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Çѱ¹È¯°æ»ýÅÂÇÐȸ / v.23, no.4, 2009³â, pp.365-375
°íâ ±¸½ÃÆ÷ ÇØ¾È °õ¼Ö¸²ÀÇ »ýÀ寝¼º¿¡ °üÇÑ ¿¬±¸
( Study on Growth Characteristics of Pinus thunbergii Windbreak Forests around Goosipo Beach, Gochang-Gun )
¹ÚÁ¾¹Î;±è¼º¿ø;¹Ú¼ºÇÐ; ÀüºÏ´ëÇб³ »ê¸²ÀÚ¿øÇаú;Àü¶óºÏµµ °íⱺ »ê¸²ÇàÁ¤°ú;ÀüºÏ´ëÇб³ ´ëÇпø ÀÓÇаú;
 
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Àü¶óºÏµµ °íⱺ »óÇÏ¸é ±¸½ÃÆ÷ÇØ¼ö¿åÀå ÁÖº¯¿¡ À§Ä¡ÇÑ °õ¼Ö ¹æÇ³¸²À» ´ë»óÀ¸·Î °õ¼Ö¸²ÀÇ »ýÀ寝¼ºÀ» Á¶»ç ÇÏ¿´´Â ¹Ù, ±× °á°ú¸¦ ¿ä¾àÇÏ¸é ´ÙÀ½°ú °°´Ù. °õ¼Ö¸²ÀÇ Åä¾çÀº ¸ð·¡ÀÇ ÇÔ·®ÀÌ ¸¹Àº »çÅäÀ̰í, ¾à»ê¼º(pH 5.73)À̸ç, Åä¾ç¿°ºÐ³óµµ´Â 1.42dS/mÀÌ´Ù. °õ¼ÖÀÇ Èä°íÁ÷°æ, ¼ö°í, ¼ö°üÆø, Çü»óºñ(¼ö°í/Èä°íÁ÷°æ)´Â Àú¹Ðµµ ÀÓºÐ, Á߹еµ ÀÓºÐ, °í¹Ðµµ ÀÓºÐÀÇ ¼øÀ¸·Î ¾çÈ£ÇÏ¿´°í, Àý°£»ýÀå·®Àº °í¹Ðµµ ÀÓºÐÀϼö·Ï ¸¹¾Ò´Ù. ƯÈ÷ Àú¹Ðµµ ÀÔ¸ñ¹Ðµµ°¡ ³·À»¼ö·Ï ¼ö°üÆøÀÌ Å©°í, Çü»óºñ 60 ÀÌÇÏÀÎ ¼ö¸ñÀÇ ºñÀ²ÀÌ ¸¹¾Ò´Ù. À̰ÍÀº ÀÔ¸ñ¹Ðµµ°¡ ³·À»¼ö·Ï ¼ö¸ñÀÌ °ÇÀüÇÏ°Ô »ýÀåÇϰí ÀÖÀ½À» ³ªÅ¸³»´Â °ÍÀÌ´Ù. ¸¹Àº ¼ö¸ñÀÌ ¿©·¯ ¹æÇâÀ¸·Î ±â¿ï¾îÁ® »ýÀ°Çϰí Àִµ¥, À̰ÍÀº ´ëºÎºÐÀÇ ¼ö¸ñÀÌ »ýÀå Ãʱ⠴ܰ迡 ¹Ù¶÷ÀÇ ¿µÇâÀ» ¹ÞÀº °ÍÀ̰í ÀϺδ ÅÂdzÀÇ ¿µÇâÀ» ¹ÞÀº °ÍÀ¸·Î ºÐ¼®µÇ¾ú´Ù. ¼ö¸ñÀÇ ±â¿ï±â ¹æÇâÀÇ ºÐÆ÷À²ÀÌ ÀÌ Áö¿ªÀÇ ÁÖdz¹æÇâ°ú »ó°ü¼ºÀÌ ÀÖ´Â °ÍÀ¸·Î ºÐ¼®µÇ¾ú´Ù. ÀÌ Áö¿ªÀÇ ¸ð·¡¾ð´ö°ú °õ¼Ö¸² ³»ºÎ¿¡´Â ÃÑ 81ºÐ·ù±ºÀÇ °ü¼Ó½Ä¹°ÀÌ »ýÀ°Çϰí ÀÖÀ¸¸ç, ¸ñº»½Ä¹°(24ºÐ·ù±º)º¸´Ù Ãʺ»·ù(57ºÐ·ù±º)°¡ ´õ ¸¹¾Ò´Ù. »ç±¸½Ä¹°ÀÇ °æ¿ì ¸ð·¡¾ð´öÀÌ Àß ¹ß´ÞÇØ ÀÖ´Â ¸í»ç½Ê¸® ±¸¿ª¿¡´Â 10Á¾·ù°¡ ÃâÇöÇÏ¿´´Âµ¥, ¹æÆÄÁ¦ ÃàÁ¶·Î ÀÎÇØ ¸ð·¡¾ð´öÀÌ Çü¼ºµÇÁö ¾ÊÀº ±¸½ÃÆ÷ÇØ¼ö¿åÀå ±¸¿ªÀº 3Á¾ÀÇ »ç±¸½Ä¹°¸¸ÀÌ °£ÇæÀûÀ¸·Î ÃâÇöÇÏ¿´´Ù. ÀÌ Áö¿ªÀÇ °õ¼Ö¸²ÀÌ °ÇÀüÇÏ°Ô ¼ºÀåÇϰí À¯ÁöµÇ¾î ÇØ¾È¹æÇ³¸²À¸·Î¼­ÀÇ ±â´ÉÀ» ÃæºÐÈ÷ ¹ßÈÖÇÒ ¼ö ÀÖ°Ô Çϱâ À§Çؼ­´Â °í¹Ðµµ¿Í Á߹еµ ÀӺп¡ ´ëÇÑ ÀûÁ¤ÇÑ °£¹úÀÌ ÇÊ¿äÇÑ »óÅÂÀÌ´Ù.
The growth characteristics of Pinus thunbergii windbreak forest around Goosipo Beach, Sangha-Myon, Gochang-Gun, Jeollabuk-Do have been investigated, and the results are summarized as follows. The soil in the site was light acid sand with pH 5.7, and the mean sodium concentration of soils was 1.42dS/m. The tree diameter, height, crown width, and shape ratio(Height/DBH) were better with tree density was coming lower. Especially, the rate of shape ratio under 60 was more in sites with low tree density. This demonstrated that the trees have grown more soundly when the tree density was lower. The direction of main winds and distribution ratio of tree inclination had a correlation. The inclined trees are seemed to be influenced by main winds when they were younger and by Typhoon partly. Eighty one vascular plant species were found in the sites, and more number of herbaceous plants (57 taxa) lived there than woody plants (24 taxa). And more plant species of dune were found at the site where dune have developed well. Some thinning works need at high tree density areas in order to ensure effects of coastal windbreak.
 
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Çü»óºñ;ÀÔ¸ñ¹Ðµµ;¼ö¸ñ±â¿ï±â;Àý°£»ýÀå;ÇØ¾È»ç±¸;SHAPE RATIO;TREE DENSITY;TREE INCLINATION;ANNUAL GROWTH;COASTAL DUNE;
 
Çѱ¹È¯°æ»ýÅÂÇÐȸÁö / v.23, no.4, 2009³â, pp.365-375
Çѱ¹È¯°æ»ýÅÂÇÐȸ
ISSN : 1229-3857
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200933063797707)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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