Trans Alaska Oil Pipeline
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Trans Alaska Oil Pipeline traverses the tundra of Alaska's Arctic, north of the Brooks mountain range. © Patrick J. Endres
Oil was discovered at Prudhoe Bay, Alaska in 1968, after explorers had been searching since the 1950s all through Northern Alaska. A pipeline was considered the only viable system for transporting the oil to the nearest ice-free port, almost 800 miles (1,300 km) away at Valdez. Completed in 1977, the Alaska pipeline covers 800 miles of mountain,
muskeg and river valleys in its span from Prudhoe Bay to Valdez.
Stretch the pipeline over the Lower 48 and it would reach from
Los Angeles to Denver.
The pipe is a tube of 1/2-inch thick steel with a diameter of 48
inches. It looks thicker from the highway because the steel pipe
is wrapped with four inches of fiberglass insulation. The shiny
wrapping we see is a coat of aluminum sheet metal. The closer oil is to the molten core of the earth, the hotter it
is when oil companies pull it to the surface. Oil pumped from the
Prudhoe Bay field, which is 10,000-to-20,000 feet deep, is about
145 to 180 degrees Fahrenheit. Using heat exchangers that work like
a car's radiator, the oil companies cool the oil to about 120 degrees
before it enters the pipeline.

The pipeline
couldn't be buried in permafrost because the heat of the oil would
cause the icy soil to melt. The pipe would then sag, and possibly
leak. TAPS, north of the Brooks range, view of the Endicott mountains of the Brooks range. © Patrick J. Endres
If the flowing oil was cold, the pipeline wouldn't inspire nearly
as much highway conversation. Engineers would have buried the entire
pipeline had it not been for permafrost - permanently - frozen soil
lying in sheets and wedges beneath the ground surface. The pipeline
couldn't be buried in permafrost because the heat of the oil would
cause the icy soil to melt. The pipe would then sag, and possibly
leak. Because much of Alaska is underlain with permafrost, Alyeska
routed just over half the pipeline above ground.

The pipeline is supported by posts designed
to keep permafrost frozen. Topped with fan-like aluminum radiators,
the posts absorb cold from the winter air and transfer it to the
soil. © Patrick J. Endres
Where it snakes over land, the pipeline is supported by posts designed
to keep permafrost frozen. Topped with fan-like aluminum radiators,
the posts radiate heat from the ground into the cold winter air to keep the soil solidly frozen. When the air temperature is 40 below, for example, the posts
cool down to 40 below and take away heat from the soil, assuring
the ground stays frozen.

The pipeline was built in a zigzag pattern to allow the pipe to
expand and contract. © Patrick J. Endres
The pipeline was built in a zigzag pattern to allow the pipe to
expand and contract. Because workers welded much of the pipeline
at temperatures well below zero, engineers anticipated that the
metal would expand once hot oil began flowing through.

The pipeliine slides over H-shaped supports with the aid of Teflon-coated "shoes"
that stand on the crossbar between the posts holding up the pipeline. © Patrick J. Endres
The zigzag also allows the pipeline to flex during earthquakes;
it slides over H-shaped supports with the aid of Teflon-coated "shoes"
that stand on the crossbar between the posts holding up the pipeline.
Where the pipeline crosses seismic faults--weak areas of rock that
rupture during earthquakes when the plates of the earth grind against
one another--it sits on rails. Near the Denali Fault south of Delta
Junction, the pipeline rests on 20-foot steel bars that allow it
to move side-to-side should an earthquake cause the earth's crust
to slip laterally along a fault line.

The pipeliine crosses the Tanana River near Delta Junction by means of a suspension bridge. © Patrick J. Endres The temperature within the pipeline is relatively constant despite
ambient temperatures along the line that can range from nearly 100
above to 80 below, which is the Alaska record cold temperature set
on Jan. 23, 1971 at Prospect Creek Camp on the Dalton Highway. The
four inches of fiberglass insulation that surrounds the above-ground
pipeline keeps oil warm enough to flow even on the coldest winter
days. If the pipeline had to be shut down in the winter, the oil
within could sit for several months before congealing.
Powered by the heartbeat of 10 pump stations, oil flows through
the pipeline at about the speed the Yukon River carries a raft-about
5 to 7 miles per hour. At that rate, it takes about five-and-one-half
days for oil to complete the journey from Prudhoe Bay to Valdez.
This article is provided as a public service by
the Geophysical
Institute, University of Alaska Fairbanks, in cooperation with
the UAF research community & the aid of Alyeska Pipeline Service
Company's Elden Johnson. Ned Rozell is a science writer at the institute.
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