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Çѱ¹¼öÀÚ¿øÇÐȸ / v.37, no.9, 2004³â, pp.737-744
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»ê¸²½Ä»ý¿¡ µû¸¥ À¯¿ª ¹°¼öÁö ¿µÇâ Æò°¡
( Assessment of Forest Vegetation Effect on Water Balance in a Watershed ) |
| ±èö°â;±è³²¿ø; Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼öÀÚ¿ø¿¬±¸ºÎ;Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼öÀÚ¿ø¿¬±¸ºÎ;
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| º» ¿¬±¸¿¡¼´Â »ê¸²½Ä»ý¿¡ µû¸¥ Àå±âÀûÀÎ Ãø¸é¿¡¼ÀÇ À¯¿ª ¹°¼öÁö ¿µÇâÀ» »ìÆìº¸±â À§ÇÏ¿© º¸Ã»Ãµ À¯¿ªÀ» ´ë»óÀ¯¿ªÀ¸·Î ¼±Á¤Çϰí, ÁØºÐÆ÷Çü ¸Å°³º¯¼ö ¸ðÇüÀÎ SWAT ¸ðÇüÀ» Àû¿ëÇÏ¿©, ħ¿±¼ö¿Í Ȱ¿±¼ö¿¡ µû¸¥ Áõ¹ß»ê, ÁöÇ¥À¯Ãâ, Áß°£À¯Ãâ, ±âÀúÀ¯Ãâ, ÃÑ À¯ÃâÀÇ Â÷À̸¦ °ËÅäÇÏ¿´´Ù. ¸ÕÀú SWAT ¸ðÇü³» ½Ä»ý »ýÀå ¾Ë°í¸®ÁòÀ» ¼öÁ¤ÇÏ¿© ¿¬Áß ÀÏÁ¤ÇÑ ¿±¸éÀûÁö¼ö¸¦ °®´Â ±¹³» ħ¿±¼ö¸²ÀÇ »ýÀå Æ¯¼ºÀ» ¹Ý¿µÇÒ ¼ö ÀÖµµ·Ï ÇÏ¿´À¸¸ç, ´ë»óÀ¯¿ªÀ» ÇϳªÀÇ ÅäÁöÇǺ¹À» °®´Â °¡»óÀÇ À¯¿ªÀ¸·Î ¼³Á¤ÇÑ ÈÄ, ¼öÁ¤µÈ SWAT ¸ðÇüÀ» Àû¿ëÇÏ¿© °¢ ¹°¼öÁö ¿ä¼Ò º¯È¸¦ ¸ðÀÇÇÑ °á°ú, ħ¿±¼ö°¡ Ȱ¿±¼ö¿¡ ºñÇØ Áõ¹ß»ê Áõ°¡ ¹× À¯Ãâ °¨¼Ò¿¡ ´õ ¿µÇâÀ» ¹ÌÄ¡´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ±×·¯³ª, º¸´Ù Á¤·®ÀûÀÎ ±Ô¸í°ú À¯Ãâ¸ðÇüÀÇ ºÒÈ®½Ç¼ºÀ» º¸¿ÏÇϱâ À§Çؼ´Â ¼öÁ¾ ¿Ü¿¡ ¼ö·É, ½ÄÀç¹Ðµµ, ½ÄÀçÀ§Ä¡, Åä¾çƯ¼ºÀÚ·á µî ´Ù¾çÇÑ Á¶°ÇÀÌ ÃæºÐÈ÷ °í·ÁµÇ¾î¾ß ÇÒ °ÍÀÌ´Ù. |
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| In this study, to evaluate the effect of forest vegetation on the long-term water balance in a watershed, semi-distributed and physically based parameter model, SWAT was applied to the Bocheong watershed, and the variation of hydrological components such as evapotranspiration, surface flow, lateral flow, base flow, and total runoff was investigated with coniferous and deciduous forests, respectively. First, SWAT model was modified to simulate the actual plant growth pattern of coniferous trees which have the uniform value of leaf area index all the seasons of the year. The modified model was applied to the watershed that is assumed to have only one land cover in the whole watershed, and the variation of the water balance components was investigated for each land cover. It was found that coniferous forest affected the increase in evapotranspiration and decrease in runoff more than deciduous forest. However, the age and the density of stand, the location, and soil characteristics and meteorological conditions including the tree species should be also considered to examine the effect more quantitatively and to reduce the uncertainties in simulated output from the hydrological model. |
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| Ű¿öµå |
| SWAT;»ê¸²;¹°¼öÁö;Áõ¹ß»ê;À¯Ãâ;SWAT;Forest;Water balance;Evapotranspiration;Runoff; |
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Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.37, no.9, 2004³â, pp.737-744
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200413842113049)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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