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Çѱ¹Áö¹Ý°øÇÐȸ / v.18, no.6, 2002³â, pp.73-81
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ÇØ¼ºÁ¡ÅäÁö¹Ý¿¡¼ CPT¸¦ ÀÌ¿ëÇÑ ÀÀ·ÂÀÌ·Â(OCR, $sigma¸¦$p)ÀÇ »êÁ¤
( Profiling Stress History(OCR, $sigma¸¦$p) of Marine Clay Using Piezocone Penetration Test ) |
| À̰¿î;À±±æ¸²;俵¼ö; ¢ßµ¿¼º¿£Áö´Ï¾î¸µ;Çѱ¹Çؾ翬±¸¿ø, ¿¬¾ÈÇ׸¸°øÇк»ºÎ;¼ö¿ø´ëÇб³ Åä¸ñ°øÇаú;
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| ±¹³» ³²ÇØ¾È ÇØ¼ºÁ¡Åä Áö¹ÝÀÇ ÀÀ·ÂÀÌ·Â(stress history)¿¡ ´ëÇÏ¿© ÇÇÁ¶ÄÜ °üÀÔ½ÃÇè ¹æ¹ýÀ» ÀÌ¿ëÇÏ¿© Åë°èºÐ¼®°ú »ç·Ê ¿¬±¸À» ÅëÇÏ¿© Á¶»çÇÏ¿´´Ù. °æÇè½Ä°ú ÇÇÁ¶ÄÜ °üÀÔ½ÃÇèÀ¸·Î »êÁ¤ÇÑ ¼±Çà¾Ð¹ÐÀÀ·Â°ú °ú¾Ð¹Ðºñ´Â ÀÌ·ÐÀû, °æÇèÀû »ó°ü°ü°è¸¦ ã°íÀÚ È¸±ÍºÐ¼®À» ¼öÇàÇÏ¿´°í ±âÁذªÀº ½Ç³» Ç¥ÁؾйнÃÇè °á°ú¸¦ Åä´ë·Î ÇÏ¿´´Ù. Ç¥ÁؾйнÃÇè¿¡¼ ³ªÅ¸³ Á¶»ç Áö¹ÝÀÇ ÀÀ·ÂÀÌ·Â »óÅ´ ÀüüÀûÀ¸·Î ÇØ¼ö¸é ¾Æ·¡ Ç¥Ãþ l0m±îÁö´Â °ú¾Ð¹ÐµÈ »óÅ¿´À¸³ª, Ç¥Ãþ l0m ¾Æ·¡ ±íÀÌ¿¡¼´Â °ú¾Ð¹Ðºñ(OCR)°¡ 0.3±îÁöµµ Á¸ÀçÇÏ¿© Àü¹ÝÀûÀ¸·Î ÁöÃþ»óÅ´ ºÒ¾ÈÁ¤ÇÑ ±¸Á¶¸¦ °¡Áö°í ÀÖ¾ú´Ù. ÀÀ·ÂÀ̷¿¡¼ ¼±Çà¾Ð¹ÐÇÏÁßÀÇ °áÁ¤Àº Chen°ú Mayne(1996)ÀÇ °æÇè¹æ¹ý°ú Konrad¿Í Law(1987)ÀÇ À̷аø½ÄÀ» »ç¿ëÇÏ¿´´Ù. »êÁ¤°á°ú, Chen°ú Mayne(1996)ÀÇ °æÇè°ø½ÄÁß¿¡¼ °£±Ø¼ö¾ÐÀ» ÀÌ¿ëÇÑ ¿¹Ãø¹æ¹ýÀÌ °¡Àå ½Å·Ú¼ºÀÌ ³ô¾Ò´Ù. ±×¸®°í °ú¾Ð¹Ðºñµµ Chen°ú Mayne(1996)ÀÇ °æÇè½ÄÀÌ °¡Àå ³ôÀº ½Å·Ú¼ºÀ» º¸¿´´Ù. ÇÏÁö¸¸ Mayne°ú Holtz(1988), ±×¸®°í Mayne°ú Bachus(1988)¹æ¹ýÀº °¢°¢ OCRÀÌ 1.0ÀÌÇÏÀÎ ¹Ì¾Ð¹Ð Áö¹Ý¿¡¼ ÁÁÀº °á°ú¸¦ Á¦½ÃÇÏ¿´´Ù. ±×·¯¹Ç·Î ÇÇÁ¶ÄÜ °üÀÔ½ÃÇèÀ¸·ÎºÎÅÍ Áö¹ÝÀÇ ÀÀ·ÂÀÌ·ÂÀ» »êÁ¤ÇÏ´Â ´Ù¾çÇÑ ¹æ¹ýÀº ´ëºÎºÐ Áö¹ÝÁ¶°Ç°ú À§Ä¡¿¡ µû¶ó ±× °á°ú°¡ Å©°Ô ´Ù¸£¹Ç·Î Áö¿ª°ú ÇöÀ寝¼ºÀ» ¹Ý¿µÇÑ ÀûÇÕ½ÄÀ» °³¹ßÇÏ¿© Áö¹Ý ¼³°è¿¡ Ȱ¿ëÇÏ´Â °ÍÀÌ Å¸´çÇÑ °ÍÀ¸·Î ÆÇ´ÜµÇ¾ú´Ù. |
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| Various CPT-based prediction models far profiling stress history of marine clay at the southern part of the Korean peninsula were investigated by using both statistical analysis and case history study. Preconsolidation pressures($sigma'$p) and overconsolidation ratio(OCR) estimated by empirical correlations and cone penetration tests were compared with those of laboratory odometer test results. Stress history of marine clay determined by odometer test results was in general overconsolidated at below 10m depth from the mudline, whereas marine clay at below l0m depth from the mudline which has an around 0.3 overconsolidation ratio showed variable stresses and unstable states. Preconsolidation pressures were computed by both empirical methods of the Chen and Mayne(1996) and theoretical method of Konrad and Law(1987). It is estimated that Chen and Mayne(1996)'s prediction method based on pore water pressure is more reliable than any other prediction methods, and their method proved to be the most reliable for overconsolidation ratio estimation. However, it is recommended that Mayne & Holtz(1988) and Mayne & Bachus(1988) methods are more suitable than any other methods for predicting the overconsolidation ratio at an underconsolidated (OCR<1) clay. For these reasons, rather than making use of existing prediction models, development of site specific empirical correlations which considers local characteristics and site conditions may be required due to different local stress history and variable soil properties. |
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| Ű¿öµå |
| Marine clay;OCR;Piezocone;Porewater pressure;Preconsolidation;Stress history; |
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Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.18, no.6, 2002³â, pp.73-81
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200211921511339)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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