¶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

Çѱ¹Á¶°æÇÐȸ / v.37, no.6, 2010³â, pp.96-105
źõ Çϵµ»çÁÖÀÇ ÁöÇü Çü¼º°úÁ¤°ú ½Ä»ýºÐÆ÷ ¿¬±¸
( A Study of the Geomorphological Process and Vegetation Distribution of Sand-bars on the Tan-cheon River )
Ãֹ̰æ;ÀÌ»ïÈñ;ÃÖÁ¤±Ç; Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼öÀÚ¿øÈ¯°æ¿¬±¸º»ºÎ;Çѱ¹°Ç¼³±â¼ú¿¬±¸¿ø ¼öÀÚ¿øÈ¯°æ¿¬±¸º»ºÎ;°æ¿ø´ëÇб³ Á¶°æÇаú;
 
ÃÊ ·Ï
º» ¿¬±¸´Â ÇÏõ °æ°ü¿ä¼Ò Áß¿¡¼­ ºñ±³Àû ´Ü½Ã°£¿¡ °ÉÃÄ º¯È­ÇÏ´Â »çÁÖ ÁöÇü°ú ½Ä»ý ºÐÆ÷ÀÇ ¿ªµ¿Àû Çü¼º°úÁ¤À» ¹àÈ÷±â À§ÇØ ¼öÇàµÇ¾úÀ¸¸ç, ¿¬±¸ ´ë»ó ÇÏõÀº 2002³â ÀÌÈÄ »ýŰ躸ÀüÁö¿ªÀ¸·Î °ü¸®µÇ°í Àִ źõ ÇÏ·ùºÎ ±¸°£ÀÌ´Ù. À̸¦ À§Çؼ­ »çÁÖÁöÇüÀÇ º¯È­´Â Ç×°ø»çÁø°ú °æ°ü»çÁøÀ» ÅëÇØ ±× Çü¼º°úÁ¤À» ÆÄ¾ÇÇϰí ÇöÀç »çÁÖ ÁöÇü À§¿¡ Çü¼ºµÈ ½Ä»ýÀÇ ºÐÆ÷¸¦ ÇöÀåÁ¶»ç¸¦ ÅëÇØ ºÐ¼®ÇÏ¿´´Ù. ºÐ¼®ÇÑ ¿¬±¸ °á°ú´Â ´ÙÀ½°ú °°´Ù. ù°, 1980³â´ë ÈĹݿ¡ Á÷°­È­ µÇ¾ú´ø Çϵµ ³»¿¡¼­ 1990³â´ë¿¡ µé¾î »çÁÖÀÇ ¹ß´ÞÀÌ ÇöÀúÇÏ¿© ´Ù¾çÇÑ ÇüÅÂÀÇ »çÁÖ°¡ Çü¼ºµÇ¾ú°í ÀÌ´Â Áö¼ÓÀûÀ¸·Î º¯È­ÇÏ¿´´Ù. Ãʱ⿡ »çÁÖ°¡ Çü¼ºµÇ°í ½Ã°£ÀÌ °æ°úÇÔ¿¡ µû¶ó, Çϵµ ³» È帧 Ư¼º¿¡ µû¶ó »çÁÖÀÇ ¸éÀû°ú ³ôÀ̰¡ º¯ÇÏ¿´´Ù. µÑ°, ½Ä»ýÀÇ ºÐÆ÷¿¡ À־´Â ¹°°ú Á¢ÃË ºóµµ°¡ ³ôÀº ÇϾȺδ ±³¶õÀÇ Á¤µµ°¡ ½ÉÇϱ⠶§¹®¿¡ ¹«½Ä»ý »óÅÂÀ̰ųª, °£ÇæÀûÀÎ ½Ä»ýÀÌ ºÐÆ÷ÇÏ¿© Çǵµ°¡ ³·°Ô ³ªÅ¸³µÀ¸¸ç, °í¼öºÎÁö ÂÊÀ¸·Î Çü¼ºµÈ »çÁÖ¿¡´Â ¸ñº»·ù³ª Á¤¼ö½Ä¹°±º¶ôÀÌ È°ÂøµÇ¸é¼­ ½Ä»ý Çǵµ°¡ ³ô°Ô ³ªÅ¸³ª ¾ÈÁ¤½Ä»ý¿ªÀ» Çü¼ºÇÏ¿´´Ù. ¼Â°, »çÁÖ¿Í ½Ä»ýÇü¼º°úÁ¤ÀÇ °ü°è´Â »çÁÖÀÇ ÇüÅÂ¿Í ½Ä»ýÀÇ ¾ÈÁ¤¼º ¿©ºÎ¿¡ µû¶ó Àú¼ö·Îº¯ »çÁÖ, ºÒ¾ÈÁ¤ ½Ä»ý Àú¼ö·Îº¯»çÁÖ, ¾ÈÁ¤½Ä»ý ÇÏÁßÁÖ ±×¸®°í ºÒ¾ÈÁ¤½Ä»ý ÇÏÁßÁÖ 4°¡Áö À¯ÇüÀ¸·Î ³ªÅ¸³µ´Ù. º» ¿¬±¸¸¦ ÅëÇØ ¹àÈù Çϵµ ³» »çÁÖ¿Í ÇÏõ½Ä»ýÀÇ Çü¼º°úÁ¤¿¡ À־ÀÇ »óÈ£°ü°è´Â ¸ð·¡ÇÏ»óÀÇ ÇÏõºÎÁö¿¡¼­ ½Ä¹°Á¾À̳ª ½ÄÀçÀ§Ä¡ ¼±Á¤¿¡ À¯¿ëÇÒ °ÍÀ̳ª, ÇÏõ»ýÅÂ°è º¹¿øÀ» À§ÇÑ ½ÇÇà»ç¾÷ÀÇ ½ÄÀç ÁöħÀ¸·Î Ȱ¿ëµÇ±â À§Çؼ­´Â ´Ù¾çÇÑ Æ¯¼ºÀ» Áö´Ñ ÇÏõ¿¡ ´ëÇÑ º¸´Ù Æø ³ÐÀº »ç·Ê¿¬±¸°¡ µÞ¹ÞħµÇ¾î¾ß ÇÒ °ÍÀÌ´Ù.
This study identified the dynamic process of sandbar and vegetation distribution of the sandbar on the Tan-cheon River. The study area is located in the lower reaches of the Tan-cheon River that has been managed as an Ecosystem Reserve Area since 2002. For the study, the geomorphological process was analyzed through mapping analysis using a satellite image followed by analysis of the vegetation distribution through an on-site survey. The major findings were as follows : First, In the fluvial geomorphic process, various kinds of sandbars were developed in 1990s, the morphologic characteristics changing continuously. Second, In the distribution of vegetation on the sandbar, the sandbar shore was covered with bare sand substrate or intermittent annual vegetation because of the periodic fluctuation of the water-level due to intensive disturbances. Third, In the relationship between the sandbar formation and vegetation, four types of sandbars were classified: channel-shore stable bar, channel-shore unstable bar, mid-channel stable bar and mid-channel unstable bar, according to the fluvial disturbance & vegetation process. The study verifies that the vegetation distribution is reciprocally related to the geomorphological process. Accordingly, it is meaningful in the selection of plant species and the planting area of the sand bar. However, it is limited to the planting guidelines on river restoration projects. More diverse on-site experimental studies should be conducted.
 
Ű¿öµå
±³¶õ;ÇÏõº¯ ½Ä»ý;½Ã°ø°£Àû ôµµ;ÀûÀÀ°ü¸®;Disturbance;Riparian Vegetation;Spatial and Temporal Scale;Adaptive Management;
 
Çѱ¹Á¶°æÇÐȸÁö / v.37, no.6, 2010³â, pp.96-105
Çѱ¹Á¶°æÇÐȸ
ISSN : 1225-1755
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO201017337333735)
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¿