SIESMIC AND ELECTRICAL METHODS Flashcards

(30 cards)

1
Q

-Are the most commonly conducted geophysical surveys for engineering investigations.
- _________ can be classified based on different criteria, such as wave type, survey technique, and application.

A

Seismic methods

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2
Q

Any mechanical vibration is initiated by a source and travels to the location where the vibration is noted.

A

SEISMIC WAVES

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3
Q

-The direction of travel is called the ____________________

A

ray, ray vector, or ray path.

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4
Q

2 TYPES OF SEISMIC WAVES

A
  1. BODY WAVES
  2. SURFACE WAVES
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5
Q

which pass through the volume of a material. These are the fastest traveling of all seismic waves

A

BODY WAVES

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6
Q

travel through all media that support seismic waves; air waves or noise in gasses, including the atmosphere.

A

P-WAVES

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7
Q

secondary or transverse or shear wave (S-wave). S-waves therefore do not exist in liquids and gasses

A

S - WAVES

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8
Q

are produced by surface impacts, explosions, and waveform changes at boundaries. Surface waves travel slower than body waves.

A

SURFACE WAVES

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9
Q

2 types of body waves

A

P-WAVES
S-WAVES

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10
Q

2 TYPES OF SURFACE WAVES

A

LOVE WAVES
RAYLEIGH WAVES

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11
Q

A type of seismic surface wave in which particles move with a side-to-side motion perpendicular to the main propagation of the earthquake.

A

LOVE WAVES

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12
Q

an undulating wave that travels over the surface of a solid, especially of the ground in an earthquake, with a speed independent of wavelength, the motion of the particles being in ellipses.

A

RAYLEIGH WAVE

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13
Q

Seismic methods can be classified based on how seismic waves are generated and measured

A
  1. ACTIVE SEISMIC METHODS
  2. PASSIVE SEISMIC METHODS
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14
Q

3 TYPES UNDER ACTIVE SEISMIC METHODS

A

 Seismic Refraction
Seismic Reflection
Seismic Tomography

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15
Q

__________- - is the study of seismic waves generated by natural earthquakes.

A

Earthquake seismology

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16
Q

__________________ is a passive seismic technique that studies low-amplitude ground vibrations.

A

Microtremor analysis

17
Q

Seismic methods are used in various fields, leading to classification by purpose

A

Exploration seismology
 Earthquake seismology
 Engineering seismology
Environmental and groundwater studies

18
Q

The seismic method relies on four key components to effectively analyze subsurface structures

A

Seismic Source
Geophones or Hydrophones
 Seismograph
Data Processing

19
Q

seismic waves that propagate through the Earth. These sources can be natural, such as earthquakes, or artificial, like explosives, mechanical impacts, or specialized vibrators used in exploration

A

SEISMIC SOURCE

20
Q

Serve as sensors. ________ are used on land to record ground vibrations.

21
Q

are employed in water to capture pressure variations caused by seismic waves.

22
Q

The equipment that records input geophone voltages in a timed sequence is the __________. Current practice uses ___________ that store the channels’ signals as digital data at discrete time.

23
Q

It involves filtering noise, enhancing signals, and applying mathematical algorithms to generate detailed subsurface images

A

DATA PROCESSING

24
Q

detect the surface effects produced by electric current flow in the ground.

A

Electrical geophysical prospecting methods

25
is a passive electrical geophysical method based upon the measurement of spontaneous or natural electrical potential developed in the earth d
The self-potential (SP) technique
26
Also called Earth Current, natural electric current flowing on and beneath the surface of the Earth and generally following a direction parallel to the Earth’s surface.
TELLURIC CURRENT
27
is a measure of the resistance of a given size of a specific material to electrical conduction.
Resistivity
28
was one of the first electrical methods and was used as far back as 1912 by Schlumberger. As explained elsewhere in this volume, when electric energy is applied to two points at the ground surface, an electric current will flow between them because of their difference in electrical potential.
EQUIPOTENTIAL METHOD
29
use transmitters to create strong time-varying primary magnetic fields that induce electrical currents to flow in conductive rocks. These currents, in turn, create secondary electromagnetic fields that are detected by receiver antennae.
Electromagnetic (EM) methods
30
and resistivity are two electrical properties measured in near-surface sediments as indirect hydrocarbon indicators. They are usually measured at the same time by inserting two electrodes into the earth surface and passing a current through them
Induced polarization (IP)