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Çѱ¹½Ä¹°ÇÐȸ / v.28, no.2, 1985³â, pp.165-175
Áö¸®»ê ÇǾưñÀÇ ½Ä»ýÇü°ú ±× ±¸Á¶
( Vegetation Types and Their Structures of the Piagol, Mt. Chiri )
ÀåÀ±¼®;ÀÓ¾çÀç; Áß¾Ó´ëÇб³ ¹®¸®°ú´ëÇÐ »ý¹°Çаú;Áß¾Ó´ëÇб³ ¹®¸®°ú´ëÇÐ »ý¹°Çаú;
 
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Áö¸®»ê ÇǾưñÀÇ ½Ä»ýÀº ½Ä¹°»çȸÇÐÀû ¹æ¹ý¿¡ ÀÇÇØ °³¼­³ª¹«±º³«, ¼­³ª¹«±º³«, ½Å°¥³ª¹«±º³«, Á¹Âü³ª¹«±º³«, µé¸Þ³ª¹«±º³«, öÂß-Áø´Þ·¡ °ü¸ñ¸²À¸·Î ºÐ·ùµÇ¸ç, DBH-class ºÐÆ÷¿¡ ÀÇÇÏ¸é °³¼­³ª¹«±º³«, ¼­³ª¹«±º³«, ½Å°¥³ª¹«±º³«Àº ¸ðµÎ ¾ÈÁ¤µÈ ±Ø»ó¸²ÀÎ °ÍÀ¸·Î º¸ÀδÙ. ½Å°¥³ª¹«±º³«ÀÇ Á¾´Ù¾çµµ´Â Á¦ÀÏ ³·°í ¿ìÁ¡µµ´Â Á¦ÀÏ ³ô°Ô ³ªÅ¸³µÀ¸¸ç, Åä¾çÁ¶°ÇÀº ¼­³ª¹«±º³«ÀÌ ½Å°£³ª¹«±º³«¿¡ ºñÇØ ½ÀÇÏ°í ºñ¿ÁÇÑ °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ¼­³ª¹«±º³«°ú ½Å°¥³ª¹«±º³«ÀÇ Á¡ÀÌ´ë´Â DBH-class ºÐÆ÷·Î º¸¾Æ ÇöÀçÀÇ 900¡­1,000m ¿¡¼­ 1,000¡­l,100±îÁö À̵¿ÇÒ °ÍÀ¸·Î ¿¹ÃøµÈ´Ù. Polar Ordination¿¡ ÀÇÇÑ ½Ä»ýÇüÀÇ ºÐ·ù´Â ½Ä¹°»çȸÇÐÀû ¹æ¹ýÀÇ °á°ú¿Í ÀÏÄ¡Çß´Ù. °íµµ±¸¹è¸¦ µû¶ó °³¼­³ª¹«´Â 500¡­700m, ¼­³ª¹«´Â 700¡­900m, ½Å°¥³ª¹«´Â 900mÀ̻󿡼­ ÃÖ°íÀÇ Áß¿äÄ¡¸¦ ³ªÅ¸³½´Ù. RaunkiaerÀÇ life-form spectrumÀ» ³²ÇÑÀÇ °Í°ú ºñ±³Çϸé, ¹ÝÁöÁ߽ŰÀº 5.3%, ÁöÁ߽ŰÀº 5.2% ³ô°Ô ³ªÅ¸³µÀ¸¸ç, Âø»ý½Ä¹°°ú ¼öÁ߽ŰÀº ±ØÈ÷ Àû°Ô ³ªÅ¸³µ´Ù.
The natural forest vegetation of the Piagol, Mt. Chiri, was classified into five major communities, i.e. Quercus mongolica, Carpinus laxiflora, C. tschonoskii, Q. serrata and Fraxinus mandshurica community. C. tschonoskii, C. laxiflora and Q. mongolica characteristically were dominated in the range of 500¡­700 m, 700¡­900 m and 900¡­1,400 m in altitude, respectively. Abies nephrolepis and Rhododendron schlippenbachii in the ridge of Nogodan-Nalnaribong, and F. mandshurica and Q. serrata in the Yongsuam ravine were found as the dominant species. The transition between C. tschonoskii and C. laxiflora communities was relatively wide. The boundary between F. mandshurica, in the conglomerated zone, and the other communities surrounding its community was fairly abrupt. In Q. mongolica community, the canopy was relatively opened and the oak young tree of undergrowth was fairly dense. In the community of C. laxiflora and C. tschonoskii, the species composed of their understory was rich while their coverage was lower than that of Q. mongolica community. Shannon's diversity index was decreased in order of C. tschonoskii, C. laxiflora and Q. mongolica community, while their Simpson's dominance index increased conversely. Judging by the DBH-class distribution showing the negative exponential curve, these communities were considered as the climax forest. In Polar Ordination used samples (quadrats), the vegetation of the Piagol was divided into five groups, which was coincided with five communities classified by Braun-Blanquet system. In the ordination, the first axis and the second axis may be considered soil conditions and thermal conditions, respectively. It seems that two different methods, phytosociological method in macro level and ordination techniques in micro level, are useful for the vegetation classification.
 
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Journal of Plant Biology / v.28, no.2, 1985³â, pp.165-175
Çѱ¹½Ä¹°ÇÐȸ
ISSN : 1226-9239
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198511922411476)
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