The presence of radioactive materials in soil, sand and sediment samples of Potenga sea beach area, Chittagong, Bangladesh: Geological characteristics and environmental implication

被引:60
作者
Yasmin, Sabina [1 ]
Barua, Bijoy Sonker [2 ]
Khandaker, Mayeen Uddin [3 ,4 ]
Kamal, Masud [5 ]
Rashid, Md. Abdur [1 ]
Sani, S. F. Abdul [4 ]
Ahmed, H. [6 ]
Nikouravan, Bijan [7 ]
Bradley, D. A. [3 ]
机构
[1] Chittagong Univ Engn & Technol, Dept Phys, Chittagong 4349, Bangladesh
[2] Southern Univ Bangladesh, Dept Civil Engn, Chittagong 4000, Bangladesh
[3] Sunway Univ, Sch Healthcare & Med Sci, Ctr Radiat Sci, Bandar Sunway 47500, Selangor, Malaysia
[4] Univ Malaya, Dept Phys, Kuala Lumpur 50603, Malaysia
[5] Bangladesh Atom Energy Commiss, Atom Energy Ctr, Dhaka 1207, Bangladesh
[6] St Francis Xavier Univ, Dept Phys, Antigonish, NS B2G 2W5, Canada
[7] Islamic Azad Univ, Dept Phys, Varamin Pishva Branch, Tehran, Iran
关键词
Earth surface media; HPGe gamma-ray spectrometry; Th-232/U-238; ratio; Mass concentration; Granite rocks; Crustal minerals; NATURAL RADIOACTIVITY; GAMMA-RADIATION; MALAYSIAN POPULACE; VOLCANIC ISLAND; DOSE-RATE; TH-232; RADIONUCLIDES; EXPOSURE; PROVINCE; THORIUM;
D O I
10.1016/j.rinp.2018.02.013
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Accurate quantification of naturally occurring radioactive materials in soil provides information on geological characteristics, possibility of petroleum and mineral exploration, radiation hazards to the dwelling populace etc. Of practical significance, the earth surface media (soil, sand and sediment) collected from the densely populated coastal area of Chittagong city, Bangladesh were analysed using a high purity germanium c-ray spectrometer with low background radiation environment. The mean activities of Ra-226 (U-238), Th-232 and K-40 in the studied materials show higher values than the respective world average of 33, 36 and 474 Bq/kg reported by the UNSCEAR (2000). The deduced mass concentrations of the primordial radionuclides U-238, Th-232 and K-40 in the investigated samples are corresponding to the granite rocks, crustal minerals and typical rocks respectively. The estimated mean value of Th-232/U-238 for soil (3.98) and sediment (3.94) are in-line with the continental crustal average concentration of 3.82 for typical rock range reported by the National Council on Radiation Protection and Measurements (NCRP). But the tonalites and more silicic rocks elevate the mean value of Th-232/U-238 for sand samples amounting to 4.69. This indicates a significant fractionation during weathering or associated with the metasomatic activity in the investigated area of sand collection. (C) 2018 The Authors. Published by Elsevier B.V.
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页码:1268 / 1274
页数:7
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