Announcements
description
Transcript of Announcements
Announcements
• Tonight ASHRAE Student Chapter Meeting
Objectives
• Finish with review thermodynamics
• Learn about Psychrometrics
p-h diagram
Ideal gas law
• Pv = RT or PV = nRT • R is a constant for a given fluid
• For perfect gasses• Δu = cvΔt
• Δh = cpΔt
• cp - cv= R
KkgkJ314.8
Rlbf
lbmft1545
MMR
M = molecular weight (g/mol, lbm/mol)P = pressure (Pa, psi)V = volume (m3, ft3)v = specific volume (m3/kg, ft3/lbm)T = absolute temperature (K, °R)t = temperature (C, °F)u = internal energy (J/kg, Btu, lbm)h = enthalpy (J/kg, Btu/lbm)n = number of moles (mol)
Mixtures of Perfect Gasses
• m = mx my
• V = Vx Vy
• T = Tx Ty
• P = Px Py
• Assume air is an ideal gas• -70 °C to 80 °C (-100 °F to 180 °F)
Px V = mx Rx∙TPy V = my Ry∙T
What is ideal gas law for mixture?
m = mass (g, lbm)P = pressure (Pa, psi)V = volume (m3, ft3)R = material specific gas constantT = absolute temperature (K, °R)
Mass-Weighted Averages
• Quality, x, is mg/(mf + mg)• Vapor mass fraction
• φ= v or h or s in expressions below• φ = φf + x φfg
• φ = (1- x) φf + x φg
s = entropy (J/K/kg, BTU/°R/lbm)m = mass (g, lbm)h = enthalpy (J/kg, Btu/lbm)v = specific volume (m3/kg)
Subscripts f and g refer to saturated liquid and vapor states and fg is the difference between the two
Properties of water
• Water, water vapor (steam), ice• Properties of water and steam (pg 675 – 685)
• Alternative - ASHRAE Fundamentals ch. 6
Humidity Ratio, W
• W = mw/ma
• Degree of saturation, µ = W/Ws
• Humidity ratio is hard to measure, but very useful in calculations
• What are units?• Is W a function of temperature? What about
Ws? Ws = humidity ratio at saturationma = mass of dry airmw = mass of water vapor
Relative Humidity
• Φ = xw/xw,s = Pw/Pws
• Function of T
Easy to measure and useful in some contexts, but often need to know temperature as well
WWs
622.0622.0
x = mole fractionP = pressureμ = degree of saturationW = humidity ratio
Dew-point temperature, td
• Temperature at which condensation will form• Under appropriate surface conditions
• Vapor is saturated• Φ = ?• Ws(P, td) = W
Wet-bulb temperature, VBT (t*)• Temperature of wet surface or
• Temperature at which water, by evaporating into the air, will bring air to saturation adiabatically
• * superscript is designation that variable is evaluated at the wet-bulb temperature
• Note, distinct from that measured by a sling psychrometer• Section 9.5
Tables for Moist Air (P = 1 atm)
• Tables A.4 in your text• Ability to get Ws for calculations• Subscripts:
• a = dry air, s = saturated air
v = va+µvas
h = ha+µhas
s = sa+µsas
Psychrometric Chart
• Need two quantities for a state point• Can get all other quantities from a state point
• Can do all calculations without a chart• Often require iteration• Many “digital” psychrometric charts available
• Can make your own• Best source is ASHRAE fundamentals (Chapter 6)
• Also in your text (back cover fold-out)
Alternate calculation for W
• PV = mRT (IGL)
• What do we know about R ratio?• P = Pw + Pa
w
a
a
w
TRVPTRVP
a
wRR
PP
mmW
a
a
w
w
w
wPP
PW
622.0
R = gas constantP = pressureV = volumeT = absolute temperatureW = humidity ratio
Subscripts: w is water vapor, a is dry air
Calculation of psychometric quantities
• For an ideal gas,• hda = ∫cpadT, hw = ∫cpwdT
• So, hda = cp,dat which assumes a reference state of 0 °F or 0 °C – Tables A4• Note different reference
• hw = cpwt + hg0
• h = cp,dat + W(cpwt + hg0)Or you can use:• h = cpt + W∙hg0, cp = cp,da + Wcpw
cp = specific heath = enthalpyT = absolute temperaturet = temperature W = humidity ratio
Subscripts: w is water vapor, a is dry air, g is saturated water vapor
Adiabatic mixing
• Governing equation hmQhmoutin
External heat
Sensible heating
tcmQ p
Dehumidification by Cooling
Real Dehumidification Process