Abstract
X-ray fluorescence spectrometry (XRF) is a powerful tool for the analysis of solid material. That is the reason why the technique was applied for the determination of rare earth elements (REEs) since about 1970. At present, energy-dispersive XRF and wavelength-dispersive XRF are used for the analysis of pressed powder pellets or fused Li-borate beads containing REEs. The production of reliable results can only be achieved by careful optimization of the parameter, in particular the selection of spectral lines. The quantification is based on a calibration realized by using reference samples.
1 Introduction
The use of X-ray fluorescence spectroscopy (XRF) for the analysis of rare earth elements (REEs) is divided into the analysis of minors and traces in materials with natural origin and the analysis of industrial products containing REEs as main, minor or trace components.
The advantage of XRF is the direct analysis of solid material which could be presented directly as powder or pressed pellet. The disadvantage could be a high error and a high average lower limit of detection (LLD) of about 1–10 μg/g.
Nevertheless, XRF is very often used as a rapid method with high throughput. For some applications, the measurement error could be reduced by using fusion technology as sample preparation method. The LLD could be further reduced by using preconcentration methods.
One typical application is the analysis of REE in geological materials as overview or screening in addition to other techniques like inductively coupled plasma-optical emission spectrometry (ICP-OES) or inductively coupled plasma-mass spectrometry (ICP-MS).
Other typical applications are the analysis of REE as tracer in polymers [1], as impurity in pure chemicals, as component in glass, e.g., light-emitting diodes, as component in polishing powders, as component in magnets and generally as component in recycling processes.
For all these applications, the sample preparation procedure as well as the measurement conditions has to be adapted to the REE present in the samples.
2 Principle of X-ray fluorescence analysis
X-ray fluorescence radiation is an electromagnetic radiation with high energy. Energetically, it lies between γ -radiation and UV radiation.
X-ray fluorescence is generated by, among other processes, the ionization of the inner shell of an atom if radiation with high energy (0.1–100 keV) interacts with an atom. However, the probability that it will occur is small and is also dependent on the atomic number of the atom. Most of the excitation energy is translated into heat, which is the reason that XRF instruments always need to be more or less cooled.
If ionization of an inner shell does occur, i.e., an electron is removed, then the hole is filled by an electron from a higher energy shell. The energy difference is released as X-ray fluorescence radiation and is characteristic for the element. Depending on which transition takes place, it is called radiation: K, L or M.
Figure 1 shows the typical electron transitions for the different shells. The lower line represents the innermost shell of an atom. The arrows symbolize an electron transition that is accompanied by the formation of an X-ray fluorescence line, e.g., Kα1. The intensity of the lines decreases in the order Kα, K

Transition of electrons in inner shells (a schematic setup of theenergy levels for the single X-ray emission lines of the K- and L-series).
For example, an electron

A schematic setup of the excitation of X-ray fluorescence analysis.
The most important equations for XRF are listed in Table 1.
Basic equations for X-ray fluorescence analysis.
Moseley’s law | |
Fluorescence yield | |
Bragg’s law | |
d: Interplanar distance, θ: scattering angle, n: positive integer, λ: wavelength | |
Theoretical fluorescence intensity (K-shell) | |
3 XRF methods
Depending on the method of detection, instrument technology is divided into energy-dispersive (EDXRF) and wavelength-dispersive (WDXRF) X-ray fluorescence analysis [2–9].
3.1 Energy-dispersive X-ray fluorescence analysis
With EDXRF, the sample is excited by the X-ray tube directly or through a filter (Figure 3). A semiconductor detector (e.g., silicon–lithium semiconductor, pin diode or silicon drift chamber) analyzes the X-ray fluorescence radiation that comes directly from the sample.

A schematic setup of an energy-dispersive X-ray fluorescence spectrometer with direct excitation.
Here, the detector together with the associated electronics counts and sorts, according to energy, all of the photons that reach it. A pulse height spectrum that indicates the number of photons or impulses for a given energy is established. The detector typically has only a few μ s for processing, so that in case of a modern silicon drift detector (SDD), processing is accordingly limited to approximately 1,000,000 pulses/s. Using a filter, a portion of the exciting radiation can be screened out to avoid overloading the detector.
XRF with polarizing excitation represents an alternative design for EDXRF (Figure 4). Here, the radiation coming from the tube is deflected by 90° and is then used to irradiate the sample. The detector must be perpendicular to the plane determined by the tube, target and sample. The most important effect is that by deflecting the X-ray radiation by 90°, the radiation is polarized and the spectral background in the spectrum is reduced.

4c vector – “Configuration of an energy-dispersive X-ray fluorescence spectrometer with polarized excitation”.
The analysis of REE by EDXRF suffers from big overlaps between the spectroscopic lines so that detector resolution becomes the limiting factor.
3.2 Wavelength-dispersive X-ray analysis
WDXRF uses, like some EDXRF, direct excitation (Figure 5). Here, it is also possible to work with filters to block or weaken components of the excitation radiation. The major difference is the method of detection of the X-ray fluorescence radiation for WDXRF. Using a goniometer, only one wavelength from the spectrum is fed to the detector, i.e., it measures only one line from one element. In order to conduct multiple element analyses, it is necessary to create a serial measuring program that drives to and analyzes all of the lines of interest, one after another. There are, however, so-called simultaneous spectrometers: In this case, there is a set channel for each element consisting of a fixed crystal with corresponding detector arranged around the sample. When combined with a goniometer, this forms a very fast, high-performance XRF instrument that is especially useful for process control.

Schematic setup of a wavelength-dispersive X-ray fluorescence spectrometer.
Most of the XRF spectrometers nowadays are equipped with an X-ray tube with a target “Rh”. Nevertheless, for the analysis of REE, an X-ray tube with targets “Au” and “W” would be a better choice than Rh to excite the K- and L-lines of the REE [10].
The analysis of REE by WDXRF still remains a challenge even if the resolution of the goniometer is much better than for EDXRF. There are still a lot of line overlaps which cannot be totally resolved. The final performance of the XRF analysis of REE is therefore strongly depending on the availability of overlap-free analyte lines which could be used for the determination.
3.3 Comparison of EDXRF–WDXRF
In general, it is possible to say that the two techniques are complimentary; one supplements the other. EDXRF has a time advantage, as all elements are measured simultaneously, whereas the (serial) WDXRF measures the elements one after another.
WDXRF has a resolution and sensitivity advantage which is especially useful in the range of atomic numbers up to 30 and 55–80 which also includes most of REEs.
3.4 Other XRF techniques
3.4.1 Handheld XRF instruments
Handheld XRF instruments are based on EDXRF with direct excitation. Combined with a low-power X-ray tube, they suffer from low resolution and low sensitivity for REE analysis.
3.4.2 Total reflection XRF
Total reflection is a special version of XRF which works only with liquid samples. Therefore, the sample needs to be digested first and then a small amount is dried on a quartz disk which then is irradiated by X-rays under total reflection conditions [11]. An example for the determination of REE in geological materials is described in Ref. [12].
4 Sample preparation
The performance of XRF for REE analysis is strongly dependent on sample preparation. However, the sample preparation strategy must be in agreement with the chosen measurement conditions especially the analyte lines, K- or L-series.
4.1 Pressed pellets techniques
Pressing a sample leads to a defined density in the pellet. This guarantees reproducible sample preparation.
The Following procedures are used to press samples:
Direct pressing
Pressing in aluminum trays
Pressing in rings
Pressing with binders
Pressing onto a backing material
Manually mixing with mortar and pestle is arduous and not very effective. This is why, I recommend using a simple mixer, whereby the high reproducibility is also ensured.
4.1.1 In practice: Making a pellet
The complete procedure for making a pellet, from preparation of the sample to pressing, is shown in Figure 6 [2].

Illustration of all steps to produce a pressed pellet with binder.
After grinding the sample, 4 g of the sample is mixed with 1 g binder (e.g., wax [2]). Before pressing, the pressing tool can be covered with a pellet film, which prevents subsequent sticking, simplifies cleaning and prevents contamination of the pellet from the hardened steel (Cr, Fe). Aluminum cups help stabilize the pellet and enable easy labeling but have no additional usefulness. Table 2 presents figures based on experience for the pressure required depending on the diameter of the pressed pellet. Here, it is important to remember that the pressing procedure must be reproducible, i.e., the same density must be obtained in each pressed pellet. Direct pressing from 0 to, e.g., 30 tons can prevent the air contained in the sample from completely escaping. This leads to cracks in the pressed pellet. Use of a lower pressure or a pressing procedure in several steps is recommended.
Recommended pressuredepending on the diameter ofthe pressed pellet.
Diameter | Pressure (t) |
---|---|
32 mm | 15–20 |
40 mm | 20–30 |
35-mm ring inside | max. 30 |
When there is not enough sample material, but a stable pressed pellet is still required, then the sample can be pressed onto a backing. In literature [13], this is presented for yttrium oxide: 400 mg of sample (dissolved in acid and precipitated as oxalate) is mixed with an equal amount of boric acid and then pressed on a boric acid layer as backing. However, since December 1, 2010, boric acid is classified as GHS08 health hazard which means that it should be replaced by a non-hazardous material. In Ref. [2], a cellulose-type material called BOREOX is presented as a good non-hazardous replacement.
It has to be mentioned that sample thickness should always be higher than the penetration depth of the XRF line used for calibration. Table 3 lists recommended minimum sample thicknesses or masses depending on K- or L-lines for REE analysis.
4.2 Fusion technology
In XRF, most solid samples are prepared as pressed pellets, whereby the achievable precision suffers from so-called particle size effects. They describe the phenomenon that the intensity of X-ray fluorescence is depending on particle size and shape. If the achieved precision with pressed pellets is not sufficient, the sample must be prepared using a fusion process.
The fusion provides an ideally homogeneous sample with a defined density and without particle size effects. In addition, homogeneity and a perfect surface lead to a much smaller calibration error.
Figure 7 shows the fundamentals of the fusion process.

Principle of the fusion process.
The following conditions must be fulfilled for fusion of a sample:
Finely ground oxidic sample material
Borate as the fusion material and glass-forming agent
Platinum–gold crucible
Platinum–gold casting dishes
Temperatures higher than the borate melting point
For ICP-OES or ICP-MS measurements, the melted sample could be cast directly into the acid instead of casting a bead.
Further sample preparation methods using fusion known from literature:
Rock samples are mixed 1:5 with lithiumtetraborate and fused at 1,000°C in a muffel furnace. Then dissolved in HF and HNO3 followed by a separation of REE from the matrix by anion exchange and subsequent preconcentration. Finally, the REE are coprecipitated with rhodizonate and tannin. The precipitate is collected on membrane filter which is measured with XRF [14].
To fuse REE rock samples, three different dilutions between sample and flux are suggested by Nakayama and Nakamura [15]:
A ratio of 1:1 for REE, 1:2 for Th and U and 1:10 for major and minor elements. It is a challenge to perform a low-dilution fusion with a ratio 1:1 to avoid inclusions and bubbles. Therefore, the fusion had to be repeated a second time and LiCl was added to avoid devitrification. The LLDs achieved with this method are in the range of 0.6 (Th, U) and 0.7–6.5 μg/g for REE.
The authors of Ref. [16] describe a method for raw materials with major and minor concentrations of REE: the REEs are separated from the main matrix by dissolving them with HF/HNO3 and Na2CO3/Na2O2 and final precipitation as oxalate. Then, a fusion of the residue with lithiumtetraborate was done. Cr and Mo were used as internal standard. Results are presented for light REEs, Y and Th over a wide concentration range (La, Ce, Nd, Pr 0.02–25 %; Sm, Gd, Eu, Y and Th 0.005–1 %).
In Ref. [10], monazite samples were fused with pure lithiumtetraborate or a mixture of lithiumtetraborate and lithiummetaborate (90:10) in a ratio of 0.5 g sample and 9.5 g flux and a few drops of LiBr (25 %) as releasing agent.
4.3 Additional sample preparation techniques
Roelandts [17] describes the analysis of REEs in apatit. The sample is dissolved in HNO3, then the REEs are separated by a mixed solvent anion exchange and kept by the resin which is then analyzed by XRF on top of a disk.
Another preconcentration method in combination with a thin film measurement is presented in Ref. [18]: 1-g sample was fused with 4-g Na2O2 and finally dissolved in acid. The REEs were separated from the main components by ion exchange. The XRF measurement was done at an ion-exchange paper.
Also in Ref. [19], the XRF measurements were performed directly on a filter. After digestion of the sample with acid, the REEs are preconcentrated by using an arsenazo III complex which was collected on a filter by chemofiltration.
5 Practical application of REEs determination
5.1 Reference materials
To perform and to verify an XRF calibration, reference materials are required. Table 4 lists the reference materials mentioned in the literature cited in this article. Most of them are already sold out. However, there are replacements and many other reference materials which could easily be explored by free accessible databases in the internet. Table 5 gives an overview.
Reference materials cited in REE literature.
Reference material | Producer |
---|---|
SRM 613 | NIST, National Institute of Standards and Technology, USA |
JG-1a, JR-2, JR-3, JG-1, JB-1 | GSJ, Geological Survey of Japan |
SARM 1 (NIM-G) | SARM, Mintek South Africa |
IGS-36 | BGS, British Geological Survey |
BCR-1, G-2, GSP-1, BHVO-1 | USGS, U.S. Geological Survey |
Free accessible databases for the searchof reference materials containing REEs.
Database | Reference |
---|---|
FLUXearch | www.fluxearch.com |
COMAR | www.comar.bam.de |
GeoReM | georem.mpch-mainz.gwdg.de |
5.2 Measuring parameters
Starting the configuration of an XRF spectrometer for the determination of REE, first the spectral line for calibration must be selected. REEs have three K-lines and about seven L-lines which could be used. However, the sensitivity of the analyte lines differs a lot. From the K-line series, the K
K series lines could be used for La, Ce, Pr, Nd, Sm if pressed pellets are used as sample preparation. Based on the large penetration depth, particle size effects will be reduced.
Figure 8 shows the K series lines for La to Sm measured with WDXRF equipped with a target X-ray tube “Rh”, 60 kV excitation, lithium fluoride (LIF) 220 crystal, 0.15° fine collimator and SC as detector. The graph demonstrates how the sensitivity decreases from La to Sm.

Overlapped K-line spectra of REE measured at 40,000
For comparison, Figure 9 shows the K series lines of the elements La to Sm measured with an EDXRF equipped with a target X-ray tube “W”, 60 kV excitation combined with a Al2O3 polarizer target and a Silicon SDD. The resolution is better than in WDXRF and there are less line overlaps in the spectrum. Based on the fact that the concentrations for the REE shown in Figure 8 are 40,000 μg/g each and the concentrations for the REE shown in Figure 9 are only 100 μg/g each, it can be seen that also the sensitivity is much higher.

Overlapped K-line spectra of REE measured at 100
L-series lines must be used with fusion disks because of infinite thickness limitations. Figures 10–12 show the complete L-line spectra of La, Gd and Lu as an example measured with WDXRF, Rh target X-ray tube, 40 kV excitation, LIF 220 crystal, 0.15° fine collimator and flow counter detector (FPC). The L-lines show always the same line pattern (out of the L

L-series lines of 100 μg/g La in cellulose measured with WDXRF, Rh-tube, 40 kV, LIF 220, 0.15°, FPC.

L-series lines of 100 μg/g Gd in cellulose measured with WDXRF, Rh-tube, 40 kV, LIF 220, 0.15°, FPC.

L-series lines of 100 μg/g Lu in cellulose measured with WDXRF, Rh-tube, 40 kV, LIF 220, 0.15°, FPC.
For comparison, Figure 13 shows the overlap of single element L-line spectra of the REE measured with an EDXRF with W target X-ray tube, 40 kV excitation with a Mo secondary target and an SDD. However, the resolution of the detector is not sufficient to resolve the different lines.

Overlapped L-line spectra of REE measured at 100
The most difficult work in creating a measurement program for REEs is the selection of the analyte lines and the corresponding background positions. Because of the high numbers of line overlaps, a general recommendation is very difficult. Figures 14–17 show a full scan of all analyte lines in the region of the REE lines. This measurement was performed on the glass drift monitor sample FLX-S13 from FLUXANA which contains most of the elements which show lines in this spectrum. The detailed study of all line marks gives a good impression of where to select the analyte lines and the corresponding background positions for the required application.

Scan 1/4 of FLUXANA drift monitor sample FLX-S13 with WDXRF, Rh tube 40 kV, LIF 220, 0.15°, FPC.

Scan 2/4 of FLUXANA drift monitor sample FLX-S13 with WDXRF, Rh tube 40 kV, LIF 220, 0.15°, FPC.

Scan 3/4 of FLUXANA drift monitor sample FLX-S13 with WDXRF, Rh tube 40 kV, LIF 220, 0.15°, FPC.

Scan 4/4 of FLUXANA drift monitor sample FLX-S13 with WDXRF, Rh tube 40 kV, LIF 220, 0.15°, FPC.
Table 6 lists all X-ray fluorescence lines of REE which show relevant intensities and Figure 18 lists all line overlaps which have to be taken into account for REE.
Z | Element | K | K | K | L | L | L | L | L | L | L | M |
---|---|---|---|---|---|---|---|---|---|---|---|---|
57 | La | 33.4418 | 33.0341 | 37.801 | 4.65097 | 4.63423 | 5.0421 | 5.3835 | 5.1434 | 5.0618 | 5.7885 | 0.833 |
58 | Ce | 34.7197 | 34.2789 | 39.2573 | 4.8402 | 4.823 | 5.2622 | 5.6134 | 5.3653 | 5.2774 | 6.052 | 0.883 |
59 | Pr | 36.0263 | 35.5502 | 40.7482 | 5.0337 | 5.0135 | 5.4889 | 5.85 | 5.5918 | 5.4981 | 6.3221 | 0.929 |
60 | Nd | 37.361 | 36.8474 | 42.2713 | 5.2304 | 5.2077 | 5.7216 | 6.0894 | 5.8294 | 5.7216 | 6.6021 | 0.978 |
62 | Sm | 40.1181 | 39.5224 | 45.413 | 5.6361 | 5.609 | 6.2051 | 6.586 | 6.3180 | 6.1962 | 7.178 | 1.081 |
63 | Eu | 41.5422 | 40.9019 | 47.0379 | 5.8457 | 5.8166 | 6.4564 | 6.8432 | 6.3716 | 6.4378 | 7.4803 | 1.131 |
64 | Gd | 42.9962 | 42.3089 | 48.697 | 6.0572 | 6.025 | 6.7132 | 7.1028 | 6.8310 | 6.6873 | 7.7858 | 1.185 |
65 | Tb | 44.4816 | 43.7441 | 50.382 | 6.2728 | 6.238 | 6.978 | 7.3667 | 7.0961 | 6.9403 | 8.102 | 1.24 |
66 | Dy | 45.9984 | 45.2078 | 52.119 | 6.4952 | 6.4577 | 7.2477 | 7.6357 | 7.3702 | 7.2039 | 8.4188 | 1.293 |
67 | Ho | 47.5467 | 46.6997 | 53.877 | 6.7198 | 6.6795 | 7.5253 | 7.911 | 7.6518 | 7.4711 | 8.747 | 1.348 |
68 | Er | 49.1277 | 48.2211 | 55.681 | 6.9487 | 6.905 | 7.8109 | 8.189 | 7.9392 | 7.7453 | 9.089 | 1.406 |
69 | Tm | 50.7416 | 49.7726 | 57.517 | 7.1799 | 7.1331 | 8.101 | 8.468 | 8.2309 | 8.0258 | 9.426 | 1.462 |
70 | Yb | 52.3889 | 51.354 | 59.37 | 7.4156 | 7.3673 | 8.4018 | 8.7588 | 8.5368 | 8.3132 | 9.7801 | 1.521 |
71 | Lu | 54.0698 | 52.965 | 61.283 | 7.6555 | 7.6049 | 8.709 | 9.0489 | 8.8470 | 8.6065 | 10.1434 | 1.581 |
![Figure 18: X-ray fluorescence line overlaps relevant for REE in the range of 3–10 keV [2].](/document/doi/10.1515/psr-2016-0061/asset/graphic/j_psr-2016-0061_fig_018.jpg)
X-ray fluorescence line overlaps relevant for REE in the range of 3–10 keV [2].
5.3 Analyte lines
Table 7 gives an indication which analyte lines should be selected for the analysis of REE. The selection considers a minimum of line overlaps which have to be taken into account by spectrum scans or the measurement of single element standards. Also, background positions have to be chosen based on individual measurements on the samples which have to be investigated.
Recommended analyte lines of REE from the author with alternatives in brackets. For comparison, also the recommendations from literature are given.
Z | Element | Author | [10] | [22] | [3] | [16] |
---|---|---|---|---|---|---|
57 | La | L | L | L | L | L |
58 | Ce | L | L | L | L | L |
59 | Pr | L | L | L | L | L |
60 | Nd | L | L | L | L | L |
62 | Sm | L | L | L | L | L |
63 | Eu | L | L | L | L | |
64 | Gd | L | L | L | L | L |
65 | Tb | L | L | L | L | |
66 | Dy | L | L | L | L | |
67 | Ho | L | L | L | L | |
68 | Er | L | L | L | L | |
69 | Tm | L | L | L | ||
70 | Yb | L | L | L | L | |
71 | Lu | L | L | L |
A complete measurement program for WDXRF equipped with target x-ray tube “Rh” to measure rock samples is presented in Ref. [15].
5.4 Lower limit of detection (LLD)
Figures 19 and 20 show LLDs of REE in different matrices and measured with WDXRF equipped with a target x-ray tube “Rh” and EDXRF equipped with a target x-ray tube, W both working with 60 kV. While EDXRF shows here a higher sensitivity for the K-lines, WDXRF shows a higher sensitivity for most of the L-lines.

LLD of REE measured with Kα 1-line (WDXRF: 20 s per line in lithiumtetraborate matrix, EDXRF: 600 s in cellulose matrix).

LLD of REE measured with Lα 1-line (WDXRF: 20 s per line, EDXRF: 600 s, both in cellulose matrix).
6 Calibration
The calibration strategy is depending on the sample preparation. For pressed pellets, particle size effects and matrix effects dominate the interelement corrections. To build up a calibration, many standard materials analyzed by other analytical methods are required. Most of the instrument manufacturers offer such calibration packages already. In fused bead sample preparation, the sample is totally dissolved and doesn’t show any particle size effects. Additionally, matrix effects could be reduced because of the dilution or the presence of a strong absorber element. Fusion shows the advantage of building an independent calibration traceable to the weights of pure chemicals. An example of building such a calibration is given in Ref. [15]. For such a calibration, less calibration samples are required and the need of external standard materials is small. Also, FLUXANA offers calibration sets for REE applications as fused beads.
Attention has to be paid to sample thickness if K-lines are used for analysis. There is a possible risk that the samples are not infinitely thick for the high energies of K-lines. If a target x-ray tube “Rh” is used, a possible correction for the imperfect thickness and additionally for any kind of matrix effects could be the normalization to the Rh Kα Compton Peak because no absorption edges are found in between.
6.1 Other calibration strategies mentioned in literature
Macháček and Weiss [16] describe for the calibration of REE an empirical correction in combination with internal standard elements Cr and Mo.
Michelsen [22] gave an overview about the use of an internal standard like Sr for Y, the use of standard addition for REE in rock samples and dried solutions on filters.
7 Summary
The analysis of REE with X-ray fluorescence analysis remains a challenge. An XRF application of REE requires an extensive and careful development by the analyst. The significance of the final result depends on the choice of the sample preparation method, the measurement conditions, the calibration strategy and the selection of standard materials.
The choice of fusion or pressed pellets will influence the sensitivity. Sample thickness must be in agreement with line selection. The choice of the analyte line and the corresponding background has to take into account possible line overlaps. Calibration must consider matrix effects and interelement effects.
In literature, several examples are given on how to use XRF successfully for REE analysis. However, there could be always limitations based on particle size effects, line overlaps or poor sensitivity, so that other techniques like ICP-MS have to be used instead.
Finally, an intense study of the application problem has to prove that XRF could be used successfully to analyze REE in a certain sample type.
Acknowledgement
This article is also available in: Golloch, Handbook of Rare Earth Elements. De Gruyter (2016), isbn 978–3–11–036523–8.
References
[1] Bezati F, Froelich D, Massardier V, Maris E. Addition of tracers into the polypropylene in view of automatic sorting of plastic wastes using X-ray fluorescence spectrometry. Waste Manage 2009, 30, 591–6.10.1016/j.wasman.2009.11.011Search in Google Scholar
[2] Schramm R. X-Ray Fluorescence Analysis: Practical and Easy. Bedburg-Hau, FLUXANA, 2012.Search in Google Scholar
[3] Willis JP, Feather C, Turner K. Guidelines for XRF analysis. James Willis Consultants, 2014.Search in Google Scholar
[4] Willis JP, Duncan AR. Understanding XRF Spectrometry. Panalytical B.V., 2008.Search in Google Scholar
[5] Hahn-Weinheimer P, Hirner A, Weber-Diefenbach K. Röntgenfluoreszenzanalytische Methoden: Grundlagen und praktische Anwendungen in den Geo-, Material- und Umweltwissenschaften. Braunschweig and Wiesbaden, Vieweg, 1995.10.1007/978-3-642-57848-9Search in Google Scholar
[6] Jenkins R. X-Ray Fluorescence Spectrometry. 2nd edn. New York, John Wiley & Sons, Inc., 1999.10.1002/9781118521014Search in Google Scholar
[7] Grieken RE Van, Markowicz A. (ed.). Handbook of X-Ray Spectrometry. New York, Marcel Dekker, 1992.Search in Google Scholar
[8] Grieken RE Van, Markowicz A. (ed.). Handbook of X-Ray Spectrometry. 2nd edn. New York, Marcel Dekker, 2002.Search in Google Scholar
[9] Beckhoff B, Kanngießer B, Langhoff N, Wedell R, Wolff H (eds.). Handbook of Practical X-Ray Fluorescence Analysis. Berlin Heidelberg, Springer-Verlag, 2006.10.1007/978-3-540-36722-2Search in Google Scholar
[10] McNew EB, Willis JP. An evaluation of the analysis of Monazite and REE compounds by WDXRFS: a spectroscopist’s nightmare (or challenge?). Adv X-ray Anals 1999, 41, 829.Search in Google Scholar
[11] Klockenkämper R, von Bohlen A. Total-Reflection X-ray Fluorescence Analysis and Related Methods. New Jersey, Wiley, 2015.10.1002/9781118985953Search in Google Scholar
[12] Muia L, Grieken RV. Determination of rare earth elements in geological materials by total reflection X-ray fluorescence. Anal Chim Acta 1991, 251, 177.10.1016/0003-2670(91)87132-QSearch in Google Scholar
[13] Dixit RM, Deshpande SS. An XRF method for the determination of common rare earth impurities in high purity yttrium oxide. Fresenius’ Z Anal Chem 1977, 288, 180–2.10.1007/BF00439467Search in Google Scholar
[14] Bauer-Wolf E, Wegscheider W, Posch S, Knapp G, Kolmer H, Panholzer F. Determination of traces of rare earth elements in geological samples. Talanta 1993, 40, 9.10.1016/0039-9140(93)80137-GSearch in Google Scholar
[15] Nakayama K, Nakamura T. X-ray fluorescence analysis of rare earth elements in rocks using low dilution glass beads. Anal Sci 2005, 21, 7, 815–22.10.2116/analsci.21.815Search in Google Scholar PubMed
[16] Macháček V, Weiss D. X-ray fluorescence determination of light rare earth elements, Y and Th, by the fusion technique, X-Ray Spectrometry 1998, 14, 53.10.1002/xrs.1300140204Search in Google Scholar
[17] Roelandts I. Determination of light rare earth elements in apatite by X-ray fluorescence spectrometry after anion exchange extraction. Anal Chem 1981, 53, 4, 676–80.10.1021/ac00227a023Search in Google Scholar
[18] Robinson P, Higgins NC, Jenner GA. Determination of rare-earth elements, yttrium and scandium in rocks by an ion exchange-X-ray fluorescence technique. Chem Geol 1986, 55, 121.10.1016/0009-2541(86)90132-4Search in Google Scholar
[19] De Vito IE, Olsinaab RA, Masiab AN. Preconcentration and elimination of matrix effects in XRF determinations of rare earth elements by preparing a thin film through chemofiltration. J Anal At Spectrom 2001, 16, 275–8.10.1039/b008165pSearch in Google Scholar
[20] http://www.med.harvard.edu/JPNM/physics/refs/xrayemis.html (accessed 11 June 2012), from Bearden JA. X-Ray Wavelengths. Review of Modern Physics 1967, 1, 86–99.10.1103/RevModPhys.39.78Search in Google Scholar
[21] Zschornack G. Handbook of X-Ray Data. Berlin Heidelberg, Springer, 2007.Search in Google Scholar
[22] Michelsen OB. Analysis and Application of Rare Earth Materials. Nato Advanced Study Institute. Kjeller, Norway, Universitetsforlaget, 1972.Search in Google Scholar
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- Production and application of chitin
- Automated Quantitative Rare Earth Elements Mineralogy by Scanning Electron Microscopy
- Bacterial dye-decolorizing peroxidases: Biochemical properties and biotechnological opportunities
- Green Disposal of Waste Bisphenol A