Energy performance and thermal impact of a Borehole Heat Exchanger in a sandy aquifer: Influence of the groundwater velocity
• A numerical model of a Borehole Heat Exchanger with groundwater flow is created. • The model is carefully validated against analytical solutions. • The mutual influence of the BHE heat rate and the ground temperature field is shown. • For 10−1 ⩽Pe⩽1 the heat rate increase with respect to null velo...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Angelotti, A. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014 |
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| Schlagwörter: |
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| Umfang: |
9 |
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| Übergeordnetes Werk: |
Enthalten in: Preparation and catalytic properties of the triphenylarsine and triphenylstibine-stabilized tri-heteroleptic NHC - Yang, Jin ELSEVIER, 2019, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:77 ; year:2014 ; pages:700-708 ; extent:9 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.enconman.2013.10.018 |
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ELV012197807 |
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| 520 | |a • A numerical model of a Borehole Heat Exchanger with groundwater flow is created. • The model is carefully validated against analytical solutions. • The mutual influence of the BHE heat rate and the ground temperature field is shown. • For 10−1 ⩽Pe⩽1 the heat rate increase with respect to null velocity is 11–105%. • Large groundwater velocities reduce the benefits of operating in both seasons. | ||
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10.1016/j.enconman.2013.10.018 doi GBVA2014007000025.pica (DE-627)ELV012197807 (ELSEVIER)S0196-8904(13)00653-5 DE-627 ger DE-627 rakwb eng 620 620 DE-600 540 VZ 35.00 bkl Angelotti, A. verfasserin aut Energy performance and thermal impact of a Borehole Heat Exchanger in a sandy aquifer: Influence of the groundwater velocity 2014 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • A numerical model of a Borehole Heat Exchanger with groundwater flow is created. • The model is carefully validated against analytical solutions. • The mutual influence of the BHE heat rate and the ground temperature field is shown. • For 10−1 ⩽Pe⩽1 the heat rate increase with respect to null velocity is 11–105%. • Large groundwater velocities reduce the benefits of operating in both seasons. Groundwater flow Elsevier Thermal impact Elsevier Numerical methods Elsevier Ground-Source Heat Pump Elsevier Energy performance Elsevier Borehole Heat Exchanger Elsevier Alberti, L. oth La Licata, I. oth Antelmi, M. oth Enthalten in Elsevier Science Yang, Jin ELSEVIER Preparation and catalytic properties of the triphenylarsine and triphenylstibine-stabilized tri-heteroleptic NHC 2019 Amsterdam [u.a.] (DE-627)ELV001598317 volume:77 year:2014 pages:700-708 extent:9 https://doi.org/10.1016/j.enconman.2013.10.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 35.00 Chemie: Allgemeines VZ AR 77 2014 700-708 9 045F 620 |
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energy performance and thermal impact of a borehole heat exchanger in a sandy aquifer: influence of the groundwater velocity |
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Energy performance and thermal impact of a Borehole Heat Exchanger in a sandy aquifer: Influence of the groundwater velocity |
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• A numerical model of a Borehole Heat Exchanger with groundwater flow is created. • The model is carefully validated against analytical solutions. • The mutual influence of the BHE heat rate and the ground temperature field is shown. • For 10−1 ⩽Pe⩽1 the heat rate increase with respect to null velocity is 11–105%. • Large groundwater velocities reduce the benefits of operating in both seasons. |
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• A numerical model of a Borehole Heat Exchanger with groundwater flow is created. • The model is carefully validated against analytical solutions. • The mutual influence of the BHE heat rate and the ground temperature field is shown. • For 10−1 ⩽Pe⩽1 the heat rate increase with respect to null velocity is 11–105%. • Large groundwater velocities reduce the benefits of operating in both seasons. |
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• A numerical model of a Borehole Heat Exchanger with groundwater flow is created. • The model is carefully validated against analytical solutions. • The mutual influence of the BHE heat rate and the ground temperature field is shown. • For 10−1 ⩽Pe⩽1 the heat rate increase with respect to null velocity is 11–105%. • Large groundwater velocities reduce the benefits of operating in both seasons. |
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