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Çѱ¹Áö¹Ý°øÇÐȸ / v.22, no.11, 2006³â, pp.47-54
ÀÀ·ÂÀ¯µµ ¹× °íÀ¯ À̹漺¿¡ µû¸¥ Àü´ÜÆÄ ¼Óµµ Ư¼º
( Characteristics of Shear Wave Velocity as Stress-induced and Inherent Anisotropies )
ÀÌâȣ;À±Çü±¸;ÂäÈ˲á;Á¶ÅÂÇö;ÀÌÁ¾¼·; °í·Á´ëÇб³ »çȸȯ°æ½Ã½ºÅÛ°øÇаú;°í·Á´ëÇб³ »çȸȯ°æ½Ã½ºÅÛ°øÇаú;°í·Á´ëÇб³ »çȸȯ°æ½Ã½ºÅÛ°øÇаú;°í·Á´ëÇб³ »çȸȯ°æ½Ã½ºÅÛ°øÇаú;°í·Á´ëÇб³ »çȸȯ°æ½Ã½ºÅÛ°øÇаú;
 
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ºñ°í°áÈ­µÈ ÈëÀÇ Àü´ÜÆÄ ¼Óµµ´Â ¸ð¼¼°ü Çö»óÀ» ¹«½ÃÇÒ ¼ö ÀÖ´Â °æ¿ì À¯È¿ÀÀ·ÂÀÇ ÇÔ¼ö·Î Ç¥ÇöÇÒ ¼ö ÀÖ´Ù. ±×·¯³ª Áö¹Ý¿¡¼­ÀÇ ÀÀ·Â»óÅ´ µî¹æ¼ºÀÎ °æ¿ìº¸´Ù´Â À̹漺ÀÎ °æ¿ì°¡ ´ëºÎºÐÀ̹ǷΠÀÌ·¯ÇÑ À¯È¿ÀÀ·ÂÀº ÆÄ°¡ ÀüÆÄµÇ´Â ¹æÇâ°ú ÀÔÀÚ°¡ ¿òÁ÷ÀÌ´Â ¹æÇâÀÇ µÎ °¡Áö·Î ³ª´²Áø´Ù. ¶ÇÇÑ, Àü´ÜÆÄ ¼Óµµ´Â ÀÔÀÚ Æ¯¼º¿¡ µû¶ó ½ÇÇèÀûÀ¸·Î °áÁ¤µÇ´Â ${alpha}$°è¼ö¿Í ${eta}$Áö¼ö¿¡ ¿µÇâÀ» ¹Þ´Âµ¥ ${eta}$Áö¼öÀÇ °æ¿ì ÀÔ»ó ¸ÅÁú(particulate material)ÀÇ Á¢ÃË Æ¯¼º(ÀÔÀÚÅ©±â, ÀÔÀÚ¸ð¾ç, ÀÔÀÚµéÀÇ ±¸Á¶)¿¡ µû¶ó °áÁ¤µÇ¸ç, ${alpha}$°è¼ö´Â ÆÐÅ·(packing)ÀÇ ÇüÅÂ(Áï, °£±Ø·ü°ú coordination number), ÀÔÀÚ¸¦ ¸¸µå´Â Àç·áÀÇ Æ¯¼º, ÀÔÀÚ°£ÀÇ Á¢ÃË °Åµ¿, ±¸Á¶ÀÇ º¯È­¿¡ µû¶ó¼­ º¯È­ÇÑ´Ù. º» ¿¬±¸¿¡¼­´Â ÀÔÀÚ±¸Á¶ÀÇ Æ¯¼ºÀÌ ´Ù¸¥ Á¡Åä, ¸ð·¡, micaµîÀÇ Àç·á·Î ¾Ð¹Ð½ÃÇèÀ» ½Ç½ÃÇÏ°í º¥´õ ¿¤¸®¸ÕÆ®¸¦ ÅëÇÏ¿© À¯È¿ÀÀ·Â ¹æÇâ°ú ÀÔÀÚ À̹漺¿¡ µû¸¥ Àü´ÜÆÄ ¼Óµµ¸¦ ÃøÁ¤ÇÏ¿´´Ù. ¿¬±¸ °á°ú, µÕ±Ù ÀÔÀڷνá ÀÔÀÚÀÚü°¡ µî¹æ¼ºÀÎ °æ¿ì¿¡´Â ÀÀ·ÂÀ̹漺¿¡ ÀÇÇÏ¿© Àü´ÜÆÄ ¼ÓµµÀÇ Å©±â°¡ ´Þ¶óÁö´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ¶ÇÇÑ Àü´ÜÆÄ ¼Óµµ´Â µ¿ÀÏÇÑ ÀÀ·Â ÇÏ¿¡¼­ ÀÔÀÚ ¹è¿­¿¡ ÀÇÁ¸ÇÏ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. À̹ø ¿¬±¸´Â Áö¹Ý±¸Á¶¹°ÀÇ ¼³°è¿Í ½Ã°ø ½Ã Àü´ÜÆÄ ¼Óµµ¿Í Àü´Üź¼º°è¼ö´Â ¸Å¿ì ½ÅÁßÇÏ°Ô °è»êµÇ°í »ç¿ëµÇ¾îÁ®¾ß ÇÔÀ» Á¦½ÃÇϰí ÀÖ´Ù.
Shear wave velocity of uncemented soil can be expressed as the function of effective stresses when capillary phenomena are negligible. However, the terms of effective stresses are divided into the direction of wave propagation and polarization because stress states are generally anisotropy. The shear wave velocities are affected by ${alpha}$ parameters and ${eta}$ exponents that are experimentally determined. The ${eta}$ exponents are controlled by contact effects of particulate materials (sizes, shapes, and structures of particles) and the ${alpha}$ parameters are changed by contact behaviors among particles, material properties of particles, and type of packing (i.e., void ratio and coordination number). In this study, consolidation tests are performed by using clay, mica and sand specimens. Shear wave velocities are measured during consolidation tests to investigate the stress-induced and inherent anisotropies by using bender elements. Results show the shear wave velocity depends on the stress-induced anisotropy for round particles. Furthermore, the shear wave velocity is dependent on particle alignment under the constant evvective stress. This study suggests that the shear wave velocity and the shear modulus should be carefully estimated and used for the design and construction of geotechnical structures.
 
Ű¿öµå
Bender elements;Effective stress;Inherent anisotropy;Shear wave velocity;Stress-induced anisotropy;
 
Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.22, no.11, 2006³â, pp.47-54
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200604623519974)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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