Elsafi M, El-Nahal M A, Alawy M K, Nabil Islam M
Physics Department, Faculty of Science, Alexandria University, Alexandria, 21511, Egypt.
Department of Environmental Studies, Institute of Graduate Studies and Research, Alexandria University, Alexandria, 21511, Egypt.
Sci Rep. 2025 Jan 4;15(1):804. doi: 10.1038/s41598-024-82081-8.
For the purpose of this study, four natural rock samples-namely, diorite, granodiorite, tonalite, and granite-are being investigated about their radiation attenuation. The elemental composition of the rocks was obtained through Energy dispersive X-ray spectroscopy (EDX) which examines the microstructural and localized area elemental analyses of the four rock samples. A Monte Carlo simulation (MCNP) was used to determine and evaluate the investigated samples. Additionally, the samples were validated by Phy-X software (within the energy range of 0.015 to 15 MeV), and experimental measurements were achieved through the utilization of an HPGe detector (0.060, 0.662, 1.173, and 1.332 MeV). The investigation was carried out using various parameters such as linear attenuation (µ) and others. Furthermore, the Fast Neutrons Removal Cross Sections (FNRCS) were calculated using theoretical methods. In the case of granodiorite, tonalite, diorite, and granite, the values of µ were found to range from 7.931 to 0.049, 31.922 to 0.061, 17.267 to 0.060, and 23.860 to 0.056 cm, respectively. The samples of tonalite and diorite have the highest µ values due to the presence of heavy elements and the high densities of these samples. Granodiorite is the substance that possesses the highest value of FCS (0.108 cm) due to the high content of light elements (O = 0.6802%, and C = 0.2286% wt). The results of the study demonstrated that the investigated natural rocks possessed a substantial potential for shielding γ-rays and neutrons from radiation and could be suitable for use in radiological protection applications.
为了本研究的目的,正在对四种天然岩石样本——即闪长岩、花岗闪长岩、英云闪长岩和花岗岩——的辐射衰减情况进行调查。通过能量色散X射线光谱法(EDX)获得了岩石的元素组成,该方法用于检测这四种岩石样本的微观结构和局部区域元素分析。使用蒙特卡罗模拟(MCNP)来确定和评估所研究的样本。此外,利用Phy-X软件(在0.015至15 MeV的能量范围内)对样本进行了验证,并通过使用HPGe探测器(0.060、0.662、1.173和1.332 MeV)进行了实验测量。使用了诸如线性衰减(µ)等各种参数进行调查。此外,使用理论方法计算了快中子去除截面(FNRCS)。对于花岗闪长岩、英云闪长岩、闪长岩和花岗岩,µ值分别为7.931至0.049、31.922至0.061、17.267至0.060和23.860至0.056 cm。由于重元素的存在以及这些样本的高密度,英云闪长岩和闪长岩样本具有最高的µ值。花岗闪长岩由于轻元素含量高(O = 0.6802%,C = 0.2286% wt)而具有最高的FCS值(0.108 cm)。研究结果表明,所研究的天然岩石在屏蔽γ射线和中子辐射方面具有巨大潜力,可适用于放射防护应用。