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.

Download full-text PDF

Source
http://dx.doi.org/10.1038/s41598-024-82081-8DOI Listing
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC11700117PMC

Publication Analysis

Top Keywords

granodiorite tonalite
12
diorite granodiorite
8
tonalite diorite
8
samples
5
unveiling radiation
4
radiation shielding
4
shielding efficacy
4
diorite
4
efficacy diorite
4
granodiorite
4

Similar Publications

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.

View Article and Find Full Text PDF

Patterns distribution, concentrations and sources of radioactive elements from black sand in the Red Sea coast, Egypt.

J Hazard Mater

December 2024

Department of Zoology, Faculty of Science, Assiut University, 71516 Assiut, Egypt; Molecular Biology Research & Studies Institute, Assiut University, 71516 Assiut, Egypt. Electronic address:

In Egypt, the distribution of black sand in various coastal regions has been readily apparent by thorough research. Unfortunately, these investigations did not measure radioactivity in black sand, particularly in the vicinity of the Red Sea. Gamma-ray spectroscopy was used to detect the naturally occurring radioactivity from U, Th, K, and Ra in black sand samples from eight locations along the Red Sea coast: Ras Elbehar, Gemsa, Hurghada Elahiaa, Hurghada Titanic, Safaga, Qusier Elsharm Alqbly, Gabal Alrosass, and Marsa Alam.

View Article and Find Full Text PDF

Chamwino district, central Tanzania is a semi-arid granitic complex province, where groundwater is the major source of water for domestic and other uses. However, groundwater in the area is affected by salinity, thus, lowering the availability of potable water for various uses decrease in crop production, taste less, wastage of soap, and abnormal pain. Due to this, this study sought to characterize groundwater using hydrogeochemical facies and signatures in order to identify the factors influencing the distribution of salt water in the Chamwino Granitic Complex.

View Article and Find Full Text PDF

Archaean continental crust formed from mafic cumulates.

Nat Commun

January 2024

Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, 2020-2207 Main Mall, Vancouver, V6T 1Z4, Canada.

Large swaths of juvenile crust with tonalite-trondhjemite-granodiorite (TTG) composition were added to the continental crust from about 3.5 billion years ago. Although TTG magmatism marked a pivotal step in early crustal growth and cratonisation, the petrogenetic processes, tectonic setting and sources of TTGs are not well known.

View Article and Find Full Text PDF

We apply a zircon redox index to a global compilation of detrital zircons to track the variation of oxidation state, expressed as ΔFMQ, through Earth's history. Those from I-type rocks, which comprise mantle and crustal igneous protoliths, including tonalite-trondhjemite-granodiorites (TTGs), generally have a high oxidation state (ΔFMQ > 0). In contrast, zircons from igneous rocks derived from supracrustal source rocks (S-type) are commonly reduced (ΔFMQ < 0).

View Article and Find Full Text PDF

Want AI Summaries of new PubMed Abstracts delivered to your In-box?

Enter search terms and have AI summaries delivered each week - change queries or unsubscribe any time!