Abstract
미세하게 부유된 입자(alumina(Al<TEX>$_2$</TEX>O<TEX>$_3$</TEX>), quartz(SiO<TEX>$_2$</TEX>))의 침전 농도를 물리-화학적(초기농도, pH, NaCl)인 영향을 고려하면서 연구하였다. 침강실험은 입자사이의 끌어당기는 힘 때문에 Flocculation(플록 형성)이 일으키는 초기농도와 NaCl의 증가가 중요한 영향을 미치며, 더욱이 미립자(alumina(Al<TEX>$_2$</TEX>O<TEX>$_3$</TEX>))의 농도-시간 곡선에 pH의 영향이 매우 큼을 보였다. 또한 정지수면 조건하에서 미립자의 침전 거동예측을 위한 수치 모델은 부정류 1차원 이송방정식에 의해 분석되었으며 양해법, 음해법, Crank-Nicolson 기법 및 유한차분법을 이용하였다. 수치모델은 평형을 이룬 농도변화까지 예측하였으며, 실험치의 비교분석을 통해 중앙차분법을 통한 Implicit 모형의 계산이 대체로 일치하였다. The settling concentration of fine suspended solid particles(alumina(Al<TEX>$_2$</TEX>O<TEX>$_3$</TEX>) and quartz(SiO<TEX>$_2$</TEX>)) is investigated with the physico-chemical effects(initial concentration, pH and NaCl). Laboratory tests have confirmed the significant influence of increasing initial concentration and salinity which can lead to flocculation due to the intermolecular attraction. Furthermore, the influence of the pH value on the concentration-time corves of alumina has been on firmed. Besides a numerical model to predict the behaviour of cohesive deposit under still water is analyzed by solving the unsteady one-dimensional diffusion-advection equation with a explicit, implicit, Crank-Nicolson and finite difference scheme. The model predicts the existence of an equilibrium concentration. Application of the model with implicit centered difference to data from settling experiments shows a similar distribution.
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