2. R. SZ KE, I. SZIKLAI-LÁSZLÓ: EPIBORON NAA: AN OPTION TO ANALYZE UNFAVORABLE MATRICES
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Fig. 1. Schematic diagram and a picture of the boron container
For the analysis of geological and biological
materials 150–200 mg were sealed in high purity quartz
vials (Suprasil AN, Heraeus) and then packed in the
boron shielded container.
Irradiation
The bare and boron-shielded samples and flux
monitors were irradiated for 24 hours in the Budapest
Research Reactor at a thermal neutron flux density of
1.5.1013 n.cm–2.s–1, thermal-to-epithermal neutron flux
ratio f = th/ epi = 49 and = 0.015, where the
epithermal flux is represented by the 1/E1+ function
and is a form factor. Following boron-covered
irradiations, all samples were measured after a minimum
delay of approximately 1 hour on account of the
substantial reduction of matrix activities 24Na
(T1/2 = 14.95 h), 32P (T1/2 = 14.28 d) and 82Br
(T1/2 = 1.47 d). Following bare irradiations, the first
measurement of the samples were carried out after 4–5
days. Counting times varied between 1800 seconds and
10 hours. Gamma-spectrometric measurements were
performed with a Canberra HPGe detector (energy
resolution of 1.74 keV and relative efficiency of 36% for
the 1332.5 keV 60Co line), and associated linear
electronics consisting of an 8K ADC and an
ACCUSPEC/B type 16K MCA board. The spectrometer
was equipped with a Westphal-type Loss-Free Counting
(LFC) module operated in Dual Spectrum Mode
providing full compensation for all kind of counting
losses. The gamma-ray spectra were evaluated by the
program HYPERMET-PC,6 involving automatic peak
search, energy calibration, net peak counts computation.
The quantitative evaluation of the INAA multi-element
measurements was based on the k0 standardization
method using gold and zirconium flux monitors co-
irradiated with the samples. An in-house program
NAACNC was used for isotope identification and
elemental concentration calculations.7
The IAEA-Soil-7 reference material was analyzed by
ENAA to test the accuracy of the implemented
technique.
Results
Determination of boron activation ratios
The activation ratios were calculated for individual
(n, ) reactions using the specific activities of samples
induced in bare and filtered irradiations.
3. R. SZ KE, I. SZIKLAI-LÁSZLÓ: EPIBORON NAA: AN OPTION TO ANALYZE UNFAVORABLE MATRICES
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The improvement achieved by filtered irradiations may
be expressed as the so-called improvement factor:1
)1(
)2(
B
B
B
R
R
IF ,
where RB(1) refers to the determinant, and RB(2) refers to
the dominant interfering element . Table 2 lists the
nuclear data for the radionuclides used, RCd and RB and
the calculated IFB for interferences of 24Na and 46Sc.
Sodium and scandium were chosen as typical
interferences always present in biological and geological
samples.
Effect of the boron filter on the neutron flux distribution
Boron’s absorption cross section follows the 1/v law
over a wide energy range (from about 0.001 to a few
hundred eV). The resulting EB = 15.2 eV cutoff for
500 mg B/cm2 surface density allows a very effective
depression of strongly activating 1/v and low resonance
target isotopes while reducing only slightly the
activation of analytically important, higher than 10 eV
resonance elements such as As, Sb, Th, Zn, U (Fig. 2).
An additional advantage of epiboron NAA is the
significant reduction of the analysis turn-around time.
Using a boron shield, the measurements could be started
after about 1 hour waiting time. Consequently, some
short-lived trace elements as Mn, As, Mg, Ti, ,etc. can
be determined instrumentally with higher accuracy and
minimum delay (Fig. 3).
Fig. 2. Excerpt of a MathCad program showing the approximate neutron flux distributions in the
rotating channel No. 17 of the Budapest Research Reactor using 1 mm Cd and 500 mg/cm2
natural boron filters
4. R. SZ KE, I. SZIKLAI-LÁSZLÓ: EPIBORON NAA: AN OPTION TO ANALYZE UNFAVORABLE MATRICES
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Table 2. Nuclear data, Cd B ratios and improvement factors for some (n, ) reactions of interest
Nuclear data Activation ratio Improvement factor
Element Nuclear reaction
r, eV I0/ 0 RCd RB SD, % IFB(Na) IFB(Sc)
Ag 109
Ag(n, )110m
Ag 6.08 16.7 – 26 (3) 0.58 0.95
As 75
As(n, )76
As 106 13.6 4.2 6.2 (2) 2.38 3.91
Au 197
Au(n, )198
Au 5.7 15.7 3.9 26 (1) 0.56 0.92
Br 81
Br(n, )82
Br 152 19.3 – 4.7 (1) 3.16 5.16
Ce 140
Ce(n, )141
Ce 7200 0.83 – 115 0.13 0.21
Co 59
Co(n, )60
Co 136 1.99 – 45 (4) 0.34 0.54
Cs 133
Cs(n, )134
Cs 9.27 13.2 – 15 (4) 1.06 1.73
151
Eu(n, )152
Eu 0.448 0.87 – 440 (4) 0.03 0.06Eu
153
Eu(n, )154
Eu 5.8 5.66 – 40 (1) 0.37 0.61
Fe 58
Fe(n, )59
Fe 637 0.97 50 92 (2) 0.16 0.26
La 139
La(n, )140
La 76 1.24 – 69 (2) 0.22 0.35
Na 23
Na(n, )24
Na 3380 0.59 – 220 (5) – –
Rb 85
Rb(n, )86
Rb 839 14.8 – 4.7 (3) 3.15 5.16
121
Sb(n, )122
Sb 13.1 33.0 – 7.6 (5) 1.94 3.20Sb
123
Sb(n, )124
Sb 28.2 28.8 – 6.1 (3) 2.46 4.08
Sc 45
Sc(n, )46
Sc 5130 0.43 103 589 (5) – –
Se 74
Se(n, )75
Se 29.4 10.8 – 13 (6) 1.16 1.91
Th 232
Th(n, )233
Th/233
Pa 54.4 11.5 – 8.8 (2) 1.68 2.75
64
Zn(n, )65
Zn 2560 1.91 26 30 (6) 0.49 0.79Zn
68
Zn(n, )69m
Zn 590 3.19 16 18 0.81 1.34
94
Zr(n, )95
Zr 6260 5.31 10 9.3 (2) 1.60 2.63Zr
96
Zr(n, )97
Zr/97m
Nb 338 251.6 1.2 1.4 (2) 10.6 17.3
U 238
U(n, )239
U/239
Np 16.9 103.4 – 4.4 (2) 3.36 5.51
Fig. 3. A typical spectrum region of a geological sample irradiated for 24 hours in a boron filter and measured after 30-minute waiting time
6. R. SZ KE, I. SZIKLAI-LÁSZLÓ: EPIBORON NAA: AN OPTION TO ANALYZE UNFAVORABLE MATRICES
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Fig. 4. Gamma-ray spectra of the SRM NIST -613 Trace Element in Glass samples irradiated with and without a boron filter. Upper spectrum:
without B-filter ti = 24 hours, td = 53 hours, tc = 1800 s; lower spectrum: with B-filter ti = 24 hours, td =6 hours, tc = 3600 s
Table 3. Analysis results of SRM IAEA-Soil-7 by INAA and ENAA
Analysis results, mg/kg (mean SD%)
Element Certified value
by IAEA
INAA ENAA
As 13.4 (6) 14.3 (5) 14.3 (5)
Ce 61 (11) 57 (5) 57 (5)
Co 8.9 (10) 8. 7 (5) 8.9 (6)
Cr 60 (21) 67 (5) **
Cs 5.4 (14) 5.4 (14) 5.2 (10)
Br* 3–10 5.4 (6) 5.3 (5)
Hf 5.1 (7) 4.9 (5) **
La 28 (4 ) 28 (5) 25 (7)
Rb 51 (9) 52 (7) 49 (8)
Sb 1.7 (12) 1.8 (10) 1.6 (5)
Sc 8.3 (13) 8.4 (4) –
Sm 5.1 (7) 4.9 (10) **
Ta 0.8 (25) 0.7 (10) **
Th 8.2 (13) 7.9 (6) 8.2 (6)
U 2.6 (21) 2.4 (6) 2.5 (5)
Yb 2.4 (15) 2.2 (5) **
Zn 104 (6 ) 107 (6) 106 (6)
Zr 185 (6 ) 198 (12) 185 (6)
Tb 0.6 (33) 0.7 (19) **
Eu 1 (20) 0.9 (7) 0.8 (8)
Ca 163000* 160140 (6) **
Fe 25700* 25484 (4) 27336 (9)
* Information value.
** No ENAA results due to the lack of RB factors.
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Table 4. Comparison of the detection limits of INAA and ENAA for some elements
in SRM IAEA-Soil-7
LD, mg/kg
Element
with INAA with ENAA
As 0.03 0.001
Cs 0.04 0.005
La 0.01 0.001
Rb 1.2 0.82
Ta 0.05 0.002
Tb 0.01 0.001
Th 0.02 0.01
U 0.01 0.005
W 0.07 0.001
Zn 2.0 0.1
Irradiation time: 24 hrs 24 hrs
Cooling time: 6.2 days 0.3 days
Counting time: 120 min 80 min
Samples of the SRM NIST-613 Trace Element in
Glass were also irradiated with and without a boron
filter. In the case of bare irradiation the 1368 keV
photopeak for 24Na is still dominating (Fig. 4 upper
curve) after 53 hours decay time. Following boron-
filtered irradiation the activity of 24Na is significantly
reduced, consequently the background of the spectrum
decreases. Therefore, the analytical sensitivities are
much better for the isotopes with short half-lives (lower
curve).
To test the applicability of this technique SRM
IAEA-Soil-7 material was analyzed by ENAA, and for
comparison, parallel samples were measured by INAA.
Table 3 gives the element concentrations determined
with both techniques.
The initial sensitivity of the determination by ENAA
depends among other things on the ratio of resonance
integral to the thermal cross section, and on the levels of
the elements whose neutron induced radionuclides
produce the Compton continuum background below the
analytical peak of interest. The obtained detection
limits8 (LD) for some elements in IAEA Soil-7 reference
material measured by INAA and ENAA are presented in
Table 4.
The experimental results confirm that the accuracy
and precision of the two methods are comparable, so the
recently developed epiboron NAA can be integrated into
the routine NAA work of our laboratory.
Conclusions
If an NAA laboratory is engaged in routine analysis
of geological and biological materials, the use of
selective irradiation is unavoidable to unfold the
resulting complex spectra. Cd filters were generally used
to depress the activation of the so-called 1/v isotopes,
but several disadvantages of Cd make the method
unfeasible. In this study a large volume boron filter has
been constructed and tested. The filter is reusable and
following subsequent irradiations, no mechanical
damages have been observed so far.
The results of this study proved, that by using boron
irradiation filters significant improvements in detection
sensitivity were obtained for those (n, ) reactions having
strong and >10 eV resonances in the epithermal region.
The reliability of epiboron NAA is comparable to
conventional thermal neutron activation analysis, and
the number of the elements that can be determined
instrumentally in biological and geological materials is
considerably extended.
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