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Çѱ¹¼öÀÚ¿øÇÐȸ / v.13, no.4, 1980³â, pp.33-40
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¹Ì¼ÒÁøÆøÆÄ¿¡ ÀÇÇÑ ÀúÁúÀÇ ºÎÀ¯³óµµ¿¡ °üÇÑ ¿¬±¸
( A Study on Suspended Sediment Concentration Due to Small Amplitude Wave Action ) |
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| ÇØ¾ÈÁöÇü º¯ÈÀÇ ÁÖ¿øÀÎÀÎ ºÎÀ¯»ç¿¡ ´ëÇÑ ¿¬±¸°¡ ÀÌ·ÐÀû¡¤½ÇÇèÀûÀ¸·Î ´Ù¼Ò ÀÖ¾úÀ¸³ª ±×ÀÇ ¼ºÁúÀ» ¿ÏÀüÈ÷ ÇØ¼®Çϱ⿡´Â »ó´çÇÑ ³Á¡ÀÌ ÀÖ´Ù. ±× ÀÌÀ¯´Â ÀÚ¿¬»óÅÂÀÇ º¯ÇüÀÎÀÚµéÀÌ ³Ê¹« ¸¹°í ¼·Î º¹ÇÕÀûÀ¸·Î ¿¬ÇյǾî ÀÖ¾î ½ÇÇè½Ç³»¿¡¼´Â ½ÇÇèÇÒ ¶§ °í·ÁµÇ¾î¾ß ÇÒ ¸¹Àº ÀÎÀÚµéÀÇ Á¦¾àÀÌ µÚµû¸£¸ç, ½ÇÁ¦ ÇØ¾È¿¡¼ÀÇ ½ÇÃøÀº ¸¹Àº Àη ¹× °æºñ¿Í ½Ã°£Àû¡¤°ø°£Àû Á¦¾àÀÌ ¼ö¹ÝµÇ±â ¶§¹®ÀÌ´Ù. º» ¿¬±¸´Â ¹Ì¼ÒÁøÆøÆÄ¿¡ ÀÇÇÑ ºñÁ¤»ó È®»ê¹æÁ¤½ÄÀ» ÇØ¼®ÇÏ¿© ºÎÀ¯»ç ³óµµÀÇ ½Ã°£Àû º¯È¿Í ¿¬Á÷³óµµºÐÆ÷ ¹× ħ°¼ÓµµÀÇ ¿µÇâÀ» ¹àÈûÀ¸·Î½á ºÎÀ¯»çÀÇ ±âÃÊÀû ¼ºÁúÀ» ±Ô¸íÇϴµ¥ ¸ñÀûÀÌ ÀÖ´Ù. |
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| It has been very difficult to analyse, clearly, the mechanism of the suspended sediment that changes, largely, the coastline, on-shore and off-shore. It is due to not only the complexity of the factors in nature but the measurement technique of suspended sediment characteristics both in nature and loboratory. The purpose of this paper are to obtain the time-rate of change in the concentration of suspended sediment, the vertical distribution of it and the effect of the fall velocity of its particle, and to make clear the mechanism of sand transportation in suspension, analysing the diffusion equation, by the computer, due to the small amplitude wave theory. |
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.13, no.4, 1980³â, pp.33-40
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198011920089960)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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