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Indoor radon concentration: impact of geology in the 2005 Kashmir earthquake-affected Bagh area, Azad Jammu and Kashmir, Pakistan

机译:室内ra浓度:巴基斯坦阿扎德查mir和克什米尔2005年克什米尔地震影响的巴格地区的地质影响

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The early Miocene Murree Formation, late Miocene Nagri Formation and recent alluvium rock units are exposed in the sub-Himalayas of the Bagh area, State of Azad Jammu and Kashmir, Pakistan. The Bagh area was badly affected by the Kashmir earthquake of October 8th 2005 which, along the Muzaffarabad Fault, deformed both the hanging and footwall blocks. The cracks, joints, fissures and fractures in houses and bedrocks might have affected the emission of radon to the surface. Indoor radon concentration measurements were carried out in some dwellings of the Bagh area, Azad Kashmir, Pakistan. The measurements were based on passive integrative detection of radon using CN-85 plastic track detectors in box-type dosimeters. The radon concentration in dwellings was between 50 +/- 11.6 Bq.m(-3) and 167.1 +/- 21.4 Bq.m(-3) with an overall average of 95.1 +/- 15.8 Bq.m(-3) (geometric mean = 93.4 Bq.m(-3)). The average radon concentrations in pucka, semi-pucka and kucha houses were 97.6 +/- 15.4 Bq.m(-3), 89.7 +/- 15.2 Bq.m(-3) and 101.9 +/- 15.9 Bq.m(-3), respectively. The mean values of radon concentrations in the Nagri Formation, Murree Formation and recent alluvium lithology were 99.3 +/- 15.8, 90.1 and 96.2 +/- 15.5 Bq.m(-3), respectively. The annual effective dose to the Bagh population was calculated as 2.38 +/- 0.77 (1.33 +/- 0.2 to 4.7 +/- 0.5) mSv. The average radon (95.1 +/- 15.8 Bq.m(-3)) concentration in dwellings for the inhabitants of the Bagh area was safe from radon-related health hazards and was within the recommended action level (ICRP publication 65 (1993) Protection against radon at home and at work, International Commission on Radiological Protection, Ann. ICRP 23(2)). The indoor radon values obtained in the present study are more than the world average of 40 Bq.m(-3) (UNSCEAR (2000) United Nations Scientific Committee on the Effects of Atomic radiation, Report to the General Assembly, United Nations, New York).
机译:在巴基斯坦的阿扎德查姆州和克什米尔州,巴格地区的喜马拉雅山地区暴露了中新世穆里早期组,中新世纳格里晚期和最近的冲积岩单元。巴格地区受到2005年10月8日克什米尔地震的严重影响,该地震沿着Muzaffarabad断层使上悬块和下盘块变形。房屋和基岩中的裂缝,接缝,裂缝和裂缝可能已经影响了to向地表的排放。室内ra浓度的测量是在巴基斯坦阿扎德克什米尔巴格地区的一些住宅中进行的。测量是基于盒式剂量计中使用CN-85塑料径迹检测器进行的passive的被动整体检测。住宅中的concentration浓度在50 +/- 11.6 Bq.m(-3)和167.1 +/- 21.4 Bq.m(-3)之间,总体平均值为95.1 +/- 15.8 Bq.m(-3)(几何平均值= 93.4 Bq.m(-3))。 uck,半-和库车房屋中的平均ra浓度分别为97.6 +/- 15.4 Bq.m(-3),89.7 +/- 15.2 Bq.m(-3)和101.9 +/- 15.9 Bq.m(- 3)。 Nagri组,Murree组和最近的冲积层岩性中的concentrations浓度平均值分别为99.3 +/- 15.8、90.1和96.2 +/- 15.5 Bq.m(-3)。对Bagh人群的年度有效剂量经计算为2.38 +/- 0.77(1.33 +/- 0.2至4.7 +/- 0.5)mSv。巴格地区居民住宅中的平均ra浓度(95.1 +/- 15.8 Bq.m(-3))可以安全地避免与ra有关的健康危害,并且处于建议的行动水平之内(ICRP出版物65(1993)Protection)在家中和工作中针对ra的行为,国际放射防护委员会,ICRP,第23(2)条)。本研究中获得的室内values值超过了世界平均水平40 Bq.m(-3)(UNSCEAR(2000)联合国原子辐射影响科学委员会,提交大会的报告,联合国,新约克)。

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