期刊
SCIENCE OF THE TOTAL ENVIRONMENT
卷 778, 期 -, 页码 -出版社
ELSEVIER
DOI: 10.1016/j.scitotenv.2021.146235
关键词
Ground source heat pumps; Contaminant transport in porous medium; Groundwater bioremediation; Biodegradation kinetics; FEFLOW simulation
资金
- Natural Sciences and Engineering Research Council of Canada (NSERC) [RGPIN 2015-06041]
Geothermal or ground source heat pumps are a rapidly growing renewable energy technology used for heating and cooling buildings. Research shows that changes in underground temperature can significantly enhance biodegradation of contaminants, offering the potential to utilize geothermal heating as a remediation strategy.
Geothermal or ground source heat pumps (GSHPs) are among the highest growing renewable energy technologies used for heating and cooling of buildings. However, despite being a well-established technology, their geoenvironmental effects such as impact of the heat on the biosphere is still not thoroughly understood. This study uses FEFLOW software, to simulate heat and mass transport of a vertical closed-loop GSHP system. Transient flow and heat transport results for a multiple borehole system are presented which indicate long-term effects on subsurface temperature. Moreover, the impact of temperature change in a contaminated granular porous subsurface during remediation applications is examined. In particular, as subsurface temperatures are elevated due to geothermal heating, sorption will decrease and biodegradation rates will increase. These effects are examined in the context of contaminant transport, to evaluate the possibility of utilizing geothermal heating as a remediation strategy. The results revealed that temperature changes caused by GSHP operation can significantly enhance biodegradation of hydrocarbon contaminants. For instance, elevated subsurface temperature resulted in 97% reduction in benzene total mass, after one year of GSHP operation for a typical office building in Toronto. (c) 2021 The Author(s). Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
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