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Çѱ¹¼öÀÚ¿øÇÐȸ / v.44, no.2, 2011³â, pp.157-167
È«¼öÅÍ ½Ä»ýÀ» °í·ÁÇÑ ºÒ±ÔÄ¢ÇÑ ´Ü¸é¿¡¼­ÀÇ ¼öÀ§-À¯·® °î¼± ¹× ´ÜÀ§À¯·® ȾºÐÆ÷ ¿¹Ãø
( Prediction of Stage Discharge Curve and Lateral Distribution of Unit Discharge in an Arbitrary Cross Section Channel with Floodplain Vegetation )
±èŹü;ÀåÁö¿¬;½ÅÀç±¹;ÃÖ¼º¿í; ¿¬¼¼´ëÇб³ °ø°ú´ëÇÐ Åä¸ñȯ°æ°øÇаú;¿¬¼¼´ëÇб³ °ø°ú´ëÇÐ Åä¸ñȯ°æ°øÇаú;(ÁÖ)ÇѾç Åä¸ñ»ç¾÷º»ºÎ ±â¼ú¿µ¾÷ÆÀ;¿¬¼¼´ëÇб³ °ø°ú´ëÇÐ Åä¸ñȯ°æ°øÇаú;
 
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º» ¿¬±¸¿¡¼­´Â º¹´Ü¸é°³¼ö·Î¹× ºÒ±ÔÄ¢ÇÑ ÇÏ»óÀ»º¸À̴ Ⱦ´Ü¸é »ó¿¡¼­ÀÇ ¼öÀ§-À¯·®°î¼± ¹×´ÜÀ§À¯·®È¾ºÐÆ÷¿¹ÃøÀ» À§ÇÑ À¯ÇÑ¿ä¼Ò¸ðÇüÀ» °³¹ßÇÏ¿´´Ù. Áö¹è¹æÁ¤½ÄÀº Á¤»ó·ù¿Í Á¾¹æÇâ µî·ù¸¦ °¡Á¤ÇÑ ¿îµ¿·®¹æÁ¤½ÄÀ» ÀÌ¿ëÇϸç, ¼ö¸éÀº Ⱦ´Ü¸é¿¡ °ÉÃÄ ÀÏÁ¤ÇÏ´Ù°í °¡Á¤ÇÑ´Ù. È«¼öÅÍ ½Ä»ýÀÇ ¿µÇâÀ» ¹Ý¿µÇϱâ À§ÇØ ½Ä»ýÇ×·ÂÀÌ Áö¹è¹æÁ¤½Ä¿¡ Æ÷ÇԵǾúÀ¸¸ç, ¼öÄ¡ÇØ¸¦ ±¸Çϱâ À§ÇØ À¯ÇÑ¿ä¼Ò¹ýÀ» Àû¿ëÇÏ¿´´Ù. ´Ü¸éÇü»ó°ú ManningÀÇ Á¶µµ°è¼ö, ½Ä»ýÁ¤º¸, Á¾¹æÇâ ÇÏ»ó°æ»ç¸¦ ÀÔ·ÂÀÚ·á·Î ¼öÀ§-À¯·® °î¼±À» ¿¹Ãø °¡´ÉÇϸç, ÁÖ¾îÁø ¼öÀ§¿¡¼­ÀÇ È帧¹æÇâ ´ÜÀ§À¯·®ÀÇ È¾¹æÇâ ºÐÆ÷¸¦ ¿¹ÃøÇÒ ¼ö ÀÖ´Ù. °³¹ßµÈ ¸ðÇüÀÇ °ËÁõÀ» À§ÇØ ½ÇÃøÀÚ·á ¹× Darby and Thorne (1996)ÀÇ ¸ðÇü °á°ú, ±×¸®°í ºñ¼±Çü k-$epsilon$ ¸ðÇüÀÇ °á°ú¿Íµµ ºñ±³ÇÏ¿´´Ù. °ËÁõµÈ ¸ðÇüÀÇ ¾Ë°í¸®ÁòÀ» 2Â÷¿ø ¸ðÇüÀÇ »ó·ù´Ü °æ°èÁ¶°Ç ¼³Á¤¿¡ Ȱ¿ëÇÏ¿©, À¯ÀÔÀ¯·®À» ÀýÁ¡º° ´ÜÀ§À¯·®À¸·Î ºÐ¹è½ÃÄ×À» ¶§¿Í ±×·¸Áö ¾Ê¾ÒÀ» ¶§ÀÇ °á°ú¸¦ ºñ±³ÇÏ¿´´Ù.
A numerical model was developed to predict the stage-discharge curve and lateral distribution of unit discharge in open channels with nonuniform cross section or compound open-channels. The governing equation is the one-dimensional momentum equation based on assumptions of the steady and uniform flow conditions in the longitudinal direction and the uniform water surface elevation in a cross section. Vegetative drag force term was included in governing equation in order to reflect the effect of floodplain vegetation on the flow characteristics. Finite element method was applied to obtain the numerical solution of the governing equation. Stage-discharge curve and lateral distribution of unit discharge for a given water surface are calculated based on input data, such as the cross sectional geometry, Manning's roughness coefficient, vegetative information and longitudinal slope of channel bed. The developed model was verified by comparing the calculated results with the observed data and the results of Darby and Thorne's(1996) model and the nonlinear k-$epsilon$ model. The verified model was applied to estimate the upstream boundary conditions in two-dimensional flow model. The numerical results using laterally distributed unit discharge were compared with those obtained using uniformly distributed unit discharge in two-dimensional flow model.
 
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¼öÀ§-À¯·® °î¼±;´ÜÀ§À¯·® ȾºÐÆ÷;½Ä»ý;È«¼öÅÍ;stage-discharge curve;lateral distribution of unit discharge;vegetation;floodplain;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.44, no.2, 2011³â, pp.157-167
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO201108863881022)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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