Mine Backfilling in the Permafrost, Part I: Numerical Prediction of Thermal Curing Conditions within the Cemented Paste Backfill Matrix

The mechanical behavior of cemented paste backfill (CPB) in permafrost regions may depend on the thermal curing conditions. However, few experimental data are available for calibrating and validating numerical models used to predict these conditions. To fill this gap, a three-dimensional (3D) labora...

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Published in:Minerals
Main Authors: Fabrice Beya, Mamert Mbonimpa, Tikou Belem, Li Li, Ugo Marceau, Patrick Kalonji, Mostafa Benzaazoua, Serge Ouellet
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
Online Access:https://doi.org/10.3390/min9030165
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author Fabrice Beya
Mamert Mbonimpa
Tikou Belem
Li Li
Ugo Marceau
Patrick Kalonji
Mostafa Benzaazoua
Serge Ouellet
author_facet Fabrice Beya
Mamert Mbonimpa
Tikou Belem
Li Li
Ugo Marceau
Patrick Kalonji
Mostafa Benzaazoua
Serge Ouellet
author_sort Fabrice Beya
collection MDPI Open Access Publishing
container_issue 3
container_start_page 165
container_title Minerals
container_volume 9
description The mechanical behavior of cemented paste backfill (CPB) in permafrost regions may depend on the thermal curing conditions. However, few experimental data are available for calibrating and validating numerical models used to predict these conditions. To fill this gap, a three-dimensional (3D) laboratory heat transfer test was conducted on CPB placed in an instrumented barrel and cured under a constant temperature of −11 °C. Results were used to calibrate and validate a numerical model built with COMSOL Multiphysics®. The model was then used to predict the evolution of the temperature field for CPB cured under the thermal boundary conditions for a backfilled mine stope in the permafrost (at −6 °C). Numerical results indicated that the CPB temperature gradually decreased with time such that the entire CPB mass was frozen about five years after stope backfilling. However, the permafrost equilibrium temperature of −6 °C was not reached throughout the entire CPB mass even after 20 years of curing. In addition, the evolution of the temperature field in the permafrost rock showed that the thickness of the thawed portion reached about 1 m within 120 days. Afterwards, the temperature continues to drop over time and the thawed portion of the permafrost refreezes after 365 days.
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genre permafrost
genre_facet permafrost
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op_doi https://doi.org/10.3390/min9030165
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op_source Minerals; Volume 9; Issue 3; Pages: 165
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spelling ftmdpi:oai:mdpi.com:/2075-163X/9/3/165/ 2025-01-17T00:13:06+00:00 Mine Backfilling in the Permafrost, Part I: Numerical Prediction of Thermal Curing Conditions within the Cemented Paste Backfill Matrix Fabrice Beya Mamert Mbonimpa Tikou Belem Li Li Ugo Marceau Patrick Kalonji Mostafa Benzaazoua Serge Ouellet agris 2019-03-08 application/pdf https://doi.org/10.3390/min9030165 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/min9030165 https://creativecommons.org/licenses/by/4.0/ Minerals; Volume 9; Issue 3; Pages: 165 cemented paste backfill (CPB) permafrost heat transfer numerical modeling model calibration COMSOL Multiphysics ® Text 2019 ftmdpi https://doi.org/10.3390/min9030165 2023-07-31T22:06:04Z The mechanical behavior of cemented paste backfill (CPB) in permafrost regions may depend on the thermal curing conditions. However, few experimental data are available for calibrating and validating numerical models used to predict these conditions. To fill this gap, a three-dimensional (3D) laboratory heat transfer test was conducted on CPB placed in an instrumented barrel and cured under a constant temperature of −11 °C. Results were used to calibrate and validate a numerical model built with COMSOL Multiphysics®. The model was then used to predict the evolution of the temperature field for CPB cured under the thermal boundary conditions for a backfilled mine stope in the permafrost (at −6 °C). Numerical results indicated that the CPB temperature gradually decreased with time such that the entire CPB mass was frozen about five years after stope backfilling. However, the permafrost equilibrium temperature of −6 °C was not reached throughout the entire CPB mass even after 20 years of curing. In addition, the evolution of the temperature field in the permafrost rock showed that the thickness of the thawed portion reached about 1 m within 120 days. Afterwards, the temperature continues to drop over time and the thawed portion of the permafrost refreezes after 365 days. Text permafrost MDPI Open Access Publishing Minerals 9 3 165
spellingShingle cemented paste backfill (CPB)
permafrost
heat transfer
numerical modeling
model calibration
COMSOL Multiphysics ®
Fabrice Beya
Mamert Mbonimpa
Tikou Belem
Li Li
Ugo Marceau
Patrick Kalonji
Mostafa Benzaazoua
Serge Ouellet
Mine Backfilling in the Permafrost, Part I: Numerical Prediction of Thermal Curing Conditions within the Cemented Paste Backfill Matrix
title Mine Backfilling in the Permafrost, Part I: Numerical Prediction of Thermal Curing Conditions within the Cemented Paste Backfill Matrix
title_full Mine Backfilling in the Permafrost, Part I: Numerical Prediction of Thermal Curing Conditions within the Cemented Paste Backfill Matrix
title_fullStr Mine Backfilling in the Permafrost, Part I: Numerical Prediction of Thermal Curing Conditions within the Cemented Paste Backfill Matrix
title_full_unstemmed Mine Backfilling in the Permafrost, Part I: Numerical Prediction of Thermal Curing Conditions within the Cemented Paste Backfill Matrix
title_short Mine Backfilling in the Permafrost, Part I: Numerical Prediction of Thermal Curing Conditions within the Cemented Paste Backfill Matrix
title_sort mine backfilling in the permafrost, part i: numerical prediction of thermal curing conditions within the cemented paste backfill matrix
topic cemented paste backfill (CPB)
permafrost
heat transfer
numerical modeling
model calibration
COMSOL Multiphysics ®
topic_facet cemented paste backfill (CPB)
permafrost
heat transfer
numerical modeling
model calibration
COMSOL Multiphysics ®
url https://doi.org/10.3390/min9030165