Oil Extraction in Alaska Flashcards

1
Q

How does the extraction and transportation of oil impact the periglacial landscape system?

A

The extraction and transportation of oil can impact the processes, flows of material, and energy through the periglacial landscape system.

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2
Q

How are material flows affected by oil extraction?

A

Material flows are affected by the use of gravel pads, where gravel is extracted from stream and river beds for road construction. The loss of gravel alters the rate of transportation and deposition downstream, affecting the equilibrium between erosional and depositional processes in the river system.

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3
Q

What impact does gravel extraction have on the periglacial landscape system?

A

Gravel extraction disrupts the natural flow of material, altering the transportation and deposition of gravel downstream, and influencing the balance between erosional and depositional processes in river systems.

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4
Q

How are hydrological processes affected by gravel extraction?

A

Gravel extraction from a glacial outwash aquifer near Palmer resulted in a drop of over a meter in groundwater levels within a 2 km radius of the extraction site.

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5
Q

How are energy flows affected by oil extraction and drilling processes?

A

Energy flows are affected by the release and burning of gases during drilling. Flaring releases carbon dioxide into the atmosphere, contributing to the greenhouse effect. Methane is also vented without burning, further contributing to the greenhouse effect. Additionally, heat produced by extraction, transportation processes, and associated infrastructure raises temperatures in the surrounding environment.

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6
Q

What gases are released during drilling, and what are their impacts?

A

During drilling, gases such as carbon dioxide and methane are released. Carbon dioxide contributes to the greenhouse effect, while methane is a potent greenhouse gas. Both gases trap terrestrial radiation in the lower atmosphere, raising temperatures.

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7
Q

What impact does oil extraction have on the urban heat island effect?

A

In the small town of Barrow, Alaska, oil production contributes to the urban heat island effect, with mean temperatures averaging 2.2°C higher than in the surrounding rural area. On calm days, temperature differences of up to 6°C have been measured. The heat released by oil-related activities, including domestic heating systems in poorly insulated buildings, contributes to the elevated temperatures in the area.

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8
Q

How does oil production affect temperature fluctuations and freeze-thaw cycles?

A

Since drilling began, there has been a reduction of 9 percent in the number of days with temperature fluctuations around 0°C (freeze-thaw cycles). The energy released to the environment by oil-related human activities disrupts the natural freeze-thaw processes.

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9
Q

What are the consequences of oil extraction for the periglacial landscape system?

A

Oil extraction disrupts material flows, alters hydrological processes, and affects energy flows within the periglacial landscape system. These impacts can have implications for river systems, groundwater levels, temperature patterns, and natural freeze-thaw cycles.

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10
Q

What is permafrost?

A

Permafrost is perennially frozen ground that remains frozen from one year to the next, despite rising above-zero temperatures in the summer.

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11
Q

What is the active layer in permafrost regions?

A

The active layer is a shallow surface layer of material that overlays the permafrost. It thaws in the summer but freezes again during the winter.

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12
Q

Why does the permafrost experience less temperature variation compared to the active layer?

A

The permafrost is not directly exposed to the seasonal differences in air temperature, which is why it experiences less temperature variation compared to the active layer.

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13
Q

How can buildings and infrastructure impact permafrost?

A

The heat released by buildings and infrastructure can lead to the thawing of permafrost and a longer period of melting for the active layer.

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14
Q

What happens if a building is constructed directly onto the ground surface in permafrost regions?

A

If a building is constructed directly onto the ground surface in permafrost regions, some of the heat produced by the heating systems may transfer through the floor to the ground, resulting in the melting of permafrost.

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15
Q

What are the consequences of permafrost thawing due to building heat?

A

Thawing permafrost can lead to subsidence and increase the mobility of the active layer. It can also result in solifluction, a type of mass movement.

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16
Q

What is solifluction?

A

Solifluction is a type of mass movement that occurs when the thawed active layer moves downslope.

17
Q

What landforms are formed by solifluction?

A

The downslope movement of the thawed active layer forms solifluction lobes, which are tongues of debris, at the base of slopes.

18
Q

How do solifluction lobes form?

A

Solifluction lobes form when the moving material loses energy on a lower gradient, leading to the deposition of debris at the base of slopes.

19
Q

What are the consequences of solifluction lobes?

A

Solifluction lobes contribute to the redistribution of material downslope and can alter the shape of the landscape in permafrost regions.

20
Q

What is thermokarst?

A

Thermokarst is a landscape characterized by surface depressions resulting from the thawing of ground ice. It consists of hummocky ground with waterlogged hollows and can include shallow thaw lakes, alases, and alas valleys.

21
Q

What are the features of a thermokarst landscape?

A

A thermokarst landscape consists of extensive areas of hummocky ground, waterlogged hollows, shallow thaw lakes, alases (deep depressions with flat floors and steep sides), and alas valleys (valleys formed by the combination of multiple alases).

22
Q

What is the typical depth and width of shallow thaw lakes in a thermokarst landscape?

A

Shallow thaw lakes in a thermokarst landscape are usually less than 5 meters deep and 1-2 kilometers wide.

23
Q

Describe the characteristics of alases in a thermokarst landscape.

A

Alases are deep depressions in a thermokarst landscape with flat floors and steep sides. They can range from 5 to 50 meters in depth and 100 meters to 15 kilometers in length.

24
Q

What causes the development of alases in a thermokarst landscape?

A

Alases develop from the widespread thawing of ground ice, which leads to large-scale subsidence, resulting in the formation of these deep depressions.

25
Q

What are alas valleys in a thermokarst landscape?

A

Alas valleys are formed when multiple alases combine, creating interconnected valleys that can stretch for many tens of kilometers in length.

26
Q

What can initiate the thawing of ground ice in a thermokarst landscape?

A

The thawing of ground ice in a thermokarst landscape can be initiated by climate change, as well as by direct human interference such as vegetation removal for resource extraction or construction purposes.

27
Q

How does the removal of vegetation impact ground ice in a thermokarst landscape?

A

The removal of vegetation reduces the insulation of ground ice, causing it to thaw to greater depths. This leads to the formation of a thicker active layer and more extensive subsidence in the landscape.

28
Q

What were the average and maximum subsidence rates observed in thermokarst depressions on the North Slope of Alaska?

A

Research in the North Slope of Alaska recorded average subsidence rates of 3-4 centimeters per year, with a maximum rate of 12 centimeters per year.

29
Q

What are the depths of permafrost and the active layer in the North Slope of Alaska?

A

In the North Slope of Alaska, the permafrost reaches depths of 300-600 meters, while the active layer ranges from 30-80 centimeters in thickness.