Decreased acid deposition and the chemical recovery of Killarney, Ontario, lakes.
Lakes in Killarney Park near Sudbury, Ontario, Canada, have shown dramatic water quality changes including general increases in pH and alkalinity, and decreases in SO4(2-), base cations and metals. While some lakes have recovered to pH > 6.0, many are still highly acidic despite decades of improvement. Very high historical S deposition related to emissions from the Sudbury metal smelters dominated the acidification process in this region. However, since the implementation of substantial S emission controls (90%) at the smelters, the Sudbury emissions are no longer the major source of S deposition in the Sudbury area. Wet deposition of SO4(2-) and SO4(2-) concentrations in lakewaters at Killarney now approach values in the Dorset, Ontario, area, about 200 km from Sudbury. This suggests that the S deposition to the Killarney area is now primarily from long-range transport, not from local sources. Studies of Killarney lakes are revealing the complex nature of the chemical recovery process. As lake acidity decreases, other changes including decreased Ca2+ concentrations, increased transparency, and altered thermal regimes may potentially affect some of these ecosystems. It is clear that continuing assessments of the recovery of Killarney lakes, within a multiple-stressor framework, are needed.
Keller
Wendel
W
Ontario Ministry of the Environment, Department of Biology, Laurentian University, Sudbury, Canada. bkeller@vianet.on.ca
Heneberry
Jocelyne H
JH
Dixit
Sushil S
SS
D015258:Acid Rain; D000397:Air Pollution / Q000517:prevention & control*; D002118:Calcium / Q000032:analysis; D004784:Environmental Monitoring; D006863:Hydrogen-Ion Concentration; D007477:Ions; D009864:Ontario; D013455:Sulfur / Q000032:analysis* / Q000737:chemistry; D014867:Water / Q000737:chemistry; D014881:Water Supply
D015258:Acid Rain; D007477:Ions; D014867:Water; D013455:Sulfur; D002118:Calcium