Radioactivity from naturally occurring radioactive materials (NORMs) is ubiquitous in the terrestrial environment and exists in various geological formations, viz. soils, rocks, sediment, air, and construction materials (Ramasamy et al., 2013; Abbasi et al., 2022). However, the distribution of NORMs in the terrestrial and coastal sediments relies on both the distribution of rocks and the procedures through which they are concentrated. Noureddine et al. (1998) and Mahur et al. (2010) reported that, the major source of natural radionuclides in the aquatic environment results from the weathering and recycling of terrestrial minerals and rocks that give rise to 40 K, 232 Th and 238 U in marine sediments (Zakaly et al., 2021).