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Çѱ¹ÇÏõȣ¼öÇÐȸ / v.36, no.3, 2003³â, pp.269-276
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( Relationships Between the Development of Cyanobacterial Bloom and the Changes of Environmental Factors in Lake Daechung ) |
| ÀÌÁ¤ÁØ;¹ÚÁ¾±Ù;ÀÌÁ¤È£; Çѱ¹¼öÀÚ¿ø°ø»ç ¼öÀÚ¿ø¿¬±¸¿ø;Çѱ¹¼öÀÚ¿ø°ø»ç ¼öÀÚ¿ø¿¬±¸¿ø;´ë±¸´ëÇб³ »ý¹°±³À°°ú;
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| ´ëûȣÀÇ ³²Á¶·ù ¼öȸ¦ Ãʱâ¿Í Áß±â, Èıâ·Î ±¸ºÐÇÏ¿© °¢ ´Ü°èº°·Î ¼öÈ ¹ß´Þ¿¡ ´ëÇÑ ÁÖ¿ä Á¦ÇÑ ÀÎÀÚÀÇ »ó°ü°ü°è¸¦ Á¶»çÇÏ¿´°í, ÁÖ¿ä ¿µ¾ç¿°ÀÇ Áßȸ±Í¸ðÇüÀ» °³¹ßÇÏ¿´´Ù. Á¶»çÁöÁ¡Àº ´ïÀ¸·ÎºÎÅÍ ¾à 13km»ó·ù¿¡ À§Ä¡ÇÏ°í º»·ù Áß ¼öȰ¡ °¡Àå ½ÉÇÑ È¸³²´ë±³ ÁöÁ¡À» ´ë»óÀ¸·Î ÇÏ¿´À¸¸ç,½Ã·áÀÇ Ã¤ÁýÀº ¼öȹ߻ý ±â°£ÀÎ 2001°ß 6¿ù¿¡¼ 10¿ù±îÁö ¸ÅÁÖ 1ȸ ½Ç½ÃÇÏ¿´´Ù. ¼öÈ ¹ß´ÞÀÇ Ãʱ⠵¿¾È chl-a ³óµµ¿ÍÀÇ T-P¿Í $PO_4$-PÀÇ »ó°ü°è¼ö r°ªÀÌ °¢°¢ 0.986°ú 0.894·Î ¸Å¿ì ³ôÀº ¾çÀÇ »ó°üµµ¸¦ ³ªÅ¸³»¾î ÀÎÀÌ ¼öȹߴ޿¡ °¡Àå Áß¿äÇÑ È¯°æ¿äÀÎÀ¸·Î È®ÀεǾúÀ¸¸ç, Zeu/ZmÀÇ ºñ¿Í chl-a¿ÍÀÇ »ó°üµµµµ r=-0.995ÀÇ ¸Å¿ì ³ôÀº À½ÀÇ »ó°üµµ¸¦ º¸¿´´Ù. ¼öÈÀÇ ÀýÁ¤±â¿¡ ÇØ´çÇÏ´Â Á߱⿡´Â chl-a¿Í $PO_4$-P°¡ r = 0.958·Î °¡Àå ³ôÀº »ó°üµµ¸¦ °¡Á³À¸¸ç, T-P¿Í ¼ö¿Âµµ °¢°¢ r = 0.857°ú r = 0.813À¸·Î ³ôÀº »ó°üµµ¸¦ º¸¿´´Ù. Èı⿡´Â $NH_3$-N¸¸ÀÌ ³ôÀº »ó°üµµ¸¦ °¡Áö´Â °ÍÀ¸·Î Á¶»çµÇ¾ú´Ù. Áßȸ±Í¸ðÇü °³¹ßÀ» À§ÇÑ È¸±ÍºÐ¼® °á°ú ´ëûȣÀÇ ³²Á¶·ù ¼öÈ ¹ß»ý¿¡ °¡Àå Å« ¿µÇâÀ» ¹ÌÄ¡´Â ¿µ¾ç¿°Àº $PO_4$-P·Î ³ªÅ¸³µ´Ù. °á·ÐÀûÀ¸·Î ´ëûȣÀÇ ³²Á¶·ù ¼öÈ´Â Zeu/ZmÀÇ ºñ°¡°¨¼ÒÇϰí ÀÎ ³óµµ°¡ Áõ°¡ÇÔ¿¡ µû¶ó ±Þ¼ÓÈ÷ ¹ß´ÞµÇ¸ç, $NH_3$-N ³óµµÀÇ °¨¼Ò¿Í ºñ·ÊÇÏ¿© ¼Ò¸ê °úÁ¤ÀÌ ÁøÇàµÇ´Â ¾ç»óÀ» º¸¿´´Ù. ¼öÈ ¼Ò¸ê±â¿¡ $NH_3$-N ³óµµÀÇ ¸é¹ÐÇÑ °üÂûÀº ¼öÈ ¼Ò¸êÀÇ ¸ð´ÏÅ͸µ°ú ¿¹Ãø¿¡ ÀÖ¾î ¸Å¿ì À¯¿ëÇÑ ÀÎÀڷΠȰ¿ëÇÒ ¼ö ÀÖÀ» °ÍÀ¸·Î ±â´ëµÇ¾ú´Ù |
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| The study was performed to understand the relationships of cyanobacterial bloom and environmental factors in Lake Daechung. The samples were collected weekly from June to October in 2001. The cyanobacterial bloom was divided into the three phases of the early phase, the middle phase and the late phase by phytoplankton standing crops. For the early phase, the correlation coefficients between chl- a and TP, and chl- a and $PO_4$-P were 0.986 and 0.894 respectively. Therefore, phosphorus was a main environmental factor in the development of cyanobacterial bloom. Zeu/Zm ratio and chl-a showed negative correlation of r = -0.995. At the late phase, $PO_4$-P showed the highest relationship (r = 0.958), and TP and temperature showed relatively high relationships (r = 0.857 and r = 0.813). At the late phase, $NH_3$-N showed highly positive relationship (r = 0.921). It was confirmed that $PO_4$-P was the most important contribution factor for the bloom through the regression analysis on the environmental factors. As the result, the decrease of Zeu/Zm ratio and the increase of P concentration influenced cyanobacterial bloom developed rapidly in the early phase. Also the cyanobacterial bloom was decreased in proportion to decreasing of $NH_3$-N concentration in the late phase. It was expected that observation of $NH_3$-N may be a very useful factor on monitoring of the decreasing situation of the bloom. |
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| Ű¿öµå |
| Relationship;cyanobacterial bloom;environmental factors;Lake Daechung; |
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Çѱ¹ÇÏõȣ¼öÇÐȸÁö / v.36, no.3, 2003³â, pp.269-276
Çѱ¹ÇÏõȣ¼öÇÐȸ
ISSN : 1976-8087
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200318317181536)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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