Page 245 - Geotechnical Engineering Soil and Foundation Principles and Practice
P. 245

Pore Water Pressure, Capillary Water, and Frost Action
                240   Geotechnical Engineering

                 Figure 11.20
                 Settlement from
                 thawing of
                 permafrost by a
                 heated building,
                 Big Delta, Alaska.















                                    11.10.7   Premafrost and Engineering
                                    The most direct approach to prevent problems from melting of permafrost is to
                                    keep it frozen, but this is becoming more difficult because of the sensitivity of
                                    northern climates to change, with the result that these areas are the first to feel
                                    major impacts from global warming. The moisture content at which a soil
                                    becomes liquid is called the ‘‘liquid limit,’’ and when permafrost melts, the soil
                                    moisture content usually exceeds the liquid limit and is trapped until it can drain
                                    away or evaporate.

                                    Seasonal thawing can be prevented by supporting structures on piles extending
                                    into the permafrost layer and allowing winter air to circulate underneath the
                                    structures in the winter. Another method uses ducts in soil under a structure in
                                    order to force-circulate cold winter air.

                                    Oil pipelines must be protected from loss of support by thawing permafrost in
                                    order to prevent environmentally disastrous oil spills. The scheme shown in
                                    Fig. 11.21 was used for the Trans-Alaska pipeline, and employs a passive heat
                                    transfer mechanism with a vaporizing refrigerant. During winter when the soil is
                                    warmer than the air, refrigerant in the soil zone evaporates, taking heat with it,
                                    then rises and condenses in the colder ends of the tubes, releasing heat to the air.
                                    The refrigerant then flows down by gravity to replenish the supply at the bottom.
                                    During summer the cycle is broken because the refrigerant remains at the bottom
                                    of the tubes. A similar, less efficient, but less costly system uses convection, as air
                                    inside a pipe is warmed by the soil and moves up and out. The air is replenished by
                                    cold winter air from the ground surface and conducted downward through a
                                    center pipe.

                                    Roads can pose a difficult problem in permafrost areas because, if they are built
                                    up for better drainage, permafrost can rise in the road embankment and create a

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