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Çѱ¹¼öÀÚ¿øÇÐȸ / v.39, no.11, 2006³â, pp.977-984
À¯¿ªÀ» ´ëÇ¥ÇÏ´Â Horton ħÅõ ¸ðÇü³» ¸Å°³º¯¼öÀÇ ÃÖÀû °áÁ¤
( Optimal Determination of the Parameters Representative of a Basin in the Horton's Infiltration Model )
À¯ÁÖȯ; ¿µµ¿´ëÇб³ Åä¸ñȯ°æ°øÇаú;
 
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ÃÖÀûÈ­ ¹æ¹ýÀ» ÀÌ¿ëÇÏ¿© ´ëÇ¥Àû ħÅõ ¸ðÇüÀ¸·Î Àß ¾Ë·ÁÁø Horton¸ðÇüÀÇ ÃÖÀû ¸Å°³º¯¼ö¸¦ °áÁ¤ÇÏ¿´´Ù. HortonħÅõ ¸ðÇü³» Ãʱâ ħÅõ´ÉÀº 10ÀÏ ´ÜÀ§ ¼±Çà °­¼ö·®°ú ¼±Çü Á¶ÇÕÀÇ °ü°è¸¦ °®´Â´Ù°í °¡Á¤ÇÏ¿´´Ù. ±×¸®°í Á¾±â ħÅõ´É°ú °¨¼âÁö¼ö °ªÀº À¯¿ª³» ÇϳªÀÇ ´ëǥġ·Î °áÁ¤ÇÏ¿´´Ù. ÀÌ·¸°Ô ÇÏ¿© À¯¿ªÀ» ´ëÇ¥ÇÏ´Â ¸ðÇüÀÇ ¸Å°³º¯¼ö ÃÖÀûÄ¡¸¦ ¾ò¾ú°í È£¿ì »ç»óº°·Î HortonÀÇ Ä§Åõ½ÄÀ» °áÁ¤ÇÏ¿´´Ù. º» ¿¬±¸¿¡¼­ Àû¿ëÇÑ 10°³ÀÇ È£¿ì ÀÚ·á´Â ÀÓÁø°­ ³»¿¡ ÀÖ°í ¹è¼ö ¸éÀûÀÌ $8.5km^2$µÇ´Â ¼³¸¶Ãµ ½ÃÇè À¯¿ª³» ÀüÀûºñ±³ ÁöÁ¡¿¡¼­ °üÃøµÈ °ÍÀÌ´Ù.
The parameters in the Horton's model which has well known as typical infiltration model were determined by the use of the optimization technique. It was assumed the initial infiltration capacity in this model was related to the antecedent precipitation per 10 days with linear combination. And both the parameters of the ultimate infiltration capacity and the decay factor were determined uniquely on a basin. Thus the optimal model's parameters representative to a basin were obtained and the Horton's infiltration equations by rainstorm events were determined. The data of ten rainstorm events for this study were observed at the Jeonjeokbigyo station located at the Selmacheon experimental basin that was $8.5km^2$ wide in the Imjin river.
 
Ű¿öµå
Horton ħÅõ¸ðÇü;¼±Çà°­¼ö·®;¸Å°³º¯¼ö ÃÖÀûÈ­;À¯È¿°­¼ö·®;Horton infiltration model;antecedent precipitation;parameter optimization;effective precipitation;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.39, no.11, 2006³â, pp.977-984
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200604623537891)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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