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Çѱ¹ÇÏõȣ¼öÇÐȸ / v.36, no.2, 2003³â, pp.200-207
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µ¿°áÀ¶ÇØÄ§½Ä Åä»ç°¡ °è·ù¼öÀÇ ¼öÁú¿¡ ¹ÌÄ¡´Â ¿µÇâ - ºÏÇѻ걹¸³°ø¿ø ºÏµ¿»ç¸é Àϴ븦 Áß½ÉÀ¸·Î -
( Influences of the Solifluction Soil on the Physicochemistry of Stream Water Quality -With a Special Reference on Northeastern Side Slopes Area of Bughansan National Park- ) |
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| º» ¿¬±¸´Â ºÏÇѻ걹¸³°ø¿ø ºÏµ¿»ç¸é ÀÏ´ë¿¡¼ °è·ù¼öÁú¿¡ ¹ÌÄ¡´Â µ¿°áÀ¶ÇØÄ§½ÄÅä»çÀÇ ¿µÇâÀ» ÆÄ¾ÇÇÔÀ¸·Î½á ±¹¸³°ø¿ø³» °è·ù¼öÁú º¸ÀüÀ» À§ÇÑ °úÇÐÀû ±âÃÊ ÀڷḦ Á¦°øÇϱâ À§ÇÏ¿© 2002³â 3¿ùºÎÅÍ 5¿ù±îÁö ¼öÇàÇÏ¿´´Ù. Á¶»ç±â°£ µ¿¾È °è·ù¼öÀÇ Æò±Õ pH´Â µ¿°áÀ¶ÇØÄ§½ÄÅä»çÀÇ Æò±Õ pHº¸´Ù ³ô¾ÒÀ¸¸ç, °è·ù¼öÀÇ Æò±Õ Àü±âÀüµµµµ´Â »ó·ùÀ¯¿ªÀÌ ÇÏ·ùÀ¯¿ªº¸´Ù ¾à 2.1${sim}$2.8¹è ³·Àº °ªÀ» ³ªÅ¸³»¾ú´Ù. ¶ÇÇÑ, Á÷¼±È¸±ÍºÐ¼®°á°ú µ¿°áÀ¶ÇØÄ§½ÄµÈ Åä»ç¿Í °è·ù¼ö¿¡¼ÀÇ pH¿Í À½À̿·® ($Cl^-,;N0_3;^-, So_4;^{2-}$)Àº Á¤ÀÇ »ó°ü°ü°è¸¦ ³ªÅ¸³»¾ú´Ù. |
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| This research was conducted to investigate the influences caused by solifluction soil on the physicochemistry of stream water quality in the riparian area: four points of the northeastern side slopes part of the Bughansan National Park from March to May of 2002. The average pH of stream water was relatively high with the influenced of solifluction soil. The average electrical conductivity of upstream water was 2.1${sim}$2.8 times lower than that in downstream water. pH and amount of anion ($Cl^-,;N0_3;^-, So_4;^{2-}$) of stream water was correlated under the effect of solifluction soil. |
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| Bughansan National Park;physicochemistry;solifluction soil; |
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Çѱ¹ÇÏõȣ¼öÇÐȸÁö / v.36, no.2, 2003³â, pp.200-207
Çѱ¹ÇÏõȣ¼öÇÐȸ
ISSN : 1976-8087
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200318317181195)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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