Inquiry into the Temperature Changes of Rock Massif Used in Energy Production in Relation to Season

This research was undertaken to perform and evaluate the temperature measurement in the ground utilized as an energy source with the goal to determine whether significant temperature variations occur in the subsurface during the heating season. The research infrastructure situated on our University...

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Autores principales: Martin Klempa, Jan Latal, Barbora Grafova, Michal Matloch Porzer, Mojmir Vrtek, Antonin Kunz, Petr Siska
Formato: article
Lenguaje:EN
Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/443fa1ec5979417aa5494853e077d494
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spelling oai:doaj.org-article:443fa1ec5979417aa5494853e077d4942021-11-11T19:03:40ZInquiry into the Temperature Changes of Rock Massif Used in Energy Production in Relation to Season10.3390/s212170271424-8220https://doaj.org/article/443fa1ec5979417aa5494853e077d4942021-10-01T00:00:00Zhttps://www.mdpi.com/1424-8220/21/21/7027https://doaj.org/toc/1424-8220This research was undertaken to perform and evaluate the temperature measurement in the ground utilized as an energy source with the goal to determine whether significant temperature variations occur in the subsurface during the heating season. The research infrastructure situated on our University campus was used to assess any variations. The observations were made at the so called “Small Research Polygon” that consists of 8 monitoring boreholes (Borehole Heat Exchangers) situated around a borehole used as an energy source. During the heating season, a series of monthly measurements are made in the monitoring boreholes using a distributed temperature system (DTS). Raman back-scattered light is analysed using Optical Frequency Time Domain Reflectometry (OTDR). Our results indicate that no noticeable changes in temperature occur during the heating season. We have observed an influence of long-term variations of the atmospheric conditions up to the depth of a conventional BHE (≈100 m). The resulting uncertainty in related design input parameters (ground thermal conductivity) was evaluated by using a heat production simulation. Production data during one heating season at our research facilities were evaluated against the design of the system. It is possible to construct smaller geothermal installations with appropriate BHE design that will have a minimal impact on the temperature of the surrounding rock mass and the system performance.Martin KlempaJan LatalBarbora GrafovaMichal Matloch PorzerMojmir VrtekAntonin KunzPetr SiskaMDPI AGarticleborehole heat exchangerground temperature fieldground thermal conductivityground source heat pumpRaman-OTDR (DTS)temperature measurementChemical technologyTP1-1185ENSensors, Vol 21, Iss 7027, p 7027 (2021)
institution DOAJ
collection DOAJ
language EN
topic borehole heat exchanger
ground temperature field
ground thermal conductivity
ground source heat pump
Raman-OTDR (DTS)
temperature measurement
Chemical technology
TP1-1185
spellingShingle borehole heat exchanger
ground temperature field
ground thermal conductivity
ground source heat pump
Raman-OTDR (DTS)
temperature measurement
Chemical technology
TP1-1185
Martin Klempa
Jan Latal
Barbora Grafova
Michal Matloch Porzer
Mojmir Vrtek
Antonin Kunz
Petr Siska
Inquiry into the Temperature Changes of Rock Massif Used in Energy Production in Relation to Season
description This research was undertaken to perform and evaluate the temperature measurement in the ground utilized as an energy source with the goal to determine whether significant temperature variations occur in the subsurface during the heating season. The research infrastructure situated on our University campus was used to assess any variations. The observations were made at the so called “Small Research Polygon” that consists of 8 monitoring boreholes (Borehole Heat Exchangers) situated around a borehole used as an energy source. During the heating season, a series of monthly measurements are made in the monitoring boreholes using a distributed temperature system (DTS). Raman back-scattered light is analysed using Optical Frequency Time Domain Reflectometry (OTDR). Our results indicate that no noticeable changes in temperature occur during the heating season. We have observed an influence of long-term variations of the atmospheric conditions up to the depth of a conventional BHE (≈100 m). The resulting uncertainty in related design input parameters (ground thermal conductivity) was evaluated by using a heat production simulation. Production data during one heating season at our research facilities were evaluated against the design of the system. It is possible to construct smaller geothermal installations with appropriate BHE design that will have a minimal impact on the temperature of the surrounding rock mass and the system performance.
format article
author Martin Klempa
Jan Latal
Barbora Grafova
Michal Matloch Porzer
Mojmir Vrtek
Antonin Kunz
Petr Siska
author_facet Martin Klempa
Jan Latal
Barbora Grafova
Michal Matloch Porzer
Mojmir Vrtek
Antonin Kunz
Petr Siska
author_sort Martin Klempa
title Inquiry into the Temperature Changes of Rock Massif Used in Energy Production in Relation to Season
title_short Inquiry into the Temperature Changes of Rock Massif Used in Energy Production in Relation to Season
title_full Inquiry into the Temperature Changes of Rock Massif Used in Energy Production in Relation to Season
title_fullStr Inquiry into the Temperature Changes of Rock Massif Used in Energy Production in Relation to Season
title_full_unstemmed Inquiry into the Temperature Changes of Rock Massif Used in Energy Production in Relation to Season
title_sort inquiry into the temperature changes of rock massif used in energy production in relation to season
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/443fa1ec5979417aa5494853e077d494
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