Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/8286
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dc.contributor.authorAhmed, N K-
dc.contributor.authorAbbady, A-
dc.contributor.authorArabi, A M El-
dc.contributor.authorMichel, R-
dc.contributor.authorKamel, A H El-
dc.contributor.authorAbbady, A G E-
dc.date.accessioned2010-04-26T04:20:47Z-
dc.date.available2010-04-26T04:20:47Z-
dc.date.issued2006-03-
dc.identifier.issn0975-1041 (Online); 0019-5596 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/8286-
dc.description209-215en_US
dc.description.abstract The radioactivity contents of various radionuclides in rocks play an important role in health physics and geo-scientific research. The naturally occurring radionuclides 226Ra, 232Th and 40K are the main sources of radiation in soil and rocks from which traditional building materials are derived. These radionuclides pose exposure risks externally due to their gamma-ray emissions and internally due to radon and its progenies, which emit alpha particles. The activity concentration (Bq/kg) in igneous and metamorphic rock samples from different locations in Egypt and Germany has been analysed. The concentration values of samples for 226Ra, 232Th and 40K were found in the range of 3.9 : 57.4, 3.2 : 53.4 and 202 : 1211 in Egypt and 5.1 : 76, 3.4 : 70 and 10 : 2070, respectively in Germany. Even though these radionuclides are widely distributed, their concentrations depend on the local geological conditions. en_US
dc.language.isoen_USen_US
dc.publisherCSIRen_US
dc.relation.ispartofseriesH01J65/08en_US
dc.sourceIJPAP Vol.44(03) [March 2006]en_US
dc.subjectRadioactivityen_US
dc.subjectIgneousen_US
dc.subjectMetamorphic rocken_US
dc.titleComparative study of the natural radioactivity of some selected rocks from Egypt and Germanyen_US
dc.typeArticleen_US
Appears in Collections:IJPAP Vol.44(03) [March 2006]

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