Selenium Concentrations in Greater Scaup and Dreissenid Mussels During Winter on Western Lake Ontario

Abstract The alternate strategy of open-lake discharge may alleviate the need for unusually stringent treatment needed to meet water quality goals of the Hamilton Harbour Remedial Action Plan (RAP). The latest update of the RAP recommended a study of the possibility of offshore discharges. A study conducted for the City of Burlington has proposed a location for outfall in Lake Ontario. This paper utilizes a combination of physical limnological data and mathematical models to predict the waste plume characteristics for the proposed outfall in the lake. Near-field dilutions obtained from a mixing zone model show that, for treated effluents with a discharge condition of 2 m3/s at the proposed outfall site at Burlington, the dilution ratios are in the range of 13:1 to 28:1 for weak to moderate currents during summer stratification. Winter dilution ratios increased to 21:1 to 96:1 for moderate currents. The recommended site for open-lake outfall provides acceptable near-field dilutions for treated effluents under typical lake currents and density structure. The extension of outfall to a location farther offshore is only marginally beneficial. With the proposed Burlington outfall location and discharge conditions, no far-field contamination is observed near the beaches or nearby water intakes for typical summer and winter conditions. Thus, this study indicates that by discharging the treated sewage from an outfall in Lake Ontario it is possible to achieve the Hamilton Harbour RAP goals.

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Identification of Taste and Odour Compounds from Western Lake Ontario

Water Quality Research Journal ◽

10.2166/wqrj.1984.010 ◽

1984 ◽

Vol 19 (1) ◽

pp. 111-118 ◽

Cited By ~ 6

Author(s):

B.G. Brownlee ◽

D.S. Painter ◽

R.J. Boone

Keyword(s):

Water Supply ◽

Water Samples ◽

Elemental Sulfur ◽

Lake Ontario ◽

Direct Link ◽

Municipal Water Supply ◽

Municipal Water ◽

Western Lake ◽

Odour Concentration

Abstract During August, 1983 geosmin was identified in a municipal water supply drawn from western Lake Ontario. The geosmin concentrations were 0.01-0.07 μg L-1, within the range for threshold odour concentration of 0.01-0.2 μg L-1. 2-Methylisoborneol was not detected. The odour 'event' coincided with a dieoff of Cladophora in the lake, but we were not able to establish a direct link between the dieoff and geosmin production. Decomposing Cladophora in shoreline areas produced a strong odour in the air. 3-Methylindole, elemental sulfur, dimethyl tetrasulfide, and dimethyl pentasulfide were tentatively identified in water samples collected from these areas, but geosmin and 2-methylisoborneol were not detected.

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Chemico/biological investigation of contaminated sediment from the hamilton harbour area of Western Lake Ontario

Environmental and Molecular Mutagenesis ◽

10.1002/em.2850220203 ◽

1993 ◽

Vol 22 (2) ◽

pp. 61-70 ◽

Cited By ~ 40

Author(s):

C. H. Marvin ◽

L. Allan ◽

B. E. McCarry ◽

D. W. Bryant

Keyword(s):

Lake Ontario ◽

Contaminated Sediment ◽

Biological Investigation ◽

Hamilton Harbour ◽

Western Lake ◽

Harbour Area

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Subglacial water-sheet floods, drumlins and ice-sheet lobes

Journal of Glaciology ◽

10.3189/s0022143000001702 ◽

1999 ◽

Vol 45 (150) ◽

pp. 201-213 ◽

Cited By ~ 3

Author(s):

E.M. Shoemaker

Keyword(s):

New York ◽

Lake Michigan ◽

New York State ◽

Ice Sheet ◽

Lake Ontario ◽

High Water ◽

Green Bay ◽

Subglacial Lake ◽

Western Lake ◽

Subglacial Lakes

AbstractThe effect of subglacial lakes upon ice-sheet topography and the velocity patterns of subglacial water-sheet floods is investigated. A subglacial lake in the combined Michigan–Green Bay basin, Great Lakes, North America, leads to: (1) an ice-sheet lobe in the lee of Lake Michigan; (2) a change in orientations of flood velocities across the site of a supraglacial trough aligned closely with Green Bay, in agreement with drumlin orientations; (3) low water velocities in the lee of Lake Michigan where drumlins are absent; and (4) drumlinization occurring in regions of predicted high water velocities. The extraordinary divergence of drumlin orientations near Lake Ontario is explained by the presence of subglacial lakes in the Ontario and Erie basins, along with ice-sheet displacements of up to 30 km in eastern Lake Ontario. The megagrooves on the islands in western Lake Erie are likely to be the product of the late stage of a water-sheet flood when outflow from eastern Lake Ontario was dammed by displaced ice and instead flowed westward along the Erie basin. The Finger Lakes of northern New York state, northeastern U.S.A., occur in a region of likely ice-sheet grounding where water sheets became channelized. Green Bay and Grand Traverse Bay are probably the products of erosion along paths of strongly convergent water-sheet flow.

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