Abstract
Sedimentary rocks from the borders of the Upper Silesian Coal Basin are the most popular origin of building materials in whole Silesia region. In situ gamma ray spectrometry was used to determine the activity concentration of nuclides from U series, Th series and potassium 40K in almost every kind of sedimentary rocks outcropping in the studied region. Measured activity concentration of particular nuclides such as 40K, U series, and Th series are mostly not higher than average activity concentrations of these nuclides in the continental crust. However, there are some significant exceptions such as clays from Blanowice and Krasiejow. In spite of that there isn’t any reason to stop using these rocks as building or other industrial material sources.
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References
Osika R: Geology of Poland. Vol. VI. Mineral deposits. Wyd. Geol., Warszawa, 1990.
Dadlez R., Marek S., and Pokorski J: Geological map of Poland without Cainozoic deposits, PIG, Warszawa, 2000.
EG&G ORTEC: In Situ Spectroscopy M-1-B32 M-1 Setup Supervisor Program. Software User’s Manual. EG&G ORTEC Part No. 779980, Oak Ridge, 2000.
Beck, H. L., De Campo, J. and Gogolak, C. V.: In situ Ge(Li) and Na(Tl) gamma-ray spectrometry. U.S. Department of Energy, Environmental Measurements Laboratory, HASL-258, New York, 1972.
Helfer I. K. and Miller K. M.: Health Phys. 55 (1988) 15.
ORTEC: Gamma Vision — 32 for M-1. Gamma-Ray Spectrum Analysis and MCA Emulator for Microsoft Windows 95, 98, and NT. Software User’s Manual. ORTEC Part No. 774780, Oak Ridge, 2000.
Eisenbud M. and Gesell T.: Environmental radioactivity from natural, industrial, and military sources. Academic Press, San Diego, 1997.
Bolewski A.: Mineralogia szczegółowa. Wydawnictwa Geologiczne. Warszawa, 1982.
Attendorn G. H. and Bowen C. N. R.: Radioactive and Stable Isotope Geology. Chapman and Hall, 1997.
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Lizurek, G., Dorda, J. Natural radioactivity of paleozoic and mesozoic sedimentary rocks from the Upper Silesian Coal Basin borders (Poland) — in situ gamma ray measurements. Czech J Phys 56, D95–D102 (2006). https://doi.org/10.1007/s10582-006-1004-7
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DOI: https://doi.org/10.1007/s10582-006-1004-7