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05/25/22 1 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

Basic Laws of Gases and Particulates

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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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Page 1: Basic Laws of Gases and Particulates

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

Page 2: Basic Laws of Gases and Particulates

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

Page 3: Basic Laws of Gases and Particulates

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

Page 4: Basic Laws of Gases and Particulates

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

Page 5: Basic Laws of Gases and Particulates

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%

Page 6: Basic Laws of Gases and Particulates

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?

Page 7: Basic Laws of Gases and Particulates

04/24/237

Page 8: Basic Laws of Gases and Particulates

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?

Page 9: Basic Laws of Gases and Particulates

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?

Page 10: Basic Laws of Gases and Particulates

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?

Page 11: Basic Laws of Gases and Particulates

04/24/2311http://howard.engr.siu.edu/staff1/tech/MET/ET401/LAB/psychro_carrier_si.jpg

Page 12: Basic Laws of Gases and Particulates

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)

Page 13: Basic Laws of Gases and Particulates

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?

Page 14: Basic Laws of Gases and Particulates

04/24/2314

Size Range of Aerosol Particles

Hinds, Aerosol Technology, 1999

Page 15: Basic Laws of Gases and Particulates

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

Page 16: Basic Laws of Gases and Particulates

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

Page 17: Basic Laws of Gases and Particulates

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?

Page 18: Basic Laws of Gases and Particulates

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

Page 19: Basic Laws of Gases and Particulates

04/24/2319

Quick Reflection