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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Online Access: | https://doi.org/10.1002/ese3.885 |
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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 |
work_keys_str_mv |
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1721223072596361216 |