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Asst. Lecturer: Amir I. Abdelaziz, Helwan University
1
Well logging
What is a log?
 Well log is a continuous record of measurement made in bore-hole
that respond to variation in some physical properties of rocks
through which the bore hole is drilled.
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
2
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
3
 Write about Bore-hole Geometry/Environment OR Invasion effect..
 Where a hole is drilled into a formation, the borehole and the rock surrounding it are
contaminated by the drilling mud, which affects logging measurements.
1. Invaded Zone:
 The zone in which much of the original fluid is replaced by mud filtrate is called the invaded
zone.
 It consists of a flushed zone (of resistivity Rxo) and a transition or annulus zone (of resistivity
Ri). The flushed zone occurs close to the borehole. Where the mud filtrate has almost
completely flushed out a formation’s hydrocarbons and/or water (Rw).
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
4
 The transition or annulus zone, where a formation’s fluids and mud filtrate are mixed,
occurs between the flushed zone and the uninvaded zone (of resistivity Rt).
 The uninvaded zone is defined as the area beyond the invaded zone where a formation’s
fluids are uncontaminated by mud filtrate.
2. Flushed zone Resistivity (Rxo):
 The flushed zone extends only a few inches from the wellbore and is part of the invaded
zone.
 If invasion is deep or moderate, most often the flushed zone is completely cleared of its
formation water by mud filtrate (of resistivity Rmf).
 When oil is present in the flushed zone, the degree of flushing by mud filtrate can be
determined from the difference between water saturations in the flushed (Sxo) zone and
the uninvaded (Sw) zone
3. Uninvaded zone Resistivity (Rt):
 The uninvaded zone is located beyond the invaded zone.
 Pores in the uninvaded zone are uncontaminated by mud filtrate; instead, they are
saturated with formation water (Rw), oil, and/or gas.
 By using water saturation data, a geologist can determine a reservoir’s hydrocarbon
saturation. Sh = 1 – Sw (Sh = hydrocarbon saturation - water saturation of the uninvaded zone ).
Logging tools
 Gamma ray log:
 All rocks contain some radioactive material, although marine shales have a higher gamma
ray emission level than sandstone, limestone and dolomite. This difference makes the
gamma ray log especially useful for distinguishing shales from non-shales, therefore the
gamma ray is essentially a lithology log.
 Gamma ray log : Measures Natural radioactivity and main radioactive elements are
Potassium, Thorium and Uranium.
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
5
 K and TH mostly in shales while U from other sources. Clean formations have low
radioactivity level.
 Importance of GR log:
 Correlation between wells,
 Determination of bed boundaries,
 Evaluation of shale content within a formation,
GR log - Gr clean
Vsh =
GR shale - Gr clean
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
6
2. Spontaneous potential log (SP):
o Record the difference in voltage between a
moving electrode in the borehole and a
reference electrode at the surface usually
located at the mud pit.
o In order to record a potential the hole must
contain conductivemud, as it cannot be recorded
in air or oil-base mud.
o Logging rate is approximately 1500m per hour
and recordings are continuous.
 Factors affect the Sp:
 In sand A, Rw is less than Rmf.
 In sand B, the SP deflection is less than in sand A.
 In sand C, the SP is reversed, (Rw > Rmf).
 We may guess that, at about 7000 ft, Rmf and Rw are equal.
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
7
Shale Volume Calculation (Vsh) :
V shale = (SPclean – SPlog)/ (SPclean-SPshale)
Vshale: shale volume
SPclean: maximum Sp deflection from clean wet zone
SPlog: Sp in the zone of interest (read from the log)
Spshale: SP value at the shale baseline (often considered to be zero).
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
8
3. Resistivity log :
 Resistivity: The Degree to which the subsurface resist flow of current to pass through.
 Resistivity is the inverse of conductivity.
 Measures resistance of flow of electric current.
 Is function of porosity & pore fluid in rock.
 Resistivity is measured as, R in ohm per m,
 The ability to conduct electric current depends upon:
 The Volume of water,
 The Temperature of the formation,
 The Salinity of the formation.
 The Usage:
 Determine Hydrocarbon versus Water-
bearing zones,
 Indicate Permeable zones.
 There are two general types of resistivity tools:
 Electrode: forces a current through the rock and measures resistivity.
 Induction: Uses electro-magnetic field to induce electrical currents in the rock; it
measures conductivity which is converted to resistivity.
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
9
 Various electrode logs and depth of measurement:
 Water saturation calculation (Sw):
 Sw, water saturation can be estimated from a resistivity measurement using the Archie
Equation.
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
10
 Resistivity Analysis:
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
11
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
12
Porosity log types
A. Density log:
 The formation density log is a porosity log that measures
electron density of a formation.
 A radioactive source, applied to the borehole wall in a shielded
portion of the tool, emits medium-energy gamma rays into the
formations. These gamma rays may be thought of as high-
velocity particles that collide with the electrons in the formation.
At each collision a gamma ray loses some, but not all, of its
energy to the electron, and then continues with diminished
energy.
 Dense formations absorb many gamma rays, while low-density
formations absorb fewer. Thus, high-count rates at the detectors
indicate low-density formations, whereas low count rates at the
detectors indicate high-density formations.
 Therefore, scattered gamma rays reaching the detector is an
indication of formation Density.
Asst. Lecturer: Amir I. Abdelaziz, Helwan University
13
B. Neutron logs:
 The Neutron Log can be summarized as the continuous measurement of the induced
radiation produced by the bombardment of that formation with a neutron source
contained in the logging tool whose sources emit fast neutrons that are eventually slowed
by collisions with hydrogen atoms until they
are captured.
 The Neutron Log is primarily used to
evaluate formation porosity.
 It is used to detect gas in certain situations.
 Measures lithology when used with Density
Log.
 Porosity from Neutron log:
 Density-Neutron log:
 Can be an Indicator for Gas (Gas zone boundary).
 
  Nmashshsh
NhcxoNmfxoN
V1V
S1S


Asst. Lecturer: Amir I. Abdelaziz, Helwan University
14
 We can see in (Density – Neutron) log a Cross over + SEPARATION and the case may
reversal in case of Oil zone.
C. Sonic (Velocity) log:
 Acoustic energy emitted by a transmitter, travels through the formation/fluids, detected
by multiple detectors.
 Log displays the interval transit time (Dt) in msec/ft.
 Measures speed of sound in the formation in
microseconds/ft.
 Each rock type (lithology) has a characteristic DT.
 Fluids have a much slower DT, gas even slower.
 Used to determine porosity and lithology.
 Porosity from Sonic log:

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Wll logging

  • 1. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 1 Well logging What is a log?  Well log is a continuous record of measurement made in bore-hole that respond to variation in some physical properties of rocks through which the bore hole is drilled.
  • 2. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 2
  • 3. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 3  Write about Bore-hole Geometry/Environment OR Invasion effect..  Where a hole is drilled into a formation, the borehole and the rock surrounding it are contaminated by the drilling mud, which affects logging measurements. 1. Invaded Zone:  The zone in which much of the original fluid is replaced by mud filtrate is called the invaded zone.  It consists of a flushed zone (of resistivity Rxo) and a transition or annulus zone (of resistivity Ri). The flushed zone occurs close to the borehole. Where the mud filtrate has almost completely flushed out a formation’s hydrocarbons and/or water (Rw).
  • 4. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 4  The transition or annulus zone, where a formation’s fluids and mud filtrate are mixed, occurs between the flushed zone and the uninvaded zone (of resistivity Rt).  The uninvaded zone is defined as the area beyond the invaded zone where a formation’s fluids are uncontaminated by mud filtrate. 2. Flushed zone Resistivity (Rxo):  The flushed zone extends only a few inches from the wellbore and is part of the invaded zone.  If invasion is deep or moderate, most often the flushed zone is completely cleared of its formation water by mud filtrate (of resistivity Rmf).  When oil is present in the flushed zone, the degree of flushing by mud filtrate can be determined from the difference between water saturations in the flushed (Sxo) zone and the uninvaded (Sw) zone 3. Uninvaded zone Resistivity (Rt):  The uninvaded zone is located beyond the invaded zone.  Pores in the uninvaded zone are uncontaminated by mud filtrate; instead, they are saturated with formation water (Rw), oil, and/or gas.  By using water saturation data, a geologist can determine a reservoir’s hydrocarbon saturation. Sh = 1 – Sw (Sh = hydrocarbon saturation - water saturation of the uninvaded zone ). Logging tools  Gamma ray log:  All rocks contain some radioactive material, although marine shales have a higher gamma ray emission level than sandstone, limestone and dolomite. This difference makes the gamma ray log especially useful for distinguishing shales from non-shales, therefore the gamma ray is essentially a lithology log.  Gamma ray log : Measures Natural radioactivity and main radioactive elements are Potassium, Thorium and Uranium.
  • 5. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 5  K and TH mostly in shales while U from other sources. Clean formations have low radioactivity level.  Importance of GR log:  Correlation between wells,  Determination of bed boundaries,  Evaluation of shale content within a formation, GR log - Gr clean Vsh = GR shale - Gr clean
  • 6. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 6 2. Spontaneous potential log (SP): o Record the difference in voltage between a moving electrode in the borehole and a reference electrode at the surface usually located at the mud pit. o In order to record a potential the hole must contain conductivemud, as it cannot be recorded in air or oil-base mud. o Logging rate is approximately 1500m per hour and recordings are continuous.  Factors affect the Sp:  In sand A, Rw is less than Rmf.  In sand B, the SP deflection is less than in sand A.  In sand C, the SP is reversed, (Rw > Rmf).  We may guess that, at about 7000 ft, Rmf and Rw are equal.
  • 7. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 7 Shale Volume Calculation (Vsh) : V shale = (SPclean – SPlog)/ (SPclean-SPshale) Vshale: shale volume SPclean: maximum Sp deflection from clean wet zone SPlog: Sp in the zone of interest (read from the log) Spshale: SP value at the shale baseline (often considered to be zero).
  • 8. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 8 3. Resistivity log :  Resistivity: The Degree to which the subsurface resist flow of current to pass through.  Resistivity is the inverse of conductivity.  Measures resistance of flow of electric current.  Is function of porosity & pore fluid in rock.  Resistivity is measured as, R in ohm per m,  The ability to conduct electric current depends upon:  The Volume of water,  The Temperature of the formation,  The Salinity of the formation.  The Usage:  Determine Hydrocarbon versus Water- bearing zones,  Indicate Permeable zones.  There are two general types of resistivity tools:  Electrode: forces a current through the rock and measures resistivity.  Induction: Uses electro-magnetic field to induce electrical currents in the rock; it measures conductivity which is converted to resistivity.
  • 9. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 9  Various electrode logs and depth of measurement:  Water saturation calculation (Sw):  Sw, water saturation can be estimated from a resistivity measurement using the Archie Equation.
  • 10. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 10  Resistivity Analysis:
  • 11. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 11
  • 12. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 12 Porosity log types A. Density log:  The formation density log is a porosity log that measures electron density of a formation.  A radioactive source, applied to the borehole wall in a shielded portion of the tool, emits medium-energy gamma rays into the formations. These gamma rays may be thought of as high- velocity particles that collide with the electrons in the formation. At each collision a gamma ray loses some, but not all, of its energy to the electron, and then continues with diminished energy.  Dense formations absorb many gamma rays, while low-density formations absorb fewer. Thus, high-count rates at the detectors indicate low-density formations, whereas low count rates at the detectors indicate high-density formations.  Therefore, scattered gamma rays reaching the detector is an indication of formation Density.
  • 13. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 13 B. Neutron logs:  The Neutron Log can be summarized as the continuous measurement of the induced radiation produced by the bombardment of that formation with a neutron source contained in the logging tool whose sources emit fast neutrons that are eventually slowed by collisions with hydrogen atoms until they are captured.  The Neutron Log is primarily used to evaluate formation porosity.  It is used to detect gas in certain situations.  Measures lithology when used with Density Log.  Porosity from Neutron log:  Density-Neutron log:  Can be an Indicator for Gas (Gas zone boundary).     Nmashshsh NhcxoNmfxoN V1V S1S  
  • 14. Asst. Lecturer: Amir I. Abdelaziz, Helwan University 14  We can see in (Density – Neutron) log a Cross over + SEPARATION and the case may reversal in case of Oil zone. C. Sonic (Velocity) log:  Acoustic energy emitted by a transmitter, travels through the formation/fluids, detected by multiple detectors.  Log displays the interval transit time (Dt) in msec/ft.  Measures speed of sound in the formation in microseconds/ft.  Each rock type (lithology) has a characteristic DT.  Fluids have a much slower DT, gas even slower.  Used to determine porosity and lithology.  Porosity from Sonic log: