“…This result indicates that the BFRs in the sediment may have entered the river continuously from various point and non-point sources; the concentrations gradually increase in the downstream parts (NR09 and NR10), which are closed by flood gates at ordinary times, due to the repeated re-suspension and deposition of the BFR in the sediment. Moreover, the continuous discharge of effluent containing BFRs from STP and WWTP close to NR09 and NR10 also might affect the sedimentary BFRs concentration (Potvin et al, 2012;Ichihara et al, 2014;Deng et al, 2015). The sediment samples from the lakes (the NL samples) each contained similar BFR concentrations, and these concentrations were similar to the concentrations found in the sediment samples from the upstream and midstream parts of the river, suggesting that the background total PBDE concentration was 2.6 ng g À1 dw, the background TBBPA concentration was 3.0 ng g À1 dw, and the background total HBCD concentration was 0.3 ng g À1 dw (these are the average concentrations found in the lake sediment samples and the Nakdong River sediment samples NR01-NR08).…”