1976
DOI: 10.4095/102609
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Part 1: determination of radioactive disequilibrium in uranium ores by alpha-spectrometry

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“…Since there are different elements in 238 U decay series, their reactions may be different in the same environment. For example, the chemical solubilities of radium, uranium, and thorium isotopes differ and differential leaching of isotopes is also another possibility (Killen and Carmicheal, 1976 (Yaprak and Aslani, 2010).…”
Section: Radioactivity Measurements and Dose Calculationsmentioning
confidence: 99%
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“…Since there are different elements in 238 U decay series, their reactions may be different in the same environment. For example, the chemical solubilities of radium, uranium, and thorium isotopes differ and differential leaching of isotopes is also another possibility (Killen and Carmicheal, 1976 (Yaprak and Aslani, 2010).…”
Section: Radioactivity Measurements and Dose Calculationsmentioning
confidence: 99%
“…Since there are different elements in 238 U decay series, their reactions may be different in the same environment. For example, the chemical solubilities of radium, uranium, and thorium isotopes differ and differential leaching of isotopes is also another possibility (Killen and Carmicheal, 1976). Equilibrium time is determined by the half-life of the longest-lived isotope in each series, which is 234 U (t 1/2 250,000 years) in the 238 U series and 228 Ra (t 1/2 5.75 years) in the 232 Th series (Dickson et al, 1982).…”
Section: Radioactivity Measurements and Dose Calculationsmentioning
confidence: 99%
“…The sample powder was deposited from the water suspension onto a polished 22 mm stainless steel disc, evaporated and weighed. This non-destructive method (Jarka, 2007) is a modified procedure of the one described by Killeen and Carmichael (1976). Reference materials CRM 129-A (natural U oxide, isotopic) and BL-5 (U ore) were used.…”
Section: Alpha Spectroscopymentioning
confidence: 99%