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Çѱ¹È¯°æ»ýÅÂÇÐȸ / v.16, no.2, 2002³â, pp.141-148
»êÈ­°¡ Ãʺ»ÃþÀÇ ¹ß»ø ¹× Åä¾çÀÇ È­ÇÐÀû Ư¼º¿¡ ¹ÌÄ£ ¿µÇâ
( Effects of Forest Eire on Herb Layer Development and Chemical Properties of Soil )
¹Ú°ü¼ö;À̹ÌÁ¤;¼ÛÈ£°æ; Ãæ³²´ëÇб³ »ê¸²ÀÚ¿øÇаú;Ãæ³²´ëÇб³ »ê¸²ÀÚ¿øÇаú;Ãæ³²´ëÇб³ »ê¸²ÀÚ¿øÇаú;
 
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º» ¿¬±¸´Â »êÈ­°¡ Ãʺ»ÃþÀÇ ¹ß»ý ¹× Åä¾çÀÇ È­ÇÐÀû Ư¼º¿¡ ¹ÌÄ£ ¿µÇâÀ» Á¶»çÇϱâ À§ÇØ 2000³â 4¿ù ´ëÀüÀÇ °èÁ·»ê¿¡¼­ ¹ß»ýÇÑ »êÈ­Áö¸¦ ´ë»óÀ¸·Î ½Ç½ÃµÇ¾ú´Ù. ½Ä»ýÁ¶»ç´Â °õ¼Ö¿ìÁ¡¸² (ħ¿±¼ö¸²)°ú ¾Æ±î½Ã³ª¹«¿ìÁ¡¸²(Ȱ¿±¼ö¸²)¿¡¼­ 10m$ imes$10mÀÇ ¹æÇü±¸¸¦ ¼³Ä¡ÇÏ¿© ½Ç½ÃÇÏ¿´°í, Ãʺ»ÃþÀÇ ¹ß»ýÁ¶»ç´Â 7¿ù 21ÀÏ DierssenÀÇ ¿ìÁ¡µµ¹ýÀ» Àû¿ëÇÏ¿© ½Ç½ÃµÇ¾ú´Ù. Ãʺ»ÃþÀÇ Çǵµ´Â ħulcornerȰ¿±¼öÁö¿ª ¸ðµÎ¿¡¼­ »êÈ­Áö°¡ ºñ»êÈ­Áöº¸´Ù ³ô¾ÒÀ¸¸ç, ÃâÇöÁ¾¼ö´Â »êÈ­Áö¿Í ºñ»êÈ­ÁöÀÇ Â÷À̺¸´Ù ħulcornerȰ¿±¼ö °£¿¡ Â÷À̰¡ ´õ ³ô¾Ò´Ù Åä¾ç ½Ã·á´Â ºñ»êÈ­Áö, ±×¸®°í »êÈ­Áö¿¡¼­ »êÈ­ 3ÀÏ ÈÄ ±×¸®°í »êÈ­ 8°³¿ù ÈÄ¿¡ 0¢¦10cm¿Í 10¢¦20cm Åä¾ç±íÀÌ¿¡¼­ äÃëµÇ¾ú´Ù. Åä¾ç À¯±â¹°ÃþÀº ºñ»êÈ­Áö¿¡¼­´Â ±íÀ̰¡ ¾à 1.5cmÀ̾úÀ¸³ª »êÈ­Áö¿¡¼­´Â À¯±â¹°ÃþÀÌ ¾ø¾ú´Ù. »êÈ­ ¹ß»ý 3ÀÏ ÈÄ »êÈ­Áö¿Í ºñ»êÈ­Áö °£ÀÇ Åä¾ç À¯±â¹°, ÀüÁú¼Ò, À¯±âÀλê, ġȯ¼º ¾çÀÌ¿ÂÇÔ·®, pH¹× CEC´Â À¯ÀÇÀûÀÎ Â÷À̰¡ ¾ø´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ¶ÇÇÑ »êÈ­Áö¿¡¼­ »êÈ­ 3ÀÏ ÈÄ¿Í ¾à 8°³¿ù ÈÄÀÇ Åä¾çÀÇ È­ÇÐÀû Ư¼ºµéÀº ÀϺθ¦ Á¦¿ÜÇϰí´Â À¯ÀÇÀûÀÎ Â÷À̰¡ ¾ø¾ú´Ù.
This study was carried out to estimate the effect of forest fire on herb layer development and chemical properties of soil. The forest fire was in April 2000 in Pinus rigida(softwood) and Robinia pseudoacacia(hardwood) dominant forests at Gaejoksan, Daejeon. Vegetation studies were in the two communities and herb layer development study was in July using dominance of Dierssen. The coverage of herb layer was higher in the burned area than in the unburned area in the two study communities. There was no different herb layer species number between the burned and unburned areas, but there was different herb layer species number between the two communities. Soil samples were collected at 0¢¦10cm and 10¢¦20cm soil depths from the unburned and burned sites after 3 days and 8 months of forest fire. There was no forest floor in burned site, but unburned site has the forest floor of 1.5cm thick. There were no significant differences in soil organic matter, total N, available P, exchangeable K, Ca, Na, and Mg, and CEC, pH in all soil depth, between unburned and burned sites after 3 days of forest fire and between burned site after 3 days and 8 months of forest fire, except in organic matter in 10¢¦20cm soil depth in hardwood sites and in exchangeable Ca in the 10¢¦20cm soil depth, and in Mg in the two soil depths in hardwood sites. It seems to be that forest fire had not changed the chemical soil properties in this study.
 
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»êºÒ;°èÁ·»ê;½Ä»ý;Åä¾çÀ¯±â¹°;FOREST FIRE;GAEJOKSAN;VEGETATION;SOIL ORGANIC MATTER;
 
Çѱ¹È¯°æ»ýÅÂÇÐȸÁö / v.16, no.2, 2002³â, pp.141-148
Çѱ¹È¯°æ»ýÅÂÇÐȸ
ISSN : 1229-3857
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200211921389981)
¾ð¾î : Çѱ¹¾î
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