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Çѱ¹Áö¹Ý°øÇÐȸ / v.22, no.10, 2006³â, pp.173-181
¾×»óÈ­ÇØ¼®À» À§ÇÑ µÎ °³ÀÇ È°¼º¸éÀ» °¡Áø ±¸¼º¸ðµ¨
( A Two Mobilized-Plane Model for Soil Liquefaction Analysis )
¹Ú¼º½Ä; °æºÏ´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú;
 
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º» ³í¹®¿¡¼­´Â Á¤Àû ¹× ¾×»óÈ­¿Í °°Àº µ¿ÀûÇÏÁßÀ» ¹Þ´Â ÈëÀÇ °Åµ¿Çؼ®À» À§ÇÑ µÎ °³ÀÇ È°¼º¸éÀ» °¡Áø ±¸¼º¸ðµ¨À» Á¦¾ÈÇÏ¿´´Ù. ÀÌ ¸ðµ¨Àº µÎ °³ÀÇ È°¼º¸é¿¡ ±âÃÊÇϰí ÀÖÀ¸¸ç, ù¹øÂ°¸éÀº ȸÀüÇÏ´Â ÃÖ´ëÀü´Ü¸éÀ» ³ªÅ¸³»¸ç µÎ ¹øÂ°¸éÀº °íÁ¤µÈ ¼öÆò¸éÀ» ³ªÅ¸³½´Ù. ÀÌ¿Í °°Àº µÎ °³ÀÇ È°¼º¸éÀ» ÀÌ¿ëÇÏ¿© º» ¸ðµ¨Àº ÃʱâÀÇ ´Ù¸¥ ÀÀ·Â»óÅÂÇÏ¿¡ ÀÖ´Â ½Ã·áÀÇ Á÷Á¢´Ü¼øÀü´Ü½Ã¿¡ ¹ß»ýÇÏ´Â ÁÖÀÀ·ÂȸÀüÇö»óÀ» ¸ðµ¨¸µÇÒ ¼ö ÀÖ´Ù. Á¦¾ÈµÈ ¸ðµ¨Àº ÃʱâÀÇ ÀÀ·Âºñ¿¡ °ü°è¾øÀÌ Æò±ÕÀ¯È¿ÀÀ·ÂÀÌ µ¿ÀÏÇÒ °æ¿ì¿¡ À¯»çÇÑ °Åµ¿À» º¸ÀÌ´Â ÈëÀÇ ½Ç³»½ÇÇè°á°ú¸¦ ¹¦»çÇÒ ¼ö ÀÖ´Ù ±×¸®°í, ¹è¼ö½Ã ¹Ýº¹ Á÷Á¢´Ü¼øÀü´ÜÀ¸·Î ¹ß»ýÇÏ´Â ÈëÀÇ °Åµ¿ Áï Á¦ÇϽÿ¡ ³ªÅ¸³ª´Â üÀû°¨¼Ò ¹× ´ëº¯Çü¿¡¼­ ¹ß»ýÇϴ üÀûÆØÃ¢À» ¹¦»çÇÒ ¼ö ÀÖ´Ù. ºñ¹è¼ö½ÃÀÇ ÈëÀÇ Á¤Àû ¹× µ¿Àû °Åµ¿Àº ¹è¼ö°Åµ¿¿¡¼­ Èë °ñ°Ý»çÀÌ¿¡ Á¸ÀçÇÏ´Â ¹°ÀÇ ±¸¼Ó·ÂÀ» °í·ÁÇÔÀ¸·Î½á ÇØ¼®ÇÏ¿´´Ù. º» ¸ðµ¨ÀÇ ±¸¼º°ü°è½ÄÀº ÀÀ·Â-¹°ÀÇ »ó°ü°ü°è¸¦ µ¿½Ã¿¡ ¹¦»çÇÒ ¼ö ÀÖ´Â FLACÀ» ÀÌ¿ëÇÏ¿© ±¸ÇöÇÏ¿´´Ù. ¹è¼ö Á÷Á¢´Ü¼øÀü´Ü ½ÃÇèÀ» ÀÌ¿ëÇÑ Fraser River SandÀÇ ½ÇÇè°á°ú¸¦ ÀÌ¿ëÇÏ¿© ¸ðµ¨À» ¸ÕÀú °ËÁõÇÏ¿´À¸¸ç, µ¿ÀÏÇÑ ÀԷº¯¼ö¸¦ ÀÌ¿ëÇÑ Fraser River Sand ºñ¹è¼ö °Åµ¿ÀÇ ¿¹ÃøÄ¡¿Í ½ÇÇèÄ¡¸¦ ºñ±³ÇÏ¿© °ËÁõÇÏ¿´´Ù.
A Two Mobilized-Plane Model is proposed for monotonic and cyclic soil response including liquefaction. This model is based on two mobilized planes: a plane of maximum shear stress, which rotates, and a horizontal plane which is spatially fixed. By controlling two mobilized planes, the model can simulate the principal stress rotation effect associated with simple shear from different $K_0$ states. The proposed model gives a similar skeleton behaviour for soils having the same mean stress, regardless of $K_0$ conditions as observed in laboratory tests. The soil skeleton behaviour observed in cyclic drained simple shear tests, including compaction during unloading and dilation at large strain is captured in the model. Undrained monotonic and cyclic response is predicted by imposing the volumetric constraint of the water on the drained or skeleton behaviour. This constitutive model is incorporated into the dynamic coupled stress-flow finite difference program of FLAC (Fast Lagrangian Analysis of Continua). The model was first calibrated with drained simple shear tests on Fraser River sand, and verified by comparing predicted and measured undrained behaviour of Fraser River sand using the same input parameters.
 
Ű¿öµå
Principal stress rotation;Simple shear test;Two mobilized planes;
 
Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.22, no.10, 2006³â, pp.173-181
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200604623521536)
¾ð¾î : ¿µ¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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