Permafrost
Permafrost
Permafrost
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distribution. Therefore it is necessary to study the mechanism of moisture-heat transfer. At<br />
present most study on the characteristics of rock and soil engineering in cold region focus on<br />
researching characteristics of frozen soil, the study which touch on rock especially soft rock is<br />
rare; the study which deal with frost and thaw is rare. But as for rock and soil engineering in<br />
cold regions, which coexist with rock mass and soil, deformation and strength property of rock<br />
and soil show two sides from strength property of friction materials of melted rock and soil at<br />
high temperatures to strength property of crystal lattice material of frozen rock and soil at low<br />
temperatures under the freeze – thaw cycles condition or during freezing-thawing process. We<br />
must therefore make an intensive study of moisture-heat transfer and phase transformation<br />
under frost and thaw condition.<br />
In this paper, the experiment study on the moisture and heat transfer of soft rock material<br />
during its freezing and thawing is researched in the laboratory of our university. The soft rock<br />
material-concrete mortar is used during the moisture and heat transfer experiment. Two<br />
different kinds of soft rock material are experimented in the open system with temperature<br />
gradients. On the ground of experimental results and analysis we can reach some conclusions:<br />
the degree of the moisture and heat transfer is different between the different soft rock materials,<br />
the content of quartz mineral in the sample is higher, the redistributing time of the temperature<br />
field is longer; the gradient of temperature is the main driving power of the moisture transfer,<br />
the grads is higher and the moisture field redistributes quicker; the porosity ratio is higher and<br />
the process of freezing is longer.<br />
Key words: freezing and thawing, moisture and heat transfer, the study of experiment<br />
26<br />
Artificial Freezing of Ground in the Base of Deformed<br />
Buildings in the North of Siberia<br />
Grebenets V.I. 1 , Titkov S.N. 2<br />
(1. Lomonosov Moscow State University, Geographical faculty, Department of Cryolithology and Glaciology<br />
box.ru; 2. Research Institute of Bases and Underground Structures, Ministry of Building of Russia)<br />
Abstract: A problem of stability of buildings and structures in the permafrost zone has become essentially<br />
aggravated during the last decade. In cities of Northern Russia the tendency to develop mass-scale<br />
deformations of buildings and structures is observed. It was determined that the basic reasons of deformations<br />
are negative technogenic impact on the geocryological and geoecological environment while global warming<br />
has not shown detectable influence on the bearing capacity of frozen bases. A complex set of<br />
engineering-technical measures intended to stabilize the situation in large industrial centers of the Russian<br />
North as well as special methods for strengthening frozen bases has been developed and experimentally<br />
proved in Russia. The emphasis is made on the application of artificial cooling through the tapping of natural<br />
stocks of cold in rocks. Methods of cooling of boreholes by cold outer air by means of artificial and natural<br />
convection as well as by the use of spending cooling agents have been developed. "Liquid" and<br />
"steam-liquid" thermal piles demonstrated the most efficiency in operation. The positive as well as negative<br />
experience of 20-years term of operation thermal piles have been analysed. Results of geothermal