THERMAL SCIENCE

International Scientific Journal

Hu-Chao Deng

,

Jian-Jun Hu

,

Gui-Kang Liu

,

Si-Qi Ye

,

Da-Li Sun

STUDY ON THE SURFACE MORPHOLOGY AND FRACTAL CHARACTERISTICS OF GRANITE UNDER THERMAL SHOCK OF SEAWATER

ABSTRACT
Geothermal energy has become one of the new energy sources of great concern due to its wide distribution, abundant reserves and green, clean and renewable advantages. In view of the advantages of both geothermal energy development potential and abundant seawater reserves in the coastal areas, granite is taken as the research object, and the surface topography under different temperatures (100°C, 200°C, 300°C, 400°C, and 500°C) and different thermal shock cycles (0, 5, 10, 15 and 20) is obtained. Based on 3-D scanning technology, the damage details of the surface are reconstructed, and the roughness parameters of the surface are obtained. The maximum height, the maximum valley depth and the arithmetic mean height increase with the increase of the temperature and the number of times, but the maximum peak height does not change significantly. Based on fractal theory, the variation law of the fractal dimension is further discussed. The impact regions that affect the fractal dimension and thermal damage are divided: the weak impact region, the transition region, and the significant impact region. It lays a corresponding basic law for the heat exchange efficiency and strength characteristics of dry hot rock.
KEYWORDS
energy evolution, dry hot rock, seawater thermal shock, surface morphology, fractal theory
PAPER SUBMITTED: 2022-08-27
PAPER REVISED: 2022-11-13
PAPER ACCEPTED: 2022-11-24
PUBLISHED ONLINE: 2023-03-04
DOI REFERENCE: https://doi.org/10.2298/TSCI2301571D
CITATION EXPORT: view in browser or download as text file
THERMAL SCIENCE YEAR 2023, VOLUME 27, ISSUE Issue 1, PAGES [571 - 579]
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Study on the surface morphology and fractal characteristics of granite under thermal shock of seawater

© 2024 Society of Thermal Engineers of Serbia. Published by the Vinča Institute of Nuclear Sciences, National Institute of the Republic of Serbia, Belgrade, Serbia. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution-NonCommercial-NoDerivs 4.0 International licence