Utilizing Asphalt Heat Energy in Finnish Climate Conditions

Geothermal energy is a form of renewable energy, which offers carbon-free solutions for heating and cooling spaces. This study evaluates the use of renewable asphalt heat energy in frozen ground conditions. Asphalt heat energy can be harnessed using a low-energy network, heat collection pipes and he...

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Main Authors: Anne Mäkiranta, Erkki Hiltunen
Format: Article
Language:English
Published: MDPI AG 2019-06-01
Series:Energies
Subjects:
Online Access:https://www.mdpi.com/1996-1073/12/11/2101
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spelling doaj-a3a02dbaff4846b3b9c3bdb208300af22020-11-25T02:10:50ZengMDPI AGEnergies1996-10732019-06-011211210110.3390/en12112101en12112101Utilizing Asphalt Heat Energy in Finnish Climate ConditionsAnne Mäkiranta0Erkki Hiltunen1School of Technology and Innovations, University of Vaasa, 65101 Vaasa, FinlandSchool of Technology and Innovations, University of Vaasa, 65101 Vaasa, FinlandGeothermal energy is a form of renewable energy, which offers carbon-free solutions for heating and cooling spaces. This study evaluates the use of renewable asphalt heat energy in frozen ground conditions. Asphalt heat energy can be harnessed using a low-energy network, heat collection pipes and heat pumps. This study measured temperatures under the asphalt layer during a three-year period between 2014 and 2017. Measurements were made using a distributed temperature sensing method based on light scattering. Temperatures taken at four different depths under the asphalt (0.5 m, 1.0 m, 3.0 m and 10 m) are presented here. These temperatures are compared with that detected at the depth at which the temperature remains constant all year round. The temperature difference curve between 0.5 m depth and the constant soil temperature depth indicates that from April to October the soil at 0.5 m depth is warming and the temperature difference is positive, even as much as 18 °C. Instead, at the 3.0 m depth, the difference curve is smoother and it varies only from −5 to +5 °C. It is positive from June to November. The surface layer (0 m−1.0 m) is suitable for harvesting heat that can be stored in a deeper (1.5 m−3.0 m) purpose-built storage or in a bedrock heat battery. The calculated heat capacities indicate that asphalt energy, because of high temperatures, is a noteworthy renewable energy source.https://www.mdpi.com/1996-1073/12/11/2101urban energygeoenergylow-energy networkdistributed temperature sensing (DTS) measurement
collection DOAJ
language English
format Article
sources DOAJ
author Anne Mäkiranta
Erkki Hiltunen
spellingShingle Anne Mäkiranta
Erkki Hiltunen
Utilizing Asphalt Heat Energy in Finnish Climate Conditions
Energies
urban energy
geoenergy
low-energy network
distributed temperature sensing (DTS) measurement
author_facet Anne Mäkiranta
Erkki Hiltunen
author_sort Anne Mäkiranta
title Utilizing Asphalt Heat Energy in Finnish Climate Conditions
title_short Utilizing Asphalt Heat Energy in Finnish Climate Conditions
title_full Utilizing Asphalt Heat Energy in Finnish Climate Conditions
title_fullStr Utilizing Asphalt Heat Energy in Finnish Climate Conditions
title_full_unstemmed Utilizing Asphalt Heat Energy in Finnish Climate Conditions
title_sort utilizing asphalt heat energy in finnish climate conditions
publisher MDPI AG
series Energies
issn 1996-1073
publishDate 2019-06-01
description Geothermal energy is a form of renewable energy, which offers carbon-free solutions for heating and cooling spaces. This study evaluates the use of renewable asphalt heat energy in frozen ground conditions. Asphalt heat energy can be harnessed using a low-energy network, heat collection pipes and heat pumps. This study measured temperatures under the asphalt layer during a three-year period between 2014 and 2017. Measurements were made using a distributed temperature sensing method based on light scattering. Temperatures taken at four different depths under the asphalt (0.5 m, 1.0 m, 3.0 m and 10 m) are presented here. These temperatures are compared with that detected at the depth at which the temperature remains constant all year round. The temperature difference curve between 0.5 m depth and the constant soil temperature depth indicates that from April to October the soil at 0.5 m depth is warming and the temperature difference is positive, even as much as 18 °C. Instead, at the 3.0 m depth, the difference curve is smoother and it varies only from −5 to +5 °C. It is positive from June to November. The surface layer (0 m−1.0 m) is suitable for harvesting heat that can be stored in a deeper (1.5 m−3.0 m) purpose-built storage or in a bedrock heat battery. The calculated heat capacities indicate that asphalt energy, because of high temperatures, is a noteworthy renewable energy source.
topic urban energy
geoenergy
low-energy network
distributed temperature sensing (DTS) measurement
url https://www.mdpi.com/1996-1073/12/11/2101
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AT erkkihiltunen utilizingasphaltheatenergyinfinnishclimateconditions
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