Reverse diffusion

Reverse diffusion refers to a situation where the transport of particles (atoms or molecules) in a medium occurs towards regions of higher concentration gradients, opposite to that observed during diffusion. This phenomenon occurs during phase separation and is described by the Cahn–Hilliard equation. Reverse diffusion also refers to when water is forced from a region of lower concentration to high. It can occur in osmosis.

cs:Reverzní osmóza

This article does not cite any external source. HandWiki requires at least one external source. See citing external sources. Please help improve this article. Unsourced material may be removed in future.
Find sources: "Reverse diffusion" – news · newspapers · books · scholar · JSTOR (2021) (Learn how and when to remove this template message)

|

0.00

(0 votes)

Original source: https://en.wikipedia.org/wiki/Reverse diffusion. Read more

|

Retrieved from "https://handwiki.org/wiki/index.php?title=Physics:Reverse_diffusion&oldid=291172"