A study of electric field components in shallow water and water half-space models in seabed logging

Seabed logging (SBL) is an electromagnetic (EM) method to detect hydrocarbon (HC) laid beneath the seafloor, which is a development of marine controlled source electromagnetic (CSEM) method. CSEM is a method to show resistivity log of geological layers, transmitting ultra-low frequency EM wave. In S...

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Main Authors: Rostami, A., Soleimani, H., Yahya, N., Nyamasvisva, T.E., Rauf, M.
Format: Conference or Workshop Item
Published: American Institute of Physics Inc. 2016
Online Access:https://www.scopus.com/inward/record.uri?eid=2-s2.0-85006021781&doi=10.1063%2f1.4968134&partnerID=40&md5=3918d81e322b45b7187d002e93d3754a
http://eprints.utp.edu.my/30611/
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spelling my.utp.eprints.306112022-03-25T07:12:19Z A study of electric field components in shallow water and water half-space models in seabed logging Rostami, A. Soleimani, H. Yahya, N. Nyamasvisva, T.E. Rauf, M. Seabed logging (SBL) is an electromagnetic (EM) method to detect hydrocarbon (HC) laid beneath the seafloor, which is a development of marine controlled source electromagnetic (CSEM) method. CSEM is a method to show resistivity log of geological layers, transmitting ultra-low frequency EM wave. In SBL a net of receivers, placed on the seafloor, detect reflected and refracted EM wave by layers with different resistivity. Contrast of electrical resistivity of layers impacts on amplitude and phase of the EM wave response. The most indispensable concern in SBL is to detect guided wave via high resistive layer under the seafloor that can be an HC reservoir. Guided wave by HC creates a remarkable difference in received signal when HC reservoir does not exist. While the major contribution of received EM wave in large offset, especially in shallow water environment, is airwave, which is refracted by sea surface due to extremely high resistivity of atmosphere, airwave can affect received guided wave, dramatically. Our objective for this work is to compare HC delineation of tangential and normal components of electric field in shallow water area, using finite element method simulation. Will be reported that, in shallow water environment, minor contribution of air wave in normal component of E field (Ey) versus its major contribution in the tangential component (Ex), causes a considerable contrast on HC delineation of Ey for deeply buried reservoirs (more than 3000 m), while Ex is unable to show different contrasts of received data for with and without HC media at the same condition. © 2016 Author(s). American Institute of Physics Inc. 2016 Conference or Workshop Item NonPeerReviewed https://www.scopus.com/inward/record.uri?eid=2-s2.0-85006021781&doi=10.1063%2f1.4968134&partnerID=40&md5=3918d81e322b45b7187d002e93d3754a Rostami, A. and Soleimani, H. and Yahya, N. and Nyamasvisva, T.E. and Rauf, M. (2016) A study of electric field components in shallow water and water half-space models in seabed logging. In: UNSPECIFIED. http://eprints.utp.edu.my/30611/
institution Universiti Teknologi Petronas
building UTP Resource Centre
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Petronas
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url_provider http://eprints.utp.edu.my/
description Seabed logging (SBL) is an electromagnetic (EM) method to detect hydrocarbon (HC) laid beneath the seafloor, which is a development of marine controlled source electromagnetic (CSEM) method. CSEM is a method to show resistivity log of geological layers, transmitting ultra-low frequency EM wave. In SBL a net of receivers, placed on the seafloor, detect reflected and refracted EM wave by layers with different resistivity. Contrast of electrical resistivity of layers impacts on amplitude and phase of the EM wave response. The most indispensable concern in SBL is to detect guided wave via high resistive layer under the seafloor that can be an HC reservoir. Guided wave by HC creates a remarkable difference in received signal when HC reservoir does not exist. While the major contribution of received EM wave in large offset, especially in shallow water environment, is airwave, which is refracted by sea surface due to extremely high resistivity of atmosphere, airwave can affect received guided wave, dramatically. Our objective for this work is to compare HC delineation of tangential and normal components of electric field in shallow water area, using finite element method simulation. Will be reported that, in shallow water environment, minor contribution of air wave in normal component of E field (Ey) versus its major contribution in the tangential component (Ex), causes a considerable contrast on HC delineation of Ey for deeply buried reservoirs (more than 3000 m), while Ex is unable to show different contrasts of received data for with and without HC media at the same condition. © 2016 Author(s).
format Conference or Workshop Item
author Rostami, A.
Soleimani, H.
Yahya, N.
Nyamasvisva, T.E.
Rauf, M.
spellingShingle Rostami, A.
Soleimani, H.
Yahya, N.
Nyamasvisva, T.E.
Rauf, M.
A study of electric field components in shallow water and water half-space models in seabed logging
author_facet Rostami, A.
Soleimani, H.
Yahya, N.
Nyamasvisva, T.E.
Rauf, M.
author_sort Rostami, A.
title A study of electric field components in shallow water and water half-space models in seabed logging
title_short A study of electric field components in shallow water and water half-space models in seabed logging
title_full A study of electric field components in shallow water and water half-space models in seabed logging
title_fullStr A study of electric field components in shallow water and water half-space models in seabed logging
title_full_unstemmed A study of electric field components in shallow water and water half-space models in seabed logging
title_sort study of electric field components in shallow water and water half-space models in seabed logging
publisher American Institute of Physics Inc.
publishDate 2016
url https://www.scopus.com/inward/record.uri?eid=2-s2.0-85006021781&doi=10.1063%2f1.4968134&partnerID=40&md5=3918d81e322b45b7187d002e93d3754a
http://eprints.utp.edu.my/30611/
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