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Çѱ¹Áö¹Ý°øÇÐȸ / v.12, no.5, 1996³â, pp.17-26
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¾Æ»ê¸¸ ÇØ¼ºÅäÀÇ ÀÀ·Â -º¯Çü·ü °Åµ¿
( The Stress -Strain Behavior of Asan Marine Soil ) |
| ȫâ¼ö;Á¤»ó¼¶;±è¼öÀÏ; »ïº¸±â¼ú´Ü;¿¬¼¼´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú, ¿¬¼¼´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú;;
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| º» ¿¬±¸¿¡¼´Â ¾Æ»ê¸¸ Áö¿ªÀÇ ÇØ¾È ¿¬¾àÃþ¿¡¼ äÃëÇÑ ÇØ¼ºÅäÀÇ °Åµ¿À» ÀÚµ¿ÈµÈ »ïÃà½ÇÇè±â¸¦ »ç¿ëÇÏ¿© ºñ¹è¼ö »óÅÂÇÏ¿¡¼ ½Ç³»½ÇÇè°ú ¸ðµ¨¿¹ÃøÀ» ¼öÇàÇÏ¿© ÆÄ±«Àü°ú ÆÄ±«»óŽà ÀÀ·Â-º¯Çü·ü »óŸ¦ Á¡ÅäÁú ¹× ½ÇÆ®Áú Èë°ú ºñ±³ºÐ¼®ÇÏ¿´´Ù. äÃëÇÑ ÇØ¼ºÅä´Â ½ÇÆ®Áú 70%¿Í Á¡ÅäÁú 30%°¡ ¼¯ÀΠȥÇÕÅä·Î ÇöÀåÀÇ ºñ±³¶õ ½Ã·á¿Í À̸¦ Àç ¼ºÇüÇÑ ½Ã·áÀÇ 2Á¾·ù·Î ¸¸µé¾î 400kpaÀÎ À¯È¿±¸¼Ó¾Ð·Â±îÁö µî¹æ¾Ð¹Ð ½ÃŲ ÈÄ ¾Ð¹ÐÇÏÁßÀ» °¨¼Ò½ÃŰ¸ç ±¸¼Ó¾ÐÀÌ °¢°¢ 400, 200, 100, 67kpaÀÎ °æ¿ì¿¡ ºñ¹è¼ö »óÅ·Π»ïÃà¾ÐÃà ¹× ÀÎÀå½ÇÇèÀ» ÇÏ¿´´Ù. º» ¿¬±¸°á°ú ¸ðµç ½Ã·áÀÇ ±ØÇÑ»óŸ¦ ¿¬°áÇϸé ÀÏÁ¤ÇÑ ÆÄ±«¼±¿¡ µµ´ÞÇÏ¿´À¸¸ç À̶§ ÆÄ±«¼±Àº ¼ø¼öÁ¡Å䳪 ½ÇÆ®¿¡ ºñÇØ¼´Â ±× ±â¿ï±â¿¡ Â÷À̰¡ ÀÖ¾ú´Ù. ¶ÇÇÑ Á¤±Ô¾Ð¹ÐµÈ ¾Æ»ê¸¸ ÇØ¼ºÅä¿¡¼´Â Àü´ÜÃʱ⿡´Â ¼ø¼öÁ¡Åä¿Í À¯»çÇÏ°Ô Àü´ÜÇÏ¿¡¼´Â ¾çÀÇ °£±Ø¼ö¾ÐÀÌ ¹ß»ýÇÏ¿© P'ÀÌ °è¼Ó °¨¼ÒÇϳª ½ÇÆ®Áú¿¡¼ ³ªÅ¸³ª´Â »óź¯Çü¼±À» Áö³ª¼´Â üÀûÆØÃ¢°æÇâÀÌ ³ªÅ¸³ª¸ç Àü´Ü°µµ°¡ Áõ°¡Çϰí ÀÖ´Ù. °ú¾Ð¹Ð ½Ã·á´Â üÀûº¯Çü °æÇâÀ¸·Î ¼ø¼ö½ÇÆ®¿Í´Â »ó´çÈ÷ ´Ù¸¥ °Åµ¿À» º¸ÀÓÀ» ¾Ë ¼ö ÀÖ¾ú´Ù. ¼öÁ¤ Camflay¸ðµ¨ ¹× Ç׺¹°æ°è¸é ¸ðµ¨À» »ç¿ëÇÏ¿© ¿¹ÃøÇÑ °á°ú Á¤±Ô¾Ð¹ÐµÈ °æ¿ì¿¡´Â ÃÖ´ë°µµ ÀÌÀü±îÁö´Â ½ÇÁ¦°Åµ¿À» ÀûÀýÈ÷ ¿¹ÃøÇÒ ¼ö ÀÖ¾úÀ¸³ª °ú¾Ð¹Ðºñ$(2leqOCRleq6)$°¡ Ä¿Áú¼ö·Ï ±× °Åµ¿¿¡´Â Á¤·®ÀûÀÎ Â÷À̸¦ º¸ÀÓÀ» ¾Ë ¼ö ÀÖ¾ú´Ù. |
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| The undrained behavior of Asan marine soil was investigated by using an automated triaxial testing device. The stress-strain behavior at the preand postfailure state of marine soil under undrained compression and eatension conditions was compared with the behavior of pure silt, pure clay and the overall behavior of Asan marine soil was predicted with the modified Camflay model and the bounding surface model. The marine soil sampled in Asan bay area was clayey silts with 70oA silt-30% clay content and the testing samples were prepared in both undisturbed and remolded conditions. All samples are normally consolidated with 400 kPa of effective mean confining pressure and each sample is unloaded to 200, 100, 67 kPa, respectively. And then the shear test was performed with different confining pressure. According to experimental results, there exists an unique failure line whose slope is lower than silt's and higher than clay's. It is identified that the undrained shear strength of normally consolidated samples increases after crossing the phase transformation line because of volume dilation tendency which is not seen in clay. Overconsolidated samples show different soil behavior compared with pure silt due to its tendency of change in volume. It is also found that the overall behavior of Asan marine soil cannot be predicted precisely with the modified Cam-clay model and the bounding surface model. |
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| Ű¿öµå |
| Triaxial compression;Extension test;Undisturbed;Remolded sample;Failure line;Phase transformation line;Normally consolidated sample;Overconsolidated sample;Model prediction; |
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Çѱ¹Áö¹Ý°øÇÐȸÁö:Áö¹Ý / v.12, no.5, 1996³â, pp.17-26
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-215X
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199611920446795)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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