Formation of OSA and Dispersion of Polycyclic Aromatic Hydrocarbons in a Tropical Estuary As a Tool in the Prevention of Environmental Impacts: Influence of the Biogeochemical Characteristics of the Estuary

Overview

Journal Environ Monit Assess

Publisher Springer

Specialty Environmental Health

Date 2020 Jan 5

PMID 31900672

Authors

Samires Moura Malaquias Pinheiro

Marcos de Almeida

Olivia Maria Cordeiro Oliveira

Icaro Thiago Andrade Moreira

Affiliations

Soon will be listed here.

Abstract

The formation of an oil-suspended particulate material aggregate (OSA) is one of the weathering processes that occur after the spill of oil in marine environments, responsible for the dispersion of hydrocarbons. Oil and particle aggregates are formed from the interaction between small oil droplets and suspended particulate matter (SPM). In general, SPM are fine particles which may be inorganic minerals or organic particles in the water column. OSAs provide vertical dispersion of oil along the water column depending on the acquired density (buoyancy), and may remain near the surface, water column, or bottom of water bodies. The present study examines the formation of these aggregates through the laboratory simulation of an oil spill in the waters of the São Paulo river estuary. The main objective was to investigate the dispersion of polycyclic aromatic hydrocarbons (PAHs), verifying which estuary characteristics most influenced the formation of OSAs and in addition to determine the regions of probable ecotoxicological impact due to the negative buoyancy of the formed aggregate. The results show that there was greater dispersion to the water column, mainly of lighter PAHs, ranging from 85,804.05 ng g (P11C) to 566,989.84 ng g (P17C). The percentage of dispersed PAH concentration per experimental unit ranged from 9.90% in unit P2 to 75.27% in unit P18. The formation of OSAs was influenced mainly by salinity and chlorophyll a. As the most vulnerable regions, the impacts are one mouth (P2 and P4), one central region (P7, P8, and P10), and one source (P18).

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