Innovations in Ground-Source Heat Pumps

Ground source heat pumps

Problem

Ground-coupled heat pumps reduce cooling load in summer and heating load in winter by using the relatively constant temperature of the earth as the heat exchange medium instead of the outside air. By exchanging heat with the mild ground temperatures, ground-coupled heat pumps are more efficient than air-source designs and use less power during peak electricity demand. The biggest barrier to more widespread adoption of this technology is the cost.

Solution

This project, funded by the California Energy Commission, aims to increase adoption of ground-source heat pumps in California by identifying optimal designs for low-cost, shallow bore helical ground heat exchangers (GHEs) and providing the engineering information and installation guidance that is needed.

Goal and Results

2019

This past year, WCEC researchers and collaborators developed and calibrated a computational model for the shallow bore helical GHE. The model uses electrical analogies of capacitance and resistance (CaRM) to describe the heat transfer in the ground source heat pump system.

Researchers validated the model by comparing results with those reported in the literature and from field data. In addition, the researchers developed a computational fluid dynamics (CFD) model to simulate heat transfer phenomena that the simplified CaRM model neglects and to also obtain more detailed results.

2018

This past year, WCEC researchers and collaborators developed and calibrated a computational model for the shallow bore helical GHE. The model uses electrical analogies of capacitance and resistance (CaRM) to describe the heat transfer in the ground.

Researchers validated the model by comparing results with those reported in the literature and from field data, with excellent agreement as shown in the figure above. In addition, researchers developed a computational fluid dynamics (CFD) model to test other design variables that the CaRM model was unable to simulate. In both models, the temperature of water returning from the ground was predicted with an accuracy of 0.1°C .

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