Magnetotelluric monitoring of permeability enhancement at enhanced geothermal system project
被引:28
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作者:
Didana, Yohannes Lemma
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机构:
Univ Adelaide, Dept Earth Sci, Adelaide, SA, AustraliaUniv Adelaide, Dept Earth Sci, Adelaide, SA, Australia
Didana, Yohannes Lemma
[1
]
Heinson, Graham
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机构:
Univ Adelaide, Dept Earth Sci, Adelaide, SA, AustraliaUniv Adelaide, Dept Earth Sci, Adelaide, SA, Australia
Heinson, Graham
[1
]
Thiel, Stephan
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机构:
Univ Adelaide, Dept Earth Sci, Adelaide, SA, Australia
Geol Survey South Australia, Adelaide, SA, AustraliaUniv Adelaide, Dept Earth Sci, Adelaide, SA, Australia
Thiel, Stephan
[1
,2
]
Krieger, Lars
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机构:
Univ Adelaide, Dept Earth Sci, Adelaide, SA, Australia
Inst Geothermal Energy Resource Management, Bingen, GermanyUniv Adelaide, Dept Earth Sci, Adelaide, SA, Australia
Krieger, Lars
[1
,3
]
机构:
[1] Univ Adelaide, Dept Earth Sci, Adelaide, SA, Australia
[2] Geol Survey South Australia, Adelaide, SA, Australia
[3] Inst Geothermal Energy Resource Management, Bingen, Germany
Magnetotelluric (MT) data were collected across the Habanero Enhanced Geothermal System (EGS) project in the Cooper Basin, South Australia. A baseline regional MT survey consisting of two profiles were collected to delineate subsurface resistivity structure. An MT monitoring survey was conducted during stimulation of the Habanero-4 well. Inversions of the MT data in 2-D reveal three main resistivity layers to a depth of 5 km. The surface layer is <= 6 Omega m, 1.5 km thick, and composed of poorly consolidated sediments of Lake Eyre and Eromanga Basins. The second layer is <= 25 Omega m, 2 km thick, and correlated to consolidated Cooper Basin sediments. A high resistivity zone below depths of 3.5 km is interpreted as the hot intrusive granodiorite of the Big Lake Suite related to the Habanero EGS reservoir. The second MT survey was conducted during stimulation of Habanero-4, where 36.5 million liters (ML) of water with a resistivity of 13 Omega m was injected over 14 days. Analysis of pre- and post-injection residual phase tensors show possible conductive fractures oriented in a N-S direction for periods greater than 10 s. Apparent resistivity maps also revealed that injected fluids possibly propagated towards N-S direction. This result is in agreement with micro-seismic events observed at the Habanero EGS during fluid injection. The MT responses close to injection show on average 5% decrease in apparent resistivity for periods greater than 10 s. The main reasons for observing subtle changes in resistivity at Habanero EGS is the screening effect of the conductive thick sedimentary cover. Analysis of time-lapse models indicate an increase in total conductance of about 25 S in the N-S direction, which likely indicate anisotropic permeability generated by hydraulic stimulation. Overall, the MT monitoring at Habanero EGS highlights the need for favorable geological settings and/or controlled source and downhole EM methods to measure significant changes in resistivity in EGS reservoirs. (C) 2016 Elsevier Ltd. All rights reserved.
机构:
Univ Adelaide, South Australian Ctr Geothermal Energy Res, Adelaide, SA, AustraliaUniv Adelaide, South Australian Ctr Geothermal Energy Res, Adelaide, SA, Australia
Peacock, Jared R.
Thiel, Stephan
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机构:
Univ Adelaide, South Australian Ctr Geothermal Energy Res, Adelaide, SA, AustraliaUniv Adelaide, South Australian Ctr Geothermal Energy Res, Adelaide, SA, Australia
Thiel, Stephan
Heinson, Graham S.
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机构:
Univ Adelaide, Dept Geol & Geophys, TRaX, Adelaide, SA 5001, AustraliaUniv Adelaide, South Australian Ctr Geothermal Energy Res, Adelaide, SA, Australia
Heinson, Graham S.
Reid, Peter
论文数: 0引用数: 0
h-index: 0
机构:
Petratherm Ltd, Unley, AustraliaUniv Adelaide, South Australian Ctr Geothermal Energy Res, Adelaide, SA, Australia
机构:
Univ Adelaide, S Australian Ctr Geothermal Energy Res, Adelaide, SA, AustraliaUniv Adelaide, Dept Geol & Geosci, TRaX, Adelaide, SA 5005, Australia
Peacock, J. R.
Thiel, S.
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h-index: 0
机构:
Univ Adelaide, S Australian Ctr Geothermal Energy Res, Adelaide, SA, AustraliaUniv Adelaide, Dept Geol & Geosci, TRaX, Adelaide, SA 5005, Australia
Thiel, S.
Reid, P.
论文数: 0引用数: 0
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机构:
Petratherm Ltd, Adelaide, SA, AustraliaUniv Adelaide, Dept Geol & Geosci, TRaX, Adelaide, SA 5005, Australia
Reid, P.
Heinson, G.
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h-index: 0
机构:
Univ Adelaide, Dept Geol & Geosci, TRaX, Adelaide, SA 5005, AustraliaUniv Adelaide, Dept Geol & Geosci, TRaX, Adelaide, SA 5005, Australia
机构:
Chengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Prot, Chengdu 610059, Peoples R ChinaChengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Prot, Chengdu 610059, Peoples R China
Zhao, Peng
Liu, Jun
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机构:
Sichuan Univ, Inst New Energy & Low Carbon Technol, Key Lab Deep Underground Sci & Engn, Minist Educ, Chengdu 610065, Peoples R ChinaChengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Prot, Chengdu 610059, Peoples R China
Liu, Jun
Elsworth, Derek
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机构:
Penn State Univ, EMS Energy Inst, Dept Energy & Mineral Engn, University Pk, PA 16802 USA
Penn State Univ, Ctr G3, University Pk, PA 16802 USAChengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Prot, Chengdu 610059, Peoples R China
机构:
Inst Teknol Bandung, Undergrad Program Geophys Engn, Jalan Ganesha 10, Bandung 40132, IndonesiaInst Teknol Bandung, Undergrad Program Geophys Engn, Jalan Ganesha 10, Bandung 40132, Indonesia
Saputra, Rifki Mega
Widodo
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机构:
Inst Teknol Bandung, Appl & Explorat Geophys Res Grp, Jalan Ganesha 10, Bandung 40132, IndonesiaInst Teknol Bandung, Undergrad Program Geophys Engn, Jalan Ganesha 10, Bandung 40132, Indonesia
Widodo
SOUTHEAST ASIAN CONFERENCE ON GEOPHYSICS,
2017,
62