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Çѱ¹ÇÏõȣ¼öÇÐȸ / v.35, no.1, 2002³â, pp.36-44
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( Long-Term Annual Trend Analysis of Epilimnetic Water Quality and Their Longitudinal Heterogeneities in Lake Soyang )
ÀÌÇý¿ø;¾È±¤±¹;¹Ú¼®¼ø; ÀÌÈ­¿©ÀÚ´ëÇб³ °ø°ú´ëÇРȯ°æÇаú;ÀÌÈ­¿©ÀÚ´ëÇб³ °ø°ú´ëÇРȯ°æÇаú;ÀÌÈ­¿©ÀÚ´ëÇб³ °ø°ú´ëÇРȯ°æÇаú;
 
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º» ¿¬±¸´Â 1993³âºÎÅÍ 2000³â±îÁö ¼Ò¾çÈ£ÀÇ ÃÑÀÎ, ÃÑÁú¼Ò, Àü±âÀüµµµµ, ¿±·Ï¼ÒÀÇ ½Ã${cdot}$°ø°£Àû °æÇâÀ» Åë°è±â¹ýÀ» Àû¿ëÇÏ¿© ÆÄ¾ÇÇÏ¿´´Ù. È£¼ö³»ÀÇ ¼öÁúƯ¼ºÀº ¿¬°£°­¿ì·® ¹× ¼ö°èÀÇ À¯ÀÔ·®¿¡ ÀÇÇØ º¯µ¿µÇ¾úÀ¸³ª, º¯µ¿ Á¤µµ´Â Á¶»çÁö¿ª¿¡ µû¶ó ¿ªµ¿ÀûÀÎ Â÷À̸¦ º¸¿´´Ù. ¸Ç-ÄË´Þ°ËÁ¤¹ý (Mann-Kendall test)À¸·Î ¿¬º° ¼öÁúº¯È­¸¦ ºÐ¼®ÇÑ ¡¡°á°ú,¡¡Àü±âÀüµµµµ, ÃÑÀÎ, ¿±·Ï¼Ò-a´Â 8³â µ¿¾È ¸ðµç ÁöÁ¡¿¡¼­ Áõ°¡ ¹× °¨¼Ò °æÇâÀÌ ¾øÀ¸³ª TNÀº ±ØÈ÷ ¹Ì¾àÇÏ°Ô °¨¼ÒÇÏ´Â °æÇâÀ» º¸¿´´Ù. ÃÑÀÎÀº À¯ÀÔ·® ¹× °­¿ì¿¡ ÀÇÇØ °áÁ¤µÇ´Â °ÍÀ¸·Î ¹àÇôÁ³´Ù. °ø°£Àû ºÐ¼®°á°ú¿¡ µû¸£¸é, Àü±âÀüµµµµ´Â È£¼ö³» »ó·ù¿¡¼­ ÇÏ·ù·Î °¨¼ÒÇÏ´Â °æÇâÀ» º¸¿´°í À帶Áß »ó·ù¿¡¼­´Â ÁýÁß °­¿ìµ¿¾È ÃÖ¼Ò°ªÀ» º¸À̰í ÇÏ·ù¿¡¼­´Â ¼öü·ù¡¡Çö»óÀ¸·Î 10¿ù¿¡ ÃÖ¼Ò°ªÀ» ³ªÅ¸³Â´Ù. ÃÑÀÎ ¹× ÃÑÁú¼Ò´Â À帶Áß¿¡ ÃÖ´ë°ªÀ» ³ªÅ¸³»¸é¼­ Àü±âÀüµµ_µµÀÇ º¯È­ ¾ç»ó°ú ¿ª°ü°è¸¦ ³ªÅ¸³Â´Ù. È£¼ö³» 1Â÷ »ý»ê·ÂÀÇ Ã´µµ·Î¼­ ÃøÁ¤µÈ ¿±·Ï¼Ò-aÀÇ ³óµµ´Â ¿µ¾ç¿°·ùÀÇ ³óµµ ¹× °èÀý¿¡ µû¶ó Å« Â÷À̸¦ º¸¿´´Ù. °èÀýº° ÃÑÀο¡ ´ëÇÑ ¿±·Ï¼Ò ³óµµÀÇ È¸±Í ºÐ¼®°á°ú¿¡ µû¸£¸é, À帶 Àü ¹× À帶 Áß¿¡´Â $R^2$°ªÀÌ 0.003ÀÌÇÏÀÌÁö¸¸ À帶ÈÄ $R^2$°ªÀº 0.82·Î¼­ Á¶·ù»ýÀåÀÌ ÀÎÀÇ ³óµµ¿¡ ÀÇÇØ °áÁ¤µÇ´Â °ÍÀ» È®ÀÎÇÏ¿´´Ù. ¹Ý¸é Áú¼ÒÀÇ ³óµµ´Â °èÀý¿¡ »ó°ü¾øÀÌ ¿±·Ï¼ÒÀÇ ³óµµ¿Í ±ØÈ÷ ¹Ì¾àÇÑ °ü°è¸¦ º¸¿´´Ù.
The spatial and temporal trends of water qualities in Lake Soyang was statistically analyzed in this study. The water qualities include nutrients, ionic contents and chlorophyll-a (Chl-a) measured during 1993${sim}$2000. The rainfall intensity and runoff from the catchment appeared to play an important role in water quality trends in the lake. According to seasonal Mann-Kendall test, conductivity, TP, and Ctl-a did not show any trends of increase or decrease over the 8 year period, while TN declined slightly. It was found that the variation of TP was a function of interannual inflow and rainfall. In the analyses of spatial trend, conductivity, based on the mean by site, showed a downlake decline over the eight year period. Minimum conductivity was found in the headwaters during summer monsoon of July to August and near the dam during October. This result indicates a time-lag phenomenon that the headwater is diluted by rainwater immediately after summer monsoon rain and then the lake water near the dam is completely diluted in October. During summer period, TP and TN had an inverse relation with conductivity values. Concentrations of TP peaked during July to September in the headwaters and during September in the downlake. Also, TN increase during the summer and was more than 1.5 mg/L regardless of season and location, indicating a consistent eutrophic state. Values of Chl-a varied depending on location and season, but peaked in the midlake rather than in the headwaters during the monsoon. Regression analyses of log-transformed seasonal Chl-a against TP showed that value of $R^2$ was below 0.003 in the premonsoon and monsoon seasons but was 0.82 during the postmonsoon, indicating a greater algal response to the phosphorus during the postmonsoon. In contrast, TN had no any relations with Chl-a during all seasons.
 
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Nutrients;Conductivity;Rainfall;Inflow;Chlorophyll-a;Lake Soyang;
 
Çѱ¹ÇÏõȣ¼öÇÐȸÁö / v.35, no.1, 2002³â, pp.36-44
Çѱ¹ÇÏõȣ¼öÇÐȸ
ISSN : 1976-8087
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200218317179154)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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