Download presentation
Presentation is loading. Please wait.
1
Moisture Measurement
2
Sensible heat and Latent heat
3
Equation of state, gas law of dry air
Water vapor in the Air 1. Water vapor pressure
4
2. Mixing ratio, r 3. Specific humidity, q
5
Relationship between Vapor Pressure and Saturation
Saturated water vapor pressure, E
6
4. Clausius-Clapeyron equation
5. Relative humidity, h 6. Dew-point, the temperature to which air is cooled to become saturated at constant pressure.
7
7. Moist virtual effect Tv: the temperature that dry air would need to have at the given pressure in order to have the same density as moist air, assuming idea gas behavior. If it’s saturated, rl is the liquid water mixing ratio
8
Moisture measurement Dry bulb temperature Wet bulb temperature
9
Enthalpy U: internal energy (in joules), p: pressure of the system, (in pascals) V : volume, (in cubic meters) The change of enthalpy is more useful in thermodynamics The first law of thermodynamics Work may be represented by Thus, For isobaric process
10
Wet bulb temperature Since
12
Other Humidity Measurements
Physical principles: condensation
13
How to measure moisture below freezing ?
Sling psychrometer How to measure moisture below freezing ? A fan draws outside air past a thermometer to measure the ambient dry-bulb temperature, A heating device, A second thermometer to measure the dry-bulb temperature of the heated air, 4. A wet-bulb thermometer heating
14
Hair tension hygrometer
15
Electronic hygrometers
Capacitive sensor Capacitive sensors sense water vapor by measuring the change in capacitance caused by the amount of water vapor present Resistive sensor Resistive sensors use a thin film that changes conductivity according to absorbed water. Polymer membrane
16
Extinction of light At certain wavelengths the absorption and scattering of light can be a strong function of water vapor density. Lyman alpha hydrometer
Similar presentations
© 2024 SlidePlayer.com Inc.
All rights reserved.