Cookies Policy
X

This site uses cookies. By continuing to browse the site you are agreeing to our use of cookies.

I accept this policy

Find out more here

Experimental study on both ionic wind and resuspension of particles under unequal electrostatic field

No metrics data to plot.
The attempt to load metrics for this article has failed.
The attempt to plot a graph for these metrics has failed.
The full text of this article is not currently available.

Brill’s MyBook program is exclusively available on BrillOnline Books and Journals. Students and scholars affiliated with an institution that has purchased a Brill E-Book on the BrillOnline platform automatically have access to the MyBook option for the title(s) acquired by the Library. Brill MyBook is a print-on-demand paperback copy which is sold at a favorably uniform low price.

This Article is currently unavailable for purchase.
Add to Favorites
You must be logged in to use this functionality

Ionic wind and resuspension of particles under an unequal electrostatic field have been investigated experimentally using a needle electrode and grounded plate where fine particles are deposited. As voltage is applied to the needle electrode, a straight stream is immediately generated around the needle. Then the straight stream induces a new flow around it. When the straight stream impacts on the target, circulated flow is generated and grows gradually with time. Finally, an almost steady jet stream is formed. Ionic current from the needle to the target increases with almost the square of the electrostatic field between the needle and particle layer. If the strength of the electrostatic field is high enough, most of particles are resuspended from the layer immediately after the voltage is applied to the needle. However, if the strength is reduced, some heaps remain on the layer. Resuspension of particles occurred in two stages. The more the initial mass of the layer, the faster the resuspension velocity of particles in the first stage. The velocity increases almost linearly with the electrostatic field. The fact suggests that the velocity in the first stage is related to the theoretical maximum velocity of the ionic wind.

10.1163/156855206775123485
/content/journals/10.1163/156855206775123485
dcterms_title,pub_keyword,dcterms_description,pub_author
10
5
Loading
Loading

Full text loading...

/content/journals/10.1163/156855206775123485
Loading

Data & Media loading...

http://brill.metastore.ingenta.com/content/journals/10.1163/156855206775123485
Loading

Article metrics loading...

/content/journals/10.1163/156855206775123485
2017-07-25

Sign-in

Can't access your account?
  • Key

  • Full access
  • Open Access
  • Partial/No accessInformation