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Çѱ¹Áö¹Ý°øÇÐȸ / v.19, no.6, 2003³â, pp.207-216
ÇöÀå½ÃÇè¿¡ ÀÇÇÑ Smear ZoneÀÇ Æò°¡
( A Study on the Evaluation of Smear Zone by In-situ Tests )
ÀÌÀå´ö;±¸ÀÚ°©; µÎ¿ì°Ç¼³¿£Áö´Ï¾î¸µ;±¹¸³ ÇѰæ´ëÇб³ Åä¸ñ°øÇаú;
 
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º» ³í¹®¿¡¼­´Â ±¹³» ¼­ÇØ¾È ¿¬¾à Áö¹Ý ÇöÀå¿¡¼­ PBD Ÿ¼³·Î ÀÎÇÑ ±³¶õ ¿µ¿ªÀ» È®ÀÎÇϱâ À§ÇÏ¿© ÇöÀåÁö¹Ý¿¡ 10°³ÀÇ °£±Ø¼ö¾Ð°è¸¦ PBD Ÿ¼³ À§Ä¡·ÎºÎÅÍ 10cm, 20cm, 30cm, 40cm ±×¸®°í 50cm ±×¸®°í 50cm ¶³¾îÁ® ¼³Ä¡ÇÏ°í ¸àµå·¼À» ÀÌ¿ëÇÑ PBD °­Á¦ °üÀԽà ¹ß»ýÇÏ´Â °úÀ×°£±Ø¼ö¾ÐÀÇ ¼Ò»ê°úÁ¤À» 5m, 7m ±íÀÌ¿¡¼­ ÃøÁ¤ÇÏ¿´´Ù. PBD Ÿ¼³·Î ÀÎÇØ Áö¹Ý±³¶õÀÌ ¹ß»ýÇÏ¸é ¿¬¾àÁ¡Åä Áö¹ÝÀÇ Åõ¼ö°è¼ö°¡ °¨¼ÒÇÏ°Ô µÇ¾î °úÀ×°£±Ø¼ö¾ÐÀÇ ¼Ò»ê½Ã°£¿¡ ¿µÇâÀ» ¹ÌÄ¡°Ô µÇ¹Ç·Î PBD Ÿ¼³°Å¸®·ÎºÎÅÍ PBD Ÿ¼³ ÀüÈÄÀÇ °úÀ×°£±Ø¼ö¾Ð ¼Ò»ê°úÁ¤À» ÃøÁ¤ÇÏ¿© Smear ZoneÀÇ ¹üÀ§¸¦ Á¤ÇÏ¿´´Ù. ¶ÇÇÑ ÀÌ·¯ÇÑ °úÀ×°£±Ø¼ö¾Ð ¼Ò»ê°úÁ¤À» ÇØ¼®ÇÏ¿© PBDŸ¼³ ÀüÈÄÀÇ Áö¹Ý ¹è¼öƯ¼ºÀúÇϸ¦ ±Ô¸íÇÏ¿´´Ù. °úÀ×°£±Ø¼ö¾Ð ¼Ò»êÀ» ÇØ¼®Çϱâ À§ÇÏ¿© ½ÃÇè Áö¹ÝÀÇ °­¼ºÁö¼ö°¡ ÇÊ¿äÇѵ¥ ÀÌ·¯ÇÑ °­¼ºÁö¼ö ÃøÁ¤À» À§ÇÏ¿© Cone-Pressuremeter(CPM)½ÃÇèÀ» º´ÇàÇÏ¿´´Ù. ½ÃÇè°á°ú ¸àµå·¼ÀÇ È¯»êÁ÷°æÀÇ 3.0-3.6¹è¿¡ Smear ZoneÀÌ Çü¼ºµÇ´Â °ÍÀ¸·Î Á¶»çµÇ¾úÀ¸¸ç Teh & HoulsbyÀÇ ½Ä°ú CPMÀ» ÀÌ¿ëÇÑ ¼öÆò¾Ð¹Ð°è¼ö¸¦ Æò°¡ÇÑ °á°ú PBDŸ¼³ÀüÈÄ·Î Áö¹ÝÀÇ ¹è¼ö´É·ÂÀÌ 3-8¹è ÀúÇÏµÈ °ÍÀ¸·Î °è»êµÇ¾ú´Ù.
To evaluate the smear zone caused by the drain installation, 10 piezometers were installed in the typical soft ground in the western coastal area of Korea. The dynamic pore water pressure developed during the drain installation was monitored using piezometers installed at a distance of 10cm, 20cm, 30cm, 40cm and 50cm from the location of the drain. The decay of pore pressure with time after pushing piezometers to depths of 5 meters and 7 meters during the drain installation was monitored to assess flow and consolidation characteristics of the soil after disturbance of the soil due to the drain installation. The drain installation results in shear strain and displacement of the soil and it decreases the permeability of the soil. Hence, the comparison between dissipation of the pore water pressure process in 10 pieszometers before as well as after installation of the drain indicated the diameter of disturbance zone and smear zone, which is related to the cross-sectional dimension of the mandrel. In addition, Cone-pressuremeter(CPM) tests were performed to obtain rigidity index of the soil for an interpretation of the dissipation processes. It has been evaluated by in-situ tests that the smear zone is from 3.0 to 3.6 times of the cross-sectional dimension of the mandrel. The hydraulic conductivity expressed in terms of the coefficient of consolidation after the drain installation was calculated from 3 to 8 times decrease evaluated by Teh & Houlsby equation and CPM test results.
 
Ű¿öµå
CPM;Dissipation test;Hydraulic conductivity;PBD;Smear zone;
 
Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.19, no.6, 2003³â, pp.207-216
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200311922147986)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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