Negative air ions
Negative air ions are negatively charged single gas molecules or ion clusters in the air. They play a role in maintaining the charge balance of the atmosphere. The main components of air are molecular nitrogen and oxygen. Due to the strong electronegativity of oxygen and oxygen-containing molecules, they can easily capture electrons to form negatively charged air ions, most of which are superoxide radicals ·O2−, so NAI are mainly composed of negative oxygen ions, also called air negative oxygen ions.
The ions can be produced by natural means such as lightning, or artificially by methods such as a corona discharge. They can play a role in electrostatic removal of air particulates both for industrial applications and with indoor air, and there are claims that they have a beneficial health effect although the evidence for this is weak.
Generation mechanism
Various negative air ions are formed by combining active neutral molecules and electrons in the gas through a series of ion-molecule reactions.In the air, due to the presence of many water molecules, the negative air ions typically combine with water to form hydrated negative air ions, such as O−·n, O2−·n, O3−·n, OH−·n, CO3−·n, HCO3−·n, CO4−·n, NO2−·n, NO3−·n, etc. The ion clusters formed by the combination of small ions and water molecules have a longer survival period due to their large volume and the fact that the charge is protected by water molecules and is not easy to transfer. This is because in the molecular collision, the larger the molecular volume, the less energy is lost when encountering collisions with other molecules, thereby extending the survival time of negative air ions.
Generation methods
Negative air ions can be produced by two methods: natural or artificial. The methods of producing negative air ions in nature include the waterfall effect, lightning ionization and from plants. Natural methods can produce a large number of negative air ions. The artificial means of producing negative air ions include corona discharge and water vapour. Compared with the negative air ions produced in nature, although artificial methods can produce high levels of negative air ions, there are differences in the types and concentrations of negative air ions.Natural environments
Waterfall method
The mechanism of producing negative air ions by the waterfall method connects to the generation of static electricity due to water droplets hitting surfaces, first discovered by Philipp Lenard in 1892 and now called the spray electrification or waterfall effect. Falling water generates static electricity either by collisions between water drops or with the ground, leading to the finer mist in updrafts being mainly negatively charged, with positive near the lower surface. It can also occur for sliding drops. The experimental fact that charging occurs is very well documented, although details of the exact process remain a topic of debate. High speed video observations show how water spray can breakup into different droplets. Larger droplets tend to be positively charged, while smaller ones negative; this charge separation is also well documented for solids. For instance it occurs in commercial powder processing and in natural processes such as dust storms, There can be electric fields of up to 160kV/m with moderate wind conditions, which leads to Coulomb forces of about the same magnitude as gravity.There can also be contributions from contact potential differences between liquids or gases and other materials, similar to the work function differences for solids. It has been suggested that a triboelectric series for liquids is useful. One difference from solids is that often liquids have charged double layers, and most of the work to date supports that ion transfer dominates for liquids as first suggested by Irving Langmuir in 1938.
All these processes will lead to charges, relatively high electric fields and these in turn can lead to the formation of gaseous ions.
Lightning strike
In the atmosphere positive and negative charges will accumulate above and below the clouds. One of the most commonly cited ways that charge separation is generated is via the collisions of different forms of solid ice, for instance graupel and ice particles. Similar to the collisions between other types of particles mentioned above, the ice particles become positively charged and the graupel negative. The two have different densities, with the ice particles tending to rise and the graupel fall or move towards the center of the storm.This charge separation in different regions of the clouds leads to large electric fields. When the electric field strength between the cloud and the ground or different parts of a storm exceeds the dielectric strength of the air, discharge will occur and break through the air. During the lightning discharge process, charged particles bombard the surrounding air molecules, ionizing the molecules to generate negative air ions. At the moment of the lightning strike, hundreds of millions of negative air ions will be generated.