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Çѱ¹Áö¹Ý°øÇÐȸ / v.11, no.1, 1995³â, pp.41-50
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Á¤±Ô¾Ð¹ÐÁ¡¼ºÅäÀÇ À̹漺¿¡ °üÇÑ ¿¬±¸
( Study on Anisotropy of Normally Consolidated Clay Soils ) |
| ±Ç¿À¼ø;Á¤Ãæ±â; Á¤È¸¿ø, ¼¿ï´ëÇб³ Åä¸ñ°øÇаú;Á¤È¸¿ø, ¸íÁö´ëÇб³ Åä¸ñ°øÇаú Á¶±³¼ö, Á¤È¸¿ø, ¼¿ï´ëÇб³ Åä¸ñ°øÇаú Á¶±³¼ö, Á¤È¸¿ø, ¼¿ï´ëÇб³ Åä¸ñ°øÇаú;
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| ÀÚ¿¬»óÅÂÀÇ Á¡¼ºÅä´Â Ko»óÅ·ΠÁ¸ÀçÇϸç ÇÏÁßÀçÇϽà ÁÖ¿õ·Â¹æÇâ¿¡ µû¶ó ´Ù¸£°Ô °Åµ¿ÇÏ´Â À̹æÀû Ư¼ºÀ» °®´Â´Ù. ±×·¯³ª ½ÇÇè½Ç¿¡¼ Á¡¼ºÅäÀÇ °µµÆ¯¼ºÀ» ÆÄ¾ÇÇϱâ À§ÇÏ¿© ½Ç½ÃÇϰí ÀÖ´Â ½ÇÇèÀº ½Ç¿ë¼º°ú °£Æí¼º ¶§¹®¿¡ µî¹æ¾Ð¹Ð »ïÃà½ÃÇèÀÌ º¸ÆíÀûÀ¸·Î »ç¿ëµÇ°í ÀÖ´Ù. ÀÌ ¿¬±¸¿¡¼´Â Á¤±Ô¾Ð¹ÐÁ¡¼ºÅäÀÇ À̹æÀû Ư¼º°ú ¾Ð¹Ð¹æ¹ý¿¡ µû¸¥ Àü´ÜƯ¼ºÀ» °íÂûÇϱâ À§ÇÏ¿© Å䱫ÀÇ ÇüÅ·ΠäÃëÇÑ ºÒ±³¶õ Á¡¼ºÅ並 µî¹æ¾Ð¹Ð ¶Ç´Â Ko¾Ð¹Ð½ÃÄÑ Á¤±Ô¾Ð¹Ð»óÅ¿¡ µµ´ÞÇÏ°Ô ÇÑ ÈÄ ºñ¹è¼ö»ïÃà¾ÐÃà°ú ½ÅÀå½ÃÇèÀ» ½Ç½ÃÇÏ¿´´Ù. ½ÃÇè°á°ú ÁÖÀÀ·Â¹æÇâ¿¡ µû¸¥ °µµÀÇ À̹漺À» ÀÛÀÎÇÏ¿´´Ù. µî¹æ¾Ð ¹ÐÀº ¾Ð¹Ð½Ã ½Ã·á¿¡ °¡ÇØÁö´Â Ko»óź¸´Ù ³ôÀº Æò±ÕÁÖÀÀ·Â°ú ÈëÀÇ À̹æÀû ±¸Á¶ÀÇ ÆÄ±«¶§¹®¿¡ ºñ ¹è¼ö°µµ¸¦ °ú´ëÆò°¡Çϸç À̹漺ÀÌ °¨¼ÒÇϰí ÀÀ·Â-º¯Çü·ü°ú ¹ß»ý °úÀ×°£±Ø¼ö¾ÐÀÌ ¿µÇâÀ» ¹ÞÀ½À» ¾Ë ¼ö ÀÖ¾úÀ¸¸ç, °ú¾Ð¹ÐÁ¡¼ºÅäÀÇ °æ¿ì °ú¾Ð¹Ðºñ¸¦ °¨¼Ò½ÃŲ´Ù. ¶ÇÇÑ ³»ºÎ¸¶Âû°¢Àº ½ÅÀå½ÃÇèÀÌ ¾ÐÃà½ÃÇ躸´Ù Å« °ªÀ» ³ªÅ¸³»Áö¸¸ ÆÄ±«½ÃÀÇ ÀÀ·Â»óŸ¦ ÀÌ¿ëÇÏ¿© ȸ±ÍºÐ¼®ÇÑ °á°ú¿¡ µû¸£¸é ½ÅÀå½Ã Á¡Âø·Â°ú ÇÔ²² ³ªÅ¸³ª´Â ³»ºÎ¸¶Âû°¢Àº ¾ÐÃà½ÃÇè°ú °ÅÀÇ °°Àº °ªÀ» °¡ÁüÀ» ¾Ë ¼ö ÀÖ¾ú´Ù. |
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| In situ clay soils with Ko condition have anisotropic characteristics, varying the response according to the principal stress direction upon loading. But because of their practicality and simplicity, consolidated isotropic undrained compression tests are commonly used in practice to determine the behavior of cohesive soils. In this study to investigate the anisotropic characteristics and the effects of consolidation stress states on the response of normally consolidated clay soils during shearing, triaxial compression and extension tests after consolidating the undisturbed clay soil samples, which are obtained as a block sample to normalized consolidation states under isotropic or Ko state, were carried out. As a result of tests, the anisotropy of the undrained strength was confirmed. Comparing the soil responses between isotropic and Ko consolidation, the undrained strength by isotropic consolidation is overestimated because of its higher mean consolidation pressure. And isotropic consolidation reduces the anisotropy of soil response and influences on the stress-strain behavior and pore pressure response because the animotropic soil structure is partially collapsed during isotropic consolidation process. Also, OCR in overconsolidated soils is decreased by isotropic consolidatiorL Friction angle in eztension is higher than that in compression, but regression analysis shows that friction angle with cohesion in extension is almost the same as that without cohesion in compresslon. |
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Çѱ¹Áö¹Ý°øÇÐȸÁö:Áö¹Ý / v.11, no.1, 1995³â, pp.41-50
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-215X
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199511920445842)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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