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A Microfluidic-based Hydrodynamic Trap for Single Particles
Published on: January 21, 2011
16.0K
Low-temperature Bessel beam trap for single submicrometer aerosol particle studies
Jessica W Lu1, Merrill Isenor1, Egor Chasovskikh1
1Laboratory of Physical Chemistry, ETH Zürich, Vladimir-Prelog-Weg 2, CH-8093 Zürich, Switzerland.
The Review of Scientific Instruments
|October 3, 2014
Summary
Researchers developed a new instrument using optical trapping to study single aerosol particles at low temperatures. This method allows observation of freezing processes in supercooled droplets, advancing aerosol science.
Area of Science:
- Atmospheric Chemistry
- Physical Chemistry
- Optical Physics
Background:
- Understanding aerosol particle phase transitions is crucial for climate and atmospheric processes.
- Previous methods for studying single aerosol particles at low temperatures have limitations.
Purpose of the Study:
- To introduce a novel instrument for studying single aerosol particles at low temperatures.
- To investigate the freezing and evaporation behavior of individual aerosol particles.
Main Methods:
- Utilizing a dual counter-propagating Bessel beams (CPBBs) optical trap for particle levitation.
- Implementing precise temperature control down to 223 K (-50 °C) for aerosol studies.
- Capturing and stably trapping individual submicrometer to micrometer-sized aerosol particles for extended periods.
Main Results:
- Successfully trapped and froze supercooled hexadecane, dodecane, and water droplets (radius ~450 nm to 5500 nm).
- Conducted experiments on homogeneous and heterogeneous freezing, freezing-melting cycles, and evaporation.
- Achieved the first reported observation of the freezing process for levitated single submicrometer droplets using optical trapping.
Conclusions:
- The temperature-controlled CPBB trap is a powerful new tool for single aerosol particle research.
- This technique enables detailed studies of phase transitions in atmospheric aerosols.
- The findings open new avenues for understanding aerosol behavior in the atmosphere.

