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Çѱ¹Áö¹Ý°øÇÐȸ / v.24, no.10, 2008³â, pp.161-174
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ºÎÀ¯Çü PS(SPS) ¼Óµµ°ËÃþÀ» ÅëÇÑ Àü´ÜÆÄ Ư¼º °íÂû
( Investigation of S-wave Velocity Based on SPS Field Tests ) |
| Á¤³²ÈÆ;ÀÌÁ¾±Ô; (ÁÖ)Áö¿øÁö¿ÀÅØ¿£Áö´Ï¾î¸µ;´Ü±¹´ëÇб³ Åä¸ñȯ°æ°øÇаú;
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| ±¹³» Á¡¼ºÅä Áö¹Ý ¹× dzÈÅä Áö¹ÝÀÇ Àü´ÜÆÄ¼Óµµ Ư¼ºÀ» ÆÄ¾ÇÇϱâ À§ÇÏ¿© Ç¥ÁذüÀÔ½ÃÇè(SPT), ºÎÀ¯Çü PS ¼Óµµ°ËÃþ(SPS) ¹× ´Ù¿îȦ µîÀÇ ½ÃÇèÀ» ¼öÇàÇÏ¿´À¸¸ç, SPT¿Í SPS ¼Óµµ°ËÃþ °á°ú·ÎºÎÅÍ ÁöÃþº° Àü´ÜÆÄ ¼Óµµ¸¦ ºÐ¼®ÇÏ¿´´Ù. º» ¿¬±¸´ë»ó Áö¿ª¿¡¼ ÃøÁ¤µÈ Àü´ÜÆÄ ¼Óµµ¸¦ Á¡¼ºÅä¿Í dzÈÅä·Î ³ª´©¾î ºÐ¼®ÇÏ¿© Áö¹Ý°µµ¿Í Àü´ÜÆÄ¼Óµµ¿ÍÀÇ »ó°ü°ü°è·ÎºÎÅÍ °æÇè½ÄÀ» Á¦¾ÈÇÒ ¼ö ÀÖ¾ú´Âµ¥, Á¡¼ºÅä¿¡¼´Â ¿©·¯ ÇÐÀڵ鿡 ÀÇÇÏ¿© ±âÁ¸¿¡ Á¦¾ÈµÈ °æÇè½Ä°ú À¯»çÇÑ °á°ú¸¦ ³ªÅ¸³»¾úÀ¸³ª dzÈÅä¿¡¼´Â ±âÁ¸ °æÇè½Ä¿¡ ÀÇÇÑ °ª°ú ¿¬±¸´ë»ó Áö¿ª¿¡¼ ÃøÁ¤ÇÑ ½ÇÃø°ª°ú´Â ´Ù¼Ò Â÷À̰¡ ÀÖÀ½À» È®ÀÎÇÏ¿´´Ù. ¾Æ¿ï·¯ ¿¬±¸ ´ë»óÁö¿ª¿¡ ´ëÇÑ Àü´ÜÆÄ ¼ÓµµÀÇ ±íÀÌ¿¡ µû¸¥ ¿µÇâÀ» Á¦½ÃÇÏ¿´°í ÀÌ °á°ú¸¦ Ohta µî(1978)ÀÇ °æÇè½Ä°ú ºñ±³, °ËÅäÇÏ¿´´Ù. |
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| To investigate the characteristics of the shear wave velocity of cohesive soils and residual soils in Korea, Standard Penetration Test (SPT), Suspension PS Logging tests (SPS) and other soil tests were performed to analyze the shear wave velocity at each layer For these purposes, 2 study sites are selected: one is cohesive soils and the other is residual soils. As a results, new empirical formulas are proposed from the relationship between strength of the ground (N value) and shear wave velocity from the test data at each layer. In the case of cohesive soils, the proposed relationships are nearly similar to empirical formulas, however, in the case of residual soils there was a little difference between the empirical formulas and measured velocities in this study. Case examples for shear wave velocites are presented with depth, N-values and compared with Ohta et al. (1978) empirical formula. |
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| Ű¿öµå |
| N-value;S-wave velocity;Suspension PS logging test; |
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Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.24, no.10, 2008³â, pp.161-174
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200800557077768)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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