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Çѱ¹È¯°æ»ýÅÂÇÐȸ / v.24, no.1, 2010³â, pp.26-36
ÇѶó»ê±¹¸³°ø¿ø µ¿»ç¸éÀÇ ÇØ¹ß°íº° ½Ä»ýº¯È­ ¹× ±¸Á¶
( The Change and Structure of Altitudinal Vegetation on the East Side of Hallasan National Park )
ÀÌ»óö;ÃÖ¼ÛÇö;°­Çö¹Ì;Á¶Çö¼­;Á¶Àç¿ì; ºÎ»ê´ëÇб³ ´ëÇпø Á¶°æÇаú;ºÎ»ê´ëÇб³ Á¶°æÇаú;(À¯)À̾ؿ¤À¯Åä;ÁøÁÖ»ê¾÷´ëÇб³ »ê¸²ÀÚ¿øÇаú;ºÎ»ê´ëÇб³ Á¶°æÇаú;
 
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ÇѶó»ê±¹¸³°ø¿ø µ¿»ç¸é¿¡ À§Ä¡ÇÑ ¼ºÆÇ¾Ç ޹æ·Î¸¦ µû¶ó ÇØ¹ß°íº°·Î ½Ä»ý±¸Á¶¿Í º¯È­¸¦ ÆÄ¾ÇÇϱâ À§ÇÏ¿© ÇØ¹ß 750m ¿¡¼­ 1,450m±îÁö 17°³ Á¶»ç±¸(´ÜÀ§¸éÀû $400m_2$)¸¦ ¼³Ä¡ÇÏ¿© Á¶»ç¸¦ ½Ç½ÃÇÏ¿´´Ù. Classification ±â¹ýÁß ÇϳªÀÎ TWINSPANÀ» ÀÌ¿ëÇÏ¿© ±º¶ôºÐ¸®¸¦ ½ÃµµÇϰí, ordination ±â¹ýÁß DCAºÐ¼®À» ½Ç½ÃÇÏ¿© º¸¿ÏÇÑ °á°ú, ±º¶ô IÀº °³¼­ ¾î³ª¹«-¶§Á׳ª¹«±º¶ô, ±º¶ô II´Â ¶§Á׳ª¹«-Á¹Âü³ª¹«±º¶ô, ±º¶ô IIIÀº °³¼­¾î³ª¹«-Á¹Âü³ª¹«±º¶ô, ±º¶ô W´Â ½Å°¥³ª¹«-°³¼­¾î³ª¹«±º¶ô, ±º¶ô V ´Â ´ç´Üdz³ª¹«±º¶ô ±×¸®°í ±º¶ô WÀº ½Å°¥³ª¹«-±¸»ó³ª¹«±º¶ôÀÇ 6°³ÀÇ ±º¶ôÀ¸·Î ºÐ¸®µÇ¾ú´Ù. ÇØ¹ß°íº°·Î Á¾Á¶¼ºÀ» »ìÆìº» °á°ú ±º¶ôÀÇ Á¾Á¶¼ºÀÌ ÇØ¹ß 1,000m ÀÌÇÏÀÇ Áö¿ª¿¡¼­´Â ¿¬¼ÓÀûÀÌÁö¸¸ 1,000m ÀÌ»óÀÇ Áö¿ª¿¡¼­´Â ºÒ¿¬¼ÓÀûÀ¸·Î ³ªÅ¸³ª ÇѶó»ê±¹¸³°ø¿ø µ¿»ç¸éÁö¿ªÀº ÇØ¹ß 1,000m¸¦ Áß½ÉÀ¸·Î ½Ä»ýÀÇ º¯È­°¡ ¶Ñ·ÇÇÑ Æ¯Á¤À» ³ªÅ¸³»´Â °ÍÀ» ¾Ë ¼ö ÀÖ¾ú´Ù. º» Á¶»çÁö¿ªÀÇ »ê¸²½Ä»ýÀÇ ÀÓ·ÉÀº ¿¬·ûºÐ¼®°á°ú 50¿©³âÀ» »óȸÇÏ´Â °ÍÀ¸·Î ¹àÇôÁ³´Ù.
The purpose of this study is to investigate the change and structure of the altitudinal vegetation on the east side of Hallasan National Park, and to accomplish this research, seventeen plots($400m_2$ per zone) were set up along the Seongpanak trail starting from 750m to 1,450m(which was 700m long). These zones, according to the two-way indicator species analysis(TWINSPAN) and ordination analysis(DCA), were divided into six communities: Carpinus tschonoskii-Stryrax japonica community(I), Stryrax japonica-Quercus serrata community(II), Carpinustschonoskii-Q. serrata community(III), Q. mongolica-C tschonoskii community(IV), Acer pseudosieboldianum community(V), and Q. mongolica-Abies koreana community(VI). The findings of my investigation are as follows: the altitudinal vegetation structure of all the investigated zones from 750m to 1,000m above sea level is similar to one another, whereas the same zones from 1,000m to 1,450m above sea level showed dissimilarities among them. That indicates that altitudinal vegetation structure on the east side of Hallasan National Park has changed drastically at the 1,000m areas above sea level, and the forest age of this area is over 50 years.
 
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¼ºÆÇ¾Ç޹æ·Î;TWINSPAN;DCA;SEONGPANAK TRAIL;
 
Çѱ¹È¯°æ»ýÅÂÇÐȸÁö / v.24, no.1, 2010³â, pp.26-36
Çѱ¹È¯°æ»ýÅÂÇÐȸ
ISSN : 1229-3857
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO201022442398099)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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