Ramasamy V, Dheenathayalu M, Ravisankar R, Ponnusamy V, Rajamanickkam G Victor, Sahayam DajKumar, Meenakshisundram V, Gajendran V
Department of Physics, Annamalai University, Annamalai Nagar, 608 002, India.
Radiat Prot Dosimetry. 2004;111(2):229-35. doi: 10.1093/rpd/nch328. Epub 2004 Jul 20.
The concentration of primordial radionuclides in beach-rock samples of the south-east coast of Tamilnadu, India has been measured using gamma ray spectrum of rock. The mean activities of 232Th, 238U and 40K are 144.18, 29.25 and 267.48 Bq kg(-1) respectively. In situ measurements were also carried out using environmental radiation dosemeter. The linear correlation coefficient was obtained. The average activity of concentration of 232Th in the present study is 2.5 times higher than the world median value while the activity of 238U and 40K were found to be lower. This may be due to the heavy minerals present in the study area. In the present study, the calculated activity ratio (Th/U) is higher than the crustal rocks. This may be due to changes in the crustal composition through time (mafic to felsic) that are reflected by a change in the Th and U abundances in sedimentary rocks, and also increase in carbon content with time resulted in the decrease in U content and increase in Th/U ratio.
利用岩石的伽马射线能谱,对印度泰米尔纳德邦东南海岸海滩岩样本中原始放射性核素的浓度进行了测量。钍-232、铀-238和钾-40的平均活度分别为144.18、29.25和267.48贝可勒尔每千克。还使用环境辐射剂量仪进行了现场测量。获得了线性相关系数。本研究中钍-232的平均活度浓度比世界中值高2.5倍,而铀-238和钾-40的活度则较低。这可能是由于研究区域存在重矿物。在本研究中,计算得到的活度比(钍/铀)高于地壳岩石。这可能是由于随着时间推移地壳成分发生变化(从镁铁质到长英质),沉积岩中钍和铀的丰度变化反映了这一点,并且随着时间推移碳含量增加导致铀含量降低以及钍/铀比值升高。