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Problems of Waste Disposal in the Arctic Environment T. G. WATMORE, Arctic Environmental Officer Producing Department Imperial Oil Limited Edmonton, Alberta DEFINITION OF PERMAFROST Permafrost, or perennially frozen ground, is defined exclusively on the basis of temperature and refers to the thermal condition of earth materials such as soil and rock when their temperature remains below 32 F continuously for a number of years. Permafrost includes ground which freezes in one winter, remains frozen through the following summer and into the next winter. This is the minimum limit for the duration of permafrost; it may be only a few inches thick. At the other end of the scale, permafrost may be thousands of years old and hundreds of feet thick. The mode of formation of such old and thick permafrost is identical to that of permafrost only recently developed. Even a small negative heat imbalance each year results in a thin layer being added annually to the permafrost. This annually repeated process can produce a layer of permafrost hundreds of feet thick after several thousands of years. This process does not cause the permafrost to increase in thickness indefinitely but a quasi-equilibrium is reached whereby the downward penetration of frozen ground is balanced by the flow of heat from the unfrozen ground below. Permafrost is not "permanently" frozen. Changes in climate and terrain can cause the permafrost to thaw and disappear. INTRODUCTION This paper deals with some of the current waste disposal problems in the western Canadian Arctic, and more particularly at points along the Mackenzie River and its delta area on the Arctic Ocean. The political boundaries of the Yukon and Northwest Territories contain all of the Canadian Arctic. This area of Wi million square miles, of which 53,000 is fresh water, contains a total population of some 50,000 people, chiefly inhabiting the southern latitudes. Why then, do we speak of waste problems in such an enormous, sparsely-populated land? Many answers can be found. Ecologists and conservationists describe the north as one of the world's last true wilderness areas. Governments, already facing difficult pollution problems, have begun strong protective legislation to ensure protection of 815
Object Description
Purdue Identification Number | ETRIWC197176 |
Title | Problems of waste disposal in the Arctic environment |
Author | Watmore, T. G. |
Date of Original | 1971 |
Conference Title | Proceedings of the 26th Industrial Waste Conference |
Conference Front Matter (copy and paste) | http://earchives.lib.purdue.edu/u?/engext,19214 |
Extent of Original | p. 815-831 |
Series | Engineering extension series no. 140 |
Collection Title | Engineering Technical Reports Collection, Purdue University |
Repository | Purdue University Libraries |
Rights Statement | Digital object copyright Purdue University. All rights reserved. |
Language | eng |
Type (DCMI) | text |
Format | JP2 |
Date Digitized | 2009-06-25 |
Capture Device | Fujitsu fi-5650C |
Capture Details | ScandAll 21 |
Resolution | 300 ppi |
Color Depth | 8 bit |
Description
Title | page 815 |
Collection Title | Engineering Technical Reports Collection, Purdue University |
Repository | Purdue University Libraries |
Rights Statement | Digital object copyright Purdue University. All rights reserved. |
Language | eng |
Type (DCMI) | text |
Format | JP2 |
Capture Device | Fujitsu fi-5650C |
Capture Details | ScandAll 21 |
Transcript | Problems of Waste Disposal in the Arctic Environment T. G. WATMORE, Arctic Environmental Officer Producing Department Imperial Oil Limited Edmonton, Alberta DEFINITION OF PERMAFROST Permafrost, or perennially frozen ground, is defined exclusively on the basis of temperature and refers to the thermal condition of earth materials such as soil and rock when their temperature remains below 32 F continuously for a number of years. Permafrost includes ground which freezes in one winter, remains frozen through the following summer and into the next winter. This is the minimum limit for the duration of permafrost; it may be only a few inches thick. At the other end of the scale, permafrost may be thousands of years old and hundreds of feet thick. The mode of formation of such old and thick permafrost is identical to that of permafrost only recently developed. Even a small negative heat imbalance each year results in a thin layer being added annually to the permafrost. This annually repeated process can produce a layer of permafrost hundreds of feet thick after several thousands of years. This process does not cause the permafrost to increase in thickness indefinitely but a quasi-equilibrium is reached whereby the downward penetration of frozen ground is balanced by the flow of heat from the unfrozen ground below. Permafrost is not "permanently" frozen. Changes in climate and terrain can cause the permafrost to thaw and disappear. INTRODUCTION This paper deals with some of the current waste disposal problems in the western Canadian Arctic, and more particularly at points along the Mackenzie River and its delta area on the Arctic Ocean. The political boundaries of the Yukon and Northwest Territories contain all of the Canadian Arctic. This area of Wi million square miles, of which 53,000 is fresh water, contains a total population of some 50,000 people, chiefly inhabiting the southern latitudes. Why then, do we speak of waste problems in such an enormous, sparsely-populated land? Many answers can be found. Ecologists and conservationists describe the north as one of the world's last true wilderness areas. Governments, already facing difficult pollution problems, have begun strong protective legislation to ensure protection of 815 |
Resolution | 300 ppi |
Color Depth | 8 bit |
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