¶óÆæÆ®¦¢Ä«Æä¦¢ºí·Î±×¦¢´õº¸±â
¾ÆÄ«µ¥¹Ì Ȩ ¸í»çƯ°­ ´ëÇבּ¸½Ç޹æ Á¶°æ½Ç¹« µ¿¿µ»ó°­ÀÇ Çѱ¹ÀÇ ÀüÅëÁ¤¿ø ÇÐȸº° ³í¹®
ÇÐȸº° ³í¹®

Çѱ¹°Ç¼³°ü¸®ÇÐȸ
Çѱ¹°ÇÃà½Ã°øÇÐȸ
Çѱ¹µµ·ÎÇÐȸ
Çѱ¹»ý¹°È¯°æÁ¶ÀýÇÐȸ
Çѱ¹»ýÅÂÇÐȸ
Çѱ¹¼öÀÚ¿øÇÐȸ
Çѱ¹½Ä¹°ÇÐȸ
Çѱ¹½Ç³»µðÀÚÀÎÇÐȸ
Çѱ¹ÀÚ¿ø½Ä¹°ÇÐȸ
Çѱ¹ÀܵðÇÐȸ
Çѱ¹Á¶°æÇÐȸ
Çѱ¹Áö¹Ý°øÇÐȸ
Çѱ¹ÇÏõȣ¼öÇÐȸ
Çѱ¹È¯°æ»ý¹°ÇÐȸ
Çѱ¹È¯°æ»ýÅÂÇÐȸ

Çѱ¹Áö¹Ý°øÇÐȸ / v.25, no.1, 2009³â, pp.65-76
°­¿ìħÅõ½Ã °­¿ì°­µµ¿Í Æ÷È­Åõ¼ö°è¼ö°¡ ¾ÈÀüÀ²¿¡ ¹ÌÄ¡´Â ¿µÇâ
( Influence of Rainfall Intensity and Saturated Permeability on Slope Stability during Rainfall Infiltration )
À̽·¡;¿ÀűÔ;±èÀ±±â;±èÈñö; KAIST °Ç¼³ ¹× ȯ°æ°øÇаú;(ÁÖ)´ë¿ì°Ç¼³ Åä¸ñ»ç¾÷º»ºÎ;KAIST °Ç¼³ ¹× ȯ°æ°øÇаú;(ÁÖ)´ë¿ì°Ç¼³ Åä¸ñ»ç¾÷º»ºÎ;
 
ÃÊ ·Ï
º» ¿¬±¸¿¡¼­´Â ºÒÆ÷È­ Áö¹ÝÀÇ Æ¯¼ºÀ» ÆÄ¾ÇÇϰí, Æ÷È­Åõ¼ö°è¼ö($k_s$)¿Í °­¿ì°­µµ(i) ¹× ÇÔ¼öƯ¼º°î¼±(SWCC)ÀÌ »ç¸éÀÇ ¾ÈÁ¤¼º¿¡ ¾î¶°ÇÑ ¿µÇâÀ» ÁÖ´ÂÁö ¿¬°ü¼ºÀ» ÆÄ¾ÇÇϱâ À§ÇØ ±¹³» Áö¹Ý¿¡ Æø³Ð°Ô ºÐÆ÷Çϰí ÀÖ´Â È­°­Ç³È­Åä¿¡ ´ëÇØ ¿¬±¸¸¦ ¼öÇàÇÏ¿´´Ù. ±âÁ¸ ¿¬±¸ÀÚ·á ¹× ½ÇÇèÀ» ÅëÇØ ¾òÀº Á¤±ÔÈ­ÇÔ¼öƯ¼º°î¼±À» µ¥ÀÌÅͺ£À̽ºÈ­Çϰí Åë°èÀû °³³äÀ» µµÀÔÇÏ¿© »óÇÑ Æò±Õ ÇÏÇÑÀÇ ÇÔ¼öƯ¼º°î¼±À» ÃßÁ¤ÇÏ¿´´Ù. ÀÔµµºÐÆ÷°î¼±°ú »óÇÑ Æò±Õ ÇÏÇÑÀÇ ÇÔ¼öƯ¼º°î¼±°úÀÇ °ü°è¸¦ ¹ÙÅÁÀ¸·Î ÇÔ¼öƯ¼º°î¼± ÀÚ·á°¡ ¾ø´Â Áö¹ÝÀÇ ÇÔ¼öƯ¼º°î¼±À» °³·«ÀûÀ¸·Î ÃßÁ¤ÇÏ´Â ¹æ¹ý ¶ÇÇÑ Á¦¾ÈÇÏ¿´´Ù. ±×¸®°í ÃßÁ¤µÈ »óÇÑ Æò±Õ ÇÏÇÑÀÇ ÇÔ¼öƯ¼º°î¼±À» ÀÌ¿ëÇÏ¿© °­¿ì½Ã »ç¸é ±¸Á¶¹°ÀÇ ½Ã°£ ÀÇÁ¸Àû ¾ÈÀüÀ² º¯È­ ÃßÀ̸¦ ÅëÇØ ½Ç¹«ÀûÀ¸·Î »ç¿ëÇÒ ¼ö ÀÖ´Â Æ÷È­Åõ¼ö°è¼ö¿Í °­¿ì°­µµÀÇ ºñ¸¦ Á¦¾ÈÇÏ¿´´Ù. ¿¬±¸°á°ú¿¡ ÀÇÇÏ¸é °­¿ì ħÅõ¿¡ ÀÇÇÑ ¾ÈÀüÀ² º¯È­´Â °­¿ì°­µµÀÇ Àý´ë Å©±â¿¡ Á¿ìµÇÁö ¾Ê°í °­¿ì°­µµ¿Í Åõ¼ö°è¼öÀÇ ºñ¿¡ ¿µÇâÀ» ¹Þ´Â´Ù. ±×¸®°í »ç¸éÀÇ ¾ÈÀüÀ²Àº °­¿ìħÅõ¿¡ ÀÇÇØ °¨¼ÒÇϱ⠽ÃÀÛÇϸç ÀÓ°è°ª¿¡ µµ´ÞÇÑ ÀÌÈÄ ´Ù½Ã »ó½ÂÇÏ´Â °ÍÀ» ¾Ë ¼ö ÀÖ´Ù. ¼öÄ¡ÇØ¼®°á°ú °¡Àå ³·Àº ¾ÈÀüÀ²À» º¸ÀÌ´Â ¶§´Â »óÇÑÀÇ ÇÔ¼öƯ¼º°î¼±À» ÀÌ¿ëÇÒ °æ¿ì·Î, À̶§ Æ÷È­ Åõ¼ö°è¼ö°ªÀÌ °­¿ì°­µµ¿Í °°°Å³ª µÎ ¹è°¡ µÉ ¶§ÀÌ´Ù.
The unsaturated characteristics of Korean weathered granite soils have been studied to investigate the influence of saturated permeability, rainfall intensity and soil-water characteristic curve (SWCC) on the slope stability. The upper, average and lower SWCCs were estimated from the publication and experimental results using the statistical concept. The roughly estimated SWCC can be used for the soils without experimental results by relating SWCC with the particle size distribution curve. An appropriate ratio between the saturated permeability and the rainfall intensity ($k_s$/i) was also suggested for practical use in designing the slopes by investigating the time-dependent variation of slope instability during the rainfall. The slope stability was deteriorated from the initiation of rainfall and recovered again after the factor of safety reached the critical value. The FS of the slope decreased at first and then increased after reaching the critical value during the rainfall. As a result, the slope instability was not related with an absolute rainfall intensity but with the ratio between the saturated permeability and the rainfall intensity. In case of the upper SWCC, the critical condition occurred when the ratio between the saturated permeability and the rainfall intensity was in the range of $1.0{sim}2.0$.
 
Ű¿öµå
Coefficient of permeability;Rainfall infiltration;SWCC;Slope stability;Unsaturated soils;
 
Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.25, no.1, 2009³â, pp.65-76
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200908349651950)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
¸ñ·Ïº¸±â
ȸ»ç¼Ò°³ ±¤°í¾È³» ÀÌ¿ë¾à°ü °³ÀÎÁ¤º¸Ãë±Þ¹æÄ§ Ã¥ÀÓÀÇ ÇѰè¿Í ¹ýÀû°íÁö À̸ÞÀÏÁÖ¼Ò ¹«´Ü¼öÁý °ÅºÎ °í°´¼¾ÅÍ
   

ÇÏÀ§¹è³ÊÀ̵¿