Poro
s
ity 
Poro
s
ity of ro
c
k i
s
th
e
ratio of por
e
volum
e
to bulk 
volum
e
and i
s
u
s
ually 
e
xpr
esse
d a
s
p
e
r
ce
ntag
e
Vpis
pore
volume
Vbis
bulbkvolume
Vg
is
grain
volume
Total or Ab
s
olut
e
Poro
s
ity:
ú
It is the ratio of the volume of all the pores to the bulk 
volume of the material, 
Eff
ec
tiv
e
poro
s
ity
ú
It is the ratio of the interconnected pore volume to the 
bulk volume
I
nterconnected
pores
I
solated
pores
Mar-
2010
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 Pore 
Spatial arrang
e
m
e
nt-Arrang
e
m
e
nt of por
es
of diff
e
r
e
nt 
s
iz
es
w.r.t
e
a
c
h oth
e
r
Conn
ec
tivity of por
es
and throat-No of por
e
throat 
c
onn
ec
ting to por
es
Siz
e
& fr
e
q di
s
tribution-un
c
orr
e
lat
e
d, 
c
orr
e
lat
e
d
El
e
m
e
nt
s
of Por
e
Throat
The
texture
o
f
a
rock
consists
o
f
it
'
s
grain
or
mineral
crystal
size,
the
arrangement
o
f
the
grains
or
crystals,
and
the
degree
o
f
unif
ormity
o
f
the
grains
or
crystals.
Mar-
2010
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The role of Rock Texture…
Soi
=
(
1
-S
w
i)
high
Soi
=
(
1
-S
w
i)
lo
w
Mar-
2010
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Pore Network-Reconstructed using thin section IMAGE 
Analysis
Porosity
intergranular-0.23
Porosity
total-
0.28
Absolute
Permeability-426md
Porosity
intergranular-0.37
Porosity
total-
0.39
Absolute
Permeability-5600md
Mar
-
2010
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C# PDF File Compress Library: Compress reduce PDF size in C#.net
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Saturation
§
Saturation of a phase is the fraction of the 
pore volume occupied by the phase
So+Sg+Sw=1
Connate water saturation (Swc)
Critical Oil Saturation (Soc)
Critical gas Saturation (Sgc)
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§
P
e
rm
e
ability i
s
a m
e
a
s
ur
e
of ‘
e
a
se
of flow’or 
th
e
c
apa
c
ity of formation to tran
s
mit fluid
s
§
I
t
s
unit i
s
Dar
c
y nam
e
d aft
e
r a Fr
e
n
c
sc
i
e
nti
s
t
H
e
nry Dar
c
y in 1856.
ú
Ab
s
olut
e
P
e
rm
e
ability:
Wh
e
n only on
e
fluid i
s
pr
ese
nt in th
e
ro
c
k. 
I
t i
s
prop
e
rty of th
e
ro
c
k and i
s
ind
e
p
e
nd
e
nt of th
e
fluid u
se
d in th
e
m
e
a
s
ur
e
m
e
nt. Thi
s
a
ss
um
es
that th
e
fluid do
es
not int
e
ra
c
t with th
e
ro
c
k.(K)
ú
Eff
ec
tiv
e
P
e
rm
e
ability:
Eff
ec
tiv
e
p
e
rm
e
ability o
cc
ur
s
wh
e
n mor
e
than 
on
e
fluid i
s
pr
ese
nt & i
s
a fun
c
tion of th
e
fluid 
s
aturation & th
e
w
e
tting 
c
hara
c
t
e
ri
s
ti
cs
of th
e
ro
c
k. (Ko,Kw,Kg)
P
e
rm
e
ability
Mar-
2010
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P
e
rm
e
ability
Th
e
p
e
rm
e
ability i
s
m
e
a
s
ur
e
d by 
flowing a fluid of known 
vi
sc
o
s
ity µthrough a 
c
or
e
plug 
of m
e
a
s
ur
e
d dim
e
n
s
ion
s
(A and 
L) and th
e
n m
e
a
s
uring flow rat
e
and pr
ess
ur
e
drop. Dar
c
e
quation b
ec
om
es
Mar-
2010
Generated by Foxit PDF Creator © Foxit Software
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P
e
rm
e
ability
E
s
tabli
s
hing a p
e
rf
ec
t Ø-K tran
s
form 
s
till r
e
main
s
a major 
c
hall
e
ng
e
s
p
ec
ially in r
e
f to 
c
arbonat
es
Mar-
2010
The
clastics
The
carbonates
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I
mprov
e
d P
e
rm
e
ability 
es
timation
0.001
0.010
0.100
1.000
10.000
0.010
0.100
1.000
Phi Group 
RQI, micron
Phi Group - RQ
I
Plot
HU 1
HU 7
HU 6
HU 4
HU 2
HU 3
HU 5
y = 18.846x2.4585
y = 30.796x2.1428
y = 37.476x1.8785
y = 245.68x2.212
y = 355.42x2.0499
y = 1648.1x2.3492
y = 8081.6x2.5518
0.01
0.10
1.00
10.00
100.00
1000.00
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.40
Core Porosity
Core Permeability, mD
HU7,
HU6,
HU5,
HU4,
HU3,
HU2,
HU1,
Poros
ity - Permeability Plot
Mar-
2010
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http://www.foxitsoftware.com   For evaluation only.
Capillary pressure
§
Combined effect of surface and 
IFT of the rock and fluid, pore size 
and geometry & wettabilityof the 
system.
Major 
e
ff
ec
t of Cap pr
es
i
s
th
e
c
r
e
ation of
Transition
Z
one
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