1 Introduction
Energy-dispersive X-ray fluorescence (EDXRF) is an analytical method for determining the concentration of micro and major elements in different matrices. This technology is widely used in pharmaceutical analysis, antique authentication, and the exploration of mineral resources because of its rapid and nondestructive analysis process [1]. However, calibrating the efficiency of the instrument and matrix-effect correction are the most realistically difficult problems in EDXRF. Many studies focusing on these two problems have been conducted. Since the 1950s, the mutual impact coefficient method and the fundamental parameter method (FPM) have been the main methods used in X-ray fluorescence analyses. The former consists in calibrating efficiency with standard samples to solve the problem of overlapping-peak peeling, but the X-ray fluorescence spectrometer has to be rescaled when there are large matrix differences in the sample [2]. The FPM is a widely used method based on physical parameters. It can effectively reduce the absorption and enhancement effects. The major advantage of the FPM is the minimum number of standard samples required for efficiency calibration [3–5]. However, most measurements based on the FPM are developed for wavelength dispersive X-ray fluorescence (WDXRF) analysis [6–9]. By comparison, the ability to carry out in-situ measurement works is one of the major advantages of EDXRF. In conventional EDXRF, elements with an atomic number below 19 are commonly difficult to analyze in the field. Thus, a "dark matrix" must exist in the sample. To correct for the variations caused by the matrix effect, the backscatter fundamental-parameter method was proposed and developed [10, 11]. In addition, several methods were developed for EDXRF analysis, which can be referred to in a previous review [12]. In recent years, using an effective atomic number
Usually, the net characteristic X-ray intensity of each element is derived once the EDXRF spectrum is taken, and then the element concentration is calculated via the FPM [15]. This independent quantitative method has proven to be workable. However, it remains a complex and time-consuming process that requires a high degree of experience and knowledge from the instrument user [16]. The full-spectrum least-squares (FSLS) method is a multivariate calibration method that is able to, based on the conventional least-squares principle, increase the selectivity of matrix components and provide the possibility of detecting samples as outliers. Theoretically, it can deal with considerable peak overlaps owing to its lower dependence on the shape of predefined peak lines [17]. However, this multivariate calibration method is rarely applied in EDXRF except for near-infrared and infrared spectroscopic analytical studies [16-19]. Therefore, this paper explores the feasibility of using FSLS regression for the quantitative EDXRF determination of the concentration of micro and major elements, such as titanium (Ti), iron (Fe), nickel (Ni), copper (Cu), and zinc (Zn), which are common components in solid samples.
2 Theoretical descriptions
In EDXRF, the basic equations that relate the measured X-ray fluorescence intensity and the corresponding element composition were derived by Sherman and other authors [16, 20, 21]. When an X-ray beam irradiates the surface of the sample, the absorption and scattering of the original irradiated beam will occur along the trajectory path. The attenuation of the original irradiated beam caused by absorption and scattering is not only proportional to the incident X-ray intensity but also depends on the thickness, density, and the number of encountered atoms per unit cross-section of the absorber. Based on this theory, the absorption of the original irradiated beam can be divided into three processes: Ⅰ, Ⅱ, and Ⅲ, as shown in Fig. 1.
-201903/1001-8042-30-03-017/alternativeImage/1001-8042-30-03-017-F001.jpg)
ProcessⅠrepresents the attenuation of the original X-ray (whose wavelength is
These characteristic X-ray are radiated evenly in all directions and are then attenuated by being absorbed by matter in process Ⅲ. Only the X-ray with a spatial solid angle of
Here,
Here,
-201903/1001-8042-30-03-017/alternativeImage/1001-8042-30-03-017-F002.jpg)
In addition,
Thus, Eq. (2) can be simplified as follows:
where
where
Here,
Actually, in X-ray spectrum analyses, the count rate of one energy channel is not related only to the target element; it is also affected by other elements in the matrix. Therefore, the spectrum can be regarded as the sum of the contributions of a series of elements within the same matrix. Once the theoretical spectrum of a single element is obtained, the optimal-response relationship between the content of that element and the detected X-ray spectrum can be established. Based on the fluorescence formulas, the calculated intensity is just a value equal to the total area of the detected X-ray peak for one element. Thus, the intensity at the peak position needs to be Gaussian broadened [24] to the scale edge of the spectrometer, which is approximately 0–1023 channels. This can be described in the following procedure.
The Gaussian distribution prototype formula [25] is shown below.
Here,
No | KCl | H3BO3 | SiO2 | No | CaO | H3BO3 | SiO2 | No | TiO2 | H3BO3 | SiO2 |
---|---|---|---|---|---|---|---|---|---|---|---|
Component proportions (%) of the standard samples from No. 1 to No. 15 | |||||||||||
1 | 0.19 | 28.58 | 71.23 | 6 | 0.14 | 28.57 | 71.29 | 11 | 0.17 | 28.57 | 71.26 |
2 | 0.96 | 28.57 | 70.47 | 7 | 0.70 | 28.57 | 70.73 | 12 | 0.83 | 28.57 | 70.59 |
3 | 1.91 | 28.57 | 69.52 | 8 | 1.40 | 28.57 | 70.03 | 13 | 1.68 | 28.62 | 69.69 |
4 | 9.54 | 28.57 | 61.89 | 9 | 6.99 | 28.57 | 64.43 | 14 | 8.35 | 28.56 | 63.09 |
5 | 19.08 | 28.57 | 52.35 | 10 | 13.99 | 28.57 | 57.44 | 15 | 16.69 | 28.57 | 54.74 |
No | Fe2O3 | H3BO3 | SiO2 | No | Ni | H3BO3 | SiO2 | No | ZnO | H3BO3 | SiO2 |
Component proportions (%) of the standard samples from No. 16 to No. 30 | |||||||||||
16 | 0.14 | 28.57 | 71.29 | 21 | 0.11 | 28.57 | 71.32 | 26 | 0.13 | 28.57 | 71.31 |
17 | 0.71 | 28.57 | 70.72 | 22 | 0.51 | 28.57 | 70.93 | 27 | 0.62 | 28.57 | 70.81 |
18 | 1.43 | 28.57 | 70.00 | 23 | 1.00 | 28.57 | 70.43 | 28 | 1.24 | 28.57 | 70.18 |
19 | 7.15 | 28.57 | 64.28 | 24 | 5.00 | 28.57 | 66.43 | 29 | 6.23 | 28.57 | 65.20 |
20 | 14.30 | 28.57 | 57.13 | 25 | 10.00 | 28.57 | 61.43 | 30 | 12.47 | 28.57 | 58.97 |
No | SrCl2•6H2O | H3BO3 | SiO2 | No | ZrO2 | H3BO3 | SiO2 | No | MoO3 | H3BO3 | SiO2 |
Component proportions (%) of the standard samples from No. 31 to No. 45 | |||||||||||
31 | 0.29 | 28.58 | 71.14 | 36 | 0.13 | 28.57 | 71.30 | 41 | 0.15 | 28.57 | 71.28 |
32 | 1.54 | 28.57 | 69.89 | 37 | 0.67 | 28.57 | 70.76 | 42 | 0.75 | 28.58 | 70.68 |
33 | 3.05 | 28.57 | 68.38 | 38 | 1.35 | 28.57 | 70.08 | 43 | 1.51 | 28.57 | 69.92 |
34 | 15.22 | 28.57 | 56.22 | 39 | 6.76 | 28.57 | 64.67 | 44 | 7.51 | 28.57 | 63.92 |
35 | 30.43 | 28.57 | 41.00 | 40 | 13.51 | 28.57 | 57.92 | 45 | 15.01 | 28.57 | 56.42 |
Once the
This equation can be simplified as follows.
Here,
3 Experiments
Determining factor
Here, SiO2 was used as the matrix in the sample and H3BO3 was used as an adhesive for different contents. The
-201903/1001-8042-30-03-017/alternativeImage/1001-8042-30-03-017-F004.jpg)
As can be seen from Fig. 3, the fitted formula between factor
-201903/1001-8042-30-03-017/alternativeImage/1001-8042-30-03-017-F003.jpg)
The square of the correlation coefficient (R2) is 0.9721. Therefore, the
Here,
where
-201903/1001-8042-30-03-017/alternativeImage/1001-8042-30-03-017-F005.jpg)
Rayleigh and Compton scattering peaks exist in the net EDXRF spectrum. Many researchers have concluded that the coherent-to-Compton scattering cross-section ratio depends only on the effective atomic number of composite materials [30]. Duvauchelle et al. [31] pointed out that a given
-201903/1001-8042-30-03-017/alternativeImage/1001-8042-30-03-017-F006.jpg)
The relationship between
The square of the correlation coefficient is 0.9608. The mass-absorption coefficient for a multi-component sample is equal to the sum of the weighted mass-absorption coefficient of each component, including the known contents and the "dark matrix." This parameter can be derived [14] as follows.
Here,
-201903/1001-8042-30-03-017/alternativeImage/1001-8042-30-03-017-F007.jpg)
4 Results and discussion
In this paper, thirteen National Standard Soil (Nss) samples were used to verify the feasibility of the FSLS algorithm. The iterations stop when the difference between the current and the former calculated contents is less than 0.005%. The results of the algorithm are shown in Table 2.
Nss | Ti | Fe | Ni | Cu | Zn | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
No | Standard content % | Calculated content % | Relative error % | Standard content % | Calculated Content % | Relative error % | Standard content µg/g | Calculated content µg/g | Relative error % | Standard content µg/g | Calculated content µg/g | Relative error % | Standard content µg/g | Calculated content µg/g | Relative error % |
2 | 0.271±0.008 | 0.204±0.014 | 25 | 2.462±0.070 | 2.003±0.071 | 19 | 19.4±1.3 | 61.6±4.6 | 218 | 16.3±0.9 | 22.9±1.6 | 40 | 42±3 | 70±6 | 67 |
3 | 0.224±0.008 | 0.190±0.011 | 15 | 1.399±0.050 | 1.243±0.011 | 11 | 12.0±2.0 | 47.1±1.2 | 293 | 11.4±1.1 | 13.4±0.8 | 18 | 31±3 | 53±4 | 70 |
4 | 1.080±0.031 | 0.975±0.095 | 10 | 7.205±0.110 | 6.993±0.046 | 3 | 64.0±5.0 | 113.0±3.0 | 76 | 40.0±3.0 | 55.6±3.7 | 39 | 210±13 | 259±14 | 23 |
5 | 0.629±0.021 | 0.657±0.094 | 4 | 8.828±0.180 | 8.859±0.772 | 0 | 40.0±4.0 | 101.6±8.0 | 154 | 144.0±6.0 | 133.7±25.6 | 7 | 494±25 | 592±69 | 20 |
6 | 0.439±0.012 | 0.413±0.055 | 6 | 5.659±0.130 | 5.558±0.029 | 2 | 53.0±4.0 | 107.2±13.5 | 102 | 390.0±14.0 | 424.2±18.2 | 9 | 97±6 | 124±8 | 28 |
8 | 0.380±0.012 | 0.298±0.021 | 22 | 3.134±0.050 | 2.865±0.019 | 9 | 31.5±1.8 | 64.5±5.5 | 105 | 24.3±1.0 | 32.7±1.6 | 35 | 68±4 | 104±8 | 54 |
9 | 0.424±0.023 | 0.386±0.034 | 9 | 3.358±0.100 | 3.479±0.035 | 4 | 33.0±3.0 | 88.3±5.4 | 168 | 25.0±3.0 | 31.1±1.6 | 24 | 61±5 | 103±5 | 69 |
10 | 0.427±0.006 | 0.383±0.052 | 10 | 2.917±0.030 | 3.029±0.022 | 4 | 26.0±1.0 | 62.5±4.0 | 141 | 19.0±1.0 | 22.3±0.3 | 17 | 60±4 | 95±12 | 58 |
12 | 0.392±0.006 | 0.313±0.029 | 20 | 3.295±0.040 | 3.017±0.028 | 8 | 32.0±1.0 | 77.1±5.0 | 141 | 29.0±1.0 | 40.6±1.9 | 40 | 78±5 | 117±13 | 50 |
13 | 0.382±0.011 | 0.295±0.015 | 23 | 2.875±0.040 | 2.480±0.030 | 14 | 28.5±1.2 | 65.5±4.3 | 130 | 21.6±0.8 | 27.5±1.4 | 28 | 65±3 | 97±5 | 50 |
14 | 0.466±0.013 | 0.366±0.023 | 21 | 3.722±0.060 | 3.746±0.007 | 1 | 33.0±2.0 | 73.3±5.6 | 122 | 27.4±1.0 | 37.2±1.86 | 36 | 96±3 | 142±7 | 48 |
15 | 0.527±0.020 | 0.451±0.048 | 14 | 4.505±0.070 | 4.104±0.538 | 9 | 41.0±1.0 | 83.7±2.1 | 104 | 37.0±2.0 | 45.7±1.38 | 23 | 94±4 | 139±16 | 48 |
16 | 0.578±0.026 | 0.497±0.045 | 14 | 3.805±0.050 | 3.693±0.026 | 3 | 27.4±0.9 | 80.7±4.0 | 195 | 32.0±2.0 | 34.9±2.06 | 9 | 100±8 | 149±10 | 49 |
Ti, Fe, Ni, Cu, and Zn were the most common elements in the geological samples. From Table 2, Ti and Fe, whose concentration exceeded several thousands of ppm, were labeled using percentage symbols (%), whereas the unit used for Ni, Cu, and Zn was micrograms per gram (µg/g). It is clear that the calculated contents for high-concentration elements are close to the standard contents. In particular, the calculated results for Fe are in good agreement with the standard contents and the corresponding relative errors are comparatively lower than those of the low-concentration elements. To intuitively analyze the trend changes of the content of each element, the resulting data were plotted as column graphs, with the error bars [34] representing standard deviation, in Fig. 8. The red columns stand for the standard contents, and the shadow columns represent the calculated contents. The blue line is the relative error level.
-201903/1001-8042-30-03-017/alternativeImage/1001-8042-30-03-017-F008.jpg)
As can be seen from Fig. 8, the calculated content has the same variation tendency as the standard content among the 13 Nss samples, which reflects the feasibility of using the FSLS algorithm. There is a close relationship between the calculated content and the standard content except for Ni, whose relative error is larger than 100%. The analysis results are as follows.
(1) For high-concentration elements, such as Fe (as shown in Fig. 8b), whose maximum standard content is 8.828%, the minimum relative error is 0.35% (Nss 5). However, the relative error increases with the decrease of its standard content. When the standard content is 2.462%, the relative error reaches 18.64% (Nss 2), which is acceptable in EDXRF analyses. This is mainly because Fe is the major element in the solid samples; its concentration exceeds 1.39%. The background scattering intensity of the original X-ray beam can be considered inversely proportional to the element contents. Therefore, comparatively low backscattered radiation contributes little to the characteristic peak area of Fe during the background-deducing step. In addition, the count rate of the detector is proportional to the content of Fe, as shown in Fig. 9a. Increasing the count rate would effectively reduce the statistical error. The calculation results of Ti, which is also a major element in the Nss samples, are similar to those of Fe. The differences between the red columns and the shadow columns for Ti in Fig. 8a exist for the same reason as for Fe.
-201903/1001-8042-30-03-017/alternativeImage/1001-8042-30-03-017-F009.jpg)
(2) Ni, Cu, and Zn are micro-elements in the 13 Nss samples because their average contents are just 33.91 µg/g, 62.85 µg/g, and 115.08 µg/g, respectively. Their actual characteristic X-ray peaks are probably affected by the high backscattered radiation. As shown in Figs. 8c, d, and e, the shadow columns of the calculated contents for these elements are almost higher than the red columns of their standard contents. This may be due to the absorption-enhancement effects of other trace elements, such as Ce, Ba, Pb, etc., which leads to the actual characteristic X-ray intensity line deviating from the true intensity line. Among the 13 Nss samples, the one with a high content of Ni, Cu, and Zn has a smaller relative error than the other samples. The differences found between them are significantly related to measurement accuracy.
(3) However, for micro-element Ni and as can be seen from Fig. 8c, the maximum relative error is 292.69%, which corresponds to 12 µg/g (Nss 3), and the minimum relative error is 76.49%, which corresponds to 64 µg/g (Nss 4). The average error is up to 149.80%, and the reason for this is not just related to the trace amount of Ni in the solid samples. Except for the absorption-enhancement effect of the other micro-elements (which are neglected in this FSLS algorithm), the peak-overlap effect caused by the elements (such as Co) adjacent to Ni is another main factor. Besides, the net characteristic X-ray intensity of Ni is heavily affected by the characteristic Kβ rays of Fe, which are beyond the resolution capability of our detector. This leads to a strong increase in the weak peak area of the characteristic X-ray for Ni, and thus the calculated content of Ni is far in excess of the standard value. The former can be used to calibrate the inter-element effects via empirical coefficient approaches and, in the subsequent step, increasing the number of the spectral variables in the P0 matrix will, to some extent, reduce the mutual interference between elements. Furthermore, as can be seen from Fig. 9c, there is a non-linear relationship between the content of the Ni element and the counting rate of the system. Therefore, statistical fluctuations during the spectral data acquisition will seriously influence the final calculated results. It is crucial to improve the accuracy of detection systems. In addition, a single residual matrix is needed to optimize the FSLS algorithm, which can effectively modify the mismatch between the algorithm model and the X-ray characteristic spectrum data caused by statistical fluctuations, backscattered radiation, etc.
5 Conclusion
This paper introduces an FSLS method to quantitatively perform EDXRF analysis for unknown solid samples. Compared with the conventional FPM approach, it is a multivariate calibration method that is able to increase component selectivity and provide the possibility of detecting a sample as an outlier. The
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