Ramasamy V, Suresh G, Meenakshisundaram V, Ponnusamy V
Department of Physics, Annamalai University, Tamilnadu, India.
Appl Radiat Isot. 2011 Jan;69(1):184-95. doi: 10.1016/j.apradiso.2010.07.020. Epub 2010 Aug 11.
The natural radionuclide ((238)U, (232)Th and (40)K) contents and mineral characteristics have been analyzed for the different depth sediment samples of Ponnaiyar River with an aim of evaluating the radiation hazard and its relation to specific minerals. To know the complete radiological characteristics, the radiological indices have been calculated and compared with recommended values. In an FTIR study, the extinction coefficient and crystallinity index is calculated to find the relative distribution of major minerals and the crystallinity of quartz, respectively. Both horizontal and vertical distributions of radionuclides and major minerals are studied. Multivariate statistical analyses (cluster and factor) were carried out to determine the relationship between the radioactivity and the minerals. Statistical analyses suggest that the kaolinite is the major mineral to increase the level of radioactivity in the river sediments.
对波纳伊亚尔河不同深度的沉积物样本进行了天然放射性核素((238)U、(232)Th 和 (40)K)含量及矿物特性分析,目的是评估辐射危害及其与特定矿物的关系。为了解完整的放射学特征,计算了放射学指标并与推荐值进行比较。在傅里叶变换红外光谱(FTIR)研究中,分别计算了消光系数和结晶度指数,以确定主要矿物的相对分布和石英的结晶度。研究了放射性核素和主要矿物的水平及垂直分布。进行了多变量统计分析(聚类和因子分析)以确定放射性与矿物之间的关系。统计分析表明,高岭土是增加河流沉积物中放射性水平的主要矿物。