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Çѱ¹¼öÀÚ¿øÇÐȸ / v.6, no.1, 1973³â, pp.13-18
µ¿°áµÈ ÈëÀÇ °­µµ¿¡ °üÇÑ ½ÇÇèÀû ¿¬±¸
( The Strength of Frozen Soil )
ÁÖ¸¶¼­; Á¤È¸¿ø¡¤¿¬¼¼´ëÇб³Åä¸ñ°øÇаú-1973. 3. 28 ¼ö¸®-;
 
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If the temperature of free water drops below the freezing point the water turns into ice and its volume increases. Analyzing of the results in test, it is hoped that these is broadly used in engineering plan. The compressive strength of frozen soils and the unconfined compressive strength of the ice. The creep strength depends on factors including creep ratio, time, strain and temperature. For a linear decreases in temperature, strength predicts an exponential increasing. The relationships between dry unit weight and compressive strength, water content and freezing with compacted soil samples, have been analyzed to understand the strength of frozen soil. Therefore, it is thankful that the results of analsis shall find useful application as a framework for generalizing experimental information as well as a basis for solving various frozen soil mechanics problems.
 
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.6, no.1, 1973³â, pp.13-18
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO197311920088250)
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