|Year : 2019 | Volume
| Issue : 1 | Page : 5-9
A comparative study for 235U radioactivity concentration calculation methods in phosphate samples
A Salman1, Z Ahmed2, Kh A Allam3, S El-Sharkawy1
1 Department of Physics, Faculty of Science, Sohag University, Sohag, Egypt
2 Department of Safeguards, Egyptian Nuclear and Radiological Regulatory Authority, Nasr City, Cairo, Egypt
3 Department of Nuclear Law, Egyptian Nuclear and Radiological Regulatory Authority, Nasr City, Cairo, Egypt
|Date of Submission||17-Dec-2018|
|Date of Decision||18-Feb-2019|
|Date of Acceptance||19-Feb-2019|
|Date of Web Publication||3-Jun-2019|
Department of Physics, Faculty of Science, Sohag University, Sohag,
Source of Support: None, Conflict of Interest: None
In this study, a comparison is made between the selection of the most proper and accurate methods for 235U activity determination according to the available conditions with the smallest error possible. The detection of 235U activity is used to determine the mass of the 235U in the samples and consecutively, the uranium enrichment which is important for the nuclear safeguards' needs and the monitoring of the radionuclides in the environment. Various methods have been studied to distinguish between counting rate contributions from both235U and 226Ra to the 186 keV energy region in samples of uranium in natural form.
Keywords: 235U activity, activity ratios, gamma-ray spectrometry, phosphate samples
|How to cite this article:|
Salman A, Ahmed Z, Allam KA, El-Sharkawy S. A comparative study for 235U radioactivity concentration calculation methods in phosphate samples. Radiat Prot Environ 2019;42:5-9
|How to cite this URL:|
Salman A, Ahmed Z, Allam KA, El-Sharkawy S. A comparative study for 235U radioactivity concentration calculation methods in phosphate samples. Radiat Prot Environ [serial online] 2019 [cited 2019 Oct 18];42:5-9. Available from: http://www.rpe.org.in/text.asp?2019/42/1/5/259674
| Introduction|| |
The validation of the gamma nondestructive assay technique to quantify the radioactivity of the uranium radioisotopes and to derive a reliable estimation of their isotopic activity ratios (ARs) in samples containing measurable uranium concentrations has become easier, especially after the advent of high-resolution gamma-ray spectrometric techniques.
Furthermore, these measurements are convenient because they generally require less time and cost in comparison with the destructive radioanalytical methods such as α-spectrometry or mass spectrometry. This technique is proper in cases where the measured items are sealed or products that cannot be opened or sampled.
The gamma spectroscopic determination of 238U/235U AR has been used as an indication of the presence of depleted uranium (DU) in the environment where it is well known that naturally occurring uranium has a constant238U/235U AR of 21.7.
Hyper-pure germanium (HpGe) detectors are widely used for gamma spectrometry measurements. They have special features over other detectors due to their high characteristic resolution. In a few cases, some of the gamma rays emitted by one isotope are very close in energy to gamma rays emitted by other isotopes in the sample. An explicit example of that is the interference between the 185.7 keV photopeak of the 235U and the 186.1 keV photopeak of the 226Ra with branching ratios (f-value) of 57.2% and 3.5% for 235U and 226Ra, respectively. This problem can be easily solved by many methods to calculate the activity of 235U.
By using the other gamma transitions (143.76 keV [10.96%] and 163.33 keV [5.08%]) with their reasonable branching ratios, one can calculate the activity of 235U. Another approach in deducing235U and 226Ra radioactivity is the determination of 226Ra activity from its daughters (214Pb and 214 Bi) in secular equilibrium and subtracts its contribution from the multiple at 186 keV providing an indirect determination of 235U activity. This method is improper in the case of no radioactive equilibrium between238U and 226Ra. If a radioactive equilibrium exists between238U and 226Ra, the contributions of the photons emitted from235U and 226Ra recorded to this multiple photopeak may be calculated, thus allowing for an estimation of the activities of the two isotopes. A mathematical treatment can be performed to extract the net counts contributed by the 185.7 keV photopeak of the 235U and the 186.1 keV photopeak of the 226Ra.235U activity can also be determined through the determination of 238U assuming235U/238U isotopic ratio to be constant for the samples in natural ratio at 7.2 × 10−3.
This work aims to study various methods to distinguish between counting rate contributions from both235U and 226Ra to the 186 keV energy region and also the effects on the results, discuss the advantages and disadvantages of each method to easily calculate both uranium isotopes, and distinguish between samples containing normal, enriched, and DU.
| Techniques and Methods|| |
Nineteen representative samples of phosphate ore were collected from El-Sebaiya area, Aswan, Egypt. These samples were prepared for the gamma measurement.
The samples were transferred to cylindrical containers. The container material was polypropylene with a density of 0.946 g/cm3, inner diameter of 6.5 cm, wall thickness of 1.0 mm, height of 6.0 cm, and tare weight of 22.0 g.
The samples were analyzed for their gamma emitters using a spectrometer based on HpGe detector for 43,200 s. The HpGe detector (EG and G Ortec Model GEM100P4) has 100% relative efficiency and a 2.1-keV full width at half-maximum at the 1.33-MeV gamma transition of 60Co. The Ortec® GammaVision software (Model A66-B32, version 6.00) was used for data analysis.
In the first method, the Ortec GammaVision analytical technique is used to obtain peak areas of the components of a multiplet. It uses peak areas from other parts of the spectrum to determine the areas of some of the components and calculates the remaining areas. It is called peak-interference correction. The activity of 235U is calculated from the area of the peak at the next most probable energy, i.e., 143.76 keV (10.96%). Then, the area of the 185.72 keV (57.2%)235U peak is calculated using the branching ratio of that gamma ray, the efficiency, and the activity. The235U area is subtracted from the area of the peak at 186 keV to obtain the area due to226Ra. From this, the activity of 226Ra in the sample is calculated.
This technique is useful for calculating the activity of 235U and 226Ra, especially in samples that are rich with uranium in natural ratios. That condition is verified in these samples as shown in [Table 1].
|Table 1: The specific activities of 238U and the calculated specific activities of 235U by using the interested methods for the measured samples|
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In the second method,235U activity can be determined through the determination of 238U assuming235U/238U isotopic ratio to be constant for the samples of phosphate at 7.2 × 10−3. Then,235U activity is calculated using the following equation:
235U (Bq/kg) = (T1/2[238U] × M [238U]/T1/2[235U] × M [235U]) ×238U (Bq/kg) × F (1)
Where T1/2(AX) is the half-life and M (AX) is the atomic mass of the radionuclide AX. Factor F is the 235U/238U isotopic ratio, which is assumed to be constant for soil and rocks at 7.2 × 10−3.
This technique is useful for calculating the activity of 235U and 226Ra, especially in samples that are rich in uranium in a natural ratio and also in226Ra which is not in equilibrium with238U.
The specific activity of 238U activity was determined indirectly from the energy transitions of its daughter234m Pa based on 1001.03 keV (0.837%).
In the third method, 226Ra activity in the sample is estimated using the average activity of 214 Bi and 214Pb, where226Ra is in equilibrium with214 Bi and 214Pb. Using the reference branching values of 226Ra and 235U,235U activity is determined by the following equation:
AU= 1.75 (CRT/ε186) – 0.063 (ARa) (2)
Where AU and ARa are the activities of 235U and 226Ra, respectively. ε186 is the detection efficiency (ε) at 185.7 keV and 186.2 keV, which was considered the same for simplicity since the difference would be minimal.
This technique is useful for calculating the activity of 235U and 226Ra, especially in samples that are rich with uranium in a natural ratio and also in226Ra which is not in equilibrium with238U.
In the fourth method, Ebaid et al., 2005, have suggested a reliable empirical equation to separate between counting rate contributions from both235U and 226Ra to the 186 keV energy region. The equation is based on an assumption that226Ra is in equilibrium with238U in the natural samples. It showed that the total count rate of the 186 keV peak consists of 58.3% of 226Ra and 41.7% of 235U at radioactivity equilibrium. Then,
CRT(186) = CRRa(186.21) + CRU(185.72) (3)
CRU(185.72) = 0.417 × CRT(186) (4)
CRRa(186.21) = 0.583 × CRT(186) (5)
Where CRT is the total count rate (counts/s) in the 186 keV energy peak, CRU is the count rate due to 185.72 keV of 235U, and CRRa is the count rate due to 186.21 keV of 226Ra. In addition, these calculations are useful in estimating the 226Ra in samples with no need for the secular equilibrium to happen between226Ra and its respective progenies.
[TAG:2]Results and Discussion[/TAG:2]
The specific activities of 238U and 235U in the samples were calculated in Bq/kg by using the previous four methods, and the values are illustrated in [Table 1].
The specific activity of 238U is ranged from 731.9 ± 106.9 to 905.7 ± 195.0 Bq/kg with an average of 796.1 ± 112.4 Bq/kg. The high errors associated with238U activities are due to the low probability of gamma line intensity of 234m Pa (1001.03 keV [0.837%]).
For235U, it is ranged from 26.4 ± 2.0 to 47.6 ± 3.7 Bq/kg with an average of 37.3 ± 2.7 Bq/kg, from 33.9 ± 5.0 to 41.9 ± 9.0 Bq/kg with an average of 36.9 ± 5.2 Bq/kg, from 26.8 ± 0.8 to 48.6 ± 2.0 Bq/kg with an average of 37.0 ± 1.1 Bq/kg, and from 32.7 ± 1.5 to 43.2 ± 3.1 Bq/kg with an average of 35.7 ± 1.9 Bq/kg by using the methods 1, 2, 3, and 4, respectively.
The agreement in the maximum values of 238U and 235U activity concentrations with the sample number 13 and approximate agreement of the average values of 235U activity concentrations in Bq/kg (37.3 ± 2.7, 36.9 ± 5.2, 37.0 ± 1.1, and 35.7 ± 1.9, by using the methods 1, 2, 3, and 4, respectively) verify the validation of all these methods for calculating the 235U activity, and 235U can be measured directly if corrected to subtract the contribution from226Ra.
By using the activity concentrations of 238U and 235U in [Table 1], the average values of the 238U/235U ARs were 22.0, 21.6, 21.9, and 22.3 by using the methods M1, M2, M3, and M4, respectively. [Figure 1] shows how238U/235U ratios vary from the natural ratio (21.7).
|Figure 1:238U/235U ratios versus the sample ID by using the different methods|
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By using the first method (M1), the little deviation in the 238U/235U AR (22.0) from the natural ratio (21.7) maybe due to the self-absorption effects and the low yield value in 143.76 keV (10.96%) gamma line. The low precision of the 238U/235U ARs around the natural ratio (21.7) as shown in [Figure 1] and the absence of correlation (R2= −0.021) within the results as shown in [Figure 2] would have also been arisen from these effects. Despite these effects, this method provides an uncertainty of 1.5% based on the natural ratio 21.7.
By using the second method (M2), the tiny deviation in the 238U/235U AR (21.6) from the natural ratio (21.7) maybe due to the low probability of gamma line intensity (low yield value) of 234m Pa (1001.03 keV [0.837%]) and the low value of the detector efficiency at high energies that used of calculating of 238U by234 m Pa in 1001.03 keV. An extreme precision in the 238U/235U ARs around the natural ratio (21.7) is clear as shown in [Figure 1], and a perfect correlation (R2 = 1.0) within the results as shown in [Figure 3] that can be attributed to the 238U activity is the only variable factor in the calculations. Hence, this method provides an insignificant uncertainty of 0.5% based on the natural ratio 21.7.
By using the third method (M3), the little deviation in the 238U/235U AR (21.9) from the natural ratio (21.7) can be interpreted due to the emanation of radon from the sealed sample, the samples' homogeneity error effects, the collection of the gaseous radon on the surface of the samples, the self-absorption effects, especially in 295.1 keV and 351.93 keV gamma lines, and the low values of the detector efficiency at the high energies that are used in calculating214 Bi by using 1120.28 keV (15.12%) and 1764.5 keV (15.4%) gamma line emission. The low precision of the 238U/235U ARs around the natural ratio (21.7) as shown in [Figure 1] and the small correlation (R2 = 0.04) within the results as shown in [Figure 4] may be because the calculations depend on the assumption226Ra is in equilibrium with214 Bi and 214Pb, the 226Ra /Avg.214 Bi &214Pb activity ratio has always a little deviation from unity resulting from the previous effects, and in addition to these effects, the calculations are depending on variable factors CRT and ARa also the detection efficiencies (ε) at 185.7 keV and 186.2 were considered the same for simplicity as described in details in an earlier work. However, this method provides an uncertainty of 1.0% based on the natural ratio 21.7.
By using the fourth method (M4), the little deviation in the 238U/235U AR (22.3) from the natural ratio (21.7) is maybe due to the self-absorption effects, especially in 185.72 keV gamma line, the low probability of gamma line intensity (low yield value) of 234m Pa (1001.03 keV [0.837%]), and the low value of the detector efficiency at high energies that used of calculating of 238U by234 m Pa in 1001.03 keV. This method appears to have a high precision of the 238U/235U ARs around the natural ratio (21.7) as shown in [Figure 1] and a strong correlation (R2 = 0.54) within the results as shown in [Figure 5]. In addition, this method gave the largest average238U/235U AR above the natural ratio (21.7) because the total count rate of the 186 keV peak consists of 58.3% of 226Ra and 41.7% of 235U at radioactivity equilibrium as shown in an earlier work. This method provides an uncertainty of 2.9% based on the natural ratio 21.7.
| Conclusions|| |
Various methods have been used to distinguish between counting rate contributions from both235U and 226Ra to the 186 keV energy region provided consistent and similar results in the calculation of the radioactivity of 235U either226Ra in equilibrium or not with238U.
The comparison between the activity concentration results of 235U calculated by using different methods has been studied with associated uncertainties. The studied methods provide a mean238U/235U AR with little deviations from the natural ratio.
By comparing the 238U/235U ARs by using different methods, it is clear that the second method gives the most accurate and precise results in the present studied samples. Hence, it is recommended to use this method in the similar samples.
The proposed work might be very useful to calculate the concentration of 235U in other types of samples, especially low-activity samples by using different HPGe crystals.
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Conflicts of interest
There are no conflicts of interest.
| References|| |
Nassef MH, El Mowafi W, El Tahawy MS. Non-destructive assay for 235U determination in reference materials of uranium oxide. J Nucl Radiat Phys 2009;4:65-73.
Al-Hamarneh I. Radiometric Investigation of Uranium Isotopic Ratio in the Jordanian Environment Dirasat Pure Sci 2006;33:49-59.
Smith HA Jr, and Schillebeeckx P
Fri.“Nondestructive assay of special nuclear material for uranium fuel-fabrication facilities”. United States. Available from: https://www.osti.gov/servlets/purl/510319
. [Last accessed on 2019 Mar 02].
Ivanovich M, Harmon RS. Uranium Series Disequilibrium: Applications to Earth, Marine, and Environmental Sciences. Oxford: Clarendon Press; 1992.
Delgado JU, Morel J, Etcheverry M. Measurements of photon emission probabilities from the decay of 226Ra and daughters. Appl Radiat Isot 2002;56:137-43.
Ebaid YY. Use gamma-ray spectrometry for uranium isotopic analysis in environmental samples. Rom J Phys 2010;55:69-74.
Ebaid YY, El-Mongy SA, Allam KA. 235U-γ Emission contribution to the 186 KeV energy transition of 226Ra in environmental samples activity calculations. Int Congr Ser 2005;1276:409-11.
Rohit ME, Manmohan SI. Estimation of radiological risk due to concentration of 238U, 226Ra, 232Th and 40K in soils of different geological origins in Northern India. Turk J Phys 2012;36:289-97.
Murray AS, Aitken MJ. Analysis of low-level natural radioactivity in small mineral samples for use in thermoluminescence dating, using high-resolution gamma spectrometry. Int J Radiat Appl Instrum Part A Appl Radiat Isot 1988;39:145-58.
Sutherland RA, de Jong E. Statistical analysis of gamma-emitting radionuclide concentrations for three fields in Southern Saskatchewan, Canada. Health Phys 1990;58:417-28.
Allam KA, Ahmed Z, El-Sharkawy S, Salman A. Analysis and statistical treatment of 238U series isotopic ratios using gamma ray spectrometry in phosphate samples. Radiat Prot Environ 2017;40:110-5. [Full text]
[Figure 1], [Figure 2], [Figure 3], [Figure 4], [Figure 5]