Prospects for Assessing Enhanced Geothermal System (EGS) Basement Rock Flow Stimulation by Wellbore Temperature Data
We use Matlab 3D finite element fluid flow/transport modelling to simulate localized wellbore temperature events of order 0.05–0.1 °C logged in Fennoscandia basement rock at ~1.5 km depths. The temperature events are approximated as steady-state heat transport due to fluid draining from the crust in...
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ftrepec:oai:RePEc:gam:jeners:v:10:y:2017:i:12:p:1979-:d:121024 2024-04-14T08:11:27+00:00 Prospects for Assessing Enhanced Geothermal System (EGS) Basement Rock Flow Stimulation by Wellbore Temperature Data Peter Leary Peter Malin Tero Saarno Ilmo Kukkonen https://www.mdpi.com/1996-1073/10/12/1979/pdf https://www.mdpi.com/1996-1073/10/12/1979/ unknown https://www.mdpi.com/1996-1073/10/12/1979/pdf https://www.mdpi.com/1996-1073/10/12/1979/ article ftrepec 2024-03-19T10:31:15Z We use Matlab 3D finite element fluid flow/transport modelling to simulate localized wellbore temperature events of order 0.05–0.1 °C logged in Fennoscandia basement rock at ~1.5 km depths. The temperature events are approximated as steady-state heat transport due to fluid draining from the crust into the wellbore via naturally occurring fracture-connectivity structures. Flow simulation is based on the empirics of spatially-correlated fracture-connectivity fluid flow widely attested by well-log, well-core, and well-production data. Matching model wellbore-centric radial temperature profiles to a 2D analytic expression for steady-state radial heat transport with Peclet number P e ≡ r 0 φv 0 /D (r 0 = wellbore radius, v 0 = Darcy velocity at r 0 , φ = ambient porosity, D = rock-water thermal diffusivity), gives P e ~ 10–15 for fracture-connectivity flow intersecting the well, and P e ~ 0 for ambient crust. Darcy flow for model P e ~ 10 at radius ~10 m from the wellbore gives permeability estimate κ ~ 0.02 Darcy for flow driven by differential fluid pressure between least principal crustal stress pore pressure and hydrostatic wellbore pressure. Model temperature event flow permeability κ m ~ 0.02 Darcy is related to well-core ambient permeability κ ~ 1 µDarcy by empirical poroperm relation κ m ~ κ exp(α m φ) for φ ~ 0.01 and α m ~ 1000. Our modelling of OTN1 wellbore temperature events helps assess the prospect of reactivating fossilized fracture-connectivity flow for EGS permeability stimulation of basement rock. enhanced geothermal systems (EGS); crustal permeability; finite element flow modelling; crustal wellbore temperatures; wellbore injection; well logs; well core Article in Journal/Newspaper Fennoscandia RePEc (Research Papers in Economics) |
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Open Polar |
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RePEc (Research Papers in Economics) |
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ftrepec |
language |
unknown |
description |
We use Matlab 3D finite element fluid flow/transport modelling to simulate localized wellbore temperature events of order 0.05–0.1 °C logged in Fennoscandia basement rock at ~1.5 km depths. The temperature events are approximated as steady-state heat transport due to fluid draining from the crust into the wellbore via naturally occurring fracture-connectivity structures. Flow simulation is based on the empirics of spatially-correlated fracture-connectivity fluid flow widely attested by well-log, well-core, and well-production data. Matching model wellbore-centric radial temperature profiles to a 2D analytic expression for steady-state radial heat transport with Peclet number P e ≡ r 0 φv 0 /D (r 0 = wellbore radius, v 0 = Darcy velocity at r 0 , φ = ambient porosity, D = rock-water thermal diffusivity), gives P e ~ 10–15 for fracture-connectivity flow intersecting the well, and P e ~ 0 for ambient crust. Darcy flow for model P e ~ 10 at radius ~10 m from the wellbore gives permeability estimate κ ~ 0.02 Darcy for flow driven by differential fluid pressure between least principal crustal stress pore pressure and hydrostatic wellbore pressure. Model temperature event flow permeability κ m ~ 0.02 Darcy is related to well-core ambient permeability κ ~ 1 µDarcy by empirical poroperm relation κ m ~ κ exp(α m φ) for φ ~ 0.01 and α m ~ 1000. Our modelling of OTN1 wellbore temperature events helps assess the prospect of reactivating fossilized fracture-connectivity flow for EGS permeability stimulation of basement rock. enhanced geothermal systems (EGS); crustal permeability; finite element flow modelling; crustal wellbore temperatures; wellbore injection; well logs; well core |
format |
Article in Journal/Newspaper |
author |
Peter Leary Peter Malin Tero Saarno Ilmo Kukkonen |
spellingShingle |
Peter Leary Peter Malin Tero Saarno Ilmo Kukkonen Prospects for Assessing Enhanced Geothermal System (EGS) Basement Rock Flow Stimulation by Wellbore Temperature Data |
author_facet |
Peter Leary Peter Malin Tero Saarno Ilmo Kukkonen |
author_sort |
Peter Leary |
title |
Prospects for Assessing Enhanced Geothermal System (EGS) Basement Rock Flow Stimulation by Wellbore Temperature Data |
title_short |
Prospects for Assessing Enhanced Geothermal System (EGS) Basement Rock Flow Stimulation by Wellbore Temperature Data |
title_full |
Prospects for Assessing Enhanced Geothermal System (EGS) Basement Rock Flow Stimulation by Wellbore Temperature Data |
title_fullStr |
Prospects for Assessing Enhanced Geothermal System (EGS) Basement Rock Flow Stimulation by Wellbore Temperature Data |
title_full_unstemmed |
Prospects for Assessing Enhanced Geothermal System (EGS) Basement Rock Flow Stimulation by Wellbore Temperature Data |
title_sort |
prospects for assessing enhanced geothermal system (egs) basement rock flow stimulation by wellbore temperature data |
url |
https://www.mdpi.com/1996-1073/10/12/1979/pdf https://www.mdpi.com/1996-1073/10/12/1979/ |
genre |
Fennoscandia |
genre_facet |
Fennoscandia |
op_relation |
https://www.mdpi.com/1996-1073/10/12/1979/pdf https://www.mdpi.com/1996-1073/10/12/1979/ |
_version_ |
1796309150756503552 |