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Çѱ¹¼öÀÚ¿øÇÐȸ / v.12, no.1, 1979³â, pp.56-59
»ç´ëÁ¾È®»ê ¸ðÇü¿¡ ÀÇÇÑ À¯ÃâÇØ¼®
( RUNOFF ANALYSIS BY DEAD ZONE LONGITUDINAL DISPERSION ANALOGY )
À±¿ë³²;Â÷¿µ±â; ÇѾç´ëÇб³ Åä¸ñ°øÇаú;ÇѾç´ëÇб³ ´ëÇпø;
 
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Á÷Á¢À¯Ãâ ¼ö¹®°î¼±ÀÇ °¨¼öºÎ¸¦ À¯¹ßÇÏ´Â ÁöÇ¥ÇÏ·ùÃâ °úÁ¤ÀÌ »ç´ëÁ¾È®»ê¸ðÇü±â¹ý¿¡ ÀÇÇÏ¿© ¸ðÀǵǾú´Ù. À¯Ãâ°úÁ¤Àº Çʽðµµ¿¡ ÀÇÇÑ ¼ÒÀ¯¿ªÀ» ´ëÇ¥ÇÏ´Â °³±ÞÀû ¼±Çü ¼ö·Î¸¦ ÅëÇÏ¿© »ó·ù¼±Çü¼ö·ÎÀÇ À¯Ãâ°ú ÇÙ½É ¼ÒÀ¯¿ªÀÇ À¯È¿°­¿ì·®À» ÃßÀûÇÏ¿© ¼öÇàµÈ´Ù. À¯Ãâ ¼Óµµ, È®»êÀÎÀÚ, ħÅõ¿Í ÁöÇ¥ÇÏÈ帧 ¿µ¿ª¿¡ °üÇÑ ¸Å°³º¯¼öÀÇ »êÃâ°úÁ¤ÀÌ ±â·ÏµÈ´Ù.
A prompt subsurface runoff producing mechanism whih creaters a depletion curve of direct runoff hydrograph is simulated by a dead zone dispersion model technique. Runoff processes are carried out by routing of the outflow resulted from previous linear channel and effective rainfall from its corresponding subwatershed through a series of conceptual linear channels representing subwatersheds of a catchment. Working rules are explained for evaluation the model parameters such as translatory velocity, diffusive factor, and parameters concerning the infiltration and relative magnitude of the prompt subsurface flow region.
 
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.12, no.1, 1979³â, pp.56-59
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO197911920089498)
¾ð¾î : ¿µ¾î
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