## In a glance

This module calculates the potential of shallow geothermal energy to be used in ground source heat pumps for selected regions in the form of a raster file. The inputs are raster files with initial ground temperatures, depth-averaged ground thermal conductivity and depth-averaged ground thermal capacity.

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## Introduction

It aims to compute the shallow geothermal potential based on r.green.gshp.theoretical according to the G.pot methodology. In this module the output is the theoretical maximum energy that can be converted in the ideal case without considering the financial and spatial constraints.

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## Inputs and outputs

The input parameters and layers as well as output layers and parameters are as follows.

Input layers and parameters are:

• Vector with depth-averaged ground thermal conductivity [W m-1 K-1]
• Value with the Heating Season [0-365] days
• Raster with the initial ground temperature T0 [°C]
• Value with depth-averaged ground thermal capacity [MJ m-3 K-1]
• Value with depth-averaged ground thermal capacity [MJ m-3 K-1]

• Borehole thermal resistance [m K W-1]
• Borehole length [m]
• Number of pipes in the borehole
• Thermal conductivity of the borehole filling (geothermal grout) [W m-1 K-1]
• Minimum or maximum fluid temperature [°C]
• Simulated lifetime of the plant [years]

Output layers and parameters are:

• a raster map with the geothermal power potential [W]
• a raster map with the geothermal energy potential [MWh]

A deeper explanation of the default input raster is available in the Hotmaps repository

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## Method

The method to define the energy potential is based on the G.pot. The potential of shallow geothermal energy is computed by means of and empirical relationship proposed by Casasso et al. (2016).

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## Test Run 1

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### Test Run 1: default input values

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### Test Run 2: modified input values

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## Authors and reviewers

Institute of Renewable Energy Drususallee/Viale Druso 1 I-39100 Bozen/Bolzano Italy

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