Ultrasonic particle size fractionation in a moving air stream.
Identification of bio-aerosol particles may be enhanced by size sorting before applying analytical techniques. In this paper, the use of ultrasonic acoustic radiation pressure to continuously size fractionate particles in a moving air stream is described. Separate particle-laden and clean air streams are introduced into a channel and merged under laminar flow conditions. An ultrasonic transducer, mounted flush to one wall of the channel, excites a standing ultrasonic wave perpendicular to the flow of the combined air stream. Acoustic radiation forces on the particles cause them to move transverse to the flow direction. Since the radiation force is dependent upon the particle size, larger particles move a greater transverse distance as they pass through the standing wave. The outlet flow is then separated into streams, each containing a range of particle sizes. Experiments were performed with air streams containing glass microspheres with a size distribution from 2-22 microm, using a centerline air stream velocity of approximately 20 cm/s. An electrostatic transducer operating at a nominal frequency of 50 kHz was used to drive an ultrasonic standing wave of 150 dB in pressure amplitude. The microsphere size distributions measured at the outlet were compared with the predictions of a theoretical model. Experiments and theory show reasonable correspondence. The theoretical model also indicates an optimal partitioning of the particle-laden and clean air inlet streams.
Budwig
Ralph S
RS
Department of Mechanical Engineering, University of Idaho, Moscow, ID 83844-0902, USA.
Anderson
Michael J
MJ
Putnam
Gabriel
G
Manning
Chris
C
D000388:Air; D005591:Chemical Fractionation / Q000379:methods*; D003198:Computer Simulation; D008956:Models, Chemical; D009038:Motion; D010316:Particle Size; D052638:Particulate Matter / Q000032:analysis / Q000737:chemistry* / Q000528:radiation effects*; D013010:Sonication / Q000379:methods*
D052638:Particulate Matter