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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Main Authors: Peter Leary, Peter Malin, Tero Saarno, Ilmo Kukkonen
Format: Article in Journal/Newspaper
Language:unknown
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Online Access:https://www.mdpi.com/1996-1073/10/12/1979/pdf
https://www.mdpi.com/1996-1073/10/12/1979/
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spelling 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)
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id 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/
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