A Metallic Magnetic Calorimeter for Hard X-Ray and Gamma Ray Spectrometry

2008 ◽  
Vol 151 (3-4) ◽  
pp. 1080-1086 ◽  
Author(s):  
M. Rodrigues ◽  
E. Leblanc ◽  
M. Loidl ◽  
J. Bouchard ◽  
B. Censier ◽  
...  
1982 ◽  
Vol 16 ◽  
Author(s):  
John H. Howes ◽  
John Watling

ABSTRACTThis paper describes the fabrication of mercuric iodide nuclear radiation detectors suitable for X and gamma ray spectrometry at room temperature. The active area of the detectors studied are between 0.2 and 1.5cm sq and they are up to 0.5mm thick. The method of producing a stable electrical contact to the crystal using sputtered germanium has been studied. The X-ray resolution of a 1.5cm sq. area detector at 32 keV is 2.3 keV FWHM when operated at room temperature in conjunction with a time variant filter amplifier. A factor which is important in the fabrication of the detector is the surface passivation necessary to achieve a useful detector life.This type of detector has been used on a wavelength dispersive X-ray spectrometer for energy measurements between 10 and 100 keV. The advantages over the scintillation counter, more commonly used, is the improved resolution of the HgI2 detector and its smaller size. The analyser is primarily used for the detection of low levels of heavy metals on particulate filters. The detectors have also been used on an experimental basis for gamma ray backscatter measurements in the medical field.


2020 ◽  
Vol 98 (9) ◽  
pp. 877-882
Author(s):  
S.M. Karabıdak ◽  
S. Kaya

Pile up and dead time are two important corrections in the analysis of X-ray and gamma ray spectra. The most important of these is pile up correction because these peaks do not really exist in the spectra; they only seem to exist. For this reason, these peaks affect both the qualitative and quantitative accuracy of the analysis. In addition, the pile up pulses forming the pile up peaks increase the background count in the spectrum. Companies that produce X-ray or gamma ray detector systems design pile up reject circuits and integrate them into detector systems to prevent these pulses. These circuits have time limitations because they are made up of electronic devices. For this reason, the pile up problem cannot be solved completely in these circuits. Therefore, mathematical models based on a statistical approach are needed. Such a model was developed in this study. A computer program based on this model was developed. This developed program has been applied to X-ray and gamma ray spectra. It has been shown that this model provides about 2% correction in the main peak regions and significantly reduces background counts.


2015 ◽  
Vol 184 (1-2) ◽  
pp. 351-355 ◽  
Author(s):  
C. Bates ◽  
C. Pies ◽  
S. Kempf ◽  
D. Hengstler ◽  
A. Fleischmann ◽  
...  

2015 ◽  
Vol 95 ◽  
pp. 63-71 ◽  
Author(s):  
Natara D.B. de Castilhos ◽  
Fábio L. Melquiades ◽  
Edivaldo L. Thomaz ◽  
Rodrigo Oliveira Bastos

2008 ◽  
Vol 151 (1-2) ◽  
pp. 357-362 ◽  
Author(s):  
W.-T. Hsieh ◽  
J. A. Adams ◽  
S. R. Bandler ◽  
J. Beyer ◽  
K. L. Denis ◽  
...  

1963 ◽  
Vol 7 ◽  
pp. 584-589
Author(s):  
M. C. Farquhar ◽  
M. M. English

AbstractA method is presented for the quantitative determination of thorium in monazite by fluorescent X-ray speetrometry. Strontium is used as an internal standard, and sample preparation consists of mechanically blending the finelyground (325-mesh) sample with reagent grade strontium carbonate. The prepared sample blend is packed into a sample cup and irradiated at 50 kV and 27 mA. A lithium fluoride analyzing crystal is used, and the intensity of the Th Lα1 and Sr Kα peaks are scaled. Intensities are corrected fov background. Calibration is achieved with a single sample of monazite of known thorium content. National Bureau of Standards monazite sample number 2601 (9.65% ThO2) was used in this work. The standard monazite is blended with strontium carbonate, irradiated, and scaled under the same conditions as the sample. The thorium content of the sample is then calculated by the equation: %ThO2 = (R sample) (%ThO2 standard)/R standard, where R = Thcounts/sec/Srcounts/sec. Replicate results agreed within 0.2% ThO2 on six samples of monazite which contained from 4.4% to 6.8% ThO2. Independent results by a second laboratory show no significant difference in precision.The method was used to determine the thorium content gf several rare-earth materials which contained approximately 0.5% to 1.0% TriOs. The results agree closely with values obtained by gamma-ray spectrometry.


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