A METHOD OF MEASURING GAMMA-RAY ABSORPTION COEFFICIENTS AT 0.51 Mev

1951 ◽  
Vol 29 (1) ◽  
pp. 83-85 ◽  
Author(s):  
P. E. Argyle ◽  
G. M. Griffiths ◽  
J. B. Warren

The coincidence method described makes use of the angular correlation between pairs of annihilation quanta to eliminate the effect of scattered radiation usually present in absorption measurements. Mass absorption coefficients in (gm./cm.2)−1 found by this method are as follows:[Formula: see text]

2017 ◽  
Vol 50 (1) ◽  
pp. 1-13 ◽  
Author(s):  
R. W. Alkire

In an effort to improve the characteristics of a fluorescing metal-foil-based beam position monitor, a new bimetal ultra-thin (0.98/0.67 µm) Ti–Ni foil was introduced to replace an existing single-element ultra-thin 0.5 µm thick Cr foil. During characterization it was determined that absorption measurements on the bimetal foil could be used to fit the Ni mass absorption coefficients accurately in the vicinity of the Ni K edge. Comparison with experimental results from the literature demonstrated that the fitting procedure produced coefficients with uncertainties of the order of ±1%. Once determined, these fit coefficients allowed the thickness of an independently mounted 8 µm thick Ni foil to be computed from absorption measurements instead of relying on a tool-based measurement of the foil thickness. Using the 8 µm thick foil, a continuous map of Ni mass absorption coefficients was produced at 1 eV resolution throughout the near-edge region. This high-resolution map marks a significant improvement over the existing NIST XCOM or FFAST database mass absorption coefficients, which have estimated errors of 10–20% for the near-edge region.


Soil Research ◽  
1973 ◽  
Vol 11 (1) ◽  
pp. 83 ◽  
Author(s):  
BJ Bridge ◽  
N Collis-George

A traversing mechanism is described in which 100 mCi sources of americum-241 and caesium-137 are alternately brought into line with a sodium iodide (thallium) scintillation counter connected to a single-channel pulse height analyser equipped with two preset base lines. The equipment is capable of scanning a 10 cm diameter soil column equipped with sensors to a height of 200 cm, and facilities are provided for automatic indexing at preset intervals to an accuracy of 0.01 cm. Non-linear counting losses in the spectrometer system are described, and were found to be dependent on the window setting of the pulse height analyser. With the window setting adjusted to cover the apparent spread of the gamma peak, counting losses were negligible. Mass absorption coefficients of various materials were obtained using a compartmented box. Measured mass absorption coefficients of water, silica sand, and a chernozemic soil were 0.201, 0.247, and 0.303 cm2 g-1 respectively for americum-241, and 0.0826, 0.0746, and 0.0728 respectively for caesium-137. The precision of the apparatus was demonstrated by determining the moisture characteristic and bulk density characteristic of 0.5-1.0 mm aggregates of Narrabri soil during absorption and desorption. Gamma ray attenuation measurements and direct volumetric measurements were comparable. The standard deviations in the gamma ray measurements were found to be 0.03 g cm-3 for bulk density and 0.04 cm3 cm-3 for water content. Most of this inaccuracy arose from lack of precision in the americum-241 mass attenuation coefficient for the soil. By contrast, changes in moisture content and bulk density, at any level, of 0.004 cm3 cm-3 and 0.004 g cm-3 respectively, were statistically very significant.


Author(s):  
Samir A. Hamouda ◽  
Essam al-Talhi ◽  
Mohamed B. Abdelmalik

Information about gamma-ray mass absorption coefficients in different geological compounds with different percentage to their rations is vital for accurate gamma-ray spectroscopy analysis. In this paper, gamma-ray absorption coefficients for energy (10-150 keV) were calculated for Corundum (AL2O3), Quartz (SiO2), Calcite (CaCO3), Hematite (Fe2O3), and Magnetite (Fe3O4) compounds with their % mixtures.


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