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Atomic Absorption Spectroscopy: Atomization Methods

Atomic Absorption Spectroscopy (AAS) atomizes samples through flame atomization or electrothermal atomization. Flame atomization typically involves a nebulizer and spray chamber assembly to combine the sample with a fuel–oxidant mixture, creating a fine aerosol mist that enters a burner. Typically, the fuel and oxidant are combined in an approximately stoichiometric ratio. However, for atoms that are easily oxidized, a fuel-rich mixture may be more advantageous. Only about 5% of the aerosol...
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A Microfluidic-based Hydrodynamic Trap for Single Particles
10:13

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Published on: January 21, 2011

Can aerosols be trapped in open flows?

Rafael D Vilela1, Adilson E Motter

  • 1Max Planck Institute for the Physics of Complex Systems, 01187 Dresden, Germany.

Physical Review Letters
|February 1, 2008
PubMed
Summary

Finite-size aerosols can become permanently trapped in open chaotic advection flows, contrary to previous assumptions. This trapping occurs even for heavy particles, influenced by multiple vortices and realistic density ratios.

Area of Science:

  • Fluid dynamics
  • Particle transport
  • Chaos theory

Background:

  • Aerosol behavior in open flows is crucial for understanding particle transport.
  • Previous studies suggested finite-size particles always escape chaotic advection.
  • The dynamics of aerosols are influenced by fluid flow characteristics and particle properties.

Purpose of the Study:

  • To investigate the fate of aerosols in open chaotic advection flows.
  • To analyze aerosol dynamics under varying conditions, including gravity and fluid particle behavior (hyperbolic vs. nonhyperbolic).
  • To identify mechanisms leading to aerosol trapping or escape.

Main Methods:

  • Analysis of aerosol dynamics in open flows.
  • Consideration of gravitational effects on particle trajectories.

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  • Examination of both hyperbolic and nonhyperbolic fluid particle dynamics.
  • Investigation of flows with multiple vortices.
  • Main Results:

    • Demonstrated that aerosols can be permanently trapped in open chaotic advection.
    • Showed this trapping occurs irrespective of gravitational effects or fluid dynamics type (hyperbolic/nonhyperbolic).
    • Identified the presence of multiple vortices as the key factor for trapping.
    • Confirmed the phenomenon for realistic particle-fluid density ratios.

    Conclusions:

    • Finite-size aerosols can exhibit permanent trapping in open chaotic advection, challenging prior assumptions.
    • The phenomenon of aerosol trapping is robust, occurring under various physical conditions including realistic density ratios.
    • Multiple vortices in the flow are critical for inducing permanent aerosol trapping.