| Literature DB >> 27446748 |
Abstract
In setting up the conditions for quantitative wavelength-dispersive electron microprobe analysis a number of parameters have to be defined for each element, namely accelerating voltage, beam current, and (for each element) x-ray line, spectrometer crystal, pulse-height analyser settings, background offsets, and counting times for peak and background. The choices made affect both the reliability of the results and the time taken to obtain a complete analysis. It is difficult for even an experienced user to arrive at the optimum set of conditions for any particular application, in view of the large number of interacting factors involved. Furthermore, optimum choices of some parameters are dependent not only on the concentration of the element concerned (for example, counting times) but also the concentrations of other elements which may have peaks that interfere with peak and/or background measurements, requiring alternative selections of x-ray line or spectrometer crystal. The various factors involved in arriving at an optimum routine and practical possibilities for computer-aided optimization are discussed here.Entities:
Keywords: background; optimization; overlaps; virtual WDS; wavelength dispersive x-ray analysis; wavelength dispersive x-ray spectrometers
Year: 2002 PMID: 27446748 PMCID: PMC4863850 DOI: 10.6028/jres.107.042
Source DB: PubMed Journal: J Res Natl Inst Stand Technol ISSN: 1044-677X
Fig 1Typical relative intensities (in arbitrary units) of K, L, and M α lines of pure elements as a function of atomic number (Z), for 20 kV accelerating voltage, using TAP, PET, and LiF spectrometer crystals. Where the wavelength ranges overlap, the crystal with the larger interplanar spacing gives the higher intensity, but sometimes the presence of interferences necessitates the use of the crystal with smaller spacing, on account of the higher wavelength resolution obtained. The wide range of intensities must be taken into account in selecting optimal counting times.
Fig. 2Simulated spectra of rare-earth elements (LiF crystal), with relative concentrations equal to average values for the Earth’s crust (LiF crystal). The Eu Lα1 peak suffers interference from peaks of other REE, which invariably coexist in natural REE-bearing minerals. In such phases the relative REE abundances commonly show enrichment or depletion of light relative to heavy REE, the implications of which for WD analysis may be studied by spectrum simulation [Ref. 9]. Optimum background offsets can be selected without the need for time-consuming spectral plots on actual specimens.