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Çѱ¹¼öÀÚ¿øÇÐȸ / v.28, no.6, 1995³â, pp.169-181
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ÆÈ´ç´ï ¹æ·ù·® °ËÁ¤À» À§ÇÑ °í¾ÈÁöÁ¡ ¼öÀ§-À¯·® °ü°è°î¼±ÀÇ ÀÛ¼º
( The Rating Curve of Goan Station for Calibration of Discharge of Paldang Dam ) |
| ¼±Ô¿ì;ÇãÁØÇà; ¿¬¼¼´ëÇб³ Åä¸ñ°øÇаú;¿¬¼¼´ëÇб³ Åä¸ñ°øÇаú Á¶±³¼ö, ¿¬¼¼´ëÇб³ Åä¸ñ°øÇаú ±³¼ö, ¿¬¼¼´ëÇб³ Åä¸ñ°øÇаú ¸í¿¹±³¼ö;
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| 1986³â ÀÌÈÄ ±Þ°ÝÇÑ Çϻ󺯵¿¿¡µµ ºÒ±¸ÇÏ°í °í¾ÈÁöÁ¡ÀÇ ¼öÀ§-À¯·® °ü°è°î¼±¿¡ ´ëÇÑ ¼öÁ¤ÀÛ¾÷ÀÌ ÀÌ·ç¾îÁöÁö ¾Ê¾Æ '90³â È«¼ö½Ã ÇѰȫ¼öÅëÁ¦¼Ò·Î Á¦º¸µÈ ÆÈ´ç´ï ÇÏ·ùºÎ ¼öÀ§³ª ¹æ·ù·® ÀÚ·áµéÀÌ °í¾ÈÁöÁ¡¿¡¼ °èÃøµÈ ¼öÀ§ÀÚ·á¿¡ ÀÇÇÑ À¯·®ÀÚ·á¿ÍÀÇ ºñ±³¿¡¼ ¼·Î °£ÀÇ ½Å·Úµµ¿¡ ¹®Á¦°¡ ¹ß»ýÇÏ¿´´Ù. µû¶ó¼ º» ¿¬±¸¿¡¼´Â ´ïÇÏ·ùºÎÀÇ Çϻ󺯵¿À» °í·ÁÇÏ¿© ÆÈ´ç´ï¿¡¼ °í¾ÈÁöÁ¡ ÇÏ·ù¸¦ Æ÷ÇÔÇÏ´Â ¾à 2.2km ±¸°£¿¡ ´ëÇØ 1/100 ÃàôÀÇ ¼ö¸®¸ðÇü½ÇÇèÀ» ½Ç½ÃÇÏ¿´À¸¸ç, À̸¦ ÅëÇØ »õ·ÎÀÌ ÀÛ¼ºµÈ ÆÈ´ç´ï ¹æ·ù·® »êÁ¤°ø½Ä¿¡ ÀÇÇÑ ¹æ·ù·®ÀÚ·á¿Í °í¾ÈÁöÁ¡¿¡¼ÀÇ ¼öÀ§ÀڷḦ ÀÌ¿ëÇÏ¿© »õ·Î¿î ¼öÀ§-À¯·® °ü°è°î¼±À» ÀÛ¼ºÇÏ¿´´Ù. ÇÑÆí ¼ö¸®¸ðÇü ½ÇÇ輺°ú·Î ÀÛ¼ºÇÑ ¼öÀ§-À¯·® °ü°è°î¼±À» RMA-2V¸ðÇü¿¡ ÀÇÇÑ ¼öÄ¡¸ðÇüÀ» ÀÌ¿ëÇÏ¿© ±âÁ¸ÀÇ ¼öÀ§-À¯·® °ü°è °î¼± ¹× »õ·Î¿î ¼öÀ§-À¯·® °ü°è°î¼±À» ºñ±³, °ËÁ¤ÇÏ¿´´Ù. |
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| No correction has been made for the rating curve of Goan Station since 1986 even though there has been a severe bed degradation until now. Furthermore, it was informed to Han River Flood Control Center that there was a difference between the discharge released from Paldang dam and the discharge observed at Goan station during 1990 flood. By considering such river bed changes, hydraulic model experiment with 1/100 scale was performed for the range of 2.2 km, which covers from Paldang dam to the downstream of Goan station. From this experiment, the rating curve was obtained by considering the discharges from Paldang dam and the corresponding water levels at Goan station. Also, the exsitingand the proposed rating curves were compared with those by computational method of RMA-2V. |
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.28, no.6, 1995³â, pp.169-181
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199511920096499)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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