Permafrost
Permafrost
Permafrost
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influence its temperature change process. The temperature increase and decrease process in the<br />
layer of high ice content is relatively slow.<br />
2) The factors of drilling methods<br />
Drilling in different methods disturbs the frozen ground to varying degrees. In the process<br />
of percussion boring, the circulation of slurry carries a great quantity of heat into the ground<br />
and brings about great heat exchange with the frozen ground and causes the increase of the<br />
frozen ground. For instance, after 2 months of the boring process the temperature of frozen<br />
ground at the center of piles group increases about 0.5℃.<br />
For the rotary drilling, the frozen ground temperature increase caused by the friction heat is too<br />
small to be neglected comparing with the percussion boring.<br />
3) The factors of volume and thermal physical properties of concrete<br />
The bigger the concrete pile is, the greater thermal disturbance to the frozen soil<br />
foundation will be. Especially for the piles group, the influence between the piles will lead to<br />
superimposed effect, and causes the temperature of the frozen soil rising obviously.<br />
The concrete mix proportion, the cement hydration heat and the concrete temperature<br />
before pouring influence the temperature of frozen soil and the refreezing process of the<br />
foundation greatly. The greater the cement hydration heat and the higher temperature of<br />
concrete, the larger quantity heat will be carried into the ground and the more difficult for<br />
foundation to refreeze.<br />
The adfreezing force between large-diameter cast-in-situ pile and the frozen soil<br />
dependents on the temperature of frozen soil around the pile. The regression analysis result of<br />
pile load in-situ tests shows that the adfreezing force increases 0.08~0.1MPa while the<br />
temperature of frozen soil around the pile decreasing 1℃ in the range from –0.3 to –2.5℃.<br />
Strength Behavior and Unfrozen Water Content of Saline Fine-grained<br />
Frozen Soils<br />
Xi-zhong Yuan 1,2 , Yuan-lin Zhu 1 , Wei Ma 1<br />
(1 State Key Laboratory of Frozen Soil Engineering, CAREERI, CAS, Lanzhou Gansu 730000)<br />
(2 Key Laboratory for Special Area Highway Engineering of Ministry of Education, Chang’an University,<br />
Xi’an 710064)<br />
Abstract: The influence of soil type, initial water content, temperature, strain rate and salinity<br />
on strength of three different fine-grained saline frozen soil under conditions of unconfined<br />
constant strain rate tests is studied in this paper. The soils include silt, silty clay and clay which<br />
were taken from the sites along the Qinghai-Xizhang railway in construction. The range of<br />
initial water content is from 4% to 50%, and the salinity varies from 0 to 40 parts per thousand<br />
(ppt). The range of temperature of strength test is from –2 to –10℃, and the range of strain rate<br />
is from 1.1*10 -3 to 1.1*10 -6 s -1 .<br />
The effects of temperature and salinity can be normalized through unfrozen water content<br />
in frozen soil, so the measurement of unfrozen water content at different temperature<br />
corresponding to the strength test condition were carried out using pulsed nuclear magnetic<br />
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