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GROMIT project: GROund coupled heat pumps MITigation potential Anne Verhoef on behalf of the GROMIT team Department of Soil Science, University of Reading 1 GSHPA meeting, 21 January 2010, Milton Keynes NERC research grant
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GROMIT team 2 GSHPA meeting, 21 January 2010, Milton Keynes UoR/NCAS-Climate (land surface modelling & fieldwork): Raquel Garcia-Gonzalez, Bruce Main, Pier Luigi Vidale, Anne Verhoef Nottingham University (modelling of GCHPs): Yupeng Wu & Guohui Gan BGS (Groundwater modelling): Majdi Mansour & Andrew Hughes CEH-Wallingford (UK 1 km driving data): Eleanor Blyth & Jon Finch EarthEnergy Ltd (GCHP expertise): Robin Curtis Aim: To investigate and optimise the CO 2 mitigation potential of horizontal GCHPs under current and future UK environmental conditions
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Infiltration Rates / Evaporation Energy balance/ground water level; vary in time and space) Water (vapour) flux, induced by heat extraction/rejection Thermal regime Thermal soil properties Soil water freezing/melting 3 GSHPA meeting, 21 January 2010, Milton Keynes GCHPs and environmental factors Primary source of energy, R n Top Boundary condition R n –(H+LE) = G Net Thermal Recharge Ground water Flow ~1.5 m Heat pump Horizontal GCHP Heat extraction / Cooling Lower Boundary condition F h =0 (T=constant) Diagram: Heat and water exchange processes near GCHP G, soil heat flux H, sensible heat flux E, evaporation Key variables: soil moisture content and soil temperature Largely affected by climate, soil texture & vegetation Courtesy of Raquel Garcia, Reading University
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Type of horizontal GCHP Spacing of loops Installation depth Back-filling material Fluid in HE Pumps 4 GSHPA meeting, 21 January 2010, Milton Keynes GCHP-related technical & design factors Pump Compressor Evaporator Condenser Ground loop Load T1T1 T2T2 T2T2 T1T1 m m W T soil (W) Will affect COP, together with soil environment ! Courtesy of: Yupeng Wu, Nottingham University
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5 GSHPA meeting, 21 January 2010, Milton Keynes Project approach Model development (combined Land surface- Groundwater-GCHP model Experimental campaigns (UK field sites) Model simulation –Driving variables (UK 1 km grid) –Verification –Sensitivity - Varying model parameters –Climate change impact – COP under future environmental conditions –Climate change scenarios (UKCIP) Dissemination
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Land surface model 6 GSHPA meeting, 21 January 2010, Milton Keynes
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GCHP modelling 7 GSHPA meeting, 21 January 2010, Milton Keynes Plan view of isotherms generated from prediction for a slinkey heat exchanger, at 1, 10, 50 and 140 hours Courtesy of: Yupeng Wu, Nottingham University
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UK driving variables 8 GSHPA meeting, 21 January 2010, Milton Keynes Rainfall Rate (kg m -2 d -1 ), 1 January 2003 Air Temperature (K) 1 January 2003 Courtesy of: Tongfei Zhang, CEH-Wallingford
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UK soil textures 9 GSHPA meeting, 21 January 2010, Milton Keynes The National soil map, NATMAP (NSRI) Soil properties such as: Dry bulk density Hydraulic properties Thermal properties Soil texture
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10 Field campaign started 2 th October 2009, near Oxford GCHP Profile over ~ 1m: - 8 Thermistors - 6 Thetaprobes slinky Cooling near the slinky due to heat extraction… how will this affect the water and heat transfer and hence the performance of GCHP…
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GSHPA meeting, 21 January 2010, Milton Keynes 11 GCHP PROFILE REFERENCE PROFILE 4 trenches every 5 m 2 Profiles: -GSHP profile -Reference profile Soil temperature at 2 cm Soil temperature at 5 cm Soil temperature at ~1 m Soil moisture at 17.5 cm Soil moisture at 75 cm Soil moisture at ~1 m Courtesy of Raquel Garcia, Reading University
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Conclusions 12 GSHPA meeting, 21 January 2010, Milton Keynes GROMIT is an excellent opportunity to address many unexplored issues related to horizontal GCHP performance in the UK Any questions/suggestions? Do you have a field-site available??? Thank you for listening!
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UK driving variables 13 GSHPA meeting, 21 January 2010, Milton Keynes Surface temperature, 1 July 2003Surface temperature, 1 January 2003 Courtesy: Tongfei Zhang, CEH-Wallingford
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