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단원의 주제 입자상물질의 분포함수(Particle Size Distribution) Page 4
- 입자상분포함수의 이해
* 누적율
F a ( ) = ò
0aq d (
p) dd
pdp (mm)
0 10 20 30 40 50
Cumulative Fraction (%)
0 10 20 30 40 50 60 70 80 90 100
적색점의 의미는 무엇인가 ?
* 입자분포함수의 형태
dp (mm)
0 10 20 30 40 50
q(dp) Probability Density Function 0.00 0.02 0.04 0.06 0.08 0.10
수농도 분포 (Number Distribution)
dp (mm)
0 10 20 30 40 50
Mass fraction/mm
0.00 0.01 0.02 0.03 0.04
질량농도분포 (Mass Distribution)
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학과목 집진공학(集塵工學) 담당교수 장혁상 (810-2547)
단원의 주제 입자상물질의 분포함수(Particle Size Distribution) Page 5
- 입자상분포함수의 Fitting
이산분포를 연속분포로 표현하였을 때 연속분포를 수식적으로 가장 잘 표현할 수 있는 함수는 ? 주어진 입자분포를 어떻게 표현할 것인가 ? 대상 입자상물질이 어떤분포함수를 따르는가 ?
.단순정규분포(= Gauss 분포) .대수정규분포
.Rosin-Rammler 분포
* 단순정규분포함수
* 대수정규분포함수
* Fitting 함수의 선정
대수-확률지 혹은 정규-확률지 사용에 의한 분포도 평가 .Fitting 되는 종류에 따라 분포결정
.분포용지의 판독으로부터
log
log
log
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학과목 집진공학(集塵工學) 담당교수 장혁상 (810-2547)
단원의 주제 입자상물질의 분포함수(Particle Size Distribution) Page 6
- 분포함수의 매개변수
* 통계변수
.최빈값 (Mode) / 중앙값 (Median) .평균값(Mean)
▶산술평균:
,▶기하평균:
* 입경의 정의 및 상관식
.개수 중앙입경(Number Median Diameter)
주어진 입자분포에서 입자의 갯수누적율이 50%가 되는 점의 입자직경 .질량 중앙입경(Mass Median Diameter)
주어진 입자분포에서 입자의 질량누적율이 50%가 되는 점의 입자직경 .표면적 중앙입경(Surface Median Diameter)
주어진 입자분포에서 입자의 표면적누적율이 50% 가 되는 점의 입자직경
.평균체적 입경(Diameter of the particle with average volume)
,
m ax m ax
ni : 분포 구간 i를 차지하는 입자의 갯수 vi : 분포구간 i의 입자의 평균부피 N : 분포전체의 입자갯수
.평균질량 입경(Diameter of the particle with average mass)
,
m ax
mi : 분포 구간 i를 차지하는 입자의 질량 N : 분포전체의 입자갯수
ρp : 모든 입자의 평균밀도
모든 입자의 밀도가 동일할 경우: d v = d m .개수 평균입경(Number Mean Diameter) : dp,n
m ax m ax
: 분포 구간 i를 차지하는 입자의 갯수
: 분포구간 i의 입자의 중간입경
: 분포전체의 입자갯수
.질량 평균입경(Mass Mean Diameter) : dp,m
m ax
m ax
: 분포 구간 i를 차지하는 입자의 질량
: 분포구간 i의 입자의 중간입경
: 분포전체의 입자질량
.표면적 평균입경(Surface Mean Diameter) : dp,s
m ax
m ax
: 분포 구간 i를 차지하는 입자의 표면적
: 분포구간 i의 입자의 중간입경
: 분포전체의 입자표면적
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학과목 집진공학(集塵工學) 담당교수 장혁상 (810-2547)
단원의 주제 입자상물질의 분포함수(Particle Size Distribution) Page 7
* Hatch-Choate 변환 방정식(복합 분포 함수) .Median Diameter (중앙입경)
exp ln
: dimensional weighting factor with respect to : 변환대상 입자분포누적중간입경
: number median diameter ( = 대수정규분포에서 ) : 분포의 표준 편차
.Mean Diameter (평균입경)
exp
ln
: dimensional weighting factor with respect to
: 변환대상 입자분포평균입경 : number median diameter : 분포의 표준 편차
.Hatch-Choate 변환 방정식 적용 예
: Mass Mean Diameter의 경우 입자질량이 d 3에 비례하므로 q=3. 따라서 exp
ln
: Mass Median Diameter의 경우 입자질량이 d 3에 비례하므로 q=3. 따라서 exp ln
: Surface Mean Diameter의 경우 입자표면적이 d 2에 비례하므로 q=3. 따라서 exp
ln
: Surface Median Diameter의 경우 입자표면적이 d 2에 비례하므로 q=2. 따라서 exp ln
: Diameter of particle with average mass와 NMD의 관계 exp ln
: Mode(ˆ )와 NMD의 관계 d
exp ln
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학과목 집진공학(集塵工學) 담당교수 장혁상 (810-2547)
단원의 주제 입자상물질의 분포함수(Particle Size Distribution) Page 8
● 단원에서의 검토사항
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학과목 집진공학(集塵工學) 담당교수 장혁상 (810-2547)
단원의 주제 입자상물질의 분포함수(Particle Size Distribution) Page 9
● 참고문헌
Hinds, W.C. Aerosol Technology: Properties, Bahavior, and Measurement of Air borne Particles, Chap. 4, Wiley(1982)
입자상 물질의 특성화
Hyuksang Chang, 영남대학교 1
Linear-Probability Graph
Cumulative Percent (%)
0.1 1 10 30 50 70 90 99
Particle Size in Diamater (um or cm)
10 20 30 40 50 60 70 80 90 100
입자상 물질의 특성화
Hyuksang Chang, 영남대학교 2
Log-Probability Graph
Cumulative Percent (%)
0.1 1 10 30 50 70 90 99
Particle Size in Diamater (um or cm)
0.1 1 10 100
입자상 물질의 특성화
Hyuksang Chang, 영남대학교 1
Linear-Probality Graph
Cumulative Percent (%)
0.1 1 10 30 50 70 90 99
Particle Size in Diameter (
m m
or cm)
20 40 60 80 100
입자상 물질의 특성화
Hyuksang Chang, 영남대학교 2
Log-Probality Graph
Cumulative Percent (%)
0.1 1 10 30 50 70 90 99
Particle Size in Diameter (
m m
or cm)
0.1 1 10 100
2016-07-13 Environmental Aerosol Engineering Laboratory 1
Particle Size Distribution
• Monodisperse - All the particles are of the same size
• Polydisperse - Particles are of more than one size (more realistic)
Typical data from measurement
Size Range (m)
Count (#)
Fraction Percent (%) Cumulative Percent (%)
Fraction/size (m
-1)
0-4 104 0.104 10.4 10.4 0.026
4-6 160 0.16 16.0 26.4 0.08
6-8 161 0.161 16.1 42.5 0.0805
8-9 75 0.075 7.5 50.0 0.075
9-10 67 0.067 6.7 56.7 0.067
10-14 186 0.186 18.6 75.3 0.465
14-16 61 0.61 6.1 81.4 0.0305
16-20 79 0.79 7.9 89.3 0.0197
20-35 103 0.103 10.3 99.6 0.0034
35-50 4 0.004 0.4 100.0 0.0001
> 50 0 0 0 100.0 0
Total 1000 100.0
Reading: Hinds, Chap 4
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Histogram of frequency(count) versus particle size
d
pi( m )
0 10 20 30 40 50
Frequency/Count
0
50
100
150
200
Q: Which size range has the most particles?
Size Range
(m) Count (#)
0-4 104
4-6 160
6-8 161
8-9 75
9-10 67
10-14 186
14-16 61
16-20 79
20-35 103
35-50 4
> 50 0
Total 1000
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Frequency/d
p(distribution function) vs particle size
d
pi( m )
0 10 20 30 40 50
n i (d pi ) Size Distribution Funct ion (frequency/ d p
0 20 40 60 80
Q:Total # of particles ?
Size Range
(m) Count/d
pi(#/m)
0-4 26
4-6 80
6-8 80.5
8-9 75
9-10 67
10-14 46.5
14-16 30.5
16-20 19.25
20-35 6.87
35-50 0.27
> 50 0
pi i
i
d
Count
n
2016-07-13 Environmental Aerosol Engineering Laboratory 4
Standardized frequency/d
pvs particle size
d
pi( m )
0 10 20 30 40 50
f i (d pi ) Probability Density F unction (fraction/ d pi )
0.00 0.02 0.04 0.06 0.08
Q: What is the value of the total area?
Size Range
(m) Fraction/size (1/m)
0-4 0.026
4-6 0.08
6-8 0.0805
8-9 0.075
9-10 0.067
10-14 0.465
14-16 0.0305 16-20 0.0197 20-35 0.0034 35-50 0.0001
> 50 0 0
N
f
i n
i2016-07-13 Environmental Aerosol Engineering Laboratory 5
Continuous Particle Size Distribution
If the size range is very small, the discrete PSD will approach continuous PSD .
d p ( m )
0 10 20 30 40 50
q(d p ) Probability Density Function
0.00 0.02 0.04 0.06 0.08 0.10
q d f d
df
p
dd
i
pi p
( )
02016-07-13 Environmental Aerosol Engineering Laboratory 6
Cumulative Distribution
• Definition:
– The fraction that is less than a specific size
• Why cumulative distribution?
– Can be used to determine some statistical values.
Provide another viewpoint to observe the distribution.
F a ( )
0aq d (
p) dd
pd
p( m )
0 10 20 30 40 50
Cumulative Fraction ( %)
0 10 20 30 40 50 60 70 80 90 100
Q: What’s the RED spot?
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MEAN (arithmetic average):
The sum of all the particles sizes divided by the number of particles
MEDIAN :
The diameter for which 50% of the total are smaller and 50% are larger; the diameter corresponds to a
cumulative fraction of 50%
MODE:
Most frequent size; setting the derivative of the frequency function to 0 and solving for d p .
For a symmetrical distribution, the mean, median and mode have the same value.
d d
N
n d
n d q d dd
p
p i pi
i
p p p
0 ( )
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• GEOMETRIC MEAN :
the Nth root of the product of N values
Expressed in terms of ln(d p )
• For a monodisperse aerosol, otherwise,
• Very commonly used because the an aerosol system typically covers a wide size range from 0.001 to 1000 m
d
p d
pgp g
p
d
d
d pg d d d p n 1 1 p n 2 2 p n 3 3 ... 1 / N d pi n d (
pi) 1 / N
ln ln
exp ln
exp ( ) ln( )
( )
d n d
N
d n d
N
n d d dd n d dd
pg
i pi
pg
i pi p p p
p p
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Weighted Distributions
• Why do we need other distributions?
– Aerosols may be measured in different ways, and in indirect ways (e.g. impactors, light scattering)
• What are the other distributions?
– Surface area, mass (volume), volume square ...etc
• Definition: frequency of the property (e.g. mass) contributed by particles of the size interval
• What is the effect?
Ex. A system containing spherical particles (mode size?) Number Concentration: Mass Concentration:
100 #/cc 1m & =1.91g/cm 3 10 -11 g/cc 1m 1 #/cc 10m 10 -9 g/cc 10m
Q: How will the PSD on page 5 look like?
2016-07-13 Environmental Aerosol Engineering Laboratory 10 dp(m)
0 10 20 30 40 50
Mass fraction/ m
0.00 0.01 0.02 0.03 0.04
dp(m)
0 10 20 30 40 50
q(d p ) Probability Density Function
0.00 0.02 0.04 0.06 0.08 0.10
Number Distribution Mass Distribution
Q: What is the mode size of the distribution?
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• Count Mean Diameter: based on number of particles.
• Mass Mean Diameter: based on mass of particles.
d d
N
n d
n d n d dd
pn
p i pi
i
p p p
0 ( )
d m d
m d m d dd
pm
i pi i
p p p
0 ( )
m p n p p n d p k n d p 6
3
1
Conversion 3
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Moments of the PSD
• Definition: The quantity proportional to particle size raised to a power; an integral aerosol property
M
n n d
i(
pi) d
pin
0n d (
p) d dd
pn pQ: What is M o ?
M
o n d
i(
pi)
0n d (
p) dd
pQ: What is M 1 ?
Q: What is M 1 /M 0 ?
Q: What is M 2 /M 0 ? M 3 /M 0 ?
Q: Which is larger? M 1 /M 0 ? (M 2 /M 0 ) 1/2 ? (M 3 /M 0 ) 1/3 ?
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Volume Moments
• Particle volume, instead of particle diameter, is also used as a variable (i.e. the x-axis is particle volume, not size)
• Definition:
• Conversion of n to n dp :
M
k n
i(
pi)
pik
0n (
p)
pkd
pQ: What is M 1 /M 0 ?
p d p 3 / 6 d p d p 2 / 2 dd p
dN n d
dN n d dd
p p
d p p
( )
( )
(1) (2) (3)
n ( p ) d p 2 / 2 dd p n d ( d p ) dd p
n d ( d p ) d p 2 / 2 n ( p ) (4)
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Lognormal PSD
• Various distributions: Power law, Exponential, ...etc. Very limited application in aerosol science
• Normal Distribution: widely used elsewhere, but typically not for aerosol science, because
– most aerosols exhibit a skewed distribution function – if a wide size range is covered, a certain fraction of the
particles may have negative values due to symmetry.
df d d
dd
n d d N
p p
p
i p p
1
2 2
1
2
2
2 1 2
exp
/
standard deviation
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• The application of a lognormal distribution has no theoretical basis, but has been found to be
applicable to most single source aerosols
• Useful for particle of a wide range of values (largest/smaller size > 10)
• Its mathematical form is very convenient when handling weighted distributions and moments.
• How to use it? Simply replace d p by ln(d p ).
ln ln
d n d
pg
N
i pi
geometric mean diameter
Why using Lognormal?
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ln (ln ln )
gn
id
pid
pg N
21
df
d d
d d
g
p pg
g
p
1
2 2
2
ln exp
2ln ln
(ln ) ln
(1)
(2)
d ln d
p dd
p/ d
p(3)
df d
d d
dd
p g
p pg
g
p
1
2 2
2
ln exp
2ln ln
(ln ) (4)
df d
g
p pg
g
p
1
3 2 18
2
2
ln exp ln ( / )
ln (5)
geometric standard deviation
Convert dlnd p to dd p
2016-07-13 Environmental Aerosol Engineering Laboratory 17
• Features of Lognormal PSD
Q: How much is ln(d
84%/d
16%)?
ln ln ln
ln( / )
gd d
d d
84% 50%
84% 50%
) /
ln(
ln
2
g d
97.5%d
50% Log-probability graph
For a given distribution, g remains constant
(nondimensional) for all
weighted distributions.
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Moments for lognormally distributed aerosols:
M k M g k k g
0
2 2
9
exp 2 ln
ln 2 ln 0 2
1 2
1
g 9 M M
M
g M
M M
1
2
0 3 2
2 1 2
/ /
The statistical variables can be easily determined through the moments!
Ref: Lee, K. W. and Chen, H., Aerosol Sci. Technol., 3, 1984, 327-334.
Lee, K. W., Chen, H. and Gieseke, J. A., Aerosol Sci. Technol., 3, 1984, 53-62.
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