¶óÆæÆ®¦¢Ä«Æä¦¢ºí·Î±×¦¢´õº¸±â
¾ÆÄ«µ¥¹Ì Ȩ ¸í»çƯ°­ ´ëÇבּ¸½Ç޹æ Á¶°æ½Ç¹« µ¿¿µ»ó°­ÀÇ Çѱ¹ÀÇ ÀüÅëÁ¤¿ø ÇÐȸº° ³í¹®
ÇÐȸº° ³í¹®

Çѱ¹°Ç¼³°ü¸®ÇÐȸ
Çѱ¹°ÇÃà½Ã°øÇÐȸ
Çѱ¹µµ·ÎÇÐȸ
Çѱ¹»ý¹°È¯°æÁ¶ÀýÇÐȸ
Çѱ¹»ýÅÂÇÐȸ
Çѱ¹¼öÀÚ¿øÇÐȸ
Çѱ¹½Ä¹°ÇÐȸ
Çѱ¹½Ç³»µðÀÚÀÎÇÐȸ
Çѱ¹ÀÚ¿ø½Ä¹°ÇÐȸ
Çѱ¹ÀܵðÇÐȸ
Çѱ¹Á¶°æÇÐȸ
Çѱ¹Áö¹Ý°øÇÐȸ
Çѱ¹ÇÏõȣ¼öÇÐȸ
Çѱ¹È¯°æ»ý¹°ÇÐȸ
Çѱ¹È¯°æ»ýÅÂÇÐȸ

Çѱ¹¼öÀÚ¿øÇÐȸ / v.43, no.5, 2010³â, pp.455-469
´ï ÇÏ·ù ÃæÀûÇÏõ¿¡¼­ ½Ä»ýÀÌÀÔ ¹× õÀÌ - ³«µ¿°­ ¾Èµ¿/ÀÓÇÏ ´ï ÇÏ·ùÇÏõÀ» Áß½ÉÀ¸·Î -
( Recruitment and Succession of Riparian Vegetation in Alluvial River Regulated by Upstream Dams - Focused on the Nakdong River Downstream Andong and Imha Dams - )
¿ìÈ¿¼·;¹Ú¹®Çü;Á¶°­Çö;Á¶ÇüÁø;Á¤»óÁØ; Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼öÀÚ¿øÈ¯°æ¿¬±¸º»ºÎ ÇÏÃµÇØ¾ÈÇ׸¸¿¬±¸½Ç;Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼öÀÚ¿øÈ¯°æ¿¬±¸º»ºÎ ÇÏÃµÇØ¾ÈÇ׸¸¿¬±¸½Ç;ÀÎÇÏ´ëÇб³ ÀÚ¿¬°úÇдëÇÐ »ý¸í°úÇаú;ÀÎÇÏ´ëÇб³ ´ëÇпø »ý¸í°úÇаú;Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼öÀÚ¿øÈ¯°æ¿¬±¸º»ºÎ ÇÏÃµÇØ¾ÈÇ׸¸¿¬±¸½Ç;
 
ÃÊ ·Ï
³«µ¿°­ »ó·ù¿¡ À§Ä¡ÇÑ ¾Èµ¿, ÀÓÇÏ ´ï ÇÏ·ù ÇÏõ¿¡¼­ µÎ ´ï¿¡ ÀÇÇÑ ÃæÀûÇÏõÀÇ º¯È­¿Í ½Ä»ýÀÌÀÔ Çö»óÀ» Á¤¼ºÀû, Á¤·®ÀûÀ¸·Î Á¶»ç, ºÐ¼®ÇÏ¿´´Ù. ÇÏõÇüÅ ¹× ÇÏ»óÀç·á ºÐ¼® °á°ú, ´ï ÇÏ·ù´Â Àü¹ÝÀûÀ¸·Î ÀúÇϵǾú°í ÀϺΠ±¸°£Àº ÃÖ´ë 3m ÀÌ»ó ¼¼±¼ µÇ¾ú´Ù. ÇÏ»óÀç·áµµ Àü¹ÝÀûÀ¸·Î ÀÓÇÏ´ï °Ç¼³ Àü Æò±Õ 1.5mm¿¡¼­ °Ç¼³ ÈÄ 2.5mm·Î Á¶¸³È­µÇ¾ú´Ù. ´ï °Ç¼³·Î ÀÎÇÑ ÇÏ»ó¼Ò·ù·ÂÀÇ °¨¼Ò´Â »çÁÖ¿¡ ½Ä»ý È°ÂøÀ» ÃËÁø½ÃÄ×À¸¸ç, ±× °á°ú »çÁÖÀÇ ½Ä»ýÀÌÀÔ·üÀº 1971³â ÀÚ¿¬ »óÅ¿¡¼­ 8% ¼öÁØ¿¡¼­ ¾Èµ¿´ï °Ç¼³ ÈÄ 1988³â¿¡ 25%·Î Áõ°¡ÇÏ¿´´Ù. ÀÓÇÏ´ïÀÌ ¿Ï°øµÈ 1992³â ÀÌÈÄ »çÁÖ »ó ½Ä»ýÀÌÀÔÀº °¡¼ÓÈ­µÇ¾î °Ü¿ì 3³âÀÌ Áö³­ 1995³â¿¡ »çÁÖ ½Ä»ýÀÌÀÔ·üÀº 43%°¡ µÇ°í, ±× ÈÄ 10³âÀÌ Áö³­ 2005³â¿¡´Â 74%±îÁö Áõ°¡ÇÏ¿´´Ù. ¼¼ºÎÁ¶»ç±¸°£ Áß ÇϳªÀÎ À­Àý¿¡¼­ Ç×°ø»çÁø¿¡ ÀÇÇÑ ½Ä»ýõÀÌ Çö»óÀ» ºÐ¼®ÇÑ °á°ú ¸ð·¡¿Í ÀÚ°¥ÀÌ ³ëÃâµÈ '¸Ç' »çÁÖ¿¡¼­ ½ÃÀÛÇÏ¿© Å«°³¿©²î, ´Þ»Ñ¸®Ç®, ¹öµå³ª¹«·ù À¯½Ä¹° µî °³Ã´ ´Ü°è¸¦ Áö³ª, ÀϺΠ´Þ»Ñ¸®Ç®Àº À¯ÁöµÇ°í ¹öµå³ª¹« °ü¸ñÀÌ µîÀåÇÏ°í ³ªÁß¿¡´Â ¼±¹öµéÀ̳ª ¿Õ¹öµé °°Àº ±³¸ñ¸²À¸·Î Á¤ÂøµÇ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ÇÏȸ¸¶À» ¾Õ°ú °­ °Ç³Ê Á¡ »çÁÖÀÇ °æ¿ì Ÿ ³í¹®¿¡¼­ ±âÁ¦½ÃµÈ ¿©°Ç µîÀ¸·Î 2005³â Ç×°ø»çÁø¿¡¼­ ½Ä»ýÀÌÀÔÀº ¾ïÁ¦µÇ´Â °ÍÀ¸·Î º¸¿´Áö¸¸, 2009³â¿¡ ÃÔ¿µÇÑ »çÁø¿¡ »ó´ç ºÎºÐ È®´ëµÇ´Â °ÍÀ¸·Î ³ªÅ¸³ª ÀÌ¿¡ ´ëÇÑ ´ëÃ¥ÀÌ ÇÊ¿äÇÏ´Ù. »çÁÖ »ó ½Ä»ýÀÌÀÔÀÇ °¡¼ÓÈ­´Â ±¸´ã½ÀÁö µî ÀÚ¿¬ »óÅÂÀÇ ¸ð·¡ÇÏõ¿¡¼­ ã¾Æº¸±â ¾î·Á¿î µ¶Æ¯ÇÑ ¹èÈĽÀÁö¸¦ âÃâÇÏ¿© ȯ°æÀûÀ¸·Î Á¾ÀÇ ´Ù¾ç¼ºÀÌ Ä¿Á®¼­ ¼­½Äó·Î¼­ °¡Ä¡ ÀÚü´Â ³ô¾ÆÁú ¼ö ÀÖ´Ù. ¸¶Áö¸·À¸·Î, ´ï¿¡ ÀÇÇÑ È«¼ö·® °¨¼Ò¿Í ±×¿¡ µû¸¥ ÇÏ»ó¼Ò·ù·Â °¨¼Ò°¡ »çÁÖ »ó ½Ä»ýÀÌÀÔ ¹× È°ÂøÀ» °¡¼ÓÈ­½ÃÄ×´Ù´Â °¡¼³Àº ´ëÇ¥ ´Ü¸é¿¡¼­ ¹«Â÷¿ø ÇÏ»óÀü´ÜÀÀ·ÂÀÇ °ËÅä °á°ú È®ÀεǾú´Ù.
Changes of geomorphology in alluvial river and vegetation recruitment on its floodplain downstream from dams are investigated both qualitatively and quantitatively focusing on the downstream of Andong dam and Imha dam on the Nakdong River. Results of the analyses of river morphology and bed material in the study site show a general trend of riverbed degradation with a max scour of 3 m and bed material coarsening from pre-dam value of 1.5 mm in D50 to post-dam value of 2.5 mm. Decrease in bed shear stress due to the decrease in flood discharge have caused vegetation recruitment on the once-naked sandbars. As result, the ratio of area of vegetated bars over total area of bars has drastically changed from only 7% in 1971 before the Andong dam (constructed in 1976) to 25% after it, and increased to 43% only three year after the Imha dam (constructed in 1992) and eventually to 74% by 2005. Analysis of the vegetation succession at Wicjeol subreach, one of the three subreaches selected in this study for detailed investigation, has clearly shown a succession of vegetation on once-naked sand bars to a pioneering stage, reed and grass stage, willow shrub and eventually to willow tree stages. At the second subreach selected, two large point bars in front of Hahoe Village seem to have maintained their sand surfaces without a signifiant vegetation recruitment until 2005. The sand bars, however, seem to have been invaded by vegetation recently, which warns river managers to have a countermeasure to protect the sand bars from vegetation invasion in order to conserve them for the historical village of Hahoe. On the other hand, recruitment and establishment of vegetation on the sand bars by artificial disturbance of the river, such as damming, can create an unique habitat of backmarsh in the sandy river, as shown in the case of Gudam Wetland, and may increase the biodiversity as compared with relatively monotonous sand bars. Last, the premise in this study that decrease in flood discharge due to upstream dams and decrease in bed shear stress can induce vegetation recruitment on the naked sand bars in the river has been verified with the analyses of the distribution of dimensionless bed shear stress along the selected cross section in each subreach.
 
Ű¿öµå
ÃæÀûÇÏõ;´ï;½Ä»ýÀÌÀÔ;½Ä»ýõÀÌ;ÇÏ»óÀúÇÏ;ÇÏ»ó¼Ò·ù·Â;alluvial river;dam;vegetation recruitment;riverbed degradation;riverbed shear stress;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.43, no.5, 2010³â, pp.455-469
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO201016264960184)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
¸ñ·Ïº¸±â
ȸ»ç¼Ò°³ ±¤°í¾È³» ÀÌ¿ë¾à°ü °³ÀÎÁ¤º¸Ãë±Þ¹æÄ§ Ã¥ÀÓÀÇ ÇѰè¿Í ¹ýÀû°íÁö À̸ÞÀÏÁÖ¼Ò ¹«´Ü¼öÁý °ÅºÎ °í°´¼¾ÅÍ
   

ÇÏÀ§¹è³ÊÀ̵¿