03 - Porosity Flashcards
Definition
Porosiy
fraction of rock bulk volume occupied by pore space
Formula
phi
phi = V_pore / V_bulk
Formula
V_pore
V_pore = V_bulk - V_solidmatrix
What is needed to calculated porosity?
! important to know this card
2 of the 3 volumetric parameters need to be measured:
- Bulk volume: V_bulk
- Pore volume: V_pore
- Matrix/Solid volume: V_solid
Definition
Total porosity
ratio of the total void space in the rock to the bulk volume of the rock
Definition
Effective porosity
ratio of the interconnected void space in the rock to the bulk volume of the rock
Porosity can be determined by
- direct measurements
- -> V_bulk & V_solid
- -> gas expansion or displacement tequniques
- indirect measurements
–> correlation between porosity & properties
(like density, neutron response, seimic wave velocity)
Definition
Primary porosity
Void volume of a sediment when it was deposited
pre-diagenetic in clastic sediments
grain size distribution, grain packing & particle shape
Definition
Secondary porosity
Void volume that is created by diagenetic processes
result of mechanical or geochemical processes
compaction, deformation, fracturing
dissolution, precipitation, mineralogical changes
Pore Size classification
d = diameter
Rough pore
d > 2mm
macrocapillary
2 mm > d > 50 μm
capillary
50 μm > d > 2 μm
microcapillary
2 μm > d > 50 nm
Pore Size classification
d = diameter
rough pore
d > 2mm
macrocapillary
2 mm > d > 50 μm
capillary
50 μm > d > 2 μm
microcapillary
2 μm > d > 50 nm
Definition
Bulk volume:
- can be calculated for samples with ..
V_bulk
.. the exact cylindrical shape -> measurement of diameter and length
or measurement of the volume of mercury displaced (mercury does not penetrate the pores)
sample types for methods
core plugs -> most methods
multiple samples -> statistically representative
technique imortant !
which volume will be determined with He-pycnometer?
matrix/solid volume V_m
Bulk Volume
direct calculation
for cylindrical
for regulary shaped cores or core plugs
V_bulk = (pid^2L)/4
Bulk Volume
fluid displacement methods (2)
Gravimetric
Volumetric (mercury pycnometer)
Pore Volume
- Gravimetric
Archimedes principle
weight dry W_dry
weight saturated W_sat
weight submerged in water W_sub
Pore Volume
- Boyle’s Law
p1 * V1 = p2 * V2
Gas expansion
Archimedes principle
Problems?
complete fluid saturation of pore space
depending on better and poorer quality rocks
reactions of fluid with rocks
Archimedes principle
V_pore
V_pore = (W_sat-W_dry) / rho_fluid
Archimedes principle
V_matrix
V_matrix = (W_dry - W_sub) / rho_fluid
Archimedes principle
V_bulk
V_bulk = (W_sat - W_sub) / rho_fluid
Archimedes principle
porosity phi
phi = (W_sat - W_dry) / (W_sat - W_sub)