Streamer discharge

A streamer discharge, also known as filamentary discharge, is a type of transient electrical discharge. Streamer discharges can form when an insulating medium (for example air) is exposed to a large potential difference. When the electric field created by the applied voltage is sufficiently large, accelerated electrons strike air molecules with enough energy to knock other electrons off them, ionizing them, and the freed electrons go on to strike more molecules in a chain reaction. These electron avalanches (Townsend discharges) create ionized, electrically conductive regions in the air near the electrode creating the electric field. The space charge created by the electron avalanches gives rise to an additional electric field.This field can enhance the growth of new avalanches in a particular direction.Then the ionized region grows quickly in that direction, forming a finger-like discharge called a streamer. A streamer discharge, also known as filamentary discharge, is a type of transient electrical discharge. Streamer discharges can form when an insulating medium (for example air) is exposed to a large potential difference. When the electric field created by the applied voltage is sufficiently large, accelerated electrons strike air molecules with enough energy to knock other electrons off them, ionizing them, and the freed electrons go on to strike more molecules in a chain reaction. These electron avalanches (Townsend discharges) create ionized, electrically conductive regions in the air near the electrode creating the electric field. The space charge created by the electron avalanches gives rise to an additional electric field.This field can enhance the growth of new avalanches in a particular direction.Then the ionized region grows quickly in that direction, forming a finger-like discharge called a streamer. Streamers are transient (exist only for a short time) and filamentary, which makes them different from corona discharges. They are used in applications such as ozone production, air purification or plasma medicine. Streamers pave the way for arcs and lightning leaders, in which the ionized paths created by streamers are heated by large currents. Streamers can also be observed as sprites in the upper atmosphere. Due to the low pressure, sprites are much larger than streamers at ground pressure, see the similarity laws below. The theory of streamer discharges was preceded by John Sealy Townsend's discharge theoryfrom around 1900.However, it became clear that this theory was sometimes inconsistent with observations.This was especially true for discharges that were longer or at higher pressure.In 1939, Loeband Raetherindependently described a new type of discharge, based on their experimental observations.Shortly thereafter, in 1940, Meek presented the theory of spark discharge,which quantitatively explained the formation of a self-propagating streamer.This new theory of streamer discharges successfully explained the experimental observations. Streamers are used in applications such as ozone generation, air purification and plasma-assisted combustion.An important property is that the plasma they generate is strongly non-equilibrium: the electrons have much higher energies than the ions.Therefore, chemical reactions can be triggered in a gas without heating it.This is important for plasma medicine, where 'plasma bullets', or guided streamers, can be used for wound treatment, although this is still experimental. 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: 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).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. There are positive and negative streamers.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.