CSAMT method for determining depth and shape of a sub-surface conductive object
Abstract
The depth to and size of an underground object may be determined by sweeping a CSAMT signal and locating a peak response when the receiver spans the edge of the object. The depth of the object is one quarter wavelength in the subsurface media of the frequency of the peak.
- Inventors:
-
- Albuquerque, NM
- (Albuquerque, NM)
- Issue Date:
- Research Org.:
- Sandia National Laboratories (SNL), Albuquerque, NM, and Livermore, CA (United States)
- OSTI Identifier:
- 866009
- Patent Number(s):
- 4616184
- Assignee:
- United States of America as represented by United States (Washington, DC)
- Patent Classifications (CPCs):
-
G - PHYSICS G01 - MEASURING G01V - GEOPHYSICS
- DOE Contract Number:
- AC04-76DP00789
- Resource Type:
- Patent
- Country of Publication:
- United States
- Language:
- English
- Subject:
- csamt; method; determining; depth; shape; sub-surface; conductive; size; underground; determined; sweeping; signal; locating; peak; response; receiver; spans; edge; quarter; wavelength; subsurface; media; frequency; quarter wavelength; quarter wave; /324/
Citation Formats
Lee, David O, Montoya, Paul C, and Wayland, Jr., J. Robert. CSAMT method for determining depth and shape of a sub-surface conductive object. United States: N. p., 1986.
Web.
Lee, David O, Montoya, Paul C, & Wayland, Jr., J. Robert. CSAMT method for determining depth and shape of a sub-surface conductive object. United States.
Lee, David O, Montoya, Paul C, and Wayland, Jr., J. Robert. Wed .
"CSAMT method for determining depth and shape of a sub-surface conductive object". United States. https://www.osti.gov/servlets/purl/866009.
@article{osti_866009,
title = {CSAMT method for determining depth and shape of a sub-surface conductive object},
author = {Lee, David O and Montoya, Paul C and Wayland, Jr., J. Robert},
abstractNote = {The depth to and size of an underground object may be determined by sweeping a CSAMT signal and locating a peak response when the receiver spans the edge of the object. The depth of the object is one quarter wavelength in the subsurface media of the frequency of the peak.},
doi = {},
journal = {},
number = ,
volume = ,
place = {United States},
year = {1986},
month = {1}
}
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