Streamers can emerge when a strong electric field is applied to an insulating material, typically a gas. Streamers can only form in areas where the electric field exceeds the
dielectric strength (breakdown field, disruptive field) of the medium. For air at atmospheric pressure, this is roughly 30 kV per centimeter. The electric field accelerates the few
electrons and
ions that are always present in air, due to natural processes such as
cosmic rays,
radioactive decay, or
photoionization. Ions are much heavier, so they move very slowly compared to electrons. As the electrons move through the medium, they collide with the neutral molecules or atoms. Important collisions are: •
Elastic collisions, which change the direction of motion of the electrons. •
Excitations, where the neutral particle is excited, and the electron loses the corresponding energy. •
Impact ionization, where the neutral particle becomes ionized, with the incident electron losing the energy. •
Attachment, where the electron attaches to the neutral to form a negative ion. When the electric field approaches the breakdown field, the electrons gain enough energy between collisions to ionize the gas atoms, knocking an electron off the atom. At the breakdown field, there is a balance between the production of new electrons (due to impact ionization) and the loss of electrons (due to attachment). Above the breakdown field, the number of electrons starts to grow exponentially, and an
electron avalanche (
Townsend avalanche) forms. The electron avalanches leave behind positive ions, so in time more and more
space charge is building up. (Of course, the ions move away in time, but this a relatively slow process compared to the avalanche generation as ions are much heavier than electrons). Eventually, the electric field from all the space charge becomes comparable to the background electric field. This is sometimes referred to as the "avalanche to streamer transition". In some regions the total electric field will be smaller than before, but in other regions it will get larger, which is called electric field enhancement. New avalanches predominantly grow in the high-field regions, so a self-propagating structure can emerge: a streamer.
Positive and negative streamers In
direct current (DC) circuits, the streamers that form at electrodes with positive and negative voltages are different in appearance and form by different physics mechanisms. Negative streamers propagate against the direction of the electric field, that is, in the same direction as the electrons
drift velocity. Positive streamers propagate in the opposite direction. In both cases, the streamer channel is electrically neutral, and it is shielded by a thin space charge layer. This leads to an enhanced electric field at the end of the channel, the "head" of the streamer. Both positive and negative streamers grow by impact ionization in this high-field region, but the source of electrons is very different. For negative streamers, free electrons are accelerated from the channel to the head region. However, for positive streamers, these free electrons have to come from farther away, as they accelerate into the streamer channel. Therefore, negative streamers grow in a more diffuse way than positive streamers. Because a diffuse streamer has less field enhancement, negative streamers require higher electric fields than positive streamers. In nature and in applications, positive streamers are therefore much more common. As noted above, an important difference is also that positive streamers need a source of free electrons for their propagation. In many cases
photoionization is believed to be this source. In nitrogen-oxygen gas mixtures with high oxygen concentrations, excited nitrogen emits UV photons which subsequently ionize oxygen. In pure nitrogen or in nitrogen with small oxygen admixtures, the dominant production mechanism of photons, however, is the
Bremsstrahlung process.
Streamer velocity and other parameters The electric streamer, strictly speaking, is an ionization front in the shape of a growing filament. One may identify, at least approximately, a set of parameters that characterizes this particularly shaped front, such as the velocity of its growth, the radius of the head etc, as well as physical laws (equations) that relate these parameters to each other. In one theory of electric streamers in air, the streamer "chooses" the maximum available velocity (with other parameters being uniquely determined by the said laws), similarly to how a linear instability, e.g., in a plasma, would "choose" the wavelength that gives the fastest growth. This approach gives good agreement with experimental data on positive streamer speeds and on the negative streamer threshold, as well as with the results from a simulation by directly solving hydrodynamic equations.
Similarity laws Most processes in a streamer discharge are two-body processes, where an electron collides with a neutral molecule. An important example is
impact ionization, where an electron ionizes a neutral molecule. Therefore, the
mean free path is inversely proportional to the gas
number density. If the electric field is changed linearly with the gas number density, then electrons gain on average the same energy between collisions. In other words, if the ratio between electric field E and number density N is constant, we expect similar dynamics. Typical lengths scale as 1/N, as they are related to the mean free path. This also motivates the
Townsend unit, which is a physical unit of the E/N ratio. == Emission of run-away electrons and high-energy photons ==