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Çѱ¹¼öÀÚ¿øÇÐȸ / v.44, no.1, 2011³â, pp.9-22
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Á¤¼ö½Ä»ýÀÌ Á¸ÀçÇÏ´Â ÀÚ¿¬Çϵµ¿¡¼ 1Â÷¿ø ¼öÄ¡¸ðÇü
( 1D Numerical Model for Rivers Flows with Emergent Vegetations on Floodplains and Banks ) |
| ¼ÛÁÖÀÏ;±èÁ¾¿ì;ÀÓâ¼ö;À±¼¼ÀÇ; °æ±â´ëÇб³ Åä¸ñ°øÇаú;°æ±â´ëÇб³ Åä¸ñ°øÇаú;°æ±â´ëÇб³ Åä¸ñ°øÇаú;°æ±â´ëÇб³ Åä¸ñ°øÇаú;
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| º» ¿¬±¸¿¡¼´Â ¿¡³ÊÁö ¹æÁ¤½Ä¿¡ ±âÃÊÇÏ¿© Á¤¼ö ½Ä»ýÀÌ Á¸ÀçÇÏ´Â ÀÚ¿¬Çϵµ¿¡ Àû¿ë °¡´ÉÇÑ 1Â÷¿ø ¼öÄ¡¸ðÇüÀ» Á¦½ÃÇÏ¿´´Ù. ¼öÀ§°è»êÀ» À§ÇÑ ¸¶Âû°æ»ç´Â Darcy-WeisbachÀÇ ¸¶Âû½Ä¿¡ ÀÇÇØ °è»êµÇ¾ú´Ù. °¢ ´Ü¸éÀÇ Àüü Darcy-Weisbach ¸¶Âû°è¼ö´Â ÇÏ»óÁ¶µµ³ôÀÌ, ½Ä»ý, ½Ä»ý±¸¿ª°ú ºñ½Ä»ý±¸¿ª »çÀÌÀÇ Àü´ÜÀúÇ×, ±×¸®°í È«¼öÅÍ¿Í ÁÖ¼ö·ÎÀÇ °æ°è¸é Àü´ÜÀúÇ×À» °í·ÁÇÏ¿© »êÁ¤ÇÏ¿´´Ù. °æ°è¸é ¸¶Âû°è¼ö´Â Mertens¹æ¹ý°ú Nuding¹æ¹ý¿¡ ÀÇÇØ °è»êµÇ¾ú´Ù. Á¦½ÃµÈ ¸ðÇüÀ» °¡»óÇϵµ¿¡ Àû¿ëÇϰí HEC-RAS¸ðÇü ¸ðÀǰá°ú¿Í ºñ±³, °ËÁõÇÏ¿´°í, ½Ä»ý¹Ðµµ µî¿¡ ´ëÇÏ¿© ¸¶Âû°è¼öÀÇ ¹Î°¨µµ ºÐ¼®À» ½Ç½ÃÇÏ¿´´Ù. ¸ðÇüÀÇ Àû¿ë¼º°ËÅ並 À§ÇÏ¿© µ¶ÀÏ Enz° ÀϺα¸°£À» ´ë»óÀ¸·Î ¼öÄ¡¸ðÀǸ¦ ½Ç½ÃÇÏ°í ½ÇÃø¼öÀ§¿Í ºñ±³ÇÏ¿´´Ù. ½Ä»ýÀÌ Á¸ÀçÇÏ´Â Enz°ÀÇ ½ÇÃø¼öÀ§¿Í °è»ê¼öÀ§¸¦ ºñ±³ÇÑ °á°ú ½Ä»ýÀÇ ¿µÇâÀ» °ÅÀÇ ¹ÞÁö ¾Ê°í ÁÖ¼ö·Î¿¡ È帧ÀÌ Çü¼ºµÇ´Â ÀúÀ¯·®ÀÇ °æ¿ì¿Í ½Ä»ýÀÇ ¿µÇâÀ» Áö¹èÀûÀ¸·Î ¹Þ´Â °íÀ¯·® È帧 ¸ðµÎ¿¡¼ ÇÕ¸®ÀûÀÎ ¼öÀ§¸¦ ¿¹ÃøÇÏ¿© Á¦½ÃµÈ ¸ðÇüÀÇ Àû¿ë °¡´É¼ºÀ» È®ÀÎÇÏ¿´´Ù. |
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| A 1D numerical model for steady flow, based on the energy equation, was developed for natural rivers with emergent vegetations on floodplains and banks. The friction slope was determined by the friction law of Darcy-Weisbach. The composite friction factor of the each cross section was calculated by considering bottom roughness of the main channel and the floodplains, the flow resistance of vegetations, the apparent shear stress and the flow resistance caused by the momentum transfer between vegetated areas and non-vegetated areas. The interface friction factor caused by flow interaction was calculated by empirical formulas of Mertens and Nuding. In order to verify the accuracy of the suggested model, water surface elevations were calculated by using imaginary compound channels and the results of calculations were compared with that of the HEC-RAS. The sensitivity analysis was performed to confirm changed friction factors by vegetations density etc. The suggested model was applied to the reach of the Enz River in Germany, and estimated water surface elevations of the Enz River were compared with measured water surface elevations. This model could acceptably compute not only water surface elevations with low discharge but also that with high discharge. So, the suggested model in this study verified the applicability in natural rivers with emergent vegetations. |
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| Ű¿öµå |
| ½Ä»ýÇϵµ;È帧ÀúÇ×;¸¶Âû°è¼ö;¿îµ¿·® ±³È¯;vegetated channel;flow resistance;friction factor;momentum transfer;Mertens;Nuding; |
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Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.44, no.1, 2011³â, pp.9-22
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO201107049668120)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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