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Permafrost

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initial thermal erosion. The research indicates that: (1) melt belt would exist not less than ten<br />

years when the temperature of initial thermal erosion was positive temperature, which will<br />

become hidden trouble of embankment through the long-term working; (2) whereas, when the<br />

temperature of initial thermal erosion was negative temperature, permafrost table ascend 6~10m<br />

in the first three years, and the disappearance time of melt belt was 10 yeas ahead of scheduled<br />

comparing with the normal construction method; (3) the effect of initial thermal erosion of<br />

negative temperature did not linearly increase with the temperature descending, and the lower<br />

negative temperature was not easy realized, therefore, the suggestion best temperature during<br />

construction was -1℃. In conclusion, the temperature field of embankment under the conjunct<br />

effect of air temperature and ground temperature will come into beneficial circulation in the<br />

condition that initial thermal erosion was negative temperature; accordingly, long-term stability<br />

of high-filling embankment can be safeguarded effectively.<br />

Key words: initial thermal erosion; high-filling embankment; permafrost table; melt belt<br />

34<br />

In-situ study on cooling effect of two-phase closed thermosyphon &<br />

insulation combinational roadbed<br />

Junjie Wu,Wei Ma<br />

(State Key Laboratory of Frozen Soil Engineering, CAREERI,CAS, Lanzhou Gansu 730000, China)<br />

Abstract: In 2003, a new testing roadbed—two-phase closed thermosyphon & insulation<br />

combinational roadbed was built in Beiluhe region, which lies in the hinterland of<br />

Qinghai-Tibet plateau. By analyzing the ground temperature of the testing roadbed, we make<br />

some conclusions below. Firstly, the thermosyphons worked consecutively from around<br />

October 10 th to about March 1 st in the first year, and they worked possibly at later proper time.<br />

Secondly, if we choose -2 isotherm as the boundary of the cooling effect, the effective radius<br />

of these thermosyphons is 1.92m in the east slope and, 2.12m in the west slope. Finally, the<br />

combinational configuration makes the roadbed keep a very low ground temperature, so it is a<br />

very successful roadbed configuration for the high-temperature permafrost.<br />

Key words: permafrost; two-phase closed thermosyphon; insulation<br />

Selecting an Appropriate Type of Basement in Regions with<br />

Complicated <strong>Permafrost</strong> Conditions<br />

(an example for north of Western Siberia)<br />

K. Baldunova<br />

(Lomonosov Moscow State University, Geographical faculty, Department of Cryolithology and Glaciology)<br />

Abstract: Western Siberia is a strategically important region of Russia. Analyzing natural<br />

conditions, 4 regions differing in permafrost conditions could be selected of oil-and-gas<br />

provinces, localized in permafrost area of Western Siberia. They are as follows: Yamal, Tar

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