Forward modeling and inversion of IP effects in TEM response using measured rock samples data

Hesham M. El-Kaliouby; Safwat Hussain; Esam A. El Diwany; Esam Hashish; Abdel Rahim Bayoumi; Mary M. Poulton

Forward modeling and inversion of IP effects in TEM response using measured rock samples data

Hesham M. El-Kaliouby, Safwat Hussain, Esam A. El Diwany, Esam Hashish, Abdel Rahim Bayoumi, Mary M. Poulton

Mining and Geological Engineering

Research output: Contribution to conference › Paper › peer-review

Abstract

Forward modeling is made for the transient voltage response of a coincident loop system above layered ground containing polarizable water-saturated clay-bearing sandstone and hematitic sandstone. The electrical properties of the water-saturated layer are obtained from laboratory measurements. For the clay bearing sandstone these properties are not described by a Cole-Cole model in the frequency range of interest for TEM response from 5 Hz-500 kHz. Modular neural network inversion of the transient response is performed to find its main Cole-Cole dispersive parameters. Forward modeling for a water aquifer with an upper partially saturated layer shows a negligible effect of such layer.

Original language	English (US)
State	Published - 2001
Event	2001 Society of Exploration Geophysicists Annual Meeting, SEG 2001 - San Antonio, United States Duration: Sep 9 2001 → Sep 14 2001

Other

Other	2001 Society of Exploration Geophysicists Annual Meeting, SEG 2001
Country/Territory	United States
City	San Antonio
Period	9/9/01 → 9/14/01

ASJC Scopus subject areas

Geophysics

Cite this

@conference{5bd2fa9455134bd1a5960a58942e8d79,

title = "Forward modeling and inversion of IP effects in TEM response using measured rock samples data",

abstract = "Forward modeling is made for the transient voltage response of a coincident loop system above layered ground containing polarizable water-saturated clay-bearing sandstone and hematitic sandstone. The electrical properties of the water-saturated layer are obtained from laboratory measurements. For the clay bearing sandstone these properties are not described by a Cole-Cole model in the frequency range of interest for TEM response from 5 Hz-500 kHz. Modular neural network inversion of the transient response is performed to find its main Cole-Cole dispersive parameters. Forward modeling for a water aquifer with an upper partially saturated layer shows a negligible effect of such layer.",

author = "El-Kaliouby, {Hesham M.} and Safwat Hussain and {El Diwany}, {Esam A.} and Esam Hashish and Bayoumi, {Abdel Rahim} and Poulton, {Mary M.}",

note = "Publisher Copyright: {\textcopyright} 2001 Society of Exploration Geophysicists. All rights reserved.; 2001 Society of Exploration Geophysicists Annual Meeting, SEG 2001 ; Conference date: 09-09-2001 Through 14-09-2001",

year = "2001",

language = "English (US)",

}

TY - CONF

T1 - Forward modeling and inversion of IP effects in TEM response using measured rock samples data

AU - El-Kaliouby, Hesham M.

AU - Hussain, Safwat

AU - El Diwany, Esam A.

AU - Hashish, Esam

AU - Bayoumi, Abdel Rahim

AU - Poulton, Mary M.

PY - 2001

Y1 - 2001

N2 - Forward modeling is made for the transient voltage response of a coincident loop system above layered ground containing polarizable water-saturated clay-bearing sandstone and hematitic sandstone. The electrical properties of the water-saturated layer are obtained from laboratory measurements. For the clay bearing sandstone these properties are not described by a Cole-Cole model in the frequency range of interest for TEM response from 5 Hz-500 kHz. Modular neural network inversion of the transient response is performed to find its main Cole-Cole dispersive parameters. Forward modeling for a water aquifer with an upper partially saturated layer shows a negligible effect of such layer.

AB - Forward modeling is made for the transient voltage response of a coincident loop system above layered ground containing polarizable water-saturated clay-bearing sandstone and hematitic sandstone. The electrical properties of the water-saturated layer are obtained from laboratory measurements. For the clay bearing sandstone these properties are not described by a Cole-Cole model in the frequency range of interest for TEM response from 5 Hz-500 kHz. Modular neural network inversion of the transient response is performed to find its main Cole-Cole dispersive parameters. Forward modeling for a water aquifer with an upper partially saturated layer shows a negligible effect of such layer.

UR - http://www.scopus.com/inward/record.url?scp=85054060169&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=85054060169&partnerID=8YFLogxK

M3 - Paper

AN - SCOPUS:85054060169

T2 - 2001 Society of Exploration Geophysicists Annual Meeting, SEG 2001

Y2 - 9 September 2001 through 14 September 2001

ER -

Forward modeling and inversion of IP effects in TEM response using measured rock samples data

Abstract

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ASJC Scopus subject areas

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