|
|
|
Çѱ¹¼öÀÚ¿øÇÐȸ / v.18, no.3, 1985³â, pp.235-241
|
¿ì¸®³ª¶ó ¼ÇؾÈÀÇ Á¶¼®»çÁÖ
( Tidal Sand Banks in the West Coast of Korea ) |
| ÃÖº´È£; ¼º±Õ°ü´ëÇÐ °ø°ú´ëÇÐ Åä¸ñ°ú;
|
|
|
 |
|
| |
| ÃÊ ·Ï |
| Çѱ¹¼ÇØ¾È Á¶¼®°£Á¶µéÀÇ Åä»çÀ̵¿¹æÇâÀ» Kenyon µî(1981)ÀÌ Á¦½ÃÇÑ ¹æ¹ý¿¡ ÀÇÇØ ÃßÁ¤ÇÏ¿´´Ù. ÀÌ ÃßÁ¤°á°ú¿Í µ¿Áö³ªÇØ Á¶¼®¼öÄ¡ ¸ðµ¨¿¡ ÀÇÇÑ M2¿Í M4 ºÐÁ¶ÀÇ ÃÖ´ëÇØ¾È¸¶ÂûÀÀ·Âº¤ÅͰ¡ Á¦½ÃÇÑ ÀüȸÀÇ ÃßÁ¤(ÃÖ, 1983)°ú ºñ±³ÇÑ °á°ú´Â ÁÁÀº ÀÏÄ¡¸¦ º¸¿´´Ù. Áö¿ªÀû Åä»çÀ̵¿ÀÌ ±Ù·¡ ÁØ#µÈ ¼ö·Î¹æÇâÀ¸·Î ÃßÁ¤µÇ´Â Áß¾Ó#ÅðÀÇ Ã¶ÀúÇÑ Á¶»ç°¡ ÃßÈÄÀÇ ¿¬±¸·Î¼ Á¦½ÃµÇ¾ú´Â ¹Ù º» ¿¬±¸´Â È²ÇØÀÇ ÅðÀûµ¿¿ªÇÐÀ» ±Ô¸íÇÏ·Á´Â ÀÏ·ÃÀÇ ¿¬±¸ÀÇ ÃʱâÀÛ¾÷À¸·Î ¼öÇàµÇ¾ú´Ù. |
|
| The predictions of the local and regional sand transport of the offshore tidal sand banks tn the west coast of Korea, east of the Yellow San have been performed on the basis of diagrammatical method suggested by Kenyon et al(1981). There is general agreements between these predictions and the earlier predictions(Choi, 1983) of net regional sand transport paths from the numerical simulation of maximum bottom stress vector during the semidiurnal period due to m2 and m4 tides. Further detailed investigations are proposed for the study of Choongang Chontoe where the predicted net sand transport direction is to the dredged navigation channel. |
| |
| Ű¿öµå |
|
| |
|
|
 |
|
Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.18, no.3, 1985³â, pp.235-241
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198511920091341)
¾ð¾î : Çѱ¹¾î |
|
| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
|
|
|
|
|
|