Heavy metal fluxes in Bang Pakong River Estuary, Thailand: Sedimentary vs diffusive fluxes

Abstract

Estimates of the flux of heavy metals into the sediments (sedimentary flux) of Bang Pakong River Estuary and the diffusive flux of these metals across the sediment-water interface provide quantitative approximations on the movement of heavy metals from the water column into the sediments, and vice versa. Results showed higher sedimentary flux of Cu, Pb, Zn, Cd, Cr and Ni (0.1–16.8 μg cm−2 yr−1) relative to the diffusive flux of these metals (0.01–4.8 μg cm−2 yr−1). The percentage diagenetic contribution (ratio of diffusive flux to sedimentary flux) of these metals ranged from 10–91%. This suggests that diagenetic remobilization and release of these metals from the sediments into the overlying water may contribute to the subsequent redeposition of these metals into the sediments. Metal enrichment at the surface sediments when compared with deeper sections of the sediment may not necessarily be interpreted as evidence of recent natural, anthropogenic inputs alone, but may also be a consequence of the deposition of metals previously released from the sediments through diagenesis.