"--a"031]0"

-SC

~o0

"'r

Effects of coincidence summing in the 154Eu Marinelli-

beaker standard.

Figure 1

they involve radionuclides with potential coinci-dence summing problems.

The coincident gamma-ray radionuclides 60Co,88y, 133Ba, 152Eu, and 154Eu have been used in variouscombinations to extend the energy range or the use-fullife of gamma-ray calibration standards. Whenusing calibration standards containing any of theseradionuclides in high-efficiency counting situations,coincidence summing problems should be assessed.

Marinelli-beaker standards, with known activi-ties of the five, coincident gamma-ray radionuclides,were measured by germanium gamma-ray spectros-copy using the coincidence-free efficiency curve. Asdiscussed above, the measured value for 60Co(1173 keY) was 96% of the known value. Examina-tion of the decay scheme for 60CO indicates that thee~ected coincidence summing correction for the1332-keV gamma ray is approximately equal to thecoincidence summing correction for the 1173-keVgamma ray. For this detector both the 1173-keV and1332-keV gamma rays from 60CO require a 4-5% cor-rection for coincidence summing.

The measured value for 88y using the 898-keVgamma ray was 98% of the known value. The 1836-keY gamma ray was not used due, again, to the largeextrapolation. Examination of the decay scheme for88y indicates that the coincidence summing correc-tion for the 1836-keV gamma ray should be of thesame order of magnitude as for the 898-keV gammaray. The coincidence summing corrections for boththe 898-keV and 1836-keV gamma rays for this detec-tor/geometry combination are on the order of a few

percent.Figure 1 shows the ratio of measured-to-known

values determined from the 154Eu Marinelli-beakerstandard. The following gamma rays were used:123.1 keY, 247.7 keY, 591.8 keY, 723.3 keY,873.2 keY, 996.3 keY, 1004.7 keY, and 1274.5 keY.The results in Figure 1 emphasize the fact that the co-incidence summing factor varies for each gamma-ray transition. The results also show that in order touse 154Eu for calibration in the Marinelli-beaker ge-ometry, coincidence summing corrections-some aslarge as 17%-must be applied.

The ratios of measured-to-known values, deter-mined from eight gamma rays of 152Eu, are shown inFigure 2. Gamma rays at 121.8 keY; 244.7 keY;

344.3 keY; 444 keY; 778.9 keY; 964.1 keY;1085.9 keY, and 1112.1 keVwere used. These resultsshow that coincidence summing corrections must beapplied in order to use 152Eu for accurate calibra-tions in the Marinelli-beaker geometry.

Five gamma rays from 133Ba (81 keY, 276.3 keY,302.7 keY, 355.9 keY, and 383.7 keY) were measuredto obtain the results in Figure 3. These results showthat 133Ba also requires coincidence summing correc-tions in the Marinelli-beaker geometry. Even thoughthe 383.7-keV efficiency is very close to the coinci-dence-free curve in this case, the coincidence sum-ming correction for that gamma-ray line should al-ways be investigated carefully as there is a "summingin" contribution.3

The measured values presented here apply onlyto this particular detector and beaker and are pre-sented only to indicate the order of magnitude of co-incidence summing problems. More efficient detec-tors might be expected to have larger coincidencesumming problems. Also, extended-range detectorswith higher efficiency in the low-energy (less than60 keY) range would be expected to have differentcoincidence summing characteristics due to the in-creased probability of x-ray/gamma-ray coincidence

summIng.What can be done about coincidence summing

problems in the Marinelli-beaker geometry? The

Reprint of "From the CountinR Room", Vol. 2, No.3, 1991 73

Radioactivity &- Radiochemistry

The Counting Room: Special Edition

-!f-

A

j~OO;Enerqy (ke\

Figure 2 Effects of coincidence summing in the 152Eu Marinelli-

beaker standard.

Figure 3 Effects of coincidence summing in the 133Ba Marinelli-

beaker standard.

measured in-house using counting geometries whichminimize coincidence summing. Aliquots can betransferred gravimetrically to Marinelli beakers andthe coincidence summing correction factors derived.The alternative, accurate determination of the coinci-dence summing correction factors in the primarycalibration standards, is a more complicated process.In the future, calculational procedures may provevaluable if the characteristics of each germanium de-tector can be accurately determined.4

ideal but generally impractical scheme would be tocalibrate with certified standards of each radionu-clide to be measured and use radionuclide-specificefficiencies, not efficiency curves. Another approachwould be to calibrate with coincidence-free radionu-clides and measure coincidence summing correc-tions with known (not necessarily certified) solu-tions of the coincident gamma-ray radionuclides tobe measured. If these two schemes are not practical,efficiency calibrations can be performed with coinci-dent gamma-ray radionuclides. Obviously, if the co-incidence summing correction is known to be smallcompared to the acceptable uncertainty in a meas-urement, it can be ignored. Relatively small coinci-dence summing correction factors can be roughly es-timated without adding significantly to theuncertainty in measurements. If calibrations are per-formed with coincident gamma-ray radionuclidesknown to have large (10-20%) coincidence sum-ming effects, accurate corrections must be per-formed to obtain accurate measurements.

The easiest approach appears to be to calibratewith standards having little or no coincidence sum-ming and either estimate the correction factors orneglect them and increase the uncertainty in the fi-nal measurements. Correction factors for radionu-clides being measured (e.g., 134CS) can be directly de-termined. For this procedure solutions can be

References1. D.H. Gray, D.B. Golas, J.M. Calhoun, "Review of the USCWNIST

Measurement Assurance Program for the Nuclear Power Indus-

try," Radioact Radiochem., 2 (1), 30-41, (1991).

2. R.c. McFarland, "Coincidence Summing Considerations in the

Measurement of Radionuclides on Filter Paper Using Germa-

nium Gamma-Ray Spectroscopy," Radioact Radiochem., 2 (2),

6-9,(1991).

3. FJ. Schima, D.O. Hoppes, "Tables for Cascade-Summing Correc-

tions in Gamma-Ray Spectrometry," Appl. Radiat Isot, 34 (8),

1109-1114, (1983).

4. K. Sinkko, H. Aaltonen, "Calculation of the True Coincidence Sum-

ming Correction for Different Sample Geometries in Gamma-

Ray Spectroscopy," Finnish Centre for Radiation and Nuclear

Safety, Report No. STUK-B-Valo 40, Helsinki, (1985). R&R .74 Reprint of "From the Counting Room", Vol. 2, No.3, 1991