Dispersion of Kraft-Mill Effluent from a Submarine Diffuser in Stuart Channel, British Columbia
Stuart Channel is a stratified, estuarine region typical of British Columbia coastal "inside" waters. Tidal currents are mostly less than 1 kt at all depths, and set to the northwest on the flood and southeast on the ebb, along the axis of the channel. Effluent released by a submarine diffuser, from the kraft pulp mill at Crofton, mixes in a ratio of about 1:22 with sea water as it rises to the surface. The entrainment of cold, saline water in the ascent gives the effluent–sea water mixture at the "boil" above the diffuser a density usually greater than that of surface sea water. Therefore, the mixture generally sinks and spreads in a thin sheet at a depth between 3 and 10 m. Non-tidal currents at the surface and at 9–10 m depth could be expected to give the effluent present in these layers a net displacement seaward through Sansum Narrows. Effluent at a depth of 4–5 m would receive a net transport in the opposite direction (northwest) and could be expected to be retained in the channel much longer.