Effect of groundwater flow in vertical and horizontal fractures on borehole heat exchanger temperatures

Verfasser / Beitragende:
[S. Dehkordi, Bo Olofsson, Robert Schincariol]
Ort, Verlag, Jahr:
2015
Enthalten in:
Bulletin of Engineering Geology and the Environment, 74/2(2015-05-01), 479-491
Format:
Artikel (online)
ID: 605454795
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024 7 0 |a 10.1007/s10064-014-0626-4  |2 doi 
035 |a (NATIONALLICENCE)springer-10.1007/s10064-014-0626-4 
245 0 0 |a Effect of groundwater flow in vertical and horizontal fractures on borehole heat exchanger temperatures  |h [Elektronische Daten]  |c [S. Dehkordi, Bo Olofsson, Robert Schincariol] 
520 3 |a Vertical closed loop systems, also known as borehole heat exchangers (BHEs), are a popular way of extracting the ground source heat energy. Primary factors affecting the performance of BHEs are the thermal and hydrogeological properties of the subsurface. Groundwater flow is known to potentially influence heat transport and system performance. The effect of groundwater movement is more commonly studied under homogeneous conditions. However, in heterogeneous fractured rocks, BHEs are more common than horizontal or open loops due to lack of sufficient soil layers and productive aquifers. The finite-element modelling shows that fractures can play an important role in BHE functioning. Especially, vertical open fractures (≥1mm) near the borehole (≤10m) can have a considerable impact. Although increase in fracture aperture continuously affects the subsurface and BHE temperatures, the increase in its effect progressively lessens. Depending on the distance and aperture, one major fracture influencing the BHE operation performance can be identified; yet a larger number of fractures may govern heat transport (thermal plume outline) and thermal recovery. Individually, horizontal fractures may have less influence than vertical fractures. However, as the density of horizontal fractures increases, their impact can be major, exceeding that of fracture aperture. In particular, we propose that measurements of rock thermal properties be combined with fracture mapping, to better analyse the thermal response testing results and integrate the configuration of fractures in design and layout of the BHE(s). This is particularly valid for (vertical) fractures not intersecting with the borehole. 
540 |a Springer-Verlag Berlin Heidelberg, 2014 
690 7 |a Crystalline rock  |2 nationallicence 
690 7 |a FEFLOW  |2 nationallicence 
690 7 |a Fractured rock  |2 nationallicence 
690 7 |a Groundwater flow  |2 nationallicence 
690 7 |a Heat transport  |2 nationallicence 
690 7 |a Thermal response test  |2 nationallicence 
700 1 |a Dehkordi  |D S.  |u Department of Earth Sciences, University of Western Ontario, N6A 5B7, London, ON, Canada  |4 aut 
700 1 |a Olofsson  |D Bo  |u Department of Land and Water Resources Engineering, Royal Institute of Technology (KTH), 100 44, Stockholm, Sweden  |4 aut 
700 1 |a Schincariol  |D Robert  |u Department of Earth Sciences, University of Western Ontario, N6A 5B7, London, ON, Canada  |4 aut 
773 0 |t Bulletin of Engineering Geology and the Environment  |d Springer Berlin Heidelberg  |g 74/2(2015-05-01), 479-491  |x 1435-9529  |q 74:2<479  |1 2015  |2 74  |o 10064 
856 4 0 |u https://doi.org/10.1007/s10064-014-0626-4  |q text/html  |z Onlinezugriff via DOI 
898 |a BK010053  |b XK010053  |c XK010000 
900 7 |a Metadata rights reserved  |b Springer special CC-BY-NC licence  |2 nationallicence 
908 |D 1  |a research-article  |2 jats 
949 |B NATIONALLICENCE  |F NATIONALLICENCE  |b NL-springer 
950 |B NATIONALLICENCE  |P 856  |E 40  |u https://doi.org/10.1007/s10064-014-0626-4  |q text/html  |z Onlinezugriff via DOI 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Dehkordi  |D S.  |u Department of Earth Sciences, University of Western Ontario, N6A 5B7, London, ON, Canada  |4 aut 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Olofsson  |D Bo  |u Department of Land and Water Resources Engineering, Royal Institute of Technology (KTH), 100 44, Stockholm, Sweden  |4 aut 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Schincariol  |D Robert  |u Department of Earth Sciences, University of Western Ontario, N6A 5B7, London, ON, Canada  |4 aut 
950 |B NATIONALLICENCE  |P 773  |E 0-  |t Bulletin of Engineering Geology and the Environment  |d Springer Berlin Heidelberg  |g 74/2(2015-05-01), 479-491  |x 1435-9529  |q 74:2<479  |1 2015  |2 74  |o 10064