Yoshiaki
Ito†
a,
Tatsunori
Tochio
b,
Michiru
Yamashita
c,
Sei
Fukushima
d,
Łukasz
Syrocki
e,
Katarzyna
Słabkowska
f,
Marek
Polasik
f,
José Pires
Marques
gh and
Fernando
Parente
*i
aLaboratory of Atomic and Molecular Physics, ICR, Kyoto University, Gokasho, Uji, Kyoto 611-0011, Japan
b1-24-14 Inadera, Amagasaki 661-098, Hyogo, Japan
cHIT, 3-1-12 Yukihira, Suma-ku, Kobe 654-0037, Japan
dKobe Material Testing Laboratory Co., Ltd, 47-13 Nijima, Harima-cho, Kako-gun, Hyogo 675-0155, Japan
eInstitute of Plasma Physics and Laser Microfusion, Hery 23, 01-497 Warsaw, Poland
fFaculty of Chemistry, Nicolaus Copernicus University in Toruń, Gagarina 7, 87-100 Toruń, Poland
gLaboratório de Instrumentação e Física Experimental de Partículas, Av. Prof. Gama Pinto 2, 1649-003 Lisboa, Portugal
hFaculdade de Ciências da Universidade de Lisboa, Campo Grande, C8, 1749-016 Lisboa, Portugal
iDepartamento de Física, Laboratório de Instrumentação, Engenharia Biomédica e Física da Radiação (LIBPhys-UNL), Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa, Monte da Caparica, 2892-516 Caparica, Portugal. E-mail: facp@fct.unl.pt
First published on 23rd February 2024
To investigate the natural linewidths of Cu Kα1,2 diagram lines, the spectra of these lines were recorded in detail using an anti-parallel double-crystal X-ray spectrometer. The values obtained for the measured Cu Kα1 and Kα2 natural linewidths are 2.264(18) eV and 2.534(73) eV, respectively. The contribution of the Coster–Kronig (CK) transition for the Kα2 linewidth is found to be approximately 0.27 eV. Theoretical values 2.1454 eV for the Kα1 line and 2.1292 eV for the Kα2 line were calculated, using the GRASP and FAC codes. A detailed study of the same spectra using Si and Ge crystals and several Bragg surfaces was performed. In addition, the spectral measurements of Cu Kα3,4 satellite lines were made, and information on the energy values, FWHMs, and intensity ratios of these satellite lines was obtained from multiple-peak fitting analyses.
Ito et al.8,9 measured the Kα1,2 lines for elements in the range 20 ≤ Z ≤ 42, including Cu, using a high-resolution double crystal X-ray spectrometer and, taking into account the instrumental function through Tochio's method,10 examined the asymmetry and the contribution of [1s3d] shake processes, confirming that, for 3d transition elements, the asymmetry of the Kα1,2 lines was mainly due to those processes, and evaluated the natural linewidths for each element. In this paper, we extend the measurements reported in ref. 8 to include the element Cu. More recently, Mendenhall et al.11 evaluated the natural width of Kα1,2 lines and the structure of Kα3,4 satellite lines using a two channel-cut crystal (+,−; −,+) spectrometer.
The presence of hidden satellites, resulting from the shake processes, within the diagram lines, makes it difficult to accurately measure the natural widths, as the measured width depends on the crystal plane used for the measurement. To obtain the natural widths more reliably, we measured the Kα1,2 lines using several crystal planes with the same crystal spectrometer. To the best of our knowledge, there is no other crystal monochromator capable of making high-resolution spectral measurements suitable for such studies than the two-crystal monochromator.
The Cu Kα1,2 lines are suitable for analysis, from the angular point of view, through various changes in the crystal plane. Furthermore, as noted by Deutsch et al.,6 the width values of these lines have varied considerably among researchers. The Rietveld method of powder analysis software uses the widths and intensity ratios of these lines. So, these are very important values. Therefore, we measured the Cu Kα1,2 lines using the Si and Ge planes, (220), (333), and (440), with this high-resolution double crystal X-ray spectrometer and evaluated their natural widths, after taking into account the instrumental function.
Moreover, to investigate the complex structure of the Cu Kα1,2,3,4 lines in detail, the Kα3,4 satellite lines were measured using the same spectrometer. Finally, the application to materials based on this multiple-peak analysis will be mentioned.
Crystal | Step in 2θ (deg) | Integr. time (s) | Target | Times |
---|---|---|---|---|
(a) | ||||
Si(220) | 0.0005 | 4 | Rh(SPC) | 4 |
Si(333) | 0.002 | 150 | Rh(SPC) | 10 |
Si(440) | 0.0005 | 115 | Rh(SPC) | 3 |
Ge(220) | 0.0005 | 0.5 | Rh(SPC) | 4 |
Ge(333) | 0.001 | 50 | W(FPC) | 5 |
Ge(440) | 0.0005 | 20 | Rh(SPC) | 3 |
![]() |
||||
(b) | ||||
Si(220) | 0.001 | 150 | Rh(SPC) | 3 |
The instrumental function of the double-crystal spectrometer can be very well described from Monte Carlo simulations as has been shown in ref. 11 and 16–18 and by simply computing the rocking curve of the Si crystals through dynamical diffraction theory.17 From this instrumental function, one can obtain the natural linewidths as well as some other broadening mechanisms. In the present case, given the large natural widths of the diagram lines of neutral atoms when compared to the spectrometer instrumental function, we can use the simple broadening method described by Tochio et al.10 without increasing the final uncertainty.
In the MCDF method, the effective relativistic Hamiltonian for an N-electron atom has the form:
![]() | (1) |
The wave function for the N-electron system (characterized by the quantum numbers determining the value of the square of the total angular momentum J, projection of the angular momentum in the chosen direction M, and parity p) in the MCDF method is assumed in the form:
![]() | (2) |
![]() | (3) |
The natural width of the atomic level of the i-th hole can be obtained in the form of a sum of the natural radiative width Γradi and the natural nonradiative width Γnradi of the i-hole state:
Γi = Γradi + Γnradi = ΓXi + ΓAi + ΓCi. | (4) |
The natural widths of the Kα1 and the Kα2 X-ray radiative transitions can be expressed as follows
ΓKα1 = ΓK + ΓL3, | (5) |
ΓKα2 = ΓK + ΓL2, | (6) |
Contribution | Coulomb gauge (eV) | Babushkin gauge (eV) |
---|---|---|
K−1 → L2,3−1 | 0.5834 | 0.6017 |
K−1 → M2,3−1 | 0.0763 | 0.0795 |
K−1 → M4,5−1 | 0.0001 | 0.0001 |
K level sum | 0.6598 | 0.6813 |
L2−1 → M1−1 | 0.0003 | 0.0004 |
L2−1 → M4,5−1 | 0.0054 | 0.0061 |
L2 level sum | 0.0057 | 0.0065 |
L3−1 → M1−1 | 0.0003 | 0.0004 |
L3−1 → M4,5−1 | 0.0053 | 0.0060 |
L3 level sum | 0.0056 | 0.0064 |
Contribution | Width (eV) |
---|---|
K − LL | 0.6472 |
K − LM | 0.1596 |
K − LN | 0.0017 |
K − MM | 0.0097 |
K − MN | 0.0002 |
K level sum | 0.8184 |
L2 − L3M | |
L2 − L3N | 0.0042 |
L2 − MM | 0.6170 |
L2 − MN | 0.0018 |
L2 level sum | 0.6230 |
L3 − MM | 0.6378 |
L3 − MN | 0.0016 |
L3 level sum | 0.6394 |
Line | Coulomb gauge (eV) | Babushkin gauge (eV) |
---|---|---|
Γ Kα1 | 2.1231 | 2.1454 |
Γ Kα2 | 2.1068 | 2.1292 |
To obtain the correct value for the natural linewidths of the Cu Kα lines, we performed a detailed study of these lines using Si and Ge crystals and several Bragg surfaces. The results are presented in Table 5. When higher-order crystal surfaces are used, the spectrometer adjustment is extremely difficult. Therefore, to obtain natural linewidths from the recorded spectra with this double-crystal X-ray spectrometer, the best procedure consists in using a low-order crystal plane and estimating the natural width by correcting for the instrumental function. We find Si crystals to be the best choice for the evaluation of the instrumental function in devices using spectroscopic crystals. The crystalline integrity of the Si crystals used in this work was confirmed by X-ray topography.
Lines | Energy | FWHM | AI | CF | Rel. int. | Area (%) | |
---|---|---|---|---|---|---|---|
Si(220) | Kα1 | 8047.780(42) | 2.698(10) | 1.145(9) | 100 | ||
Kα2 | 8027.823(40) | 3.104(19) | 1.158(15) | 50.71(21) | |||
Kα1 − Kα2 | 19.953(12) | 0.406(21) | |||||
Kα11 | 8047.780(42) | 2.414(18) | 2.264(18) | 100 | 60.08 | ||
Kα12 | 8045.227(67) | 2.87(14) | 10.00(91) | 6.01 | |||
Kα21 | 8028.034(60) | 2.679(73) | 2.534(73) | 40.40(2.57) | 24.27 | ||
Kα22 | 8026.45(11) | 3.23(12) | 16.04(2.90) | 9.64 | |||
Kα11 − Kα21 | 19.746(31) | 0.270(75) | |||||
Si(333) | Kα1 | 8047.842(69) | 2.643(23) | 1.228(19) | 100 | ||
Kα2 | 8027.754(66) | 3.147(42) | 1.186(35) | 51.44(55) | |||
Kα1 − Kα2 | 20.088(29) | 0.504(48) | |||||
Kα11 | 8047.798(68) | 2.338(34) | 2.298(34) | 100 | 59.31 | ||
Kα12 | 8045.32(14) | 3.11(33) | 11.84(2.17) | 7.02 | |||
Kα21 | 8027.933(75) | 2.654(95) | 2.617(95) | 42.16(3.73) | 25 | ||
Kα22 | 8026.34(14) | 2.94(26) | 14.63(4.18) | 8.67 | |||
Kα11 − Kα21 | 19.865(44) | 0.32(10) | |||||
Si(440) | Kα1 | 8047.762(46) | 2.695(15) | 1.198(9) | 100 | ||
Kα2 | 8027.731(42) | 3.123(16) | 1.171(10) | 53.04(48) | |||
Kα1 − Kα2 | 20.028(5) | 0.428(22) | |||||
Kα11 | 8047.747(68) | 2.322(34) | 2.296(27) | 100 | 57.03 | ||
Kα12 | 8045.445(64) | 3.70(13) | 14.82(1.61) | 8.45 | |||
Kα21 | 8027.909(39) | 2.662(37) | 2.638(37) | 45.08(1.20) | 25.71 | ||
Kα22 | 8026.310(35) | 3.069(84) | 15.46(1.40) | 8.82 | |||
Kα11 − Kα21 | 19.838(44) | 0.342(46) | |||||
Ge(220) | Kα1 | 8047.70(14) | 3.242(16) | 1.080(9) | 100 | ||
Kα2 | 8027.80(14) | 3.645(23) | 1.087(15) | 50.86(25) | |||
Kα1 − Kα2 | 19.902(20) | 0.403(28) | |||||
Kα11 | 8047.74(14) | 2.982(28) | 2.579(29) | 100 | 60.72 | ||
Kα12 | 8045.14(14) | 3.66(26) | 8.98(1.54) | 5.45 | |||
Kα21 | 8028.06(12) | 3.229(80) | 2.836(80) | 41.08(2.91) | 24.95 | ||
Kα22 | 8026.409(96) | 3.78(15) | 14.62(3.25) | 8.88 | |||
Kα11 − Kα21 | 19.681(28) | 0.257(85) | |||||
Ge(333) | Kα1 | 8047.828(70) | 2.752(9) | 1.227(9) | 100 | ||
Kα2 | 8027.783(77) | 3.351(17) | 1.221(25) | 52.91(25) | |||
Kα1 − Kα2 | 20.045(20) | 0.599(19) | |||||
Kα11 | 8047.789(71) | 2.418(18) | 2.362(18) | 100 | 58.1 | ||
Kα12 | 8045.34(11) | 3.40(15) | 12.81(1.10) | 7.44 | |||
Kα21 | 8027.954(82) | 2.795(78) | 2.743(78) | 40.64(3.28) | 23.61 | ||
Kα22 | 8026.51(15) | 3.510(15) | 18.66(3.29) | 10.84 | |||
Kα11 − Kα21 | 19.835(28) | 0.381(80) | |||||
Ge(440) | Kα1 | 8047.904(24) | 2.778(12) | 1.285(13) | 100 | ||
Kα2 | 8027.807(25) | 3.470(25) | 1.313(17) | 55.58(21) | |||
Kα1 − Kα2 | 20.097(2) | 0.692(28) | |||||
Kα11 | 8047.842(29) | 2.389(18) | 2.330(18) | 100 | 55.14 | ||
Kα12 | 8045.467(88) | 3.83(20) | 15.40(1.23) | 8.49 | |||
Kα21 | 8027.861(26) | 2.64(13) | 2.59(13) | 35.16(4.43) | 19.39 | ||
Kα22 | 8026.887(90) | 4.71(15) | 30.81(6.22) | 16.99 | |||
Kα11 − Kα21 | 19.980(8) | 0.26(13) | |||||
Si(220)* | Kα1 | 8047.773(75) | 2.701(7) | 1.142(6) | 100 | ||
Kα2 | 8027.813(81) | 3.115(13) | 1.158(9) | 50.689(203) | |||
Kα1 − Kα2 | 19.957(26) | 0.414(15) | |||||
Kα11 | 8047.773(76) | 2.422(12) | 2.273(12) | 100 | 60.22 | ||
Kα12 | 8045.207(90) | 2.871(84) | 9.76(0.53) | 5.88 | |||
Kα21 | 8028.038(82) | 2.673(32) | 2.527(32) | 39.52(1.25) | 23.8 | ||
Kα22 | 8026.476(92) | 3.260(61) | 16.77(1.29) | 10.1 | |||
Kα11 − Kα21 | 19.736(24) | 0.254(34) |
The best correction value for Kα1,2 is obtained by using Si(220) planes, as seen in Fig. 3 and Table 5. Furthermore, from the same table, the area intensity of Kα12 + Kα22 satellite lines, resulting from the shake process,5,6,8 relative to the total area, is ∼15%, very close to the values in Melia et al.26 and references therein. The widths of the Cu Kα1 and Kα2 lines obtained from these spectra are 2.260 eV for the Kα11 line (Kα1 line) and 2.530 eV for the Kα21 line (Kα2 line), respectively, as seen in Table 5. The width of the Cu Kα2 line is likely to be enhanced by the contribution of the L2 − L3M4,5 CK transition. The width of this CK transition will be within the energy range limited by the difference between (Kα2 linewidth − Kα1 linewidth), where it is assumed that the shake process is included in each spectrum and (Kα21 linewidth − Kα11 linewidth), where the shake process is not included in these spectra, or between 0.41 eV and 0.27 eV, agreeing with the difference of Campbell and Papp recommended values25 for the corresponding levels including the shake process, 0.43 eV, the experimental value of Yin et al.,23 0.44 eV, and the calculated value, 0.43 eV, for the CK transition reported by Ohno et al.27
![]() | ||
Fig. 3 The corrected FWHMs in the Cu Kα1,2 diagram lines together with the data reported using a double-crystal or high-resolution X-ray spectrometer [Deutsch et al.,5 Tochio et al.,10 Mendenhall et al.,11 and Ito et al.15]. The symmetric crystals, Si(220), Si(333), Si(440), Ge(220), Ge(333), and Ge(440) were used in this study, respectively. The ΓCK value is taken from Yin et al.23 Calculated values for both Coulomb and Babushkin gauges of the half-widths of the Kα1,2 lines for Cu atoms are included with Krause and Oliver (semiempirical values),24 and Campbell and Papp (recommended values).25 |
The width of the CK transition was estimated to be in the range of 0.45 to 0.55 eV based on the excitation energy dependence of the Cu L3/L2 emission intensity ratio by Magnuson et al.28 The value of Nyholm et al.,29 0.68 eV, is slightly larger. The calculated width of the L2 − L3M4 CK transition by Yin et al.23 is 0.287 eV. This value is well in agreement with our experimental value, not taking in account the [1s3d] shake processes.
The FWHM values of the Kα11 line obtained with the Si(220) crystal planes and with the Ge(220) ones should, in principle, be the same, when the instrumental function is taken into account. However, we found the FWHM of the line obtained with the former crystal to be 0.3 eV less than the latter one. This difference suggests that the Ge crystal surface is probably not in good condition. However, when higher-order Ge lines are used, the half-widths of the Kα11 and Kα21 lines, corrected for the device function, are found to be closer to their natural widths.
To better visualize the above results, each FWHM (CF) obtained from the multiple peak fitting analysis, corrected by the instrument function, is plotted against the spectral crystal (2θ angle) in Fig. 3. The corrected values (CF) of the Kα1 and Kα2 linewidths obtained with the Ge(333) and Ge(440) planes are not as large as the values obtained with the Ge(220) ones. The use of higher-order Bragg planes removes the influence of the profile base, but the background is higher, which may be reflected in the natural width for the Kα2 line. This seems to be particularly the case for Ge spectral crystals, although there may also be problems with crystal integrity.
From the theoretical point of view, as shown in Tables 2–4 and Fig. 3, the calculated natural widths of Cu Kα1 and Kα2 lines obtained in this work are 2.1231 eV and 2.1068 eV in the Coulomb gauge, and 2.1454 eV and 2.1292 eV in the Babushkin gauge, respectively.
Using the ΓK width 1.49 eV from Campbell and Papp25 and the ΓL2 and ΓL3 linewidths, obtained by Yin et al.23 without the contribution of the L2 − L3M4,5 CK transition, the Kα1 and Kα2 linewidths are 2.041 eV and 2.010 eV, respectively. The semi-empirical Cu linewidths from Krause and Oliver24 are 2.11 eV for the Kα1 line and 2.17 eV for the Kα2 line, the ΓK width being 1.554 eV. These values are also in good agreement with our calculations. It should be added that the calculated Kα2 line broadening due to the L2 − L3M4,5 CK transition for Cu is 0 eV, suggesting that in future more advanced theoretical and experimental studies are needed to explain this CK transition.
Lines | This study | Mendenhall | Fritsch | Illig |
---|---|---|---|---|
Energy | ||||
Kα11 | 8047.807(41) | 8047.8254(3) | 8047.947(18) | |
Kα12 | 8045.221(28) | 8045.2956(47) | 8044.142(12) | |
Kα21 | 8028.012(70) | 8028.0503(27) | 8028.272(17) | |
Kα22 | 8026.567(74) | 8026.5386(92) | 8026.645(18) | |
Kα11 − Kα21 | 19.8(5) | 19.7751 | ||
Kα31 | 8079.12(34) | 8078.627(58) | 8078.0(3) | |
Kα32 | 8083.39(16) | 8083.3528(38) | 8082.7(1) | |
Kα33 | 8075.15(88) | 8074.954(146) | 8070.0(3) | |
Kα34 | 8087.50(34) | 8088.109(57) | 8087.5(2) | 8076.623(25) |
![]() |
||||
FWHM | ||||
Kα11 | 2.294(5)* | 2.275(1) | 2.484(2) | |
Kα12 | 2.903(48) | 2.915(9) | 0.755(4) | |
Kα21 | 2.531(25)* | 2.529(5) | 2.489(2) | |
Kα22 | 3.428(37) | 3.274(8) | 3.089(2) | |
Kα31 | 4.83(2.00) | 5.51(14) | 3.85(30) | |
Kα32 | 4.39(1.06) | 5.51(14) | 3.11(11) | |
Kα33 | 5.75(3.15) | 3.22(21) | 1.29(47) | |
Kα34 | 3.52(1.35) | 3.22(21) | 1.70(1.9) | 3.844(3) |
![]() |
||||
R.I. | ||||
Kα11 | 100 | 100 | 100 | |
Kα12 | 9.99(25) | 12.123 | 1.4 | |
Kα21 | 37.36(89) | 39.13 | 37.867 | |
Kα22 | 19.00(90) | 19.284 | 14.683 | |
Kα31 | 0.20(13) | 0.391 | 36.30(3.90) | |
Kα32 | 0.240(88) | 0.465 | 67.7(4.0) | |
Kα33 | 0.075(90) | 0.041 | 5.00(1.00) | |
Kα34 | 0.074(46) | 0.087 | 1.40(62) | 0.332 |
Furthermore, when the area intensities of the Kα3,4 lines obtained by single crystal spectroscopy using Si(111)30 and the intensity of the Kα3,4 lines obtained through the analytical method of deconvolution are compared with the intensities of the Kα3,4 lines obtained by high-resolution X-ray spectroscopy, the intensity of the Kα3,4 lines obtained with Si(111) is the smallest.
Footnote |
† Present address: Rigaku Corporation, 14-8, Akaoji-cho, Takatsuki, Osaka 569-1146, Japan. |
This journal is © The Royal Society of Chemistry 2024 |