|
|
|
Çѱ¹¼öÀÚ¿øÇÐȸ / v.34, no.6, 2001³â, pp.687-699
|
ħ½Ä·ü ÃøÁ¤ÀڷḦ ÀÌ¿ëÇÑ 2Â÷¿ø ÅðÀû¹° ¼ö¼Û¸ðÇüÀÇ °³¹ß
( Development of Two-Dimensional Sediment Transport Model Using Observed Erosion Rate ) |
| Á¤Å¼º; Çѳ²´ëÇб³ Åä¸ñȯ°æ°øÇаú;
|
|
|
 |
|
| |
| ÃÊ ·Ï |
| ħ½Ä·ü ÃøÁ¤ÀåÄ¡ÀÎ SEDFLYMEÀ» »ç¿ëÇÏ¿© Á÷Á¢ ÃøÁ¤ÇÑ Ä§½Ä·ü ÀڷḦ ÀÌ¿ëÇÏ´Â ÅðÀû¹° ¼ö¼Û¿¡ °üÇÑ 2Â÷¿ø ¸ðÇüÀÌ °³¹ßµÇ¾ú´Ù. °³¹ßµÈ ¸ðÇüÀº ÇöÀå Àû¿ë¼ºÀ» ³ôÀ̱â À§ÇÏ¿© °æ°è¹ÐÂøÁÂÇ¥°è¸¦ ¼öÆò¹æÇâ¿¡ ´ëÇØ »ç¿ëÇϸç, ÅðÀû¹° À̵¿ ¸ðÀǽà ħ½Ä·ü »êÁ¤¿¡¼ ºÒÈ®½Ç¼ºÀ» ÁÙÀ̱â À§ÇØ Ä§½Ä·ü ÃøÁ¤ÀڷḦ Á÷Á¢ »ç¿ëÇÑ´Ù. °³¹ßµÈ ¸ðÇüÀº ºÎÀ¯»ç¿Í ¼ÒÀ¯»ç À̵¿À» ¸ðµÎ °í·ÁÇÑ´Ù. ¸ðÇüÀÇ Á¤È®¼ºÀ» °ËÅäÇϱâ À§ÇÏ¿© 1Â÷¿ø ¼ö·Î¿¡¼ Àå°©È Çö»óÀ» ¸ðÀÇÇÏ°í ½ÇÇèÀÚ·á¿Í ºñ±³ÇÏ¿´´Ù. ºñ±³ÇÑ °á°ú¿¡ ÀÇÇϸé, º» ¸ðÇüÀº ±âÁ¸ÀÇ 1Â÷¿ø ¸ðÇüÀÇ ¿¬±¸°á°ú¿¡ ºñÇÏ¿© ÀÔµµºÐÆ÷ º¯È°úÁ¤À» º¸´Ù Á¤È®È÷ ¸ðÀÇÇÏ¿´´Ù. ¶ÇÇÑ, ¼ö·ÎÆøÀÌ È®ÀåÇÏ´Â 2Â÷¿ø ¼ö·Î¿¡¼ ÅðÀû°ú ħ½Ä Çö»óÀ» ¸ðÀÇÇÑ °á°ú, ¸ðÇüÀº Á¤»óÀûÀ¸·Î ÀÛµ¿ÇÏ¿´À¸¸ç Àå°©È Çö»óÀÌ Ä§½Ä°ú ÅðÀûÀ» ¾ïÁ¦ÇÏ´Â µ¥ ±â¿©ÇÏ´Â °ÍÀ» È®ÀÎÇÒ ¼ö ÀÖ¾ú´Ù. |
|
| A 2-dimensional numerical sediment transport model has been developed by using erosion rates observed by SEDFLUME. The model un boundary-fitted coordinate can reduce inaccuracy of sediment model with accurate erosion data. Suspended transport and bed load transport are included in the model together. The model results gave good agreement with particle size distributions in 1-d channel and was more accurate than that of HIDAS of 1-dimensional model. The model applied to an enlarging channel to check model performance in 2-dimensional domain. Bed coarsening reduced erosion and deposition. |
| |
| Ű¿öµå |
| °¡¹³Áö¼ö;°¡¹³;°¡¹³ÁöÇ¥;°¡¹³ºÐ¼®;sediment model;erosion;armoring;sediment transport; |
| |
|
|
 |
|
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.34, no.6, 2001³â, pp.687-699
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200111920877920)
¾ð¾î : Çѱ¹¾î |
|
| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
|
|
|
|
|
|