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Çѱ¹¼öÀÚ¿øÇÐȸ / v.27, no.3, 1994³â, pp.115-121
¸ðÀÇ·ù»çÀÇ ÂʰŸ® Â÷¿ø
( FRACTAL DIMENSION OF SIMULATED SEDIMENTS )
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Çϱ¸¼ö¸®°è¿¡ À־ Á¡Âø¼º·ù»çÀÇ ¿îµ¿Àº ÀÀ°á°ú ÀÀÁý(aggregation) Çö»ó¿¡ ÀÇÇØ Å©°Ô Á¿ìµÇ¸ç, À̵é Çö»ó¿¡ ÀÇÇÏ¿© ÀǰáµÈ ÀÔÀÚµéÀÇ Å©±â, ¸ð¾ç, °­µµ´Â ±× ÅðÀûÀ²°ú ±×¸®°í ºÎÀ¯·ù»ç¿Í ¿À¿°¹°ÁúÀÇ º¯µ¿°úÁ¤¿¡ ¿µÇâÀ» ¹ÌÄ£´Ù. º» ¿¬±¸¿¡¼­´Â Brownian ¿îµ¿¿¡ ÀÇÇØ Áö¹èµÇ´Â À̵¿¼º ºÎÀ¯¿µ¿ª°ú Á߷¿¡ ÀÇÇØ Áö¹èµÇ´Â Á¤Ã¼¼º ºÎÀ¯¿µ¿ªÀ¸·Î ºÐ¸®ÇÏ¿© Á¡Âø¼ºÀÔÀÚµéÀÇ ÀÀÁý°ú ÀÀ°á°úÁ¤À» ¸ðÀÇÇÏ¿´´Ù. À̵¿¼º ºÎÀ¯¿µ¿ª¿¡ À־´Â Smoluchowski ¸ðÇüÁß ÀÔÀÚµéÀÇ ¹«ÀÛÀ§ ȸÀüÀ» ÀÌ¿ëÇÑ Ãִ뿬¼â ¸ðÇüÀ¸·Î ÀÀÁý¹°ÁúÀÇ »ç¿µµéÀ» µµÃâÇÏ¿´À¸¸ç, ±× ȸÀü¹Ý°æ¿¡ ÀÇÇØ »ç¿µµéÀÇ ÂʰŸ® Â÷¿øÀ» ±¸ÇÏ¿´´Ù. Àú¿¡¼º ºÎÀ¯¿µ¿ª¿¡¼­ÀÇ ÀÀÁý¹°Áú(Brownian ¿µ¿ªÀ» ¹þ¾î³ª ħ°­ÇÏ´Â ÀÀÁý¹°Áú)´Â ºñ±¸Çü ÀÔÀÚµéÀÇ Ä§°­À¸·Î °£ÁֵǾîÁø´Ù. ÃÖÁ¾ ħ°­¼Óµµ Â÷ÀÌ·Î À̵é ÀÀÁý¹°µéÀº ÀçÂ÷ Ãæµ¹, °áÇÕÇÏ¿© º¸´Ù Å« ÀÀÁý ÀÔÀÚµéÀ» Çü¼ºÇϸç, À̵é ÃÖÁ¾ ÀÀÁýÀÔÀÚµéÀÇ »ç¿µÀÌ ¸ðÀǵǾîÁø´Ù. ÃÖ´ë Feret's Á÷°æ°ú Minkowski's sausage logic °³³äµéÀ» ÀÌ¿ëÇÏ¿© ¸ðÀǵǾîÁø »ç¿µµéÀÇ µÑ·¹ ±æÀÌ¿¡ ´ëÇÏ¿© ÂʰŸ® Â÷¿øµéÀ» ±¸ÇÏ¿´´Ù.
Cohesie sediment movement in estuarine systems is strongly affected by the phenomena of aggregation and flocculation. Aggregation is the process where primary particles are clustered together in tightly-packed formations; flocculation is the process where aggregates and single particles are bonded together to form large particle groups of very low specific density. The size, shape and strength of the flocculants control the rate of deposition and the processes of pollutant exchange between suspended sediments and ambient water. In estuarine waters, suspended sediments above the lutocline form the mobile suspension zone while below the lutocline they form the stationary suspension zone. Suspended particles in the mobile zone are generally in a dispersed state and the controlling forces are the Brownian motion and the turbulent flow fluctuations. In the stationary suspension zone, the driving force is the gravity. This paper discusses the settling and particle flocculation characteristics under quiescient flow conditions. Particles are entering the study domain randomly. Particles in the mobile suspension zone are simulated by using the Smoluchowski's model. Flocs created in the mobil suspension zone are moving into the stationary suspension zone where viscosity and drag effects are important. Utilizing the concepts of the maximum Feret's diameter and the Minkowski's sausage logic, the fractal dimension of the flocs within the stationary suspension is estimated and then compared with results obtained by other studies.
 
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.27, no.3, 1994³â, pp.115-121
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199411920095079)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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