Issa Shams A M, Uosif M A M, Abd el-Salam L M
Physics Department, Faculty of Science, Al-Azhar University, Assiut Branch, Egypt.
Radiat Prot Dosimetry. 2012 Jul;150(4):488-95. doi: 10.1093/rpd/ncr437. Epub 2011 Dec 5.
Different types of granites, used extensively in local construction, were collected from five localities in Egypt, namely: Abu Ziran (Central Eastern Desert), Gabal El Maesala (Aswan) and three areas from Wadi Allaqi, (Gabal Abu Marw, Gabal Haumor and Gabal um Shalman), in the South Eastern Desert. Granite samples were studied radiologically, petrographically and geochemically. The contents of natural radionuclides ((226)Ra, (232)Th and (40)K) were measured in investigated samples by using gamma spectrometry [NaI (Tl) 3'×3']. The activity concentrations of (226)Ra, (232)Th and (40)K in the selected granite samples ranged from 9±0.5 to 111±7, 8±1 to 75±4 and 100±6 to 790±40 Bq kg(-1), respectively. The external hazard index (H(ex)), absorbed dose and annual effective dose rate were evaluated to assess the radiation hazard for people living in dwellings made of the materials studied. The calculated radium equivalents were lower than the values recommended for construction materials (370 Bq kg(-1)). The excess lifetime cancer risks were also calculated. Petrographically, the granites studied are varied in the form of potash-feldspar, quartz, plagioclase, mica and hornblende. The accessory minerals are zircon, apatite and allanite. Geochemically, the chemical composition of the granite is studied especially for major oxides. They are characterized to have SiO(2), K(2)O, Na(2)O and Al(2)O(3) with depletion in CaO, MgO, TiO(2) and P(2)O(5).
广泛用于当地建筑的不同类型花岗岩,是从埃及的五个地点采集的,分别是:阿布齐兰(中东沙漠)、加巴尔·迈萨拉(阿斯旺)以及东南沙漠中瓦迪·阿拉奇的三个地区(加巴尔·阿布马尔夫、加巴尔·豪莫尔和加巴尔·乌姆·沙尔曼)。对花岗岩样品进行了放射学、岩相学和地球化学研究。通过伽马能谱法[碘化钠(铊)3'×3']测量了所研究样品中天然放射性核素(镭-226、钍-232和钾-40)的含量。所选花岗岩样品中镭-226、钍-232和钾-40的活度浓度分别为9±0.5至111±7、8±1至75±4和100±6至790±40贝克勒尔/千克。评估了外照射危害指数(H(ex))、吸收剂量和年有效剂量率,以评估居住在用所研究材料建造房屋中的人们所面临的辐射危害。计算得出的镭当量低于建筑材料推荐值(370贝克勒尔/千克)。还计算了终生患癌超额风险。在岩相学方面,所研究的花岗岩在钾长石、石英、斜长石、云母和角闪石的形态上各不相同。副矿物有锆石、磷灰石和褐帘石。在地球化学方面,对花岗岩的化学成分进行了研究,特别是对主要氧化物。其特征是含有二氧化硅、氧化钾、氧化钠和氧化铝,而氧化钙、氧化镁、二氧化钛和五氧化二磷含量较低。