2016
DOI: 10.1016/j.ijheatmasstransfer.2016.03.057
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Investigation on groundwater velocity based on the finite line heat source seepage model

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Cited by 12 publications
(3 citation statements)
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“…For example, it can be observed in Figure 4a that for high values of Pe , optimal designs have a lower total cost. For example, at 12)- (16). As a result, optimal fraction of the load assumed by the GCHP system increases with Pe in Figure 4d.…”
Section: Figure 4 Effect Of Péclet Number and Ground Thermal Conductivity On: (A) Minimal Total Cost (B) Optimal Boreholes Depth (C) Optimentioning
confidence: 90%
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“…For example, it can be observed in Figure 4a that for high values of Pe , optimal designs have a lower total cost. For example, at 12)- (16). As a result, optimal fraction of the load assumed by the GCHP system increases with Pe in Figure 4d.…”
Section: Figure 4 Effect Of Péclet Number and Ground Thermal Conductivity On: (A) Minimal Total Cost (B) Optimal Boreholes Depth (C) Optimentioning
confidence: 90%
“…Groundwater flow can significantly affect heat transfer around boreholes [7]- [11]. Many analytical models have been developed to quantify its effects [12]- [16]. Previous studies have also developed relatively fast heat transfer computational methodologies with groundwater flow, such as calculating a thermal ground resistance [17] or a thermal conductivity [18], using fast Fourier transform combined with cubic spline [19], or correlations for G-functions based on analytical models for groundwater flow [20].…”
Section: Introductionmentioning
confidence: 99%
“…Accounting for the effects of groundwater flow has also resulted in several improvements to the analyses of geothermal thermal-response tests and the data deduced from them, as demonstrated, for example, by the works of Gehlin and Hellström (2003), Lee and Lam (2012), Therrien et al (2010), Raymond et al (2011), Wagner et al (2013), , , and Zhang et al (2016). It should also be noted that the heterogeneity of the soil hydraulic conductivity and the mixing of flowing groundwater at the pore scale, could create disparities between the longitudinal (parallel to the direction of groundwater flow) and the transverse (perpendicular to the direction of groundwater flow) dispersion of heat, as discussed, for example, in the works of Hsu and Cheng (1990), Metzger et al (2004), Hidalgo et al (2009), Hecht-Méndez et al (2010), Diersch et al (2011a;, Molina-Giraldo et al (2011a), Chiasson and O'Connell (2011), and Nield and Bejan (2013).…”
Section: Introductionmentioning
confidence: 99%