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POROSITY
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Definition: Porosity is the fraction of a rock that
is occupied by voids (pores).
Discussion Topics
• Origins and descriptions
• Factors that effect porosity
• Methods of deterination
RESERVOIR POROSITY
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ROCK MATRIX AND PORE SPACE
Rock matrix Pore space
Note different use of “matrix”b !eo"o!ists and en!ineers
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Porosity: The fraction of a rock that is
occupie !y pores
b
mab
b
p
V
VV
V
V
Porosit
POROSIT" DE#INITION
• Porosity is an intensive property describing the
f!uid storage capacity of rock
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ROCK MATRIX AND PORE SPACE
Rock matrix #ater Oi" and$or !as
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O$%ECTI&ES
To pro'ie an unerstanin( of
) The concepts of rock *atri+ an porosity
) The ifference !et,een ori(ina- .pri*ary/ an
inuce .seconary/ porosity) The ifference !et,een tota- an effecti'e porosity
) 0a!oratory *ethos of porosity eter*ination
) Deter*ination of porosity fro* ,e-- -o(s
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C0ASSI#ICATION O# ROCKS
"#D$M#%T&'
R o c k % f o r m i n !
p r o c e s s
S o u r c e o f
m a t e r i a "
$%#O*"
M#T&MO'P+$,
&o"ten materia"s in
deep crust and
upper mant"e
'rsta""i(ation
)So"idification of me"t*
#eat+erin! and
erosion of rocks
exposed at surface
Sedimentation, buria"
and "it+ification
Rocks under +i!+
temperatures
and pressures in
deep crust
Recrsta""i(ation due to
+eat, pressure, or
c+emica"" acti-e f"uids
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SEDIMENTAR" ROCKS• '"astics
•'arbonates
•E-aporites
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'./STI' /ND '/R0ON/TE RO'1S
'"astic Rocks
,onsist Priari!y of "i!icate Minera!s
&re ,!assified on the -asis of:
rain "i/e Minera! ,oposition
'arbonate Rocks
,onsist Priari!y of ,arbonate Minera!s
(i.e. Minera!s 0ith a ,O &nion roup)
1iestone Predoinate!y ,a!cite (,a!ciu
,arbonate2 ,a,O2)
Do!oite Predoinate!y Do!ostone (,a!ciu
Magnesiu ,arbonate2 ,aMg(,O3)4 )
34
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Re"ati-e /bundances
Si"tstone
and s+a"e
)c"astic*3456
Sandstone
and con!"omerate
)c"astic*
3776
.imestone and
do"omite
3786
SEDIMENTAR" ROCK T"PES1
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"andrains
,!ayMatri5
,heica!,eent
Quartz Feldspar Rock Fragments
Quartz Calcite
Hematite
IlliteKaoliniteSmectite
/-era!eSandstone
/-era!e&udrock)S+a"e*
&!!ocheica!rains
,heica!,eent
Microcrysta!!ineMatri5
Calcite
FossilsPelloidsOolitesIntractlasts
Calcite
/-era!eSparr
.imestone/-era!e&icritic
.imestone
'"astic Rocks 'arbonate Rocks
'omparison of 'ompositions of '"asticand 'arbonate Rocks
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rain"i/e ,!assification for ,!astic "edients
%ae Mi!!ieters Microeters
-ou!der ,obb!ePebb!eranu!e
6ery ,oarse "and,oarse "andMediu "andFine "and6ery Fine "and
,oarse "i!tMediu "i!tFine "i!t6ery Fine "i!t,!ay
7289
4;
77
4<8.;
8.4;8.
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/-era!e Detrita" &inera" 'omposition
of S+a"e and Sandstone
&inera" 'omposition S+a"e Sandstone
,!ay Minera!s
>uart/
Fe!dspar
'ock Fragents
,arbonate
Organic Matter2+eatite2 andOther Minera!s
9: )6*
2:
8
;5
2
;2
5 )6*
95
7:%75
75
;7
;7
(odified fro -!att2
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S/NDSTONE './SSI
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ORI2INS O# POROSIT" IN
C0ASTICS AND CAR$ONATES.2enetic C-assification/
) Pri*ary .ori(ina-/
) Seconary .inuce/
.2enera--y *ore co*p-e+ than pri*ary porosity/
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PRIMAR" .ORI2INA0/ POROSIT"
) De'e-ope at eposition
) Typifie !y
3 Inter(ranu-ar pores of c-astics or
car!onates
3 Intercrysta--ine an fenestra- pores of car!onates
) 4sua--y *ore unifor* than inuce porosity
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SECONDAR" .IND4CED/ POROSIT"
) De'e-ope !y (eo-o(ic processes aftereposition .ia(enetic processes/
) E+a*p-es
3 2rain isso-ution in sanstones or car!onates
3 &u(s an so-ution ca'ities in car!onates
3 #racture e'e-op*ent in so*e sanstones1 sha-es1an car!onates
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S/NDSTONES POROSITY TYPES
Inter!ranu"ar )Primar*
Disso"ution
&icropores
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#ACTORS T5AT A##ECT POROSIT"
) Partic-e sphericity an an(u-arity
) Packin(
) Sortin( .'aria!-e (rain si6es/
)Ce*entin( *ateria-s
) O'er!uren stress .co*paction/
) &u(s1 isso-ution1 an fractures
PRI&/RY
SE'OND/RY )dia!enetic*
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RO?NDNESS /ND SPERI'ITY
O< './STI' GR/INS
i!+
S P E R I '
I T Y
.oA
Ver
/n!u"ar /n!u"ar
Sub%
/n!u"ar
Sub%
RoundedRounded
#e""%
Rounded
RO?NDNESS
Porosity
P o r o s i t y
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#ACTORS T5AT A##ECT POROSIT"
) Partic-e sphericity an an(u-arity
) Packin(
) Sortin( .'aria!-e (rain si6es/
)Ce*entin( *ateria-s
) O'er!uren stress .co*paction/
) &u(s1 isso-ution1 an fractures
PRI&/RY
SE'OND/RY )DI/GENETI'*
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1ine of Traverse
(using icroscope)
,eent
Matri5(c!ays2 etc.)
Tangentia! ,ontact
"utured ,ontact
1ong ,ontact
,oncavo,onve5,ontact
GR/IN P/'1ING IN S/NDSTONE
)modified from 0"att, 7@JF*
T+is Examp"e
Packing Pro5iity @ 78A
Packing Density @ 8.=
7 Types of rain ,ontacts
Packing Pro5iity
Packing Density
& easure of the e5tent to?hich sedientary partic!esare in contact ?ith theirneighbors
& easure of the e5tent to?hich sedientary partic!es
occupy the rock vo!ue
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'?0I' P/'1ING O< SPERESPorosit K 8J6
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Porosity Ca-cu-ations 7 4nifor*
Spheres
) $u-k 'o-u*e 8 .9r/: 8 ;r :
) Matri+ 'o-u*e 8
) Pore 'o-u*e 8 !u-k 'o-u*e 7 *atri+ 'o-u*e
2
r 82
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69842F
7r J
r 2 $8r J
Vo"ume0u"k Vo"ume&atrixVo"ume0u"k
Vo"ume0u"kVo"umePorePorosit
2
22
π
π
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RO&0I' P/'1ING O< SPERESPorosit K F4 6
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#ACTORS T5AT A##ECT POROSIT"
) Partic-e sphericity an an(u-arity
) Packin(
) Sortin( .'aria!-e (rain si6es/
) Ce*entin( *ateria-s
) O'er!uren stress .co*paction/
) &u(s1 isso-ution1 an fractures
PRI&/RY
SE'OND/RY )DI/GENETI'*
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Packing of T?o "i/es of "pheresPorosit K 786
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Grain%Si(e Sortin! in Sandstone
6ery 0e!!
"orted
0e!!
"orted
Moderate!y
"orted
Poor!y
"orted
6ery Poor!y
"orted
SORTING
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,hange of ,oposition ,hange of "i/e
,hange of "hape ,hange of Orientation
,hange of Packing
"and
"ha!e
#o!ian
F!uvia!
"!o? ,urrent
Fast ,urrent
'iver
-each
TYPES O< TECT?R/. '/NGES SENSED
0Y TE N/1ED EYE /S 0EDDING
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STS97/%8F%::57 &ississippi Ri-er De"ta, .ouisiana, ?S/ October 7@J5
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STS:J8%4F7%:F@ Se"en!a Ri-er De"ta, .ake 0aka", Russia &a 7@@4
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#ACTORS T5AT A##ECT POROSIT"
) Partic-e sphericity an an(u-arity
) Packin(
) Sortin( .'aria!-e (rain si6es/
) Ce*entin( *ateria-s
) O'er!uren stress .co*paction/
) &u(s1 isso-ution1 an fractures
PRI&/RY
SE'OND/RY )DI/GENETI'*
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DI/GENESIS
,arbonate,eented
Oi!"tained
Diagenesis is the Post
Depositiona! ,heica! andMechanica! ,hanges thatOccur in "edientary 'ocks
"oe Diagenetic #ffects $nc!ude
,opactionPrecipitation of ,eentDisso!ution of Frae?ork rains and ,eent
The #ffects of Diagenesis May#nhance or Degrade 'eservoir >ua!ity
0ho!e ,oreMisoa Foration2 6ene/ue!a P+oto b # /ers
D?/. POROSITY IN S/NDSTONE
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D?/. POROSITY IN S/NDSTONE
&/TRIC
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S/NDSTONE 'O&POSITION,
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POROSITY IN S/NDSTONE
>uart/rain
Pore
"canning #!ectron Micrograph%orph!et "andstone2 Offshore &!abaa2 *"&
Porosity in "andstoneTypica!!y is 1o?er ThanThat of $dea!i/ed Packed"pheres O?ing to:
6ariation in rain "i/e
6ariation in rain "hape
,eentation
Mechanica! and ,heica!
,opaction
P+otomicro!rap+ b R. 1u!"er
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POROSITY IN S/NDSTONE
"canning #!ectron MicrographTordi!!o "andstone2 %euEuen -asin2 &rgentina
Pore Throats in"andstone May
-e 1ined 0ith & 6ariety of ,eent Minera!sThat &ffectPetrophysica!
Properties
P+otomicro!rap+ b R. 1u!"er
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POROSITY IN S/NDSTONE
"canning #!ectron Micrograph
%orph!et Foration2 Offshore &!abaa2 *"&
Pores Provide the
6o!ue to "tore
+ydrocarbons
Pore Throats 'estrict
F!o? through pores
Pore
T+roat
' S
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Secondar E"ectron &icro!rap+
'"a &inera"s in Sandstone Reser-oirs,/ut+i!enic '+"orite
Burassic Norp+"et SandstoneOffs+ore /"abama, ?S/ )P+oto!rap+ b R. 1u!"er*
Occurs as T+in'oats on Detrita"Grain Surfaces
Occurs in Se-era"Deep" 0uriedSandstones #it+i!+ Reser-oir=ua"it
Iron%Ric+Varieties React#it+ /cid
3 7: µm
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E"ectron P+otomicro!rap+
'"a &inera"s in Sandstone Reser-oirs,
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INTERGR/N?./R PORE /ND &I'ROPOROSITY
$ntergranu!ar Pore
Microporosity
ao!inite>uart/Detrita!rain
$ntergranu!ar Pores
,ontain +ydrocarbonF!uids
Micropores ,ontain$rreducib!e 0ater
-ackscattered #!ectron Micrograph,arter "andstone2 -!ack 0arrior -asin2
&!abaa2 *"& )P+oto!rap+ b R. 1u!"er*
'"a &inera"s in Sandstone Reser-oirs
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'"a &inera"s in Sandstone Reser-oirs,/ut+i!enic 1ao"inite
"econdary #!ectron Micrograph
,arter "andstone%orth -!o?horn ,reek Oi! *nit
-!ack 0arrior -asin2 &!abaa2 *"&
"ignificant Pereabi!ity'eduction
+igh $rreducib!e 0ater "aturation
Migration of Fines
Prob!e
(Photograph by '.1. ug!er)
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DISSO.?TION POROSITY
Thin "ection Micrograph P!ane Po!ari/ed 1ight
&vi!e "andstone2 %euEuen -asin2 &rgentina
Disso!ution of
Frae?ork rains
(Fe!dspar2 for
#5ap!e) and
,eent ay#nhance the
$nterconnected
Pore "yste
This is "econdaryPorosity
Pore
>uart/ Detrita!
rain
Partia!!y
Disso!ved
Fe!dspar
P+oto b R. 1u!"er
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DISSO.?TION POROSITY
"canning #!ectron Micrograph
Tordi!!o Foration2 %euEuen -asin2 &rgentina
Partia!!y
Disso!ved
Fe!dspar
Disso!ution Pores
May be $so!ated andnot ,ontribute to the
#ffective Pore "yste
P+oto b R. 1u!"er
' i f ' iti f '" ti
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"andrains
,!ayMatri5
,heica!,eent
Quartz Feldspar Rock Fragments
Quartz Calcite
Hematite
IlliteKaoliniteSmectite
/-era!eSandstone
/-era!e&udrock)S+a"e*
&!!ocheica!rains
,heica!,eent
Microcrysta!!ineMatri5
Calcite
FossilsPelloidsOolitesIntractlasts
Calcite
/-era!eSparr
.imestone/-era!e&icritic
.imestone
'"astic Rocks 'arbonate Rocks
'omparison of 'ompositions of '"asticand 'arbonate Rocks
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I"es Gambier
Tuamotu /rc+ipe"a!o
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&a"di-e Is"ands
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'/R0ON/TES POROSITY TYPES
Interpartic"e
Intrapartic"e
Intercrsta"
&o"dic
Pores -et?een Partic!es or rains
Pores 0ithin $ndividua! Partic!es or rains
Pores -et?een ,rysta!s
Pores Fored by Disso!ution of an$ndividua! rain or ,rysta! in the 'ock
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$nterpartic!e $ntrapartic!e $ntercrysta! Mo!dic
Fenestra! "he!ter ro?thFrae?ork
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'/R0ON/TE POROSITY % EC/&P.E
Thin section icrograph p!anepo!ari/ed !ight
"ackover Foration2 &!abaa)P+oto!rap+ b D' 1opaska%&erke"*
&o"dicPores
• Due to disso!ution
and co!!apse of ooids
(a!!ocheica! partic!es)
• $so!ated pores
• 1o? effective porosity
• 1o? pereabi!ity
-!ue areas are pores.
'a"cite
Do"omite
&o"dic
Pore
'/R0ON/TE POROSITY EC/&P.E
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'/R0ON/TE POROSITY % EC/&P.E
Thin section icrograph
"ackover Foration2 &!abaa
-!ack areas are pores.
)P+oto!rap+ b D' 1opaska%&erke"*
• ,obination pore syste
• Mo!dic pores fored through
disso!ution of ooids (a!!ocheica!
partic!es)
• ,onnected pores
• +igh effective porosity
• +igh pereabi!ity
&o"dic
Pore
Interpartic"e
Pores
&o"dic and
Interpartic"e Pores
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PORE SPACE
C0ASSI#ICATION
.In Ter*s of #-ui Properties/
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PORE7SPACE C0ASSI#ICATION
) Tota- porosity1 φt 8
) Effecti'e porosity1 φe 8
&o-u*e$u-k
PoreVolumeTotal
&o-u*e$u-k
Pore Spacected Interconne
• Effecti-e porosit M of !reat importancecontains t+e mobi"e f"uid
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COMPARISON O# TOTA0 AND
E##ECTI&E POROSITIES
) &ery c-ean sanstones : φe → φt
) Poor-y to *oerate-y ,e-- 7ce*ente
inter(ranu-ar *ateria-s: φt ≈ φe
) 5i(h-y ce*ente *ateria-s an *ostcar!onates: φe < φt
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MEAS4REMENT O# POROSIT"
) Core sa*p-es .0a!oratory/
) Openho-e ,ire-ine -o(s
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>uar t/(Fr ae?or k)
"a!!Por es
$so!atedPor es
1ar ge2$nter connectedPor es
,!ay"ur f aces$nter !ayer s,!ay1ayer s$r r educib!eor $obi!e0ater +ydr ationor -ound0ater
+ydr ocar bonPor e6o!ue
"tr uctur a !(O+)0ater 'ockMatr i5 Tota!Por osity%eutr on1ogTota!Por osityDensity1og &bso!uteor Tota!Po r osityOvenDr ied,or e &na!ysis Por osity+uidityDr ied,or e &na!ysisPor osity
,api!!ar y0ater 6"ha!e"andstonePor osity Measur edby6ar iousTechn iEues
>uar t/(Fr ae?or k)
"a!!Por es
$so!atedPor es
1ar ge2$nter connectedPor es
,!ay"ur f aces$nter !ayer s,!ay1ayer s$r r educib!eor $obi!e0ater +ydr ationor -ound0ater
+ydr ocar bonPor e6o!ue
"tr uctur a !(O+)0ater 'ockMatr i5 Tota!Por osity%eutr on1ogTota!Por osityDensity1og &bso!uteor Tota!Po r osityOvenDr ied,or e &na!ysis Por osity+uidityDr ied,or e &na!ysisPor osity
,api!!ar y0ater 6"ha!e"andstonePor osity Measur edby6ar iousTechn iEues
S/NDSTONE POROSITY &E/S?RED
0Y V/RIO?S TE'NI=?ES
>uart/(Frae?ork)
"a!!Pores
$so!atedPores
1arge2 $nterconnectedPores
,!ay "urfaces $nter!ayers
,!ay1ayers
$rreducib!e or $obi!e 0ater
+ydration or -ound 0ater
+ydrocarbonPore 6o!ue
"tructura!(O+ %) 0ater
'ockMatri5
Tota! Porosity %eutron 1og
Tota! Porosity Density 1og
&bso!ute or Tota! Porosity
OvenDried ,ore &na!ysis Porosity+uidityDried
,ore &na!ysis Porosity
,api!!ary
0ater
6"ha!e
)modified from Es"in!er and Pe-ear, 7@JJ*
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IN#ORMATION #ROM CORES=
) Porosity
) 5ori6onta- per*ea!i-ity toair
) 2rain ensity
) &ertica- per*ea!i-ity to air
) Re-ati'e per*ea!i-ity
) Capi--ary pressure
) Ce*entation e+ponent .*/
an saturation e+ponent .n/
Standard /na"sis Specia" 'ore /na"sis
/""oAs ca"ibration of Aire"ine "o! resu"ts
CORIN2 ASSEM$0"
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PD' 'utters
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COMIN2 O4T O# 5O0E
>IT5 CORE $ARRE0
>5O0E CORE
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#+o"e 'ore P+oto!rap+,&isoa “'” Sandstone,
Vene(ue"a
>5O0E CORE
P+oto b # /ers
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SIDE>A00 SAMP0IN2 24N
'ore bu""ets
'ore samp"e
A00 CORIN2 TOO0
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SIDE>A00 CORIN2 TOO0
'orin! bit
Samp"es
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>5O0E CORE ANA0"SIS 's?
P042S OR SIDE>A00 CORES
>5O0E CORE
) Pro'ies -ar(er sa*p-es
) $etter an *ore consistent representation of
for*ation
) $etter for hetero(eneous rocks or for *ore
co*p-e+ -itho-o(ies
#O.E 'ORE /N/.YSIS -s
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) S*a--er sa*p-es
) 0ess representati'e of hetero(eneous for*ations
) >ithin @ to 9 of ,ho-e cores for *eiu*7to hi(h7
porosity for*ation
) In -o,7porosity for*ations1 φ fro* core p-u(s tens
to !e *uch (reater than φ fro* ,ho-e cores
) Sca-ar effects in fracture reser'oirs
P.?GS OR SIDE#/.. 'ORES
P.?GS OR SIDE#/.. 'ORES
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'ORE P.?G