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Çѱ¹¼öÀÚ¿øÇÐȸ / v.36, no.6, 2003³â, pp.1083-1095
GIS¸¦ ÀÌ¿ëÇÑ °Çõȭ ÇÏõÀÇ Æ¯¼ººÐ¼®
( Analysis of Drying Streams Characteristics Using a GIS )
Á¤°ü¼ö;Á¶È¿¼·;±èÁ¤¿±;½É¸íÇÊ; Ãæ³²´ëÇб³ Åä¸ñ°øÇаú;ÀϽÅÇÏÀÌÅØ ±â¼ú¿¬±¸¼Ò;Ãæ³²´ëÇб³ ´ëÇпø Åä¸ñ°øÇаú;ÀÎÇÏ´ëÇб³ Åä¸ñ°øÇаú;
 
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Áß¼ÒÇÏõÀÇ °Çõȭ ¿øÀκм® ±â¼ú°³¹ßÀ» À§ÇØ 500¿©°³ ÇÏõ¿¡ ´ëÇÏ¿© 19°³ Á¶»çÇ׸ñÀ¸·Î ÇöÀåÁ¶»ç¸¦ ÅëÇØ ÃëµæµÈ Á¶»çÀڷḦ ±â¹ÝÀ¸·Î °Çõȭ ÇÏõƯ¼ºÀ» ºÐ¼®ÇÏ¿´°í, ÇöÁöÁ¶»ç ´ë»ó ÇÏõ Áß¿¡¼­ °¡¿ëÇÒ ¼ö ÀÖ´Â ¼ö¹®ÀÚ·áÀÇ È®º¸¿©ºÎ, ÇÏõÀÇ ¿¬Àå ¹× À¯¿ª¸éÀû, Áö¿ªº° Ư¼º¿¡ ´ëÇÑ ¼±Á¤±âÁØÀ» ¼ö¸³ÇÏ¿© ÃÖÁ¾ÀûÀ¸·Î 8°³ÀÇ ´ë»óÇÏõÀ» ¼±Á¤ÇÏ¿´´Ù. ¼±Á¤µÈ 8°³ÇÏõ¿¡ ´ëÇÏ¿© ÇöÀåÀÇ »ó¼¼Á¶»ç¸¦ ¼öÇàÇÏ¿´°í, ÇÏõ ½Ã¼³¹° ¹× ¼ö¹®ÀÚ·á°¡ ºñ±³Àû Àß ±¸ÃàµÈ 5°³ ÇÏõÀ» Áß½ÉÀ¸·Î GIS¸¦ ÀÌ¿ëÇÏ¿© °Çõȭ ÇÏõÀÇ Æ¯¼ºÀ» ºÐ¼®ÇÏ¿´´Ù. GISÀÇ °ø°£ºÐ¼®Àº °Çõȭ ÇÏõÀÇ ±¸°£¿¡ ´ëÇÑ °æ»çºÐ¼®, ÇÏõÀÇ ½Ã¼³¹°Á¤º¸¿Í ÇÏõÀÇ À¯½É¼±À» Áß½ÉÀ¸·Î °ø°£¿µ¿ªºÐ¼®À» ÅëÇÏ¿© ÇÏõ³» À¯¼ö¸¦ »ç¿ëÇϱâ À§ÇÑ À̼ö½Ã¼³¹°ÀÌ ÇÏõ¿¡ ÁÖ´Â ¿µÇâ±ÇºÐ¼®, °Çõȭ ÇÏõÀÇ »çÇ൵¸¦ ºÐ¼®ÇÏ¿´´Ù. º» ¿¬±¸ °á°ú 500¿©°³ÀÇ ÇöÁöÁ¶»ç¸¦ ÅëÇÑ °Çõȭ ÇÏõÀÇ Æ¯¼ºÀº ´ëºÎºÐÀÌ Åä»ç ¹× ÀÚ¿¬Á¦¹æ, ÇÏõ´Ü¸éÀº »ç´Ù¸®²Ã, »çÇàÇÏõ, ÇÏ»óÀç·á´Â ÀÚ°¥ ¹× ¸ð·¡, ÇÏõ½Ã¼³¹°Àº ´ëºÎºÐÀÌ º¸°¡ ¸¹ÀÌ Á¸ÀçÇϴ Ư¼ºÀ» º¸¿©Áá´Ù. ¶ÇÇÑ GIS¸¦ ÀÌ¿ëÇÑ °ø°£ºÐ¼®°á°ú º¸°¡ ÀÖ´Â À§Ä¡¿¡¼­ ÇÏõÀÇ »óÇÏ·ùÀÇ °æ»çºÐÆ÷´Â º¸¿¡ °¡±î¿î °æ¿ì ÇÏ·ùÂÊÀÇ °æ»ç°¡ ½ÉÇϰí, º¸¿¡¼­ ¸Ö¼ö·Ï »ó·ùÂÊ ±âº¹ÀÌ ½ÉÇÑ °ÍÀ¸·Î ³ªÅ¸³µ´Ù. °Çõȭ ÇÏõ±¸°£³» ´ëºÎºÐÀÇ °üÁ¤Àº ÇÏõÁ߽ɼ±À¸·ÎºÎÅÍ ¹Ý°æ 500mÀ̳»¿¡ Á¸ÀçÇÏ¿´À¸¸ç, °¢ °Çõȭ ÇÏõÀÇ Æò±Õ »çÇ൵´Â ÃÖ¼Ò 1.229¡­ÃÖ´ë 1.475·Î¼­ ºñ±³Àû »çÇ൵°¡ ½ÉÇÑ °ÍÀ¸·Î ³ªÅ¸³µ´Ù.
The analysis of drying stream characteristics for about 500 streams from field survey data with 19 items has been fulfilled. Also, a study area has been determined, and criteria of estimation has been established : criteria such as, available hydrological data, the size of stream lengths and basin areas and regional characteristics. Then they are applied to designated study areas. The final selected study areas are 8 basins. The analysis of drying stream characteristics using a GIS has been applied to 5 basins in which spacial data is comparatively implemented among the final 8 target catchments. The spacial analysis using a GIS is applied to stream slopes for upstream and downstram at weirs, overlaying the map of buffering stream networks and ground water pump stations map, sinuosity of drying stream. As a result of drying streams survey analysis, drying stream characteristics are followed; levee types are earth and natural, cross sectional shapes are trapezoid, stream bed materials are gravels and sands, facilities in streams are weirs. As a result of GIS analysis, stream slopes are comparatively larger downstream than upstream close to weirs. There are arranged ground water pump stations less than 500m from stream networks. Also the average of sinuosity for each drying stream is in the range of 1.229¡­1.475, comparatively a serious.
 
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º¸;»çÇ൵;ÇÏõ°æ»ç;°Çõȭ ÇÏõ Ư¼º;GIS;Weir;Sinuosity;Stream Slope;Drying Stream Characteristics;GIS;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.36, no.6, 2003³â, pp.1083-1095
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200311922122626)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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