Abstract
Microplastics have long-term negative effects on marine environment. One of the most significant threats of microplastics is their ability to absorb chemicals which enhances the transfer of pollutants. These pollutants eventually enter the tissues of living organisms e.g. through ingestion. To shed a light on the way these particles accumulate in the surface water of Persian Gulf and the Arabian Sea and the spatial and temporal distribution of their concentrations, a combination of field sampling, remote sensing techniques, and numerical modelling methods were used. Samples were collected using a Neuston net at 31 stations in 2018 and 2021. A hydrodynamic model was used to study the transport of these materials by tide, wind and density-driven currents, and microplastic pathways were mapped. Also, CYGNSS satellite data were used to estimate the particles concentration by measuring the roughness of the ocean surface. It was shown that the northeastern part of the Arabian Sea had the highest concentration of microplastics in winter. Oman's northern border and the Strait of Hormuz had relatively higher concentrations than other parts. This accumulation increases in winter and continues to rise until the end of summer. In autumn, the accumulation decreases, but it begins to increase again in the north of Oman during winter. During winter, the southern part of the Persian Gulf had high concentration, while from summer to autumn, the concentration in the northwest region had increased. In 2021, the average microplastic concentration in the Arabian Sea and the Gulf of Oman varied seasonally from 2.6x104 to 1.8x104 particle per km2. Meanwhile, the average concentration of pollutants in the Persian Gulf was almost invariable throughout the year, ranging from 2.8 x104 to 2.6 x104 particle per km2. Furthermore, the study reveals that these concentrations are influenced by various environmental factors. In the Persian Gulf, water density is the most significant factor controlling the surface concentration of microplastics, while in the Arabian Sea, the interaction of wind speed and sea surface currents is crucial.
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