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Çѱ¹¼öÀÚ¿øÇÐȸ / v.38, no.10, 2005³â, pp.871-883
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½Ä»ýµÈ °³¼ö·Î È帧¿¡¼ÀÇ ³·ùÀÇ ºñµî¹æ¼º
( Anisotropy of Turbulence in Vegetated Open-Channel Flows ) |
| °Çü½Ä;ÃÖ¼º¿í; ¿¬¼¼´ëÇб³ »çȸȯ°æ½Ã½ºÅÛ°øÇкÎ;¿¬¼¼´ëÇб³ »çȸȯ°æ½Ã½ºÅÛ°øÇкÎ;
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| º» ³í¹®Àº ½Ä»ýµÈ °³¼ö·Î È帧¿¡¼ ³·ùÀÇ ºñµî¹æ¼ºÀÌ Æò±ÕÀ¯¼Ó ¹× ³·ù±¸Á¶¿¡ ¹ÌÄ¡´Â ¿µÇâÀ» ÆÄ¾ÇÇϱâ À§ÇÑ ¼öÄ¡¸ðÀÇ ¿¬±¸ÀÌ´Ù. ºñµî¹æ¼º ³·ù¸ðÇüÀÎ ·¹À̳îÁîÀÀ·Â¸ðÇüÀ» ÀÌ¿ëÇÏ¿© ½Ä»ýÀÌ ¾ø´Â ÀÏ¹Ý °³¼ö·Î È帧°ú ħ¼ö ¹× Á¤¼ö½Ä»ýµÈ °³¼ö·Î È帧¿¡¼ÀÇ Æò±ÕÀ¯¼Ó ¹× ³·ù±¸Á¶¸¦ ¼öÄ¡¸ðÀÇÇÏ¿´´Ù. ¼öÄ¡¸ðÀÇ °á°ú¸¦ ±âÁ¸ÀÇ ½ÇÇè°á°ú ¹× k-$epsilon$ ¸ðÇü°ú ÀÀ·Â´ë¼ö½Ä¸ðÇü¿¡ ÀÇÇÑ °è»ê °á°ú¿Í ºñ±³ÇÏ¿´´Ù. ½Ä»ýÀÌ ¾ø´Â ÀÏ¹Ý °³¼ö·Î È帧°ú Á¤¼ö½Ä»ýµÈ °³¼ö·Î È帧¿¡¼ÀÇ Æò±ÕÀ¯¼Ó°ú ·¹À̳îÁîÀÀ·ÂÀ» °è»êÇÑ °á°ú µî¹æ¼º ¹× ºñµî¹æ¼º ³·ù¸ðÇü¿¡ ÀÇÇÑ ÇØ¼® °á°úÀÇ Â÷À̰¡ °ÅÀÇ ³ªÅ¸³ªÁö ¾Ê¾Ò´Ù. Áï, ³·ùÀÇ ºñµî¹æ¼ºÀÇ ¿µÇâÀÌ ¸Å¿ì ÀÛÀº °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ±×·¯³ª ÀÚÀ¯¼ö¸é ¹× ¹Ù´Ú ±Ùó¿¡¼ ¹ß»ýµÇ´Â ³·ùÀÇ °¨¼èÈ¿°ú¿¡ ÀÇÇÑ ³·ùÀÇ ºñµî¹æ¼ºÀº ·¹À̳îÁîÀÀ·ÂÀÌ °¡Àå Àß ¿¹ÃøÇÏ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ħ¼ö½Ä»ýµÈ °³¼ö·Î È帧ÀÇ °æ¿ì ½Ä»ý³ôÀÌ ºÎ±Ù¿¡¼ ³·ùÀÇ ºñµî¹æ¼ºÀÌ °ÇÏ°Ô ¹ß»ýÇÏ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. °è»êµÈ Æò±ÕÀ¯¼Ó ¹× ³·ù±¸Á¶´Â ·¹À̳îÁîÀÀ·Â¸ðÇüÀÌ ´Ù¸¥ ¸ðÇü º¸´Ù °¡Àå Á¤È®ÇÑ ¿¹ÃøÀ» ¼öÇàÇÏ¿´À¸¸ç, µî¹æ¼º ¸ðÇüÀÎ k-$epsilon$ ¸ðÇüÀº ½Ä»ý³ôÀÌ º¸´Ù ³ôÀº ¿µ¿ª¿¡¼ Æò±ÕÀ¯¼Ó ¹× ³·ù°µµ¸¦ °¢°¢ °ú´ë ¹× °ú¼Ò ¿¹ÃøÇÏ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ¶ÇÇÑ °è»êµÈ °á°ú¸¦ ÀÌ¿ëÇÏ¿© ½Ä»ýµÈ °³¼ö·Î È帧¿¡¼ÀÇ ºÎÀ¯»ç·®À» »êÁ¤ÇÑ °á°ú µî¹æ¼º ³·ù¸ðÇüÀÌ ºÎÀ¯»ç·®À» °ú¼Ò »êÁ¤ÇÏ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. |
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| This paper investigates the impacts of turbulent anisotropy on the mean flow and turbulence structures in vegetated open-channel flows. The Reynolds stress model, which is an anisotropic turbulence model, is used for the turbulence closure. Plain open-channel flows and vegetated flows with emergent and submerged plants are simulated. Computed profiles of the mean velocity and turbulence structures are compared with measured data available in the literature. Comparisons are also made with the predictions by the k-$epsilon$ model and by the algebraic stress model. For plain open-channel flows and open-channel flows with emergent vegetation, the mean velocity and Reynolds stress profiles by isotropic and anisotropic turbulence models were hardly distinguished and they agreed well with measured data. This means that the mean flow and Reynolds stress is hardly affected by anisotropy of turbulence. However, anisotropy of turbulence due to the damping effect near the bottom and free surface is successfully simulated only by the Reynolds stress model. In open-channel flows with submerged vegetation, anisotropy of turbulence is strengthenednear the vegetation height. The Reynolds stress model predicts the mean velocity and turbulence intensity better than the algebraic stress model or the k-$epsilon$ model. However, above the vegetation height, the k-$epsilon$ model overestimates the mean velocity and underestimates turbulence intensity Sediment transport capacity of vegetated open-channel flows is also investigated by using the computed profiles. It is shown that the isotropic turbulence model underestimates seriously suspended load. |
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| ½Ä»ýµÈ °³¼ö·Î È帧;·¹À̳îÁîÀÀ·Â¸ðÇü;³·ùÀÇ ºñµî¹æ¼º;³·ù±¸Á¶;ºÎÀ¯»ç·®;Vegetated open-channel flow;Reynolds stress model;anisotropic turbulence;turbulence structure;suspended load; |
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Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.38, no.10, 2005³â, pp.871-883
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200507521980650)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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