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Çѱ¹¼öÀÚ¿øÇÐȸ / v.42, no.8, 2009³â, pp.619-629
µî°¡Á¶°í¸¦ ÀÌ¿ëÇÑ ÀÚ°¥ÇÏõÀÇ ÇÏ»óÀúÇ× »êÁ¤
( Estimation of Bed Resistance in Gravel-bed Rivers Using the Equivalent Roughness Height )
±èÁö¼º;±è¿ëÀü;ÀÌÂùÁÖ;±è¿ø; Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼öÀÚ¿ø.ȯ°æ¿¬±¸º»ºÎ ÇÏõ.ÇØ¾ÈÇ׸¸¿¬±¸½Ç;Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼öÀÚ¿ø.ȯ°æ¿¬±¸º»ºÎ ÇÏõ.ÇØ¾ÈÇ׸¸¿¬±¸½Ç;Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼öÀÚ¿ø.ȯ°æ¿¬±¸º»ºÎ ÇÏõ.ÇØ¾ÈÇ׸¸¿¬±¸½Ç;Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼öÀÚ¿ø.ȯ°æ¿¬±¸º»ºÎ ÇÏõ.ÇØ¾ÈÇ׸¸¿¬±¸½Ç;
 
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º» ¿¬±¸´Â ÇÏ»ó¸¶ÂûÀÇ Ã´µµÀÎ µî°¡Á¶°í¸¦ ÀÌ¿ëÇÏ¿© ÀÚ°¥ÇÏõÀÇ ÇÏ»óÀúÇ×À» »êÁ¤ÇÏ´Â °ÍÀÌ´Ù. À̸¦ À§ÇÏ¿© ±¹³» 8°³ ÀÚ°¥ÇÏõ¿¡¼­ ½ÇÃøÀ» ÅëÇÏ¿© ¸¶Âû°è¼ö f¸¦ »êÁ¤ÇÏ¿´°í, ÇÏ»óÀç·áÀÇ ´©°¡ÀÔ°æºÐÆ÷¸¦ Á¶»çÇÏ¿´À¸¸ç, °¢ ´Ü¸éÀÇ ½ÇÃø ¸¶Âû°è¼ö¸¦ ³ªÅ¸³»±â À§ÇÏ¿© ´ë¼ö ¿¬Á÷À¯¼ÓºÐÆ÷¸¦ °¡Á¤ÇÏ¿© °è»êµÈ Æò±Õ µî°¡Á¶°í¿Í ´©°¡ÀÔ°æºÐÆ÷¸¦ ÀÌ¿ëÇÏ¿© °è»êµÈ ±¸°£ µî°¡Á¶°í¸¦ ºñ±³ÇÏ¿´´Ù. ´õºÒ¾î µî°¡Á¶°í¸¦ »ç¿ëÇÏ¿© °è»êµÈ Manning °è¼ö¸¦ Strickler À¯ÇüÀÇ ±âÁ¸ °æÇè½Ä¿¡ ÀÇÇÑ Manning °è¼ö¿Í ºñ±³ÇÔÀ¸·Î½á, ±¹³» ÀÚ°¥ÇÏõ¿¡¼­ ±âÁ¸ °æÇè½ÄÀ» ÀÌ¿ëÇÑ ÇÏ»óÀúÇ× »êÁ¤ÀÇ Àû¿ë¼ºÀ» °ËÅäÇÏ¿´´Ù. ºÐ¼®°á°ú, ±¸°£ µî°¡Á¶°í°¡ ´ë»ó±¸°£ÀÇ ÇÏ»óÆ¯¼ºÀ» ´ëÇ¥ÇÒ ¼ö ÀÖÀ½À» È®ÀÎÇÏ¿´°í, ±¸°£ µî°¡Á¶°í·Î °è»êµÈ Manning °è¼ö°¡ ½ÇÃø ÀÚ·á·ÎºÎÅÍ °è»êµÈ Manning °è¼ö¿Í ºñ±³ÇÏ¿© RMS ¿ÀÂ÷°¡ 0.003ÀÌÇÏ·Î °è»êµÇ¾î ½Ç¹« Àû¿ë¿¡ Ÿ´çÇÒ °ÍÀ¸·Î ÆÇµÈµÇ¾ú´Ù. ¶ÇÇÑ ½ÇÁ¦ ÇÏõ¿¡¼­ µî°¡Á¶°í $k_s$¿Í ƯÁ¤ÀÔ°æ $D_i$°úÀÇ ºñ·Ê°è¼ö »çÀÌÀÇ »ó°ü¼ºÀÌ ÀûÀº °ÍÀ¸·Î ³ªÅ¸³ª, ÇÏ»ó Æ¯Á¤ÀÔ°æÀ» »ç¿ëÇÏ¿© Manning °è¼ö¸¦ »êÁ¤ÇÏ´Â ±âÁ¸ °æÇè½ÄÀ» Àû¿ëÇÒ ¶§ ÀûÀýÇÑ ¹æÁ¤½ÄÀÇ ¼±Åÿ¡ ¾î·Á¿òÀÌ ÀÖÀ» °ÍÀ¸·Î ÆÇ´ÜµÈ´Ù.
The objective of this study is to estimate bed-resistance in gravel-bed rivers using the equivalent roughness height($k_s$). We calculated the friction factor(f) with the measured data from 8 domestic gravel-bed rivers and investigated the size distributions of the bed materials. The averaged $k_s$ in each cross-section, which is determined under the hypothesis that the vertical velocity distribution follows the logarithmic law, is compared with the reach $k_s$ which is calculated with the cumulative grain diameter distribution curve of bed materials. Moreover, the applicability of existing formulae, such as Strickler type equations, is examined by comparing with Manning's n value converted from the $k_s$. According to the results, the reach $k_s$ proves to be a good indicator of representative characteristic of bed materials in a reach, and the Manning's n based on the reach $k_s$ is appropriate for practical estimation of the bed-resistance, for RMS errors between calculated and measured Manning's n is less than 0.003. The correlation between the $k_s$ and specified bed-material size($D_i$) is very low, so it is difficult to select a proper one among the existing empirical equations.
 
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ÀÚ°¥ÇÏõ;ÇÏ»óÀúÇ×;µî°¡Á¶°í;Manning Á¶µµ°è¼ö;¸¶Âû°è¼ö;gravel-bed river;bed-resistance;equivalent roughness height;Manning's n;friction factor;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.42, no.8, 2009³â, pp.619-629
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200925836515242)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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