¶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.3, no.4, 1987³â, pp.7-20
´ÙÂ÷¿ø ¾Ð¹ÐÇØ¼®À» À§ÇÑ ÇѰè»óÅÂÀ̸¥ÀÇ Àû¿ë
( Application of the Critical State Theory to Multi-Dimensional Consolidation Analysis )
Á¤Áø¼·; Á¤È¸¿ø, ¿ø±¤´ëÇб³ °ø°ú´ëÇÐ;
 
ÃÊ ·Ï
¿¬¾àÁö¹ÝÀÇ ´ÙÂ÷¿ø ¾Ð¹ÐÇØ¼®À» À¯ÇÑ¿ä¼Ò¹ýÀ¸·Î ÇØ¼®Çϱâ À§ÇÏ¿© Á¡ÅäÀÇ ±¸¼º¹æÁ¤½ÄÀ¸·Î¼­ ½Å»ýÅðÀû Á¡ÅäÃþ¿¡¼­ ¾Ð¹Ð½Ã¿¡ ¿¹»óµÇ´Â creep¿Í °°Àº º¯ÇüÀÇ ½Ã°£ÀÇÁ¸¼º°Åµ¿À» ǥģÇϴ ź Á¡¼Ò¼º ±¸¼º¹æÁ¤½ÄÀ» »õ·ÎÈ÷ Á¦¾ÈÇϱâ À§ÇÏ¿© ÇѰè»óÅ °³³äÀ¸·ÎºÎÅÍ °³¹ßµÈ ¼öÁ¤ cam clay ¸ðµ¨À» º¸¿ÏÇÏ¿© À½·Âº¯ÇüÇØ¼®À» ÅëÇÏ¿© ½ÇÃøÄ¡¿Í ºñ±³ÇÑ °ÍÀÌ´Ù. ±× °á°ú ´ëüÀûÀ¸·Î ½ÇÃøÄ¡¿Í Á¢±ÙÇϰí ÀÖÀ½À» ¾Ë ¼ö ÀÖ¾ú´Ù.
This study was performed to investigate the effect of time-dependent creep on the deformation analysis of multi-dimensional consolidation using the finite element method for young Sedimentary clay. It was assumed that the creep in the clay had occured during consolidation. In the analysis, the Modified cam-clay theory originated from the critical state theory was used as the constitutive equation, in which a term equivalent to the creep was supplemnted. The results of the analysis were in good agreement with the observed values in the field.
 
Ű¿öµå
 
Çѱ¹Áö¹Ý°øÇÐȸÁö:Áö¹Ý / v.3, no.4, 1987³â, pp.7-20
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-215X
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198711920443075)
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¿