¶óÆæÆ®¦¢Ä«Æä¦¢ºí·Î±×¦¢´õº¸±â
¾ÆÄ«µ¥¹Ì Ȩ ¸í»çƯ°­ ´ëÇבּ¸½Ç޹æ Á¶°æ½Ç¹« µ¿¿µ»ó°­ÀÇ Çѱ¹ÀÇ ÀüÅëÁ¤¿ø ÇÐȸº° ³í¹®
ÇÐȸº° ³í¹®

Çѱ¹°Ç¼³°ü¸®ÇÐȸ
Çѱ¹°ÇÃà½Ã°øÇÐȸ
Çѱ¹µµ·ÎÇÐȸ
Çѱ¹»ý¹°È¯°æÁ¶ÀýÇÐȸ
Çѱ¹»ýÅÂÇÐȸ
Çѱ¹¼öÀÚ¿øÇÐȸ
Çѱ¹½Ä¹°ÇÐȸ
Çѱ¹½Ç³»µðÀÚÀÎÇÐȸ
Çѱ¹ÀÚ¿ø½Ä¹°ÇÐȸ
Çѱ¹ÀܵðÇÐȸ
Çѱ¹Á¶°æÇÐȸ
Çѱ¹Áö¹Ý°øÇÐȸ
Çѱ¹ÇÏõȣ¼öÇÐȸ
Çѱ¹È¯°æ»ý¹°ÇÐȸ
Çѱ¹È¯°æ»ýÅÂÇÐȸ

Çѱ¹Áö¹Ý°øÇÐȸ / v.9, no.4, 1993³â, pp.55-64
À̹æÁ¤±Ô¾Ð¹ÐÁ¡ÅäÀÇ ºñ¹è¼öÅ©¸®ÇÁ ÆÄ¾ç
( Undrained Creep Rupture of an Anisotropically Normally Consolidated Clay )
°­º´Èñ;È«ÀÇ; Á¤È¸¿ø, ÀÎÇÏ´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú;Çö´ë°Ç¼³ÁÖ½Äȸ»ç ÇØ¿ÜÅä¸ñ»ç¾÷º»ºÎ;
 
ÃÊ ·Ï
À̹æ¾Ð¹ÐÀÌ ºñ¹è¼öÅ©¸®ÇÁÆÄ±«°Åµ¿¿¡ ¹ÌÄ¡´Â ¿µÇâÀ» ¿¬±¸Çϱâ À§ÇÏ¿© 4°¡ÁöÀÇ ¾Ð¹ÐÀÀ·Âºñ(a:In'/clc': 1.0, 0.7, 0.5, 0.4)·Î¼­ Á¤±Ô¾Ð¹Ð½ÃŲ Á¡Åä½Ã·á¿¡ ´ëÇØ¼­ ºñ¹è¼öÅ©¸®ÇÁ½ÃÇèÀ» ¼öÇàÇÏ¿´´Ù. ¾î¶² ÃÖ¼Òº¯Çü·ü¼Óµµ¿¡ À̸£´Â °æ°ú½Ã°£Àº ¾Ð¹ÐÀÀ·ÂºñÀÇ °¨¼Ò¿¡ µû¶ó ÁÙ¾îµé°í ÀÌ ÃÖ¼Òº¯Çü·ü¼Óµµ¿¡ ´ëÇÑ ÆÄ±«½Ã°£µµ °¨¼ÒµÈ´Ù. Finn and Shead(1.1ÀÇ Á¦¾È½Ä¿¡ ÀÇÇØ¼­ ±¸ÇÑ »óÇÑÇ׺¹°­µµ´Â ¾Ð¹ÐÀÀ·ÂºñÀÇ Å©±â¿¡ °ü°è¾øÀÌ Å©¸®ÇÁ°­µµ¿Í Àß ÀÏÄ¡ÇÏ¸ç Æò±Õ±¸¼ÓÀÀ·ÂÀ¸·Î¼­ Á¤±ÔÈ­ÇÑ »óÇÑÇ׺¹ °­µµ´Â ¾Ð¹ÐÀÀ·Âºñ°¡ Áõ°¡ÇÒ¼ö·Ï °¨¼ÒÇÑ´Ù.
The Undrained creep tests on the normally consolidated clays with four different consolication ratios(c3c'/clc': 1.0, 0.7, 0.5, 0.4) were performed to investigate the effects of avisotropic consolidation on the undrained creep rupture behavior. The elapsed time to a certain minimum strain rate is decreased with decreasing the value of the consolidation pressure ratio, and the elapsed time to rupture for a certain minimum strain rate is also decreased with decreasing the ratio. The upper yield strength obtained from the equation suggested by Finn and Shead(1.) is coincided well with the creep strength irrespective of the magnitude of the consolidation pressure ratio, and the normallised upper yielding strength by mean confining pressure is decreased with increasing the consolidation pressure ratio. The critical strain for creep rupture, the strain at min. strain rate, is constant irrespective of the magnitude of creep stress, but it increased exponentially with increasing the ratio, It accordingly is dangerous that the potential of in-situ creep rupture is estimated only by the creep rupture test on the isotropically consolidated clay in case of K0-value below 1.0.
 
Ű¿öµå
 
Çѱ¹Áö¹Ý°øÇÐȸÁö:Áö¹Ý / v.9, no.4, 1993³â, pp.55-64
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-215X
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199311920445202)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
¸ñ·Ïº¸±â
ȸ»ç¼Ò°³ ±¤°í¾È³» ÀÌ¿ë¾à°ü °³ÀÎÁ¤º¸Ãë±Þ¹æÄ§ Ã¥ÀÓÀÇ ÇѰè¿Í ¹ýÀû°íÁö À̸ÞÀÏÁÖ¼Ò ¹«´Ü¼öÁý °ÅºÎ °í°´¼¾ÅÍ
   

ÇÏÀ§¹è³ÊÀ̵¿