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Basic Laws of Gases and Particulates. Ideal gas law Unit of concentration Vapor pressure & partial pressure Humidity & psychrometric chart Viscosity Aerosol size Aerosol size distribution Settling velocity Brownian motion and diffusion. Ideal Gas Law. P : pressure V : volume n : mole - PowerPoint PPT Presentation
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04/24/231
Basic Laws of Gases and Particulates
• Ideal gas law• Unit of concentration• Vapor pressure & partial pressure• Humidity & psychrometric chart• Viscosity• Aerosol size• Aerosol size distribution• Settling velocity• Brownian motion and diffusion
04/24/232
Ideal Gas Law
Other references:1. CRC Handbook of Chemistry & Physics2. Perry’s Chemical Engineers’ Handbook
TRnQPTRMWP
TRMWM
TRnVP
P: pressureV: volumen: moleR: Ideal gas law constantT: TemperatureM: massMW: molecular weight: densityQ: volume flow rate : molar flow raten
04/24/233
Ideal Gas Law Constant
82.057
8.314 8.314
8.314
What is the volume of 1 g-mole of air at 25 oC and 1 atm?
How many lb-moles are there for 380 ft3 of air at 60 oF and 14.7 psi?
Avogadro’s number: 6.0231023 molecules/mole
At 1 atm and 25 oC, 1 mole of air has a volume of 24.5 L
04/24/234
Unit of Concentration
Is 1 g/cm3 SO2 equal to 1 ppm SO2?
The annual standard of NO2 is 100 g/m3. What is the concentration in ppb?
Is “ppm” molar basis, volume basis or mass basis?
What’s the difference between “ACFM” and “SCFM”?
Section 7.1.2
04/24/235
Concentration on a “dry” basis• Water vapor is commonly present in a heated gas
stream, e.g., combustion of a hydrocarbon fuel. • Water vapor can condense as temperature cools down.
The amount varies and is very sensitive to temperature. • To prevent the variation, standards are written to correct
to "dry" conditions when expressing concentrations.
volume basis wet volume basis dryCO2 18% 18%*(100/88) = 20.5%
H2O 12%
O2 10% 10%*(100/88) = 11.4%
N2 60% 60%*(100/88) = 68.2%
Total = 100% (100-12)%*(100/88) = 100%
04/24/236
Vapor Pressure
The pressure required to maintain a vapor in equilibrium with the condensed vapor (liquid or solid) with a flat surface at a specified temperature
TCBATPv
)(log Pv in mmHg and T in oC (if Table 9.2 is used)
(Saturation) Vapor PressureTime to reach equilibrium
How does vapor pressure change if the temperature increases?
04/24/237
04/24/238
What is the vapor pressure of water at 20 oC? If the measurement is conducted on Mars (the atmospheric pressure is about 0.006 atm), what will be the value?
04/24/239
Partial Pressure
)100( )(
SRHTPPSv
a Supersaturation: S > 1 (RH > 100%)
Saturation Ratio (or relative humidity for water)
The pressure that a gas (or vapor) in a mixture of gases would exert if it were to occupy the entire volume occupied by the mixture
Taa PyP ya: mole fraction of component “a” in the mixture in the gas phasePT: total pressure of the system
After a shower at dusk, the temperature starts to drop. How do PV and Pa change correspondingly?
1 mole of O2 @ 1 atm
4 moles of N2
How much is PO2?
04/24/2310
Humidity in Air/Water Mixture
• Psychometric Chart (Figure 1.3)– Dry bulb temperature– Wet bulb temperature: the temperature at
which a thermometer with a wet wick wrapped around the bulb stabilizes
http://www.usatoday.com/weather/wsling.htm
• The state of an air/water mixture is determined by pressure, temperature & humidity
Properties of TDB of 40 oC and TWB of 30 oC?
Why is TDB always higher than TWB?
04/24/2311http://howard.engr.siu.edu/staff1/tech/MET/ET401/LAB/psychro_carrier_si.jpg
04/24/2312
Viscosity• A measure of frictional force between fluid layers
moving at different velocities
At 20 oC, the viscosity () of air is 1.8110-5 Pa·s (N·s/m2).The temperature dependence (on absolute temperature) is:
74.0
1
212
TT
What is the viscosity of air at 100 oC?
(Valid between -70 to 500 oC)
04/24/2313
Characterizing an Aerosol Particle How do we characterize a particle?
• Size, Shape, Density, Composition (toxicity, corrosivity, reactivity), Phase (liquid, solid)
Coal fly ash particles Iron oxide particles from arc welding
Why should we care the aerosol size?
04/24/2314
Size Range of Aerosol Particles
Hinds, Aerosol Technology, 1999
04/24/2315
Aerosol Size DistributionHow do we characterize particle”S”?
• Concentration:– Number concentration by counting– Mass concentration by weight measurement
• Size• Spread Particle size distribution
Dis
tribu
tion
func
tion
04/24/2316
Type of Size DistributionEx. A system containing spherical particlesNumber Concentration: Mass Concentration:100 #/cc 1m & = 1.91g/cm3 10-10 g/cc 1m1 #/cc 10m 10-9 g/cc 10m
Do we have “more” 1 m or 10 m particles (i.e. are the majority 1 or 10 m)? How will it impact the PSD we see?
Number Distribution
Num
ber d
istri
butio
n fu
nctio
n
Mass Distribution
Mas
s di
strib
utio
n fu
nctio
n
04/24/2317
Settling Velocity
Microscopy, Settling velocity, Light scatteringHow do we determine the particle size?
FG=mg
t=0V(t)=0
FG=mg
t=V(t)=?
FG=mg
t>3V(t)=VTS
FD=3V(t)dp
FD=3VTSdp
In settling, an aerosol experiences gravitational force (FG) and drag force (FD)
When they are equal to each other, there is no more acceleration.
mgdVFF ppGD 3
18
2gdVV ppTSp
How to get a larger settling velocity?
04/24/2318
Brownian Motion & Diffusion
• The primary transport mechanism for small particles (< 0.1 m); Important when transport distance is small: e.g. filter, airway in human lung– Brownian motion: irregular wiggling motion of a
particle caused by random bombardment of gas molecules against the particle
– Diffusion: the net transport of the particles from a region of higher concentration to a region of lower concentration
http://galileo.phys.virginia.edu/classes/109N/more_stuff/Applets/brownian/brownian.html
http://www.geocities.com/piratord/browni/Difus.html
p
c
dkTCD3
Stokes-Einstein Equation for Diffusion Coefficient How to get a
larger diffusivity?k = 1.38X10-23 J/K or 1.38X10-16 erg/K
04/24/2319
Quick Reflection