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Çѱ¹Áö¹Ý°øÇÐȸ / v.5, no.4, 1989³â, pp.37-46
¹Ýº¹ÇÏÁßÀ» ¹Þ´Â ½ÇÆ®Áú Á¡Åä¿¡ °üÇÑ ½ÇÇèÀû ¿¬±¸ -°ú¾Ð¹Ð Á¡Å並 Áß½ÉÀ¸·Î-
( An Experimental Study on Silty Clay Subjected to Repeated Loads )
±èÆÈ±Ô;±è°æÁø;¼ÛÀü¼·; Ãæ³²´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú;Ãæ³²´ëÇб³ ´ëÇпø Åä¸ñ°øÇаú, Ãæ³²´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú;;
 
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º» ³í¹®Àº ¹Ýº¹ÇÏÁßÀ» ¹Þ´Â °úÃ߹Р½ÇÆ®Áú Á¡ÅäÀÇ ÀϹÝÀû Ư¼º¿¡ °üÇÑ ¿¬±¸·Î¼­ À缺Çü ½Ã·á¸¦ °ú¾Ð¹Ð »óÅ·ΠÁ¦ÀÛÇÏ¿© ÀÏ·ÃÀÇ º¯Çü-Á¦¾î ¹Ýº¹ »ïÃà½ÃÇèÀ» ¼öÇàÇÏ¿´´Ù. ÀϹÝÀûÀ¸·Î ´ÜÀÏÇÏÁßÀÇ °æ¿ì¿¡ °ú¾Ð¹ÐÁ¡ÅäÀÇ ÃàÂ÷ÀÀ·Â-ÃຯÇü·ü °ü°è´Â ±× ÇüÅ¿¡ ÀÖ¾î Á¤±Ô¾Ð¹ÐÁ¡ÅäÀÇ °á°ú¿Í Èí»çÇÏÁö¸¸, ¹Ýº¹ÇÏÁßÀ» ¹Þ°Ô Äê¸é ½Ã·á ³»ÀÇ °£±Ø¼ö¾Ð °Åµ¿Àº ½Ã·áÀÇ ¾Ð¹Ð¸®·Â °ú ¹Ýº¹ÀÀ·ÂÀÇ Å©±â¿¡ µû¶ó º¯È­ÇÏ°Ô µÈ´Ù. ±×·¯¹Ç·Î ¼­·Î ´Ù¸¥ °ú¾Ð¹Ðºñ¸¦ °¡Áø ½Ã·á¿¡ ´ëÇÑ ¹Ýº¹ ÇÏÁß½ÃÇè °á°ú¸¦ ÅëÇÏ¿© ³ªÅ¸³­ ÀϹÝÀû ÀÀ·Â-º¯Çü Ư¼º¿¡ °üÇÏ¿© »óÈ£ ºñ±³ ºÐ¼®Çϰí,À̵éÀÇ Á¾ÇÕÀûÀÎ °ü°è·ÎºÎÅÍ º¯Çü ¹× °­µµ Ư¼ºÀ» ã°íÀÚ ÇÏ¿´´Ù. ¶ÇÇÑ ½Ã·á°¡ ÆòÇü»ó¿õ·Î Á¸ÀçÇÒ ¼ö ÀÖ´Â ¹Ýº¹ÀÀ·ÂÀÇ ÇѰèÄ¡¸¦ ÀǹÌÇÏ´Â Á÷¼± ȤÀº °î¼±ÇüÅÂÀÇ ÆòÇü»óż±À» °áÁ¤ÇÏ°í °ú¾Ð¹Ðºñ ÀÇ º¯È­¿¡ µû¸¥ÆòÇü»óż±ÀÇ °æÇâÀ» °üÂûÇÏ¿´´Ù.
The object of this paper is to study the general characteristics of overconsolidated silty clays subjected to repeated loading. The samples are first remolded. overconsolidated and a series of strain - controlled triaxial repeated tests are carried out. Generally the relationship of deviator stress - axial strain of overconsolidated clay is similar in pattern to the normally consolidated clay under single load. But the behavior of the pore water pressure build up in the sample subjected to repeated loading is dependent upon the consolidation history and the level of repeated stress. Therefore through the series of the tests, the characteristics of stress -strain relationship of soils which are differentlly overconsolidated are investigated, analysed and then compared with each soils. And also, from the relationship of test results, the strength and strain characteristics of soils are obierved. The equilibrium lines which presents the critical repeated stress and equilibrium state in the sample under repeated loading, are often straight, but may be curved. And the tendency of the equilibrium lines is observed as to the variation of overconsolidation ratio.
 
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Çѱ¹Áö¹Ý°øÇÐȸÁö:Áö¹Ý / v.5, no.4, 1989³â, pp.37-46
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-215X
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198911920443738)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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