This quiz will deal with a few different components in the study of sound, with specific reference to wave velocity, acoustic porosity, transmitters, Delta-T, P-wave, voltage, vertical resolution and electrode devices. See how much you know about it!
Shear
Mud
Surface
Compressional
Air-drilled holes
Oil-based mud
Freshwater-based mud
Saltwater-based mud
Shear wave
Compressional wave
Stoneley wave
The time required for sound to travel from the transmitter to a receiver.
The time required for sound to travel through a one foot interval of formation.
The distance traveled by a direct wave from the transmitter through the formation and detected at the receiver.
Potential for deeper depth of investigation beyond the altered zone
Enables accurate data acquisition in large diameter boreholes
Enables faster logging speeds
Increased velocity
Decreased travel times
Increased travel times
Decreased velocity
Remains constant
Decreases
Increases
Mud Waves
Compressional Waves
Stoneley Waves
Leaky Mode
Shear Waves
True
False
True
False
True
False
True
False
Offset
Spacing
Arrival
True
False
True
False
24 inches
17 inches
12 inches
10 inches
Measure formation porosity
Qualitative estimation of permeability
Measure resistivity of the drilling fluid
Determination of flushed zone water saturation
Estimation of diameter of invasion
Ampere’s law
Ohm’s law
Faraday’s law
Mitchell’s law
Emitted from the Ao electrode and returns to the upper and lower A1 electrodes.
Emitted from the Ao electrode and returns to the current return electrode.
Emitted from the current return electrode and returns to the Ao electrode.
Emitted from the upper and lower A1 electrodes and returns to the Ao electrode.
Emitted from the A0 electrode and returns to the upper and lower A1 electrodes.
Emitted from the current return electrode and returns to the A0 electrode.
Emitted from the A0 electrode and returns to the current return electrode.
Emitted from the upper and lower A1 electrodes and returns to the A0 electrode.
The Ao electrode and the current return electrode
Monitor electrodes positioned along the HRID sonde assembly
The Ao electrode and the upper and lower A1 electrodes
Receiver coils within the HRID sonde assembly
< 17 inches
< 10 inches
< 12 inches
< 5 inches
Injecting a voltage into the formation and measuring a current between two electrodes.
Inducing a current into the formation and measuring a voltage between two receiver coils.
Injecting a current into the formation and measuring a voltage drop between two electrodes.
Inducing a voltage into the formation and measuring a current between two receiver coils.
Formation water resistivity (Rw)
True resistivity of the uninvaded formation (Rt)
Mud filtrate resistivity (Rmf)
Flushed zone resistivity (Rxo)
The DSNT is used to help estimate the volume of shale in a formation when combined with density porosity or sonic porosity.
The DSNT is used to determine a value for true resitivity of a formation.
The DSNT is often used as a quantitative estimate of permeability.
True
False
Hydrogen concentration does not influence count rate.
Low concentration of hydrogen results in lower count rates.
High concentration of hydrogen results in lower count rates.
Any physical separation between a detector and formation
The centralization of the detector in the borehole
The distance between the tool and the borehole wall
Glancing
Direct
Static
Decreases the count rate
Increases the count rate
Does not change the count rate
Oxygen
Hydrogen
Helium
10%
50%
35%
40%
Measure formation porosity
Measure formation permeability
Identification of gas bearing formations
Determine formation lithology
Determine formation resitivity
The larger the hole size, the higher the count rate detected
The larger the hole size, the lower the count rate detected
Large hole size has no effect on the count rate detected
Sandstone
Dolomite
Limestone
10 eV– 0.1 eV
1 MeV – 10 eV
10 MeV – 1 MeV
Number of thermal neutron multiplied by 100
Number of epithermal neutrons multiplied by 100
Number of thermal neutrons detected in one second
Number of epithermal neutrons detected in one second
The SS/LS ratio is inversely proportional to formation pososity.
Different formation lithologies do not affect the formation porosity.
Formation lithology must be known to determine accurate formation porosity.
Increased velocity
Increased travel times
Decreased travel times
Decreased velocity
All tools are calibrated at the API test pit in Houston.
A snow block is used to verify neutron tools at the well site..
A horizontal water tank is used to calibrate neutron tools at the well site.
The standard tool is calibrated at the API test pit in Houston.
True
False
Shear
Leaky mode
Compound
Stoneley
Leaky mode
Stoneley
Compressional
Shear
Shear
Mud
Stoneley
Compressional
8
16
4
2
Mud wave
Stoneley wave
Shear wave
Compressional wave
True
False
True
False
True
False
Reflected wave
Totall refracted wave
Critically refracted wave
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