Murat Saç Müslim, Aydemir Sercan, Içhedef Mutlu, Kumru Mehmet N, Bolca Mustafa, Ozen Fulsen
Institute of Nuclear Sciences, Ege University, Bornova-İzmir 35100, Turkey.
Radiat Prot Dosimetry. 2014 Jan;158(2):148-55. doi: 10.1093/rpd/nct220. Epub 2013 Sep 11.
All over the world geothermal sources are used for different purposes. The contents of these waters are important to understand positive/negative effects on human life. In this study, natural radioactivity concentrations of geothermal waters were investigated to evaluate the effect on soils and agricultural activities. Geothermal water samples were collected from the Seferihisar Geothermal Region, and the radon and radium concentrations of these waters were analysed using a collector chamber method. Also soil samples, which are irrigated with geothermal waters, were collected from the surroundings of geothermal areas, and natural radioactivity concentrations of collected samples (U, Th and K) were determined using an NaI(Tl) detector system. The activity concentrations of radon and radium were found to be 0.6-6.0 and 0.1-1.0 Bq l(-1), respectively. Generally, the obtained results are not higher compared with the geothermal waters of the world. The activity concentrations in soils were found to be in the range of 3.3-120.3 Bq kg(-1) for (226)Ra (eU), 0.3-108.5 Bq kg(-1) for (232)Th (eTh), 116.0-850.0 Bq kg(-1) for (40)K (% K).
在世界各地,地热源被用于不同目的。了解这些水体的成分对于认识其对人类生活的正负影响至关重要。在本研究中,对地热水体的天然放射性浓度进行了调查,以评估其对土壤和农业活动的影响。从塞费里希萨尔地热区采集了地热水样本,并使用收集室法分析了这些水体中的氡和镭浓度。此外,从地热区周边采集了用地热水灌溉的土壤样本,并使用碘化钠(铊)探测器系统测定了采集样本(铀、钍和钾)的天然放射性浓度。发现氡和镭的活度浓度分别为0.6 - 6.0和0.1 - 1.0 Bq l(-1)。总体而言,与世界其他地热水体相比,所得结果并不更高。土壤中的活度浓度范围为:镭 - 226(等效铀)为3.3 - 120.3 Bq kg(-1),钍 - 232(等效钍)为0.3 - 108.5 Bq kg(-1),钾 - 40(钾含量百分比)为116.0 - 850.0 Bq kg(-1)。