¶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.13, no.1, 1997³â, pp.147-158
ÁöÁö·Â¿¡ ¹ÌÄ¡´Â ÀçÇϼӵµ¿¡ °üÇÑ ÇØ¼®Àû ¿¬±¸
( Effect of Loading Rate to Bearing Capacities )
¹ÚÁß¹è; Á¤È¸¿ø, (ÁÖ)´ë¿ì °Ç¼³±â¼ú¿¬±¸¼Ò;
 
ÃÊ ·Ï
º»¿¬±¸´Â À¯ÇÑ¿ä¼Ò¹ýÀ» ÀÌ¿ëÇÏ¿© Áß°£ÅäÁö ¹Ý¿¡ À־ÀÇ ºÎºÐ¹è¼öÀÇ Á¤µµ°¡ ÁöÁö·Â ¹× º¯Çü Ư¼º¿¡ ¹ÌÄ¡´Â ¿µÇâÀ» ÇØ¼®ÀûÀ¸·Î °íÂûÇÑ °ÍÀÌ´Ù. µ¿½Ã¿¡ °è»ê °á°ú¸¦ ¸ðÇü½ÇÇè °á°ú¿Í ºñ±³ÇÏ¿© °è»ê¹ýÀÇ Å¸´ç¼º ¹× ºÎºÐ¹è¼öÀÇ Çö»óÀÌ ¹ß»ýÇÏ´Â Áö¹ÝÀÇ ÁöÁö·Â ¹®Á¦¿¡ÀÇ Àû¿ë¼ºÀ» °ËÅäÇÏ¿´´Ù. ÇØ¼®¿¡´Â ¼öÁ¤ Cam-clay¸¦ ÀÌ¿ëÇÑ ÇÁ·Î±×·¥ CRISP90À» ÀÌ¿ëÇÏ¿´°í,¸ðµ¨½ÇÇè¿¡¼­´Â ¿ø½É ¸ðÇü½ÃÇèÀåÄ¡¸¦ ÀÌ¿ëÇÏ¿´´Ù. ÇØ¼® °á°ú, ºÎºÐ¹è¼öÀÇ ¿µÇâÀ» ¹Þ´Â Áß°£ÅäÁö¹ÝÀÇ ÇÏÁßÄ¢ÇÏ °ü°è¸¦ ÃæºÐÇÑ Á¤µµ·Î Ç¥ÇöÇÒ ¼ö ÀÖÀ¸¸ç, µ¿¹ý¿¡ ÀÇÇØ »ó´ëÀçÇϼӵµ¸¦ ¹è¼ö, ºñ¹è¼ö ¹× ºÎºÐ¹è¼ö¿µ¿ªÀÇ 3¿µ¿ªÀ¸·Î ºÐ·ù °¡´ÉÇϰí, ºÎºÐ¹è¼ö ¿µ¿ªÀÇ ¹üÀ§´Â 10ÀýµµÀÓÀ» ¹àÇû´Ù.
In this study, it is examined that partial drain has an effect of bearing capacities and deformations on intermediate soils. To compare the numerical and experimental results, this study uses CRISP90 which is composed of Modify Cam-Clay Model for calculation and Geotechnical Centrifuge in model test. As the results of analysis, we can classify relative loading rate into three ranges which are drain, undrain and partial drain. Besides it is proved that partial drain range is about 103.
 
Ű¿öµå
Intermediate soil;Relative loading rate;Deformation;Bearing Capacity;
 
Çѱ¹Áö¹Ý°øÇÐȸÁö:Áö¹Ý / v.13, no.1, 1997³â, pp.147-158
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-215X
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199711920447193)
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¿