Evaporation is one of the two forms of vaporization. It is the process whereby atoms or molecules in a liquid state (or solid state if the substance sublimes) gain sufficient energy to enter the gaseous state. It's the opposite process of condensation.
The thermal motion of a molecule of liquid must be sufficient to overcome the surface tension and evaporate, that is, its kinetic energy must exceed the work function of cohesion at the surface. Evaporation therefore, proceeds more quickly at higher temperature, at higher flow rates between the gaseous and liquid phase and in liquids with lower surface tension (i.e. higher vapor pressure). Since only a small proportion of the molecules are located near the surface and are moving in the proper direction to escape at any given instant, the rate of evaporation is limited. Also, as the faster-moving molecules escape, the remaining molecules have lower average kinetic energy, and the temperature of the liquid thus decreases. This phenomenon is also called evaporative cooling. This is the reason that evaporating sweat cools the human body.
Gas has less order than liquid or solid matter, and thus the entropy of the system is increased, which always requires energy input. This means that the enthalpy change for evaporation (ΔHevaporation) is always positive. Evaporation is a cooling process.
Evaporation is a critical component of the water cycle, which is responsible for clouds and rain. Solar energy drives evaporation of water from oceans, lakes, moisture in the soil, and other sources of water. In hydrology, evaporation and transpiration (which involves evaporation within plant stomata) are collectively termed evapotranspiration.
The ratio of the heat loss from a pond by evaporation to the heat loss due to convection, independent of windspeed, is given by:
where is the heat loss from the pond by convection, in W/(m2·K), is the heat loss from the pond by evaporation, in W/(m2·K), and are the Kelvin (or Celsius) temperatures of the water and air, and and are the vapor pressures of the pond surface and air, and is the barometric pressure, with all pressures in mm Hg. (Bowen, 1926)
For some applications, the fact that evaporative deposition proceeds in a line-of-sight fashion is an important advantage. The energy distribution of evaporated material tends to be Maxwellian, with a temperature derived from the evaporation source. In contrast, the plasmas encountered in sputtering systems are far from thermal equilibrium and may have high-energy tails that contain particles with large random velocities. Evaporation is therefore a gentler process with a better defined beam of source material that can be used to coat just one side of a substrate or even the side of etched surface features, as in MEMS processing.
The three main kinds of evaporation are thermal, electron-beam and resistive. In the thermal method, the crucible that holds the source material is radiatively heated by a filament that winds around it. In the electron-beam method, the current that heats the crucible is boiled off a filament and is attracted to the crucible by a high voltage. Electron-beam evaporation is used with the highest melting elements. Resistive evaporation is accomplished by passing a large current through a wire or foil of the material that is to be deposited. Molecular beam epitaxy is a particularly sophisticated kind of thermal evaporation.
Physical chemistry | Thermodynamics | atmospheric thermodynamics | Materials science | Thin film deposition
Isparavanje | Vypařování | Evaporation | Verdampfen | Εξάτμιση | Aurumine | Evaporación | Évaporation | התאיידות | Evaporazione | Uvukizaji | Garavimas | Verdamping | 蒸発 | fordamping | Parowanie | Evaporação | Испарение | Evaporation | Izhlapevanje | Haihtuminen | Avdunstning | 蒸发
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