JAKUBOVÁ, Petra and Jaromír LEICHMANN. Gamaspektrometrická charakteristika uhelných sedimentů boskovické brázdy a strusek vzniklých jejich spalováním (Gammaspectrometry of coal-bearing sediments from the Boskovice furrow and products of its burning). Geol. výzk. Mor. Slez. Brno: Masarykova Universita, 2011, XVII, 1-2, p. 183-186. ISSN 1212-6209.
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Basic information
Original name Gamaspektrometrická charakteristika uhelných sedimentů boskovické brázdy a strusek vzniklých jejich spalováním
Name (in English) Gammaspectrometry of coal-bearing sediments from the Boskovice furrow and products of its burning
Authors JAKUBOVÁ, Petra (203 Czech Republic, belonging to the institution) and Jaromír LEICHMANN (203 Czech Republic, guarantor, belonging to the institution).
Edition Geol. výzk. Mor. Slez. Brno, Masarykova Universita, 2011, 1212-6209.
Other information
Original language Czech
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Czech Republic
Confidentiality degree is not subject to a state or trade secret
RIV identification code RIV/00216224:14310/11:00049708
Organization unit Faculty of Science
Keywords in English Boskovice furrow; coal-bearing sediment; products of coal burning - slag; uranium (U); thorium (Th)
Tags AKR, rivok
Changed by Changed by: prof. RNDr. Jaromír Leichmann, Dr. rer. nat., učo 1923. Changed: 19/2/2011 11:52.
Abstract
Práce se zabývá gamaspektrometrickou a minerálně-chemickou charakteristikou popílků vzniklých spalováním uhlí v oslavanské elektrárně a uhelných jílovců se zvýšenou radioaktivitou boskovické brázdy
Abstract (in English)
The concentration of K, U, Th was measured by a portable gamma spectrometer on localities of radioactive anomaly (coal-bearing sediments and a slag dump) in the southern part of the Boskovice furrow, in the Rosice-Oslavany basin in Oslavany. Samples from both localities were measured by more precise laboratory gamma spectrometer and analyzed on an electron microprobe. The comparison of U and Th concentration among the samples of coal-bearing sediments and the slag samples (products of coal burning) reveal that the coal-bearing samples contain higher U concentration and lower Th than the slag samples. It was also determined that the U is bond into a limonite vein cutting the coal-bearing shale. The U is not concentrated into any of the phase found in glass of the slag, but it is distributed evenly throughout the glass.
Links
GA205/09/1257, research and development projectName: Využití gamaspektrometrie při studiu provenience siliciklastických sedimentů
Investor: Czech Science Foundation, Application of gamma-ray spectrometry in provenance studies of siliciclastic sediments
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