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Çѱ¹Áö¹Ý°øÇÐȸ / v.21, no.6, 2005³â, pp.101-115
±¹³» ³»·úÀÇ ¼³°è Áö¹Ý ¿îµ¿ °áÁ¤À» À§ÇÑ Áö¹Ý ÁõÆø °è¼ö ¹× Áö¹Ý ºÐ·ù ü°è Á¦¾È
( A Proposition of Site Coefficients and Site Classification System for Design Ground Motions at Inland of the Korean Peninsula )
¼±Ã¢±¹;Á¤Ãæ±â;±èµ¿¼ö; Çѱ¹µµ·Î°ø»ç µµ·Î±³Åë±â¼ú¿ø;¼­¿ï´ëÇб³ Áö±¸È¯°æ½Ã½ºÅÛ°øÇкÎ;Çѱ¹°úÇбâ¼ú¿ø °Ç¼³¹×ȯ°æ°øÇаú;
 
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±¹³» ³»·úÀÇ ÁöÇü ¹× ÁöÁú Ư¼ºÀ» ´ëÇ¥ÇÏ´Â µÎ Áö¿ªÀÎ °æÁÖ¿Í È«¼ºÀ» ´ë»óÀ¸·Î Àü´ÜÆÄ ¼Óµµ$(V_s)$ ȹµæ ¸ñÀûÀÇ ÇöÀå ź¼ºÆÄ ½ÃÇèÀ» Æ÷ÇÔÇÑ ´Ù¾çÇÑ Áö¹Ý Á¶»ç¸¦ ½Ç½ÃÇÏ¿© Áö¹Ý Ư¼ºÀ» Æò°¡Çϰí, À̸¦ Åä´ë·Î µî°¡ ¼±Çü ¹× ºñ¼±Çü ±â¹ýÀÇ ºÎÁö ÀÀ´ä ÇØ¼®À» ¼öÇàÇÏ¿´´Ù. ÇöÇà ±¹³» ³»Áø ¼³°èÀÇ ±Ù°£ÀÎ ¹Ì±¹ ¼­ºÎ Áö¿ª°úÀÇ Áö¹Ý Ư¼º ºñ±³ °á¿Ô ±¹³» ³»·ú Áö¿ªÀÇ ±â¹Ý¾Ï ½Éµµ´Â ¸Å¿ì ¾è°í °­¼ºÀº ´Ù¼Ò ÄÇ´Ù. Áö¹Ý ºÐ·ù ±âÁØÀÎ ½Éµµ 30m±îÁöÀÇ Æò±Õ Àü´ÜÆÄ ¼Óµµ$V_s30$´Â ´ë»ó Áö¿ª ³»¿¡¼­ $250sim650m/s$ÀÇ Á¼Àº ¹üÀ§ÀÇ ºÐÆ÷¸¦ º¸¿´°í, ±×¿¡ µû¶ó ´ëºÎºÐÀÇ ºÎÁö°¡ C¿Í D Áö¹Ý Á¶°ÇÀ¸·Î ºÐ·ùµÇ¾ú´Ù. ºÎÁö ÀÀ´ä ÇØ¼® °á°ú·ÎºÎÅÍ ÇöÇà ±¹³» ³»Áø ¼³°è¸¦ À§ÇÑ ´ÜÁÖ±â ÁõÆø °è¼ö$(F_¤±)$´Â Áö¹Ý ¿îµ¿À» °ú¼ÒÆò°¡Çϰí ÁßÀåÁÖ±â ÁõÆø°è¼ö$(F_v)$´Â °ú´ëÆò°¡Çϰí ÀÖÀ½À» È®ÀÎÇÏ¿´´Ù. ÀÌ¿¡ µû¶ó ±¹³» ³»·ú Áö¿ª¿¡ ´ëÇÑ Áö¹Ý ÁõÆø °è¼ö¸¦ Àç»êÁ¤Çϰí, Áö¿ªÀû Áö¹Ý Ư¼ºÀ» °í·ÁÇÏ¿© ±âÁ¸ Áö¹Ý ºÐ·ù C ¹× DÀÇ ¼¼ºÎ ºÐ·ù¿Í ÁöÇ¥¸é ºÎ±Ù ½Éµµ±îÁöÀÇ Æò±Õ $V_s$ÀÎ $V_s20,;V_s15,$ ¿Í $V_s10$ÀÇ Ãß°¡ ºÐ·ù ±âÁØÀÌ Àû¿ëµÈ ÇÕ¸®Àû Áö¹Ý ºÐ·ù ü°è¸¦ Á¦¾ÈÇÏ¿´´Ù. Á¦¾ÈµÈ Áö¹Ý ºÐ·ù ü°è´Â ÇöÀç·Î¼­´Â ¿¹ºñÀûÀÎ ¹æ¾ÈÀ̹ǷΠÇâÈÄ º¸¿Ï ¹× °³¼±ÀÌ ÇÊ¿äÇÒ °ÍÀ¸·Î ÆÇ´ÜµÈ´Ù.
For the site characterization at two inland areas, Gyeongju and Hongsung, which represent geomorphic and geologic characteristics of inland region in Korea, in-situ seismic tests containing borehole drilling investigations and resonant column tests were peformed and site-specific seismic response analyses were conducted using equivalent linear as well as nonlinear scheme. The soil deposits in Korea were shallower and stiffer than those in western US, from which the site coefficients and site classification system in Korea were derived. Most sites were categorized as site classes C and D based on the mean shear wave velocity $(V_s)$ of the upper 30 m $(V_s30)$, ranging between 250 and 650 m/s. According to the acceleration response spectra determined from the site response analyses, the site coefficients specified in the current Korean seismic design guide underestimate the ground motion in the short-period band and overestimate the ground motion in mid-period band. These differences can be explained by the differences in the bedrock depth and the soil stiffness profile between Korea and western US. The site coefficients, $F_a$ for short-period and $F_v$ for mid-period, were re-evaluated and the site classification system, in which sites C and D were subdivided according to $V_s20,;V_s15,;and;V_s10$ together with the existing $V_s30$ was introduced accounting for the local geologic conditions at inland region of the Korean peninsula. The proposed site classification system in this paper is still rudimentary and requires modification.
 
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Bedrock depth;Seismic design;Shear wave velocity;Site class;Asite coefficient;Site response analysis;
 
Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.21, no.6, 2005³â, pp.101-115
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200504840676379)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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