¶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

Çѱ¹È¯°æ»ýÅÂÇÐȸ / v.22, no.6, 2008³â, pp.658-665
ÃæÀûÇÏõ »çÇàÇϵµ¿¡ ¹ß´ÞÇÑ »çÁÖ¿¡¼­ÀÇ ½Ä»ýÇü¼º °úÁ¤¿¡ °üÇÑ ¿¬±¸
( A Study on the Expansion Process of Vegetation on Sand-bars in Fluvial Meandering Stream )
ÀÌ»ïÈñ;¿Á±â¿µ;ÃÖÁ¤±Ç; Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ÇÏÃµÇØ¾È¿¬±¸½Ç;ÀϺ» ±³Åä´ëÇб³ °øÇבּ¸°ú;°æ¿ø´ëÇб³ µµ½Ã°èȹÁ¶°æÇкÎ;
 
ÃÊ ·Ï
ÃæÀûÇÏõÀÇ ÀÌÁß ¸¸°îºÎÁöÇü¿¡ À§Ä¡ÇÑ ³«µ¿°­ ÇÏȸ¸¶À»Àº Çѱ¹³» ´ëÇ¥ÀûÀÎ À̵¿»ó ¸ð·¡»çÁÖ ±¸°£ÀÌ´Ù. ±×·¯³ª »ó·ù¿¡ ´ïÀÌ °Ç¼³µÈ ÀÌÈÄ Ã·µÎÀ¯·®ÀÌ Á¶ÀýµÇ°í À¯»ç·® °ø±ÞÀÌ °¨¼ÒÇϸ鼭, ÇÏȸ¸¶À»±¸°£¿¡¼­´Â ¸ð·¡»çÁÖÀÇ À̵¿¼º ÀúÇÏ, »çÁÖÀÇ ½Ä»ýÁ¤Âø ¹× ½Ä»ý¿ªÀÌ È®ÀåÇö»óÀÌ ³ªÅ¸³ª¸é¼­ »çÁÖ°¡ °íÁ¤È­µÇ°í ÀÖ´Ù. ÀÌ·¯ÇÑ Çö»óÀº ´ïÇÏ·ù¿¡ Á¸ÀçÇÏ´Â ÇÏõÀÇ ´ëÇ¥ÀûÀÎ Çö»óÀ¸·Î¼­ ±¹³» ¿ÜÀûÀ¸·Î Çϵµ³» »çÁÖ¿Í ½Ä»ý¿¡ ´ëÇÑ Ã¼°èÀûÀÎ ¿¬±¸¿Í °ü¸®ÀÇ Çʿ伺ÀÌ Áõ°¡Çϰí ÀÖ´Ù. º» ¿¬±¸´Â ³«µ¿°­ ÇÏȸÁö±¸¿¡¼­ ¸ð·¡»çÁÖÀÇ ÁöÇüº¯È­¿¡ µû¸¥ ¿øÀΰú ½Ä»ý¿ªÀÇ È®Àå°úÁ¤À» ÆÄ¾ÇÇϱâ À§ÇÑ °ÍÀ¸·Î, ¼ö¸®, ÁöÇü, Åä¾çÀÇ ÀÌÈ­ÇÐÀû Ư¼º, ½Ä»ýÁ¶»ç µîÀ» ½Ç½ÃÇÏ¿´´Ù. ¿¬±¸°á°ú¿¡ µû¸£¸é È«¼ö±â µ¿¾È ¸¸°îºÎ ³»Ãø¿¡ ¿ö½Ã·Îµå¿Í ºÎÀ¯»çÀÇ ÅðÀûÀÛ¿ëÀ¸·Î ¿µ¾ç¹°ÁúÀÇ ÇÔ·®ÀÌ ³ôÀº ¸ÅÆ®¸¯½º°¡ Çü¼ºµÇ¸é¼­ ¼±±¸½Ä¹°ÀÇ Ä§ÀÔÇÏ°Ô µÇ°í, ÀÏÁ¤±â°£ÀÇ ¹«È«¼ö ±â°£À» °ÅÄ¡´Â µ¿¾È õÀ̰úÁ¤À» °ÅÃÄ »çÁֽĻýÀÌ Á¤ÂøÇÏ°Ô µÇ¸ç, ÀÌÈÄ ¹Ýº¹ÀûÀÎ È«¼ö´Â ½Ä»ýÁ¤ÂøºÎÀÇ À¯»çÅðÀûÀ» ÃËÁøÇÏ°Ô µÇ¸é¼­ °á°úÀûÀ¸·Î Å伺ÀÇ º¯È­¸¦ °¡Á®¿À¸é¼­ ½Ä»ý¿ªÀÇ È®ÀåÀ» À¯¹ßÇÏ°Ô µÈ´Ù´Â ¸ÞÄ«´ÏÁòÀ»È®ÀÎÇÒ ¼ö ÀÖ¾ú´Ù. ÀÌ´Â ¸ð·¡»çÁÖ¿¡¼­ ½Ä»ý¿ªÀÇ È®Àå°úÁ¤ÀÌ ¹Ýº¹ÀûÀÎ È«¼ö±â¿Í ºñÈ«¼ö±âÀÇ ÃâÇö°ú À¯»çÀ̼Û, ±×¸®°í Åä¾çÀÇ ¿µ¾ç¹°Áú ÇÔ·®°ú ¹ÐÁ¢ÇÑ °ü°è¸¦ °¡Áö°í ÀÖÀ½À» ³ªÅ¸³½´Ù.
One of the characteristics of fluvial river channel with sand bed-material is the existence of movable sand bars not occupied with vegetation. However, sand bars at the Hahoe's reach of the Nakdong River showing a double-meandering channel has been changed into expanding vegetation area. Moreover, sand material, in recent years, has stopped moving to downstream in channel and the number and area of bare bars which did not occupied by vegetation have been decreased. In order to find out the mechanism, we carried out the channel characteristics surveys such as hydro-geomorphologic, soil physio-chemical and vegetation surveys were conducted twice on autumn season in 2005,2006. The results so far achieved showed that the reduced discharge of transported sediment and duration of dry season might be critical factors for the spread of luxuriant vegetation. The vegetation area was significantly expanded by floods exceeding the subsequent dominant flow discharge. Furthermore, the expansion of vegetation area was highly correlated with the supply of organic matter, nutrients and alteration of soil texture by sediment deposition during the flooding event.
 
Ű¿öµå
ÇÏȸ¸¶À»;À̵¿»çÁÖ;½Ä»ý;Åä¾ç¿µ¾ç¹°Áú;³«µ¿°­;HAHOE-VILLAGE;VEGETATION;MOVABLE SANDBAR;SOIL NUTRIENTS;NAKDONG RIVER;
 
Çѱ¹È¯°æ»ýÅÂÇÐȸÁö / v.22, no.6, 2008³â, pp.658-665
Çѱ¹È¯°æ»ýÅÂÇÐȸ
ISSN : 1229-3857
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200807653005297)
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¿