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Çѱ¹¼öÀÚ¿øÇÐȸ / v.15, no.3, 1982³â, pp.37-47
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È®Á¤·ÐÀû ¸ðÀDZâ¹ý¿¡ ÀÇÇÑ µµ½ÃÀ¯Ãâ ÇØ¼®¿¡ °üÇÑ ¿¬±¸
( A Study on urban runoff by deter ministic simulation techniques. ) |
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| º» ¿¬±¸´Â È®Á¤·ÐÀû ¸ðÀDZâ¹ý Áß ¿µ±¹µµ·Î½ÃÇ迬±¸¼Ò¿¡¼ °³¹ßÇÑ R.R.L¹ýÀ» Æ÷Àå Áö¿ªÀÌ ³ÐÀº ÀÎõ¿¡ À§Ä¡ÇÑ °£¼®µ¿ ¾ÆÆÄÆ®¿¡ Àû¿ëÇÏ¿© ±× ½Ç¿ë¼ºÀ» °ËÅäÇÏ¿´´Ù. ÀÎõÁö¹æÀÇ ÀüüÀûÀ̰í ÇÕ¸®ÀûÀÎ °á°ú¸¦ ¾ò±â À§ÇÏ¿© °ú°Å 28³â°£ ´©°¡¿ì·® °î¼±¿¡¼ ¾òÀº 10mm ÀÌ»ó µÇ´Â °¿ì 450°³¸¦ 5ºÐ °£°ÝÀ¸·Î Àоî È®·üºóµµÅë°èÀÎ HUFFÀÇ »çºÐÀ§¹ýÀ» ÀÌ¿ë È®·üºóµµ¹éºÐÀ²°î¼±À» ¾ò¾î R.R.L¹ý¿¡ Àû¿ëÇÏ¿´´Ù. ÀÎõÁö¹æÀÇ È®·üºóµµ¹éºÐ·ü °î¼±Àº Á¦2 ±¸°£ÀÌ ÀüüÀÇ 43.2%¸¦ ³ªÅ¸³»¹Ç·Î ¼³°è¿ì·®ÀÇ ¿ì·®ÁÖ»óµµ´Â Á¦À»±¸°£¿¡¼ ÃßÃâÇÔÀÌ ¹Ù¶÷Á÷ÇÏ´Ù. |
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| In the past, the design flow of the urban storm drainage systems has been used largely on a basis of empirical and experience, and the rational formula one of empirical method has been widely used for our country, as well as world wide. But the empirical method has insufficient factor because minimal consideration is given to the relationship of the parameters in the equation to the processes being considered, and considerable use of experience and judgment in setting values to the coefficients in the equation is made. The postcomputer era of hydrology has brought an acceleration development of mathematical methods, thus mathematical models are methods which will greatly increase our understanding in hydrology. On this study, a simple mathematical model of urban presented by British Road Research Laboratory is tested on urban watersheds in Ju An Ju Gong Apartment. The basin is located in Kan Seog Dong, Inchon. The model produces a runoff hydrograph by applying rain all to only the directly connected impervious area of the basin. To apply this model the basin is divided into contributing areas or subbasins. With this information the time area for contributing is derived. The rainfall hyetograph to design storm for the basin flow has been obtained by determination of total rainfall and the temporal distribution of that rainfall determined on the basis of Huff's method form historical rainfall data of the basin. The inflows from several subbaisns are successively routed down the network of reaches from the upstream end to the outlet. A simple storage routing technique is used which involves the use of the Manning equation to compute the stage discharge curve for the cross-section in question. To apply the model to a basin, the pattern of impervious areas must be known in detail, as well as the slopes and sizes of all surface and subsurface drains. |
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.15, no.3, 1982³â, pp.37-47
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198211920090484)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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