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Çѱ¹Áö¹Ý°øÇÐȸ / v.16, no.1, 2000³â, pp.99-106
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ÀÏÁ¤º¯Çü·ü ¾Ð¹Ð½ÃÇè¿¡ µû¸¥ À̾ÏdzÈÅäÀÇ ¾Ð¹ÐƯ¼º
( A Consolidation Characteristics of Decomposed Mudstone Soil by Constant Rate of Strain Consolidation ) |
| ±è¿µ¼ö;±è±â¿µ;±è´ë¸¸; °æºÏ´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú;°æºÏ´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú;°æºÏ´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú;
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| ±âÁ¸ÀÇ Oedometer ½ÃÇèÀº °£´ÜÇÑ ½ÃÇèÀåÄ¡ÀÇ Æí¸®ÇÔÀ¸·Î ÀÎÇØ ³Î¸® ÀÌ¿ëµÇ¾î ¿Ô´Ù. ±×·¯³ª ÀÌ ¹æ¹ýÀº Àå½Ã°£ÀÇ ½ÃÇè±â°£, °¢ ´Ü°è ÇÏÁß¿¡¼ÀÇ ºÒ±ÔÄ¢ÀûÀÎ ÀÀ·Â»óÅÂ, ¸Å¿ì ¿¬¾àÇÑ Á¡Åä¿¡ ´ëÇÑ ½ÃÇèÀÇ ¾î·Á¿ò ¹× ½Ã·áÀÇ Æ÷ȹ®Á¦¿Í °°Àº ¿©·¯ ¹®Á¦Á¡À» ³ëÃâÇÏ°Ô µÇ¾ú´Ù. µû¶ó¼ ÀÌ·± ´ÜÁ¡À» º¸¿Ï ÇÒ ¼ö ÀÖ´Â ½ÃÇè ¹æ¹ýÀÇ Çϳª·Î ÀÏÁ¤ º¯Çü·ü ¾Ð¹Ð½ÃÇè ÀÌ °³¹ßµÇ¾î ³Î¸® ÀÌ¿ëµÇ°í ÀÖ´Ù. º» ³í¹®¿¡¼´Â ¼¼°¡Áö º¯Çü·üÀ» ÀÌ¿ëÇÑ CRS½ÃÇèÀ» ½Ç½ÃÇÏ¿´À¸¸ç, ÀÌ °á°ú¸¦ ¼öÁ¤µÈ Wissa(1971)ÀÇ ºñ¼±Çü ÀÌ·ÐÀ» ÀÌ¿ëÇØ ÇØ¼®Çϰí, ±âÁ¸ÀÇ Oedometer½ÃÇè ¹× Á÷Á¢Åõ¼ö½ÃÇè°ú ºñ±³ºÐ¼®ÇÔÀ¸·Î¼ CRS½ÃÇèÀÇ È¿À²¼º ¹× Àû¿ë¼º À¯¹«¸¦ ÆÇ´ÜÇϰíÀÚ ÇÑ´Ù. |
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| The main advantage of incremental loading consolidation test is the simplicity of equipments that can be used. However, it is known that the incremental loading test has several deficiencies including long testing time, non-uniform stress state, high and variable rates of strain, very soft clay and problem of back pressure saturation. Due to these drawbacks, various testing methods including constant rate of strain consolidation test(CRS) were developed. In this paper, CRS consolidation test was performed with three different strain rate. The results were verified by the modified CRS theory of Wissa et al.(1971). And then the results obtained from the CRS consolidation tests were compared with those from incremental loading test and direct permeability test. |
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| Ű¿öµå |
| Decomposed mudstone soil;Constant rate of strain;Oedometer;Rowecell;Non-Linear theory.; |
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Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.16, no.1, 2000³â, pp.99-106
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200011921750073)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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