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Çѱ¹Áö¹Ý°øÇÐȸ / v.20, no.7, 2004³â, pp.141-158
»çÀüÅõ¼ö ¹× º¥Å䳪ÀÌÆ® ǰÁú¿¡ µû¸¥ GCLÀÇ Åõ¼öÁ¾°á±âÁØ¿¡ ¹ÌÄ¡´Â ¿µÇâÆò°¡
( Dependency of Compatibility Termination Criteria on Prehydration and Bentonite Quality for Geosynthetic Clay Liners )
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¸Å¸³Áö³ª ¿À${cdot}$Æó¼ö ÀúÀåÁö µî¿¡¼­ Æó±â¹° ¶Ç´Â ¿À¿°¹°ÁúÀÇ ÀúÀå ¹× Â÷´Ü¿¡ ³Î¸® »ç¿ëµÇ°í ÀÖ´Â Geosynthetic Clay Liner(GCL)ÀÇ ¹°¿¡ ÀÇÇÑ »çÀüÅõ¼ö ¹× º¥Å䳪ÀÌÆ® ǰÁúÀÌ Åõ¼öÁ¾°á±âÁØ¿¡ ¹ÌÄ¡´Â ¿µÇâÀ» Æò°¡Çϱâ À§Çؼ­ ¼Òµð¿ò º¥Å䳪ÀÌÆ®°¡ ÁÖ¼ººÐÀÎ µÎ Á¾·ùÀÇ GCLÀ» ´ë»óÀ¸·Î Áõ·ù¼ö¿Í ³óµµº¯È­¸¦ À§ÇØ 5, 10, 20, 50, 100 mM ¿ë¾×À» È¥ÇÕÇÑ ¿°È­Ä®½·¿ë¾×À» ÀÌ¿ëÇÏ¿© Åõ¼ö½ÃÇèÀ» ¼öÇàÇÏ¿´´Ù. Åõ¼öÁ¾°á±âÁصé·Î´Â ¹°¸®Àû Á¾°á±âÁصé(Áï, ASTM¿¡ ÁØÇÑ À¯Ãâ·®°ú À¯ÀÔ·®°£ÀÇ ºñÀ²°ú ¾ÈÁ¤È­µÈ Åõ¼ö°è¼ö, ÃÖ¼Ò °ø±Ø·® µÎ¹è¿¡ ÇØ´çÇÏ´Â À¯Ãâ, ±×¸®°í ¾ÈÁ¤È­µÈ ½Ã·áµÎ²²)°ú À¯ÀÔ¼ö¿Í À¯Ãâ¼ö°£ÀÇ È­ÇÐÀû ÆòÇü¿¡ µû¸¥ È­ÇÐÀû Á¾°á±âÁصé(Áï, Àü±âÀüµµµµ, pH, ±×¸®°í Ä®½·À̿°ú ¿°¼ÒÀ̿ ³óµµ)ÀÌ °í·ÁµÇ¾ú´Ù. ¿°È­Ä®½·À» ÀÌ¿ëÇÑ Åõ¼ö½ÃÇèÀÇ °æ¿ì, º¥Å䳪ÀÌÆ®¿¡ À̿°áÇÕµÈ ³ªÆ®·ý($Na^+$)¿¡ ´ëÇÑ Ä®½·($Ca^{2+}$) ġȯÀÌ GCLÀÇ Åõ¼ö°è¼ö¿¡ Áß´ëÇÑ ¿µÇâÀ» ¹ÌÄ¡´Â °Í¿¡ ±Ù°ÅÇÏ¿© À¯ÀÔ¼ö¿Í À¯Ãâ¼ö °£ÀÇ È­ÇÐÀû ÆòÇü ¹× Åõ¼ö°è¼öÀÇ ÆòÇüÀÌ ÀÌ·ç¾îÁú ¶§±îÁö ½Ç½ÃÇÏ¿´´Ù. ¿°È­Ä®½·³óµµ¿¡ µû¸¥ Åõ¼ö½ÇÇè°á°ú, ¼Ò¿äÅõ¼ö±â°£Àº ³óµµº°·Î 1ÀÏ ¹Ì¸¸¿¡¼­ 900ÀÏ ÀÌ»óÀ¸·Î Å« Â÷À̸¦ º¸¿´À¸¸ç ¿°È­Ä®½· ¿ë¾×ÀÇ ³óµµ°¡ ³·À»¼ö·Ï ÆòÇü¿¡ µµ´ÞÇϱâ±îÁö ´õ ¸¹Àº ½Ã°£ÀÌ ¼Ò¿äµÇ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ƯÈ÷, ¿°È­Ä®½· ¿ë¾×ÀÇ ³óµµ°¡ 20 mMÀÌÇÏÀÇ °æ¿ì, GCLÀÇ ¹°¿¡ ÀÇÇÑ »çÀüÅõ¼ö ¿©ºÎ¿Í º¥Å䳪ÀÌÆ®ÀÇ Ç°Áú¿¡ »ó°ü¾øÀÌ À¯ÀÔ¼ö¿Í À¯Ãâ¼ö°£ÀÇ È­ÇÐÀû ÆòÇü¸¸ÀÌ Åõ¼ö°è¼öÀÇ ÆòÇüÀ» º¸ÀåÇÒ ¼ö ÀÖ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ±×·¯³ª, ¿°È­Ä®½· ¿ë¾×ÀÇ ³óµµ°¡ 50 ±×¸®°í 100 mMÀÇ °æ¿ì, À¯Ãâ·®°ú À¯ÀÔ·®°£ÀÇ ºñÀ²°ú °ø±Ø·® µÎ¹è¿¡ ÇØ´çÇÏ´Â À¯ÃâÀ» Á¦¿ÜÇÑ ¸ðµç Á¾°á±âÁصéÀÌ Åõ¼ö°è¼öÀÇ ÆòÇüÀ» º¸ÀåÇÒ ¼ö ÀÖ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ÀÌ»óÀÇ °á°ú·ÎºÎÅÍ, ¹°¿¡ ÀÇÇÑ »çÀüÅõ¼ö ¿©ºÎ¿Í º¥Å䳪ÀÌÆ®ÀÇ Ç°Áú¿¡ »ó°ü¾øÀÌ ¿À·ÎÁö À¯ÀÔ¼ö¿Í À¯Ãâ¼ö°£ÀÇ ³óµµ ÆòÇü¿¡ ÁØÇÑ Á¾°á±âÁظ¸ÀÌ GCLÀÇ Åõ¼ö½ÃÇè¿¡ ÀûÇÕÇÒ °ÍÀ¸·Î ÆÇ´ÜµÈ´Ù.
The dependency of criteria used to terminate compatibility tests on the prehydration and quality of bentonite in geosynthetic clay liners (GCLs) is evaluated based on permeation with chemical solutions containing 5, 10, 20, 50, and 100 mM calcium chloride ($CaCl_2$). The hydraulic conductivity tests are not terminated before chemical equilibrium between the effluent and the influent chemistry has been established, resulting in test durations ranging from < 1 day to > 900 days, with longer test durations associated with lower $CaCl_2$ concentrations. The evaluation includes both physical termination criteria (i.e., volumetric flow ratio and steady hydraulic conductivity based on ASTM D 5084, ${ge}2$ pore volumes of flow, constant thickness of specimen) and chemical termination criteria requiring equilibrium between influent and effluent chemistry (viz., electrical conductivity, pH, and $Ca^{2+};and;Cl^-$ concentrations). For specimens permeated with 5, 10, and 20 mM $CaCl_2$ solutions, only the criterion based on chemical equilibrium in $Ca^{2+}$ concentration correlates well with equilibrium in hydraulic conductivity, regardless of prehydration or quality of bentonite. However, all of the termination criteria, except for the volumetric flow ratio and 2 pore volumes of flow for the prehydrated specimens, correlate well with equilibrium in hydraulic conductivity regardless of prehydration or quality of bentonite when permeated with 50 and 100 mM $CaCl_2$ solutions. The results illustrate the uniqueness of the termination criterion based on solute concentration equilibrium between the effluent and the influent with respect to both prehydration and quality of bentonite in the GCLs.
 
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Bentonite quality;Chemical equilibrium;Geosynthetic clay liners;Hydraulic conductivity;Prehydration;Termination criteria;
 
Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.20, no.7, 2004³â, pp.141-158
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200425720311210)
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