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...
Main Authors: | , , , |
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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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author | Peter Leary Peter Malin Tero Saarno Ilmo Kukkonen |
author_facet | Peter Leary Peter Malin Tero Saarno Ilmo Kukkonen |
author_sort | Peter Leary |
collection | RePEc (Research Papers in Economics) |
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 |
genre | Fennoscandia |
genre_facet | Fennoscandia |
id | ftrepec:oai:RePEc:gam:jeners:v:10:y:2017:i:12:p:1979-:d:121024 |
institution | Open Polar |
language | unknown |
op_collection_id | ftrepec |
op_relation | https://www.mdpi.com/1996-1073/10/12/1979/pdf https://www.mdpi.com/1996-1073/10/12/1979/ |
record_format | openpolar |
spelling | ftrepec:oai:RePEc:gam:jeners:v:10:y:2017:i:12:p:1979-:d:121024 2025-01-16T21:51:05+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) |
spellingShingle | Peter Leary Peter Malin Tero Saarno Ilmo Kukkonen Prospects for Assessing Enhanced Geothermal System (EGS) Basement Rock Flow Stimulation by Wellbore Temperature Data |
title | 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_short | 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/ |