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Investigation of Heat Transfer Performance and Sustainability

A special issue of Sustainability (ISSN 2071-1050). This special issue belongs to the section "Energy Sustainability".

Deadline for manuscript submissions: closed (30 July 2023) | Viewed by 2479

Special Issue Editors

Institute of Deep Earth Science and Green Energy, Shenzhen University, Shenzhen 518060, China
Interests: rock mechanics; deep-earth resource development; geothermal development and utilization
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Guest Editor
Institute of Deep Earth Sciences and Green Energy, Shenzhen University, Shenzhen 518060, China
Interests: rock mechanics and engineering geology; deep earth energy and minerals mining (coal, geothermal, unconventional natural gas); energy and resources policy

Special Issue Information

Dear Colleagues,

With the urgent demand for global clean energy, geothermal resources have gradually received increasing attention, and the development efforts in this direction have gradually increased. Geothermal energy is a green, low-carbon, recyclable renewable energy with the characteristics of large reserves, wide distribution, clean and environmentally friendly properties, stability and reliability. The development and utilization of geothermal energy are of great significance to adjusting the energy structure, saving energy and reducing emissions, and improving the environment. For deep geothermal resource development projects, the key physical processes involve the fluid flow of deep fractured rock mass as well as heat and mass transfer. The convective heat transfer mechanism and main control factors between low-temperature heat exchange working fluid and high-temperature rock mass in reservoirs are the keys to geothermal development. Deep in situ rock mass is under three-dimensional high-stress and high-temperature conditions. The role of high-pressure water is involved in the geothermal development process, and its mechanical behavior and seepage heat transfer mechanism are extremely complex. Therefore, clarifying the high-temperature mechanical behavior of deep in situ rock mass and the coupling mechanism of seepage heat and mass transfer is the theoretical basis and prerequisite for realizing the safety and rational development of deep earth resources.

This Special Issue encourages submissions which will provide new insights into the development of deep geothermal energy, focusing on rock mechanics and heat/mass transfer behaviors in geothermal reservoirs. We actively encourage participation from researchers in the fields of deep resource exploration and evaluation, reservoir simulation technology, rock mechanics theory, and heat and mass transfer.

Dr. Jun Lu
Dr. Delei Shang
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Sustainability is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2400 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • mechanical behavior of deep high-temperature rock
  • seepage heat transfer behavior and model of fracture rock
  • geothermal development systems and theoretical technologies
  • mass transfer characteristics of high-temperature fluids
  • geothermal resources

Published Papers (2 papers)

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Research

15 pages, 4098 KiB  
Article
Experimental Study on the Effect of Freeze-Thaw Cycles on the Mechanical and Permeability Characteristics of Coal
by Heng Gao, Jun Lu, Zetian Zhang, Cong Li and Yihang Li
Sustainability 2023, 15(16), 12598; https://doi.org/10.3390/su151612598 - 20 Aug 2023
Viewed by 792
Abstract
The safe and efficient mining of coal seams with low porosity, low permeability, and high heterogeneity under complex geological conditions is a major challenge, with the permeability of coal seams playing a crucial role in coal mine gas extraction. The development of coal [...] Read more.
The safe and efficient mining of coal seams with low porosity, low permeability, and high heterogeneity under complex geological conditions is a major challenge, with the permeability of coal seams playing a crucial role in coal mine gas extraction. The development of coal seam permeability enhancement technology can help coal mines produce safely and efficiently, while the extracted coal bed methane can be utilized as green energy. To study the effect of freezing and thawing on the evolution of the mechanical and permeability properties of coal, triaxial permeability tests were conducted on low-permeability coal under two different confining pressures. Simultaneously, dry, saturated, and freeze-thaw coal samples were set up for comparison, and the effects of water and freeze-thaw were isolated from each other. The triaxial mechanics and percolation laws of dry, saturated, and freeze-thaw coal rocks were obtained; the results show that saturated coal has the lowest initial permeability, while freeze-thawed coal has the highest initial permeability. Through analyzing the effects produced by water, freezing and thawing on coal specimens, the mechanism of the influence of freeze-thaw on the permeability evolution of coal was revealed. The research results can provide theoretical guidance for the development of gas extraction technology for low-permeability coal seams. Full article
(This article belongs to the Special Issue Investigation of Heat Transfer Performance and Sustainability)
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21 pages, 6137 KiB  
Article
Effect of Loading and Unloading Rates on Sandstone Deformation and Dilatancy under True Triaxial Condition
by Yingwei Wang, Weihang Du, Dongming Zhang and Beichen Yu
Sustainability 2023, 15(6), 5105; https://doi.org/10.3390/su15065105 - 14 Mar 2023
Cited by 3 | Viewed by 1191
Abstract
After conducting true triaxial tests on sandstone in a laboratory setting, this study aims to determine the safe tunnelling rate of the roadway by examining the instability and failure characteristics of surrounding rock under different disturbance stresses in deep underground roadway excavation. Results [...] Read more.
After conducting true triaxial tests on sandstone in a laboratory setting, this study aims to determine the safe tunnelling rate of the roadway by examining the instability and failure characteristics of surrounding rock under different disturbance stresses in deep underground roadway excavation. Results showed that the mechanical properties, deformation, and failure characteristics of sandstone differed under different loading and unloading rates. Specifically, as the loading rate increased, the crack initiation stress increased while the damage stress remained unchanged, and the deformation anisotropy of the rock decreased. In contrast, as the unloading rate increased, the residual stress of the rock decreased, the brittleness increased, and the deformation anisotropy of the rock increased. Additionally, the expansion of the rock went through three critical stages: (1) A–B: a sharp increase in the dilatancy of sandstone (M) in a short period, accompanied by a large number of cracks, (2) B–C: a weakened stage of expansion ability, in which M continued to decrease over time, albeit at a slower rate, and (3) C–D: a stage of enhanced expansion ability, during which M began to increase again, albeit at a slower rate than its rate of decrease. This final stage was the longest. Full article
(This article belongs to the Special Issue Investigation of Heat Transfer Performance and Sustainability)
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