3. principles of statistics 16 feb 2012
TRANSCRIPT
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Principles of Statistics
Univariable and Bivariables
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Frequency Distribution
i
Ri
ff
n
CLASS FREQUENCY VALUES FOR NUMERICAL EXAMPLE 2.1
Class i fi fri Fi0.10 < < 0.12 1 5 0.1 0.1
0.12 < < 0.14 2 9 0.18 0.28
0.14 < < 0.16 3 20 0.4 0.68
0.16 < < 0.18 4 10 0.2 0.88
0.18 < < 0.2 5 6 0.12 1.0
iifRifiF
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Total frequency distribution
Comulative Distribution Function (cdf)
Relative frequency fR3
Cdf F3
1
1N
Ri
i
f
j
i
Rij fF1
33
20 0.40.50
Rffn
3
3
1
0.1 0.18 0.4 0.68.Ri
i
F f
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0.000.010.020.030.040.050.060.070.080.090.10
0.200.180.160.140.12
(b)
0.35
0.30
0.25
0.20
0.15
0.10
0.05
0.000.20
0.40
0.180.160.140.12
(a)
0.350.30
0.25
0.20
0.15
0.10
0.05
0.00
0.20
0.40
0.180.160.140.120.1
0.68
0.200.180.160.140.120.1
Fig. 2.1 (a) Relative frequency and (b) cumulative relative frequency.
Characterizing the frequency function
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1.0
Limiting Case
Limiting Case
Frequency distribution for a largenumber of classes
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0.14 0.16 0.16
1
0
Characterizing continuous distribution
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Histogram for (a) porosity and (b) permeability data for Well 34-29.
0.200
0.150
0.100
0.050
0.000
0.300
0.250
0.2000.1000.000
Porosity, fraction
Frequency
(a)
0.500
0.400
0.300
0.200
0.100
0.000
0.600
600200 4000 800
Freq
uency
Permeability, md(b)
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0.500
0.400
0.300
0.200
0.100
0.000
0
0.600
200 400 600 800
Permeability, md
Fre
quency
(a)
0.200
0.100
0.000
-5.0
0.300
-3.0 -1.0 1.0 3.0
In k, In md
Frequency
(b)
Effect of log transform on permeability histogram: (a) permeabilitydata and (b) log kdata for Well 34-29
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0.300
0.200
0.100
0.000
0.100 0.200 0.3000.000
Porosity, fraction
Frequency
(a)
0.300
0.200
0.100
0.000
0.100 0.200 0.3000.000
Porosity, fraction
Frequency
(b)
Porosity histogram for Wells (a) 31-23 and (b) 36-16.
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Univariate
MEAN = ARITHEMTIC AVERAGE
MODE = VALUE OCCURRING WITH GREATEST FREQUENCY
MEDIAN = VALUE MIDWAY IN THE FREQUENCY DISTRIBUTION
n
i
xn
x1
1
1
2/1~ nxx
2
~ 12/2/ nn xxx
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22 1
1
n
i
i
x x
sn
2 2
1
2 1
1
n
i
x nx
sn
2s sStandard Deviation
Coefficient of Variation vs
Cx
Variance
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0.2500.200
0.150
0.100
0.050
0.000
0.000
0.300
0.100 0.150 0.200 0.250 0.300
Porosity: Well 34-29
Poro
sity:Well31-w23
(a)
0.050
0.250
0.200
0.150
0.100
0.050
0.000
0.000
0.300
0.200 0.250 0.300
Porosity: Well 34-29
P
orosity:Well36-16
(b)0.100 0.1500.050
Percentile plot (Q-Qplot) comparisons of porosities of two wells:(a) Well 34-29 vs. Well 31-w23 and (b) Well 34-29 vs. Well 36-16.
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Correlation of two variables
n
i
i
n
i
i
n
i
ii yn
xn
yxn
yxc111
111,
2 21
2 1
n
ix
x nx
sn
yx ss
yxcyxr
,,
Covariance
Variance2 2
1
2 1
n
iy
y ny
sn
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y = mx + b
3.00
1.50
2.00
2.50
30
3.50
2826242220
Y
, %
log
k
Relationship between log kand forNumerical Example 2.5.
2
,
xs
yxcm
xmyb
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Propability
6
111 XpP 6
165432 PPPPP
.16
1
6
1
6
1
6
1
6
1
6
16
1
i
ixP
.1
dxxf f (x)
a b x
Probability of value falling within an interval.
dxxfbXapb
a
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Cumulative-Distribution
Function
.4.050
20
50
15030
50
30
dxxp
0.8
0.6
0.4
0.2
0
6
1
543210
Cumulative distribution function forrolling-a-die experiment
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xXpxF
bXapaXpbXp
aFbFaXpbXpbXap
ax
i
i
xPaF
f (x)
a b x
,dxxfaFa
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Numerical Example
.3
1
6
1
6
12
6
11
2
1
1
1
i
i
i
i
xPF
xPF
aFbFbXap
2
1
3
1
6
52552 FFXp
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Summary 16 Feb 2012
1. membahas statistik dasar, memahami konsep
probability, rdf, cdf, mean, mode, median,
koef korelasi, variansi, st. deviasi.
2. Mahasiswa diharapkan prinsip dasar
probability, kecenderungan, dan beberapa
aplikasi untuk analisa error.
3. Makalah yang sudah didapatkan dianjurkan
mulai sedikit sedikit dipelajari.