Permafrost
Permafrost
Permafrost
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54<br />
Laboratory Study on the Dynamic Strength Characteristic<br />
on Frozen Silty Clay<br />
Shujuan ZHANG, Yuanming LAI, Xiaoxiao CHANG<br />
(State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering<br />
Research Institute, Chinese Academy of Sciences, Lanzhou, Gansu, 730000, China)<br />
Abstract: Using triaxial cycle tests with constant stress amplitude under confining pressures<br />
between 0.3MPa and 16.0MPa at a temperature of -4℃ and at a frequency 2Hz, dynamic<br />
strength characteristics of frozen silty clay were studied. The results showed that the dynamic<br />
strength depended not only on the confining pressure and the number of vibration, but also on<br />
maximum loading stress at constant minimum loading stress. Additionally, pressure melting of<br />
pore ice and growth of micro-cracks also influence dynamic stress response. The critical<br />
number of vibrations and the critical confining pressure were put forward. Finally, the dynamic<br />
and static strength tests were conducted to assess the design of foundation base in permafrost<br />
regions.<br />
Key words: Frozen silty clay, dynamic strength characteristic, vibrating number, confining<br />
pressure<br />
Practical Modeling for Frost Heave Estimation of Chilled Gas Pipeline<br />
Buried in Frost Susceptible Soil<br />
Shunji Kanie 1 , Satoshi Akagawa 2 and Takashi Mikami 3<br />
(1.Associate Professor, Graduate School of Engineering, Hokkaido Univ., Kita 13, Nishi 8, Kitaku,<br />
Sapporo,Japan, 0608628, Tel:+81-11-706-6175, e-mail: kanie@eng.hokudai.ac.jp (Corresponding Author);<br />
2. Professor, Graduate School of Engineering, Hokkaido Univ., Kita 13, Nishi 8, Kitaku,<br />
Sapporo,Japan,0608628,Tel:+81-11-706-7246,Fax:+81-11-706-7246,e-mail:akagawa@eng.hokudai.ac.jp;<br />
3. Professor, Graduate School of Engineering, Hokkaido Univ., Kita 13, Nishi 8, Kitaku, Sapporo,<br />
Japan,0608628, Tel:+81-11-706-6174, e-mail: tmikami@eng.hokudai.ac.jp)<br />
Abstract: It has been known that chilled gas pipeline buried through a boundary between<br />
permafrost and non-permafrost is likely to suffer bending deflection due to frost heave since the<br />
pipeline is held tightly in permafrost whereas the other end in non permafrost is surrounded by<br />
growing frost bulb and is subjected to frost heaving. As a result, large deflection of pipeline is<br />
expected to occur near the boundary and it may cause fatal damage to the pipeline.<br />
For the frost heave estimation of structure buried in frost susceptible soil, various methods<br />
have been proposed so far. However, most of those require many parameters to explain this<br />
complicated phenomenon as a numerical model since the frost heave depends on freezing rate,<br />
permeability of the soil, amount of water migration and etc. The authors, then, propose to adopt<br />
Takashi’s equation for the frost heave estimation. Introducing only three parameters obtained<br />
through indoor experiment, Takashi’s equation relates the frost heave ratio with the constraint<br />
pressure at the freezing front and its freezing rate. This equation has been confirmed to give<br />
satisfactory estimation for one-dimensional frost heave so that the procedure of the indoor