Effects of fracture parameters and roughness on heat‐flow coupling in rock masses with two‐dimensional fracture networks

Abstract Discrete fracture network (DFN) is an effective means of describing the coupling of heat flow in an underground fractured rock mass. In this paper, an improved DFN is proposed by introducing the correlation function of fracture trace length and aperture, which is more consistent with the re...

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Main Authors: Fan Huang, Chi Yao, Xiaobo Zhang, Ligong Wu, Yulong Shao, Chuangbing Zhou
Format: Article
Language:English
Published: Wiley 2021-08-01
Series:Energy Science & Engineering
Subjects:
Online Access:https://doi.org/10.1002/ese3.885
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spelling doaj-09b7d1283dd448368987d211516f3d8a2021-08-03T15:52:59ZengWileyEnergy Science & Engineering2050-05052021-08-01981216123110.1002/ese3.885Effects of fracture parameters and roughness on heat‐flow coupling in rock masses with two‐dimensional fracture networksFan Huang0Chi Yao1Xiaobo Zhang2Ligong Wu3Yulong Shao4Chuangbing Zhou5School of Civil Engineering and Architecture Nanchang University Nanchang People's Republic of ChinaSchool of Civil Engineering and Architecture Nanchang University Nanchang People's Republic of ChinaSchool of Civil Engineering and Architecture Nanchang University Nanchang People's Republic of ChinaSchool of Civil Engineering and Architecture Nanchang University Nanchang People's Republic of ChinaSchool of Civil Engineering and Architecture Nanchang University Nanchang People's Republic of ChinaSchool of Civil Engineering and Architecture Nanchang University Nanchang People's Republic of ChinaAbstract Discrete fracture network (DFN) is an effective means of describing the coupling of heat flow in an underground fractured rock mass. In this paper, an improved DFN is proposed by introducing the correlation function of fracture trace length and aperture, which is more consistent with the real fracture data. Next, based on the improved model, the influence of fracture roughness on the fluid flow and heat transmission was evaluated, and the relationship between the fracture aperture and the joint roughness coefficient (JRC) is established. Finally, based on the exponential function between confining pressure and aperture, the influence of confining pressure on the heat‐flow coupling process is considered in the improved model. Besides, the reliability of the model was verified by comparing with the analytical solution of the two‐dimensional single‐fracture heat‐flow coupling problem. The results show that under the same conditions, considering the correlation between the geometric parameters of the fracture, the seepage and heat transfer rates of the model increased, the outlet boundary flow reached the maximum value, and the average outlet temperature dropped rapidly. However, the fracture roughness reduces the outlet flow rate and the decline rate of average temperature. The confining pressure will lead to a decrease of about 3.5% in the outlet flow of the model, which is consistent with the seepage law in practical engineering. The model presented in this paper is an effective supplement to the two‐dimensional fracture network heat‐flow coupling model and can provide a theoretical basis and a numerical calculation tool for related underground rock mass engineering.https://doi.org/10.1002/ese3.885correlation functiondiscrete fracture networkheat transferheat‐flow couplingjoint roughness coefficientseepage
collection DOAJ
language English
format Article
sources DOAJ
author Fan Huang
Chi Yao
Xiaobo Zhang
Ligong Wu
Yulong Shao
Chuangbing Zhou
spellingShingle Fan Huang
Chi Yao
Xiaobo Zhang
Ligong Wu
Yulong Shao
Chuangbing Zhou
Effects of fracture parameters and roughness on heat‐flow coupling in rock masses with two‐dimensional fracture networks
Energy Science & Engineering
correlation function
discrete fracture network
heat transfer
heat‐flow coupling
joint roughness coefficient
seepage
author_facet Fan Huang
Chi Yao
Xiaobo Zhang
Ligong Wu
Yulong Shao
Chuangbing Zhou
author_sort Fan Huang
title Effects of fracture parameters and roughness on heat‐flow coupling in rock masses with two‐dimensional fracture networks
title_short Effects of fracture parameters and roughness on heat‐flow coupling in rock masses with two‐dimensional fracture networks
title_full Effects of fracture parameters and roughness on heat‐flow coupling in rock masses with two‐dimensional fracture networks
title_fullStr Effects of fracture parameters and roughness on heat‐flow coupling in rock masses with two‐dimensional fracture networks
title_full_unstemmed Effects of fracture parameters and roughness on heat‐flow coupling in rock masses with two‐dimensional fracture networks
title_sort effects of fracture parameters and roughness on heat‐flow coupling in rock masses with two‐dimensional fracture networks
publisher Wiley
series Energy Science & Engineering
issn 2050-0505
publishDate 2021-08-01
description Abstract Discrete fracture network (DFN) is an effective means of describing the coupling of heat flow in an underground fractured rock mass. In this paper, an improved DFN is proposed by introducing the correlation function of fracture trace length and aperture, which is more consistent with the real fracture data. Next, based on the improved model, the influence of fracture roughness on the fluid flow and heat transmission was evaluated, and the relationship between the fracture aperture and the joint roughness coefficient (JRC) is established. Finally, based on the exponential function between confining pressure and aperture, the influence of confining pressure on the heat‐flow coupling process is considered in the improved model. Besides, the reliability of the model was verified by comparing with the analytical solution of the two‐dimensional single‐fracture heat‐flow coupling problem. The results show that under the same conditions, considering the correlation between the geometric parameters of the fracture, the seepage and heat transfer rates of the model increased, the outlet boundary flow reached the maximum value, and the average outlet temperature dropped rapidly. However, the fracture roughness reduces the outlet flow rate and the decline rate of average temperature. The confining pressure will lead to a decrease of about 3.5% in the outlet flow of the model, which is consistent with the seepage law in practical engineering. The model presented in this paper is an effective supplement to the two‐dimensional fracture network heat‐flow coupling model and can provide a theoretical basis and a numerical calculation tool for related underground rock mass engineering.
topic correlation function
discrete fracture network
heat transfer
heat‐flow coupling
joint roughness coefficient
seepage
url https://doi.org/10.1002/ese3.885
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