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Çѱ¹»ýÅÂÇÐȸ / v.20, no.5, 1997³â, pp.385-391
»ç¹®¾Ï Áö¿ª¿¡¼­ »ýÀ°ÇÏ´Â ´ë³ª¹°(Gypsophila oldhamiana)ÀÇ Áß±Ý¼Ó ÇÔ·®
( Heavy Metal Contents of Gypsophila oldhamiana Growing on Soil Derived from Serpentine )
±è¸íÈñ;¹ÎÀϽÄ;¼Û¼®È¯; ÁߺδëÇб³ ¿ø¿¹Çаú;ÁߺδëÇб³ »ê¸²ÀÚ¿øÇаú;°í·Á´ëÇб³ Áö±¸È¯°æ°úÇаú;
 
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Ãæ³² ±¤Ãµ°ú È«¼º ÀÏ´ëÀÇ »ç¹®¾Ï°ú º¯¼º¾Ï Áö¿ªÀÇ ¾Ï¼®, Åä¾ç ¹× ÃâÇöºóµµ°¡ ³ôÀº ´ë³ª¹°ÀÇ Áß±Ý¼Ó ÇÔ·®À» ÃøÁ¤ÇÏ¿© »ç¹®¾Ï Åä¾çÀÇ µ¶¼ºÈ­ Á¤µµ¿Í ½Ä¹°Ã¼ÀÇ Èí¼ö°ü°è¸¦ Á¶»çÇÏ¿´´Ù. Ni, Cr ¹× Co´Â »ç¹®¾Ï¿¡ ¸Å¿ì ³ô¾ÒÀ¸¸ç Zn, Sc, Mo ¹× Fe ´Â º¯¼º¾Ï¿¡¼­ ´õ ³ô¾Ò´Ù. »ç¹®¾Ï dzȭÅä¿¡¼­´Â Ni, Cr ¹× Co°¡ ³ô¾ÒÀ¸¸ç Zn°ú Fe´Â ºñ»ç¹®¾Ï dzȭÅä(»ç¹®¾Ï ¹× º¯¼º¾Ï dzȭÅä¿Í º¯¼º¾Ï dzȭÅä)¿¡¼­ ³ô¾Ò°í, Åä¾çÀÇ Á߱ݼÓÀº ¾Ï¼®³»ÀÇ ÇÔ·®º¸´Ù ³·¾Ò´Ù. »ç¹®¾Ï dzȭÅä¿¡ ÃâÇöÇÏ´Â ´ë³ª¹°³» Áß±Ý¼Ó ÇÔ·®Àº È¥ÇÕ Ç³È­ÅäÀÇ ±×°Íº¸´Ù ³ô°Ô ³ªÅ¸³µÀ¸¸ç, °°Àº »ç¹®¾Ï Áö¿ªÀÌ¶óµµ È«¼ºº¸´Ù ±¤ÃµÀÇ Áß±Ý¼Ó ÇÔ·®ÀÌ ³ô¾Ò´Ù. ´ë³ª¹°ÀÇ Æò±Õ Fe:NiÀÇ ºñÀ²Àº È¥ÇÕ Ç³È­Åä¿¡¼­´Â 216ÀÌ°í »ç¹®¾Ï dzȭÅä¿¡¼­´Â 49¿´´Ù. ´ë³ª¹°³» Ni, Cr, Co, Fe ¹× Sc µîÀº Áö»óºÎº¸´Ù ÁöÇϺο¡¼­ ³ô¾ÒÀ¸¸ç, Zn°ú Mo ÇÔ·®Àº Áö»óºÎ¿¡¼­ ³ô¾Ò´Ù. ¾Ï¼®°ú ½Ä¹°Ã¼ÀÇ Áß±Ý¼Ó ÇÔ·® ºñ±³ °á°ú ½Ä¹°Ã¼¿¡¼­º¸´Ù ¾Ï¼®ÀÇ Áß±Ý¼Ó ÇÔ·®ÀÌ ³ô¾Ò°í, ´ë³ª¹°¿¡ ÀÇÇÑ ZnÀÇ Èí¼ö´Â »ç¹®¾Ï°ú º¯¼º¾Ï Áö¿ª¿¡¼­ ³ô¾ÒÀ¸¸ç Sc¿Í Fe´Â »ç¹®¾Ï Áö¿ª¿¡¼­ ¶Ñ·ÇÀÌ ³ô¾Ò´Ù.
To investigate the degrees of toxification in the serpentine areas, serpentinites and adjacent metamorphic rocks and soils from the serpentinite, metamorphic area and transitional area(mixed soil) between serpentinite and metamorphic rocks are collected from the Hongseong-Gun, Chungnam. A plant, Geochemically, the serpentinites are high in the nickel, chromium and cobalt content whereas the metamorphic rocks show high zinc, scandium, molybdenum and iron contents. The serpentine soils are high in the nickel, chromium and cobalt contents whereas the non-serpentine soils show high zinc and iron contents. Heavy metal contents in the G. oldhamiana are high in the serpentine soil relative to the mixed soil. Ratio of the iron to nickel contents for the G. oldhamiana are low in the serpentine soil(49) relative to the mixed soil(216). Of the G. oldhamiana, most of the heavy metal contents except zinc and molybdenum are high in the root relative to the aboveground vegetation. Comparing with rocks, the G. oldhamiana is low in the all of heavy metal contents relative to the serpentinite. Uptake of zinc by the G. oldhamiana is high in the serpentinites and metamorphic rocks whereas uptake of scandium and iron by the G. oldhamiana is very high in the serpentinite area.
 
Ű¿öµå
Serpentine;Gypsophila oldhamiana;Heavy metal;Metamorphic rock;
 
The Korean Journal of Ecology / v.20, no.5, 1997³â, pp.385-391
Çѱ¹»ýÅÂÇÐȸ
ISSN : 1225-0317
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199711919962817)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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