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Çѱ¹Áö¹Ý°øÇÐȸ / v.18, no.3, 2002³â, pp.105-112
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( Excess Pore Water Pressure Response in Soft Clay under Embankment ) |
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| ¼ºÅäÇϺΠ¿¬¾àÁö¹Ý¿¡¼ »óÀçÇÏÁßÀÇ º¯È°¡ ¾ø´Â »óÅ¿¡¼ °úÀ×°£±Ø¼ö¾ÐÀÇ Áõ°¡°¡ Berthierville¿Í Olga Áö¿ª¿¡¼ º¸°íµÇ¾ú´Ù. À̿Ͱ°Àº ºñÁ¤»óÀûÀÎ Çö»óµéÀ» °íÀüÀûÀÎ ¾Ð¹ÐÀÌ·ÐÀ¸·Î ¼³¸íÇϱâ´Â ¾î·Æ´Ù. º» ³í¹®Àº ºñ¼±Çü Á¡¼Ò¼º¸ðµ¨À¹ »ç¿ëÇÏ¿© ÀÚ¿¬Á¡ÅäÁö¹Ý¿¡¼ À¯¹ßµÇ´Â °£±Ø¼ö¾Ð Áõ°¡¸¦ ¼³¸íÇÏ¿´´Ù. Á¦¾ÈµÈ ¸ðµ¨Àº Darcy ¹ýÄ¢¿¡ ÀÇÇÑ °£±Ø¼ö¾Ð ¼Ò»ê°ú Á¡¼Ò¼º º¯Çü¿¡ ÀÇÇÑ °£±Ø¼ö¾Ð »ý¼º¿¡ ´ëÇÑ º¹ÇÕÀûÀÎ °Åµ¿À» ¸ð»çÇÒ »Ó¸¸ ¾Æ´Ï¶ó ½Ã°£ ÀÇÁ¸ÀûÀÎ Á¡¼Ò¼º °Åµ¿°ú º¯ÇüÀ» ¼Óµµ ÀÇÁ¸ÀûÀÎ ¼±Çà¾Ð¹ÐÇÏÁß Æ¯¼ºÀ» Ç¥ÇöÇÒ ¼ö ÀÖ´Ù. ¼öÄ¡ÇØ¼®±â¹ýÀ» Àû¿ëÇÏ¿© Berthierville°¢ Olga Áö¿ªÀÇ ¼ºÅä°úÁ¤À» ÇØ¼®ÇÏ¿´À¸¸ç, ¼öÄ¡ÇØ¼® °á°ú¿Í °èÃøµÈ °ªÀ» ºñ±³ÇÑ °á°ú Á¦¾ÈµÈ ºñ¼±Çü Á¡¼Ò¼º¸ðµ¨ºº »ç¿ëÇÏ¿© ¼ºÅä°¡ ³¡³ Á÷ÈÄ °£±Ø¼ö¾ÐÀÇ Áõ°¡Çö»óÀ» ¼³¸íÇÒ ¼ö ÀÖ´Ù. |
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| Increases in excess pore water pressure without change of surcharge load were reported in clay underneath embankment at Berthierville and Olga sites after the end of construction. These abnormal phenomena could not be explained by classical consolidation theory. This paper presents a nonlinear viscoplastic model to interpret an increase in pore water pressure on natural clay, The proposed model can consider the combined processes of pore water pressure dissipation according to Darcy's law and pore water pressure generation due to viscoplastic strain, as well as time-dependent viscoplastic behaviour and strain rate dependency of preconsolidation pressure. The calculated results using numerical analysis are compared with measured ones under embankments built on soft clay at Berthierville and Olga in Quebec, Canada. It may be possible to explain the phenomenon of excess pore water pressure increase after the end of construction using the proposed nonlinear viscoplastic model. |
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| Embankment;Excess pore water pressure;Viscoplastic behavior; |
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Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.18, no.3, 2002³â, pp.105-112
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200211921035395)
¾ð¾î : ¿µ¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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