Island growth

Island growth is a physical model of deposited film growth and chemical vapor deposition.[1]

Consider a situation where atoms are being deposited onto a flat surface at a very slow rate. The first atom deposited undergoes a random walk on the surface. Eventually a second atom is deposited and can be expected to eventually meet the first atom, given enough time. Once the two atoms meet they may bond to form a particle with a higher mass and a lower random walk velocity. Because the bonded particles are now more stable and less mobile than before, they are called an "island". Subsequent atoms deposited on the substrate eventually meet and bond with the island, further increasing its size and stability. Eventually the island can grow to fill the entire substrate with a single large grain.

If atoms are being deposited at a faster rate, there will be many atoms present on the substrate before any large stable islands form. As these atoms meet, they will bond to their local neighbors before having the chance to migrate to a distant island. In this way a large number of separate islands are formed and can grow independently. Eventually the separate islands will grow to become separate grains in the final film.

The island growth model is used to explain how fast deposition techniques (such as sputter deposition) can produce films with many randomly oriented grains, whereas slow deposition techniques (such as MBE) tend to produce larger grains with more uniform structure.

See also

Stranski–Krastanov growth

References

  1. ↑ "Film Formation: Growth and Coalescence". Uccs.edu. Retrieved 2016-06-17.
This article is issued from Wikipedia - version of the 6/17/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.