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Çѱ¹Áö¹Ý°øÇÐȸ / v.14, no.5, 1998³â, pp.77-88
Æ÷Ç× ÇØ¼ºÁ¡ÅäÀÇ ºÐÆ÷¿Í °øÇÐÀû Ư¼º
( Engineering Characteristics and D istribution of Marine Clay in Pohang City )
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º» ³í¹®Àº µ¿ÇؾÈÀÇ ÁöÇü¹ß´Þ ¹× ÇØ¼ö¸é º¯È­¿Í °ü·ÃÇÏ¿© Æ÷Ç×Áö¿ªÀÌ ¿Ë±âµÇ°í ÀÖ´Â Áõ°Å¸¦ Á¦½ÃÇϰí, ÇØ¼ºÁ¡ÅäÀÇ ºÐÆ÷¿Í °øÇÐÀû Ư¼ºÀ» ±Ô¸íÇÑ °ÍÀÌ´Ù. Áö±ÝºÎÅÍ ¾à 10,000³â Àü µ¿ÇؾÈÀÇ ÇØ¼ö¸éÀº ÇöÇØ¼ö¸éº¸´Ù ¾à 25.0m ¾Æ·¡¿¡ Á¸ÀçÇÑ °ÍÀ¸·Î ÃßÁ¤µÇ¸ç, Áö°¢º¯µ¿À¸·Î ÀÎÇÏ¿© Æ÷Ç×½ÃÀÇ ÇØ¼ö¸é ¾Æ·¡¿¡¼­ ÅðÀûµÈ ÇØ¼ºÁ¡ÅäÃþÀº ÁÖ·Î ÇØ¼ö¸é À§¿¡¼­ ¹ß°ßµÈ´Ù. Æ÷Ç׽à µÎÈ£1µ¿ ¹× À强µ¿ÀÇ ÇØ¼ºÁ¡Åä´Â GL-7.8m ÀÌÇÏ¿¡¼­ °ú¾Ð¹Ðºñ°¡ 0.77ÀÌÇÏÀ̸ç 5./P:ºñ°¡ 0.14ÀÌÇÏÀÎ °ÍÀ¸·Î ÆÇ´ÜÇØ º¼ ¶§, ¹Ì¾Ð¹Ð»óÅÂÀÎ °ÍÀ¸·Î ÃßÁ¤µÈ´Ù. ±×·¯³ª ¹Ì¾Ð¹Ð»óŸ¦ È®ÀÎÇϱâ À§Çؼ­´Â º¸´Ù Á¤È®ÇÑ ÃøÁ¤°ú ÇØ¼®ÀÌ ÇÊ¿äÇÏ´Ù.
This study discusses the engineering characteristics and distribution of marine clay in Pohang by providing evidence that Pohang area has been upheaving in connection with the changes of sea level and geographical development in the Babt Coast. It is estimated that the sea level of the East Coast about 10,000 years ago had been 25 meters below than that of the present. The corroborative fact is that the marine clay deposited below the sea level due to the changes of the crust in Pohang is usually found above the sea level. Judging from their OCR values of leas than 0.77 and Bu/po'ratio of less than 0.14 at the depth of 7.8 meters below the ground level, marine clays of Dohu 1-dong and Jangsung-dong in Pohang City are presumed to be in a state of underconsolidation. However, more sophisticated measures and analysis are needed to prove it.
 
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Marine clay;Upheaving;OCR;Underconsolidation;
 
Çѱ¹Áö¹Ý°øÇÐȸÁö:Áö¹Ý / v.14, no.5, 1998³â, pp.77-88
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-215X
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199811920448449)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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