Abstract
The physical aspects of crude oil spills on the terrain of the Mackenzie Valley were investigated. The aqueous solubility of Norman Wells crude oil has been determined and it has been established that about half of the dissolved hydrocarbon is aromatic. The distribution of hydrocarbons between the oil and aqueous phases is in good agreement with predicted values. The permeability of the surface terrain to oil at Norman Wells was found to decrease very rapidly with depth below the surface. A simple, in-situ method for determination of the profile was developed. The implication of the results is that flow will occur more readily near the surface than near the basement. The spreading rates of two crude oils on water were studied on two lakes near Inuvik. Pembina crude oil showed only one spreading front, whereas Norman Wells crude oil showed a bulk front preceded by a surface-slick. Once the initial separation occurred, wind drove both fronts across the water at about 6 percent of the wind speed. The area of surface-active contamination was several times the area of the bulk oil film. The isothermal spreading of five crude oils on ice under gravity-viscous conditions was examined. The radius of the
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Citation Formats
Mackay, D, Charles, M E, and Phillips, C R.
Physical aspects of crude oil spills on northern terrain. Task Force on Northern Oil Development, Report No. 74-25.
Canada: N. p.,
1974.
Web.
Mackay, D, Charles, M E, & Phillips, C R.
Physical aspects of crude oil spills on northern terrain. Task Force on Northern Oil Development, Report No. 74-25.
Canada.
Mackay, D, Charles, M E, and Phillips, C R.
1974.
"Physical aspects of crude oil spills on northern terrain. Task Force on Northern Oil Development, Report No. 74-25."
Canada.
@misc{etde_7301018,
title = {Physical aspects of crude oil spills on northern terrain. Task Force on Northern Oil Development, Report No. 74-25}
author = {Mackay, D, Charles, M E, and Phillips, C R}
abstractNote = {The physical aspects of crude oil spills on the terrain of the Mackenzie Valley were investigated. The aqueous solubility of Norman Wells crude oil has been determined and it has been established that about half of the dissolved hydrocarbon is aromatic. The distribution of hydrocarbons between the oil and aqueous phases is in good agreement with predicted values. The permeability of the surface terrain to oil at Norman Wells was found to decrease very rapidly with depth below the surface. A simple, in-situ method for determination of the profile was developed. The implication of the results is that flow will occur more readily near the surface than near the basement. The spreading rates of two crude oils on water were studied on two lakes near Inuvik. Pembina crude oil showed only one spreading front, whereas Norman Wells crude oil showed a bulk front preceded by a surface-slick. Once the initial separation occurred, wind drove both fronts across the water at about 6 percent of the wind speed. The area of surface-active contamination was several times the area of the bulk oil film. The isothermal spreading of five crude oils on ice under gravity-viscous conditions was examined. The radius of the slick was found to increase linearly with the ratio (time/viscosity)/sup /sup 1///sub 5//. Surface roughness effects were negligible. An attempt has been made to predict the behavior of a 50,000 barrel oil spill in the taiga region of the Mackenzie Valley, under both summer and winter conditions. The areas affected and the amounts of hydrocarbon evaporated were predicted. These predictions are valuable in providing a scenario of an oil spill incident which will assist in assessing the environmental impact of oil spills in the Mackenzie Valley and in preparing for clean-up measures. Burning as a clean-up procedure considered in some detail. Other methods specifically designed for Arctic conditions will probably prove more satisfactory.}
place = {Canada}
year = {1974}
month = {Jan}
}
title = {Physical aspects of crude oil spills on northern terrain. Task Force on Northern Oil Development, Report No. 74-25}
author = {Mackay, D, Charles, M E, and Phillips, C R}
abstractNote = {The physical aspects of crude oil spills on the terrain of the Mackenzie Valley were investigated. The aqueous solubility of Norman Wells crude oil has been determined and it has been established that about half of the dissolved hydrocarbon is aromatic. The distribution of hydrocarbons between the oil and aqueous phases is in good agreement with predicted values. The permeability of the surface terrain to oil at Norman Wells was found to decrease very rapidly with depth below the surface. A simple, in-situ method for determination of the profile was developed. The implication of the results is that flow will occur more readily near the surface than near the basement. The spreading rates of two crude oils on water were studied on two lakes near Inuvik. Pembina crude oil showed only one spreading front, whereas Norman Wells crude oil showed a bulk front preceded by a surface-slick. Once the initial separation occurred, wind drove both fronts across the water at about 6 percent of the wind speed. The area of surface-active contamination was several times the area of the bulk oil film. The isothermal spreading of five crude oils on ice under gravity-viscous conditions was examined. The radius of the slick was found to increase linearly with the ratio (time/viscosity)/sup /sup 1///sub 5//. Surface roughness effects were negligible. An attempt has been made to predict the behavior of a 50,000 barrel oil spill in the taiga region of the Mackenzie Valley, under both summer and winter conditions. The areas affected and the amounts of hydrocarbon evaporated were predicted. These predictions are valuable in providing a scenario of an oil spill incident which will assist in assessing the environmental impact of oil spills in the Mackenzie Valley and in preparing for clean-up measures. Burning as a clean-up procedure considered in some detail. Other methods specifically designed for Arctic conditions will probably prove more satisfactory.}
place = {Canada}
year = {1974}
month = {Jan}
}