There are quite a few methods for measuring moisture in gases, roughly
into two categories: a direct measurement using an alternation amount
of gaseous property. We have established a technology for trace moist
ure measurement in gases by optimizing a dew point method, one of the
direct categories of measurement. Dew points are defined as the surfac
e temperature at which dew or frost starts to form on a mirror during
cooling of the mirror. To obtain moisture concentrations from measured
dew points, calculations should be carried out based on a saturation
vapor pressure curve for moisture. However equilibrium must be reached
. That is, temperatures should be measured when moisture coexists in g
as and liquid or solid phase and their partial pressure is equal to ea
ch other. Using this principle, measuring the phase changes of moistur
e in the equilibrium state enables us to measure trace moisture in gas
es more accurately.