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Çѱ¹¼öÀÚ¿øÇÐȸ / v.42, no.1, 2009³â, pp.21-31
À¯¿ª´ÜÀ§ ÁöÇ¥¼ö-ÁöÇϼö »óÈ£ÀÛ¿ëÀÇ ½Ã°ø°£Àû º¯µ¿ºÐ¼®
( Analysis on the Spatial-temporal Variation of Surface-groundwater Interaction on the Watershed Basis )
±è³²¿ø;À¯»ó¿¬;Á¤ÀϹ®;ÀÌÁ¤¿ì; Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼ö¹®¿¬±¸½Ç;Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼ö¹®¿¬±¸½Ç;Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼ö¹®¿¬±¸½Ç;Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼ö¹®¿¬±¸½Ç;
 
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ÁöÇ¥¼ö-ÁöÇϼö »óÈ£ÀÛ¿ëÀÇ Æ¯¼º°ú °­µµ ¹× ¹æÇâÀº ÁöÇϼöµÎ, ¼ö¸®Àüµµµµ¿Í ÇÏ»óÁöÇü¿¡ ÀÇÇØ ¿µÇâÀ» ¹Þ°Ô µÈ´Ù. ÀÌ·¯ÇÑ ¿ä¼ÒµéÀº °ø°£ÀûÀ¸·Î ¸Å¿ì ºÒ±ÕÁúÇÏ¿© °á°úÀûÀ¸·Î »óÈ£ÀÛ¿ëÀº À¯¿ª Àüü ¹°¼öÁö¿¡µµ ¿µÇâÀ» ÁØ´Ù. ±×·¯³ª ÁöÇ¥¼ö-ÁöÇϼö »óÈ£ÀÛ¿ëÀÇ ½Ã°ø°£ÀûÀÎ ¹üÀ§³ª °­µµ¿¡ °üÇÑ Á¶»ç ¹× ¿¬±¸´Â ¸Å¿ì Á¦ÇÑÀûÀÌ¸ç ´ë°³ ÀÛÀº ÇÏõ ±¸°£ÀÇ ´Ü¸éÇØ¼®À¸·Î¸¸ Ä¡¿ìÃÄ À¯¿ª±â¹ÝÀÇ ÁöÇ¥¼ö-ÁöÇϼö »óÈ£ÀÛ¿ë¿¡ ´ëÇÑ Æ÷°ýÀûÀÎ ¿¬±¸°¡ ÇÊ¿äÇÑ ½ÃÁ¡ÀÌ´Ù. º» ¿¬±¸¿¡¼­´Â ¿ÏÀü¿¬µ¿Çü ÁöÇ¥¼ö-ÁöÇϼö °áÇÕ¸ðÇüÀÎ SWAT-MODFLOW¸¦ ¾È¾çõ À¯¿ª¿¡ Àû¿ëÇÏ¿© ÇÏõ°ú ´ë¼öÃþÀÇ »óÈ£ÀÛ¿ëÀÇ ¹üÀ§¿Í °­µµ¸¦ ºÐ¼®ÇÏ¿´´Ù. ºÐ¼®°á°ú ¾È¾çõ À¯¿ªÀº °­¼öÁýÁß ±â°£À» Á¦¿ÜÇϸé, ¿¬Áß ±âÀúÀ¯ÃâÀÇ °ø±ÞÀ¸·Î ÀÎÇØ À̵æÇÏõÀÇ Æ¯¼ºÀ» Àß ³ªÅ¸³»´Â °ÍÀ¸·Î ³ªÅ¸³µÀ¸¸ç, ÁöÇ¥¼ö-ÁöÇϼö »óÈ£ÀÛ¿ëÀÇ ¿µÇâ¹üÀ§´Â Ç¥°í°¡ ³·Àº ÇÏ·ù·Î °¥¼ö·Ï Á¡Á¡ Ä¿Áö´Â °ÍÀ¸·Î È®ÀεǾú´Ù.
The characteristics, intensity and direction of groundwater.surface water interactions are controlled by groundwater head gradients, hydraulic conductivity and by the riverbed geometry. As a result of the spatial heterogeneity of these factors and the subsequent variability of the impact of these interaction processes, the water balance is also characterized by highly variable spatial patterns and temporal dynamics. However, spatially detailed studies concerning the spatio-temporal variability of the extent and intensity of surface-groundwater interactions have been limited to the investigation of cross-sections or small stream reaches. Thus, the extensive study on the watershed based interaction between surface water and groundwater is to be analyzed. In this study, the intensity and the spatial extent of interactions along the stream were found by using integrated SWAT-MODFLOW model. This integrated modeling approach was applied to Anyangcheon watershed in Korea. The effluent stream characteristics were found in the watershed, namely, baseflow was annually discharged except heavy rainy periods. The intensity and the spatial extent of surface-groundwater interactions in different sub-watersheds were found on a daily basis. The influential extent of surface-groundwater interaction become larger as the watershed elevations are lower.
 
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ÁöÇ¥¼ö-ÁöÇϼö »óÈ£ÀÛ¿ë;½Ã°ø°£Àû º¯µ¿¼º;»óÈ£ÀÛ¿ëÀÇ °­µµ¿Í °ø°£¹üÀ§;Surface-groundwater interactions;SWAT-MODFLOW;Spatial-temporal variability;Intensity and spatial extent of interactions;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.42, no.1, 2009³â, pp.21-31
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200904751484419)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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