• 제목/요약/키워드: chaotic mixing

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새로운 CSC micromixer 를 이용한 유동가시화 (Flow Visualization in a new CSC micromixer)

  • 카니카싱;김형훈;민영욱;김현동;김경천
    • 한국가시화정보학회:학술대회논문집
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    • 한국가시화정보학회 2007년도 추계학술대회
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    • pp.63-65
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    • 2007
  • The paper reports on a new type of combinatorial chaotic and serpentine micromixer. Such a new and novel micromixer is simple to fabricate and easy to use. The micromixer is characterized and visualized with the help of the Micro-LIF technique. The new micromixer will e further applied to lab-on-chip device. The mixing capabilities of this mixer is about 30-33%.

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Vibration-Rotation Coupling in a Quasilinear Symmetric Triatomic Molecule

  • Lee, Jae-Shin
    • Bulletin of the Korean Chemical Society
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    • 제15권3호
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    • pp.228-236
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    • 1994
  • The effect of the vibration mode coupling induced by the vibration-rotation interaction on total energy was investigated for the states with zero total angular momentum(J=0) in a quasilinear symmetric triatomic molecule of $AB_2$ type using a model potential function with a slight potential barrier to linearity. It is found that the coupling energy becomes larger for the levels of bend and asymmetric stretch modes and smaller for symmetric stretch mode as the excitation of the vibrational modes occurs. The results for the real molecule of $CH_2^+$, which is quasilinear, generally agree with the results for the model potential function in that common mode selective dependence of coupling energy is exhibited in both cases. The differences between the results for the model and real potential function in H-C-H system are analyzed and explained in terms of heavy mixing of the symmetric stretch and bend mode in excited vibrational states of the real molecule of $CH_2^+$. It is shown that the vibrational mode coupling in the potential energy function is primarily responsible for the broken nodal structure and chaotic behavior in highly excited levels of $CH_2^+$ for J= 0.

엇갈림형 스크류 채널 내부의 스톡스 유동과 혼합특성 해석 (Analysis of the Stokes Flow and Stirring Characteristics in a Staggered Screw Channel)

  • 서용권
    • 한국전산유체공학회지
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    • 제9권4호
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    • pp.55-63
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    • 2004
  • The three-dimensional Stokes flow within a staggered screw channel is obtained by using a finite volume method. The geometry is intended to mimic the single screw extruder having staggered arrangement of flights. The flow solution is then subjected to the analysis of the stirring performance. In the analysis of the stirring performance, the stretching-mapping method developed by the author is employed for calculating the materials' stretching exponents, which are to be used in quantification of the mixing effect. The numerical results Indicate that the staggered geometry gives indeed far much better stirring-performance than the standard (nonstaggered) flight geometry. It was also shown that care must be given to the selection of the basis planes for evaluating the local stretching rate, and it turns out that the best method (H-method) has its basis plane just on the half way between the past and future evolution of fluid particles subjected to the defromation. In evaluating the stretching exponent, the expansion ratio must be considered which is one of the characteristic differences of the actual three-dimensional flows from the two-dimensionmal counterparts. The larger axial pressure-difference causes in general the smaller stirring performance while the flow rate is increased. The smaller channel length also increases the stirring performance.

미세유체 바이오칩을 이용한 DNA 마이크로어레이 Hybridization 향상 (Enhancement of DNA Microarray Hybridization using Microfluidic Biochip)

  • 이현호;김용상
    • KSBB Journal
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    • 제22권6호
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    • pp.387-392
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    • 2007
  • DNA 마이크로어레이는 바이오칩의 발전에서 가장 주목받으며 발전하고 있는 분야로서 이에 대한 연구가 점차 확장하고 있다. DNA나 RNA 등 유전자의 매우 느린 확산속도를 극복하기 위하여 마이크로플루딕 바이오칩이 DNA 마이크로어레이에 적용되는 최근의 학술적인 사례들을 연구, 비교하였다. DNA 마이크로어레이에 적용된 미세유체 바이오칩은 상당수가 효율적인 hybridization을 달성하기 위한 믹싱 시스템이 많이 보고되었으며, 이 총설에서는 그에 대한 분석을 수행하여 유전자 hybridization 강화를 이룬 시스템에 대한 최근 동향을 가늠할 수 있게 하였다. 특별히 PDMS를 이용한 마이크로 펌프의 적용 등, 앞으로의 미세유체 DNA 마이크로어레이 발전가능성과 모델링의 한계점 등을 정리 분석해 보았다.

우도응회과의 분출기기구와 분출과정 (Eruptive mechanisms and processes at Udo tuff cone, Udo Island, Korea)

  • Hwang, Sang-Koo
    • 암석학회지
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    • 제1권2호
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    • pp.91-103
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    • 1992
  • Eruptive mechanisms and processes at Udo tuff cone can be inferred from indicative characters of products, bedforms and lithofacies, and ring faults. In terms of bedforms and lithofa-cies in particular, massive lapilli tuff beds and chaotic lapilli tuff beds are derived from subaerial falls of aggregated tephra of wet tephra finger jets, occurring dominantly at the lower sequences of proximal part at the tuff cone. Crudely stratified lapilli tuff are derived from subaerial falls of slightly aggregated tephra of less wet tephra finger jets, whereas reversely graded lapilli tuff beds are from slightly disaggregated subaerial falls of continuous uprush. Both beds frequently occur in the middle sequences at proximal and near medial part of the tuff cone. Block and lapilli tephra lenses, ash-coated lapilli tephra beds(lenses) and thin-bedded tuff beds are derived from extremely disaggregated subaerial falls of dry tephra in the continuous uprush, frequently occurring at the upper sequences of medial part at the tuff cone. Udo tuff cone is a basaltic volcano emergent through the sea water surface while water could flood across or into the vent area. Emergence of the tuff cone was from the type-Surtseyan eruption characterized by earlier tephra finger jets and later continuous uprush columns of tephra with copious volumes of steam. Explosions began when boiling of wter produced a bubble column reducing the hydrostatic pres-sure, allowing exsolution of gases from the magma. This expansion of magma into a vesiculating froth fragmented the magma and permitted mixing of magma and water so that a more vigorous generation of steam could proceed. Tephra finger jetting explosions continued to build the crater rims, then remove water from the vent that their deposits flowed like slsurries until the continuous uprush explosion ensued. Continuous uprush explosions were associated with most rapid accumula-tion of tephra. The increasing volume rate led to partial removal of water from the vent area by the newly tephra ring so that more vigorous activity could be attended by a reducing water supply. This might restrain surplus of cold water entering the vent and thus enhance the vigour of the eruption by allowing optimal heat exchange. Eventually the crater became so deep and unsuported that piecemeal sliding, or massive subsidence on indipping ring faults, filled and closed the vent, and the cycle of explosions and collapse began anew.

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