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An '''electron avalanche''' is a process in which a number of [[free electron]]s in a [[transmission medium]] are subjected to strong acceleration by an [[electric field]] and subsequently collide with other atoms of the medium, thereby [[ion]]izing them ([[impact ionization]]). This releases additional electrons which accelerate and collide with further atoms, releasing more electrons—a [[chain reaction]]. In a [[gas]], this causes the affected region to become an [[electrically conductive]] [[plasma (physics)|plasma]].
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The avalanche effect was discovered by [[John Sealy Townsend]] in his work between 1897 and 1901, and is also known as the [[Townsend discharge]].
 
Electron avalanches are essential to the [[dielectric breakdown]] process within gases. The process can culminate in [[corona discharge]]s, [[streamer]]s, [[leader (spark)|leader]]s, or in a [[electric spark|spark]] or continuous [[electric arc|arc]] that completely bridges the gap between the electrical conductors that are applying the voltage. The process extends to huge sparks — streamers in [[lightning]] discharges propagate by formation of electron avalanches created in the high [[potential gradient]] ahead of the streamers' advancing tips. Once begun, avalanches are often intensified by the creation of [[photoelectron]]s as a result of [[ultraviolet]] radiation emitted by the excited medium's atoms in the aft-tip region.
 
The process can also be used to detect ionizing radiation by using the ''gas multiplication effect'' of the avalanche process. This is the ionisation mechanism of the [[Geiger–Müller tube]] and, to a limited extent, of the [[proportional counter]]<ref name= "knoll"> Glenn F Knoll, 'Radiation Detection and Measurement' 3rd edition, 2000, John Wiley and sons Inc.</ref> and is also used in [[spark chamber]]s and other [[wire chamber]]s.
 
==Analysis==
A plasma begins with a rare natural 'background' ionization event of a neutral air molecule, perhaps as the result of [[photoexcitation]] or [[background radiation]]If this event occurs within an area that has a high [[potential gradient]], the positively [[electric charge|charged]] [[ion]] will be strongly attracted toward, or repelled away from, an [[electrode]] depending on its polarity, whereas the electron will be [[acceleration|accelerated]] in the opposite direction. Because of the huge mass difference, electrons are accelerated to a much higher [[velocity]] than ions.
 
High-velocity electrons often collide with neutral atoms inelastically, sometimes ionizing them. In a [[Chain reaction|chain-reaction]] — or an 'electron avalanche' — additional electrons recently separated from their positive ions by the strong potential gradient, cause a large cloud of electrons and positive ions to be momentarily generated by just a single initial electron. However, free electrons are easily ''captured'' by neutral oxygen or water vapor molecules (so-called [[electronegativity|electronegative]] gases), forming negative ions. In air at [[Standard conditions for temperature and pressure|STP]], free electrons exist for only about 11 [[nanosecond]]s before being captured. Captured electrons are effectively removed from play — they can no longer contribute to the avalanche process. If electrons are being created at a rate greater than they are being lost to capture, their number rapidly multiplies, a process characterized by [[exponential growth]]. The degree of multiplication that this process can provide is huge, up to several million-fold depending on the situation. The multiplication factor ''M'' is given by
 
<math>M = \frac{1}{1-\int_{X_1}^{X_2} \alpha\, dx}</math>
 
Where ''X''<sub>1</sub> and ''X''<sub>2</sub> are the positions that the multiplication is being measured between, and α is the ionization constant. In other words, one free electron at position ''X''<sub>1</sub> will result in ''M'' free electrons at position ''X''<sub>2</sub>. Substituting the voltage gradients into this equation results in
 
<math>M = \frac{1}{1-|\frac{V}{V_\mathrm{BR}}|^n}</math>
 
Where ''V'' is the applied voltage, ''V''<sub>BR</sub> is the breakdown voltage and ''n'' is an empirically derived value between 2 and 6. As you can see from this formula, the multiplication factor is very highly dependent on the applied voltage, and as the voltage nears the breakdown voltage of the material, the multiplication factor approaches infinity and the limiting factor becomes the availability of charge carriers.
 
Avalanche sustenance requires a reservoir of charge to sustain the applied voltage, as well as a continual source of triggering events. A number of mechanisms can sustain this process, creating avalanche after avalanche, to create a [[corona discharge|corona]] current. A secondary source of [[plasma (physics)|plasma]] electrons is required as the electrons are always accelerated by the field in one direction, meaning that avalanches always proceed linearly toward or away from an [[electrode]]. The dominant mechanism for the creation of [[secondary electrons]] depends on the polarity of a plasma. In each case, the [[energy]] emitted as [[photon]]s by the initial avalanche is used to [[ionise]] a nearby gas molecule creating another accelerable electron. What differs is the source of this electron. When one or more electron avalanches occur between two electrodes of sufficient size, complete [[avalanche breakdown]] can occur, culminating in an electrical [[Electrostatic discharge|spark]] that bridges the gap.
 
== See also ==
* [[Townsend discharge]]
* [[Avalanche breakdown]]
* [[Avalanche diode]]
* [[Corona discharge]]
* [[Multipactor]]
* [[Geiger–Müller tube]]
* [[Geiger counter]]
* [[spark chamber]]
* [[wire chamber]]
* [[Runaway breakdown]]
* [[List of plasma (physics) articles]]
 
== References ==
{{Reflist}}
* [http://ece-www.colorado.edu/~bart/book/book/chapter4/ch4_5.htm Breakdown effects in semiconductors ]
 
[[Category:Electrical breakdown]]

Latest revision as of 19:46, 8 January 2015

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