2004
DOI: 10.1016/j.jenvrad.2004.01.004
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Specific activity and hazards of granite samples collected from the Eastern Desert of Egypt

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Cited by 174 publications
(91 citation statements)
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“…In addition, the identity and geographic origin of the stones included in this study is not known precisely because naming practices for granite are not standardized (Anjos et al, 2005). Nonetheless, the activity concentrations for 40 K, and the 232 Th and 226 Ra series observed in these stones are within the range reported for granite building materials in the scientific literature (Mustonen, 1984;NCRP, 1987a;Mustapha et al, 1997;Chowdhury, Alam and Ahmed, 1998;European Commission, 1999;Lee, Kim, Lee and Kang, 2001;IAEA, 2003;Kumar, Sengupta and Prasada, 2003;Arafa, 2004;Ahmed, 2005;ICRP, 2005;Al-Saleh and Al-Berzan, 2007;El-Taher, Uosif and Orabi, 2007;Lu, Wang, Jia and Wang, 2007;Ghosh et al, 2008;Kitto, Haines and Diaz Arauzo, 2008;Mujahid et al, 2008). Therefore, these samples of granite intended for use as interior work surfaces contain amounts of naturally occurring radioactive materials that are similar to levels in other types of granite building materials reported in the literature for which larger numbers of samples have been examined.…”
Section: Discussionmentioning
confidence: 90%
See 1 more Smart Citation
“…In addition, the identity and geographic origin of the stones included in this study is not known precisely because naming practices for granite are not standardized (Anjos et al, 2005). Nonetheless, the activity concentrations for 40 K, and the 232 Th and 226 Ra series observed in these stones are within the range reported for granite building materials in the scientific literature (Mustonen, 1984;NCRP, 1987a;Mustapha et al, 1997;Chowdhury, Alam and Ahmed, 1998;European Commission, 1999;Lee, Kim, Lee and Kang, 2001;IAEA, 2003;Kumar, Sengupta and Prasada, 2003;Arafa, 2004;Ahmed, 2005;ICRP, 2005;Al-Saleh and Al-Berzan, 2007;El-Taher, Uosif and Orabi, 2007;Lu, Wang, Jia and Wang, 2007;Ghosh et al, 2008;Kitto, Haines and Diaz Arauzo, 2008;Mujahid et al, 2008). Therefore, these samples of granite intended for use as interior work surfaces contain amounts of naturally occurring radioactive materials that are similar to levels in other types of granite building materials reported in the literature for which larger numbers of samples have been examined.…”
Section: Discussionmentioning
confidence: 90%
“…A number of studies have reported on the concentrations of natural radionuclides (i.e., activity concentrations) for granite samples obtained from Egypt, Saudi Arabia, Pakistan, South Korea, China, Brazil, Kenya, and Finland (Mustonen, 1984;NCRP, 1987a;Mustapha et al, 1997;Chowdhury et al, 1998;European Commission, 1999;Lee et al, 2001;IAEA, 2003;Kumar et al, 2003;Arafa, 2004;Ahmed, 2005;ICRP, 2005;Al-Saleh and Al-Berzan, 2007;El-Taher et al, 2007;Lu et al, 2007;Ghosh et al, 2008;Kitto et al, 2008;Mujahid et al, 2008). Although the activity concentrations for the majority of those samples were below health-based screening levels and exposure guidelines used in the US, Europe, and elsewhere, a portion of the granite samples had a radiation hazard index that exceeded the European Commission (EC) screening value for limited use as superficial building materials (external dose of 0.3 mSv/a) (European Commission, 1999).…”
Section: Introductionmentioning
confidence: 99%
“…II). (Beretka and Mathew, 1985;Arafa, 2004). The radium equivalent can be estimated using the equation (Beretka and Mathew, 1985;Ademola and Atare, 2010) purposes in terms of radiological hazard the radium equivalent activity must not exceed 370 Bq.kg -1 .…”
Section: Activity Concentrationmentioning
confidence: 99%
“…Most natural rocks contain 40 K and the decay series of 238 U and 232 Th. The concentrations of natural radionuclides in rocks vary considerably depending on the rock formation and lithologic character (Anjos et al, 2005;Abd and Saleh, 2003;Arafa, 2004).…”
Section: Introductionmentioning
confidence: 99%
“…Radon flux for these stones has been previously reported to range from 0.01 to 13.5 Bq/m 2 /h among B500 samples of structural and unidentified granite building materials obtained from several nations of Africa, Asia, and the Middle East (Khan et al, 1992;Chao and Tung, 1999;El-Dine et al, 2001;al-Jarallah, 2001;al-Jarallah et al, 2001al-Jarallah et al, , 2005Petropoulos et al, 2002;Fazal ur et al, 2003;Stoulos et al, 2003;Sundar et al, 2003;Arafa, 2004;Osmanlioglu, 2006;Singh et al, 2008;Sonkawade et al, 2008). The extent to which the granite samples examined in those studies represent inventories of natural stone countertops has not been evaluated.…”
Section: Introductionmentioning
confidence: 96%