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Permafrost

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ESS 315 Any rock/soil at or below the freezing point of water. Remains below 0 degrees Celsius continuously for two years. Ice is not necessarily present. – PowerPoint PPT presentation

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Title: Permafrost


1
Permafrost
  • ESS 315

2
What is Permafrost
  • Any rock/soil at or below the freezing point of
    water.
  • Remains below 0 degrees Celsius continuously for
    two years.
  • Ice is not necessarily present.
  • The active layer is the overlying surface that
    freezes in the winter, and thaws in the summer.

3
Types of Permafrost
  • Cold Permafrost Tolerates considerable heat
    without thawing. Remains between 10 30F.
  • Warm Permafrost Introducing very little heat
    may cause thawing. Just below 34F.
  • Ice Rich 20 - 50 visible ice.
  • Thaw-Stable Permafrost in bedrock is
    well-drained. Coarse grained sediments.
  • Thaw-Unstable Poorly drained, fine-grained
    sediment (clays and silts). Thawing results in so
    much moisture that it flows.

4
Thermokarst Lakes
  • Formed in depressions by melting from thawing
    permafrost
  • Freshwater and usually Shallow

5
  • Solifluction - Slow down slope flow of saturate
    unfrozen earth minerals

6
Ground Patterns
7
Not juston Earth
8
Zones of Permafrost
  • Continuous Zone Permafrost is found almost
    everywhere in the zone.
  • Discontinuous Zone Permafrost found in spots in
    the zone.
  • Sporadic Zone Permafrost found isolated in
    small spots of the zone.

9
Location of Permafrost in North
10
Creation of Permafrost
  • Deep permafrost takes thousands of years to
    create.

11
Construction on Permafrost
  • Heat from a building or other constructed article
    will cause thawing, and can result in sinking.
  • Three solutions are common
  • Using foundations on wood piles
  • Building on a thick gravel pad
  • Using anhydrous ammonia heat pipes
  • Additionally, sinking can be prevented by using
    stilts that extend to a depth of over 15 meters

12
Construction on Permafrost
  • Additionally, sinking can be prevented by using
    stilts that extend to a depth of over 15 meters.

13
The Alaska Pipeline
  • Approximately 75 passes through permafrost
    terrain.
  • Special designs are created to account for the
    movement, melting, and freezing characteristics
    of the ground.
  • There are three principal designs used to
    construct the pipeline. The design varies from
    area to area.

14
Pipeline Designs
  • Above-ground pipeline
  • Problems from melting are avoided in
    thaw-unstable areas by placing the pipeline on an
    elevated support system above ground.

15
Pipeline Designs
  • Below-ground, conventional burial
  • In areas where thaw-stable or unfrozen ground is
    encountered, the pipeline can be buried with no
    special provisions.
  • Below-ground, special burial
  • Where thaw-unstable permafrost is encountered,
    but the pipeline must be buried for highways,
    animal crossings, rockslides/avalanches, etc.
  • The pipeline is insulated so that the heat it
    produces does not promote melting.

16
Ecological Problems
  • Animals will not be able to effectively burrow or
    create dens.
  • Plant roots are constrained to grow in a
    near-surface pattern

17
Works Cited
  • Alaska Pipeline- http//www.alyeska-pipe.com/pipel
    inefacts/Permafrost.html
  • International Permafrost Association -
    http//ipa.arcticportal.org/
  • http//planetparadigm.wordpress.com/2009/02/05/glo
    bal-climate-change-forget-the-climate-models-where
    s-the-real-evidence/
  • http//www.uwsp.edu/geo/faculty/ritter/geog101/tex
    tbook/climate_systems/climate_change.html
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