Fractal analysis for heat extraction in geothermal system

Heat conduction and convection play a key role in geothermal development. These two processes are coupled and influenced by fluid seepage in hot porous rock. A number of integer dimension thermal fluid models have been proposed to describe this coupling mechanism. However, fluid flow, heat...

Full description

Bibliographic Details
Main Authors: Shang Xiaoji, Wang Jianguo, Yang Xiaojun
Format: Article
Language:English
Published: VINCA Institute of Nuclear Sciences 2017-01-01
Series:Thermal Science
Subjects:
Online Access:http://www.doiserbia.nb.rs/img/doi/0354-9836/2017/0354-983617025S .pdf
id doaj-e80bee5b6a1441029f5b8fb4343d834c
record_format Article
spelling doaj-e80bee5b6a1441029f5b8fb4343d834c2021-01-02T01:47:11ZengVINCA Institute of Nuclear SciencesThermal Science0354-98362334-71632017-01-0121suppl. 1253110.2298/TSCI17S1025S0354-983617025SFractal analysis for heat extraction in geothermal systemShang Xiaoji0Wang Jianguo1Yang Xiaojun2China University of Mining and Technology, State Key Laboratory for Geomechanics and Deep Underground Engineering, Xuzhou, ChinaChina University of Mining and Technology, School of Mechanics and Civil Engineering, Xuzhou, ChinaChina University of Mining and Technology, School of Mechanics and Civil Engineering, Xuzhou, ChinaHeat conduction and convection play a key role in geothermal development. These two processes are coupled and influenced by fluid seepage in hot porous rock. A number of integer dimension thermal fluid models have been proposed to describe this coupling mechanism. However, fluid flow, heat conduction and convection in porous rock are usually non-linear, tortuous and fractal, thus the integer dimension thermal fluid flow models can not well describe these phenomena. In this study, a fractal thermal fluid coupling model is proposed to describe the heat conduction and flow behaviors in fractal hot porous rock in terms of local fractional time and space derivatives. This coupling equation is analytically solved through the fractal travelling wave transformation method. Analytical solutions of Darcy’s velocity, fluid temperature with fractal time and space are obtained. The solutions show that the introduction of fractional parameters is essential to describe the mechanism of heat conduction and convection.http://www.doiserbia.nb.rs/img/doi/0354-9836/2017/0354-983617025S .pdfheat conductionheat convectionfractalDarcy’s velocitythermal fluid coupling modellocal fractional operatorractal travelling wave transformation method
collection DOAJ
language English
format Article
sources DOAJ
author Shang Xiaoji
Wang Jianguo
Yang Xiaojun
spellingShingle Shang Xiaoji
Wang Jianguo
Yang Xiaojun
Fractal analysis for heat extraction in geothermal system
Thermal Science
heat conduction
heat convection
fractal
Darcy’s velocity
thermal fluid coupling model
local fractional operator
ractal travelling wave transformation method
author_facet Shang Xiaoji
Wang Jianguo
Yang Xiaojun
author_sort Shang Xiaoji
title Fractal analysis for heat extraction in geothermal system
title_short Fractal analysis for heat extraction in geothermal system
title_full Fractal analysis for heat extraction in geothermal system
title_fullStr Fractal analysis for heat extraction in geothermal system
title_full_unstemmed Fractal analysis for heat extraction in geothermal system
title_sort fractal analysis for heat extraction in geothermal system
publisher VINCA Institute of Nuclear Sciences
series Thermal Science
issn 0354-9836
2334-7163
publishDate 2017-01-01
description Heat conduction and convection play a key role in geothermal development. These two processes are coupled and influenced by fluid seepage in hot porous rock. A number of integer dimension thermal fluid models have been proposed to describe this coupling mechanism. However, fluid flow, heat conduction and convection in porous rock are usually non-linear, tortuous and fractal, thus the integer dimension thermal fluid flow models can not well describe these phenomena. In this study, a fractal thermal fluid coupling model is proposed to describe the heat conduction and flow behaviors in fractal hot porous rock in terms of local fractional time and space derivatives. This coupling equation is analytically solved through the fractal travelling wave transformation method. Analytical solutions of Darcy’s velocity, fluid temperature with fractal time and space are obtained. The solutions show that the introduction of fractional parameters is essential to describe the mechanism of heat conduction and convection.
topic heat conduction
heat convection
fractal
Darcy’s velocity
thermal fluid coupling model
local fractional operator
ractal travelling wave transformation method
url http://www.doiserbia.nb.rs/img/doi/0354-9836/2017/0354-983617025S .pdf
work_keys_str_mv AT shangxiaoji fractalanalysisforheatextractioningeothermalsystem
AT wangjianguo fractalanalysisforheatextractioningeothermalsystem
AT yangxiaojun fractalanalysisforheatextractioningeothermalsystem
_version_ 1724362604548194304