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Geothermal heat : the great forgotten renewable energy

PHILIPPE_Mikael
Mikael Philippe
Head of the Geothermal and Energy Storage Unit, BRGM
VERGNE_Jérôme
Jérôme Vergne
physicist at the École et Observatoire des Sciences de la Terre in Strasbourg
Key takeaways
  • Geothermal energy uses the heat in the subsoil: it is captured and used in the form of electricity or heat.
  • It is particularly interesting for urban areas and will be an asset in the face of climate change.
  • However, a very small proportion of heat consumption is supplied by geothermal energy in France: in 2021, it will amount to 1% of final consumption.
  • This is because it is little known to the public and local authorities, and there are relatively few drilling companies in France.
  • Thanks to the many projects that are being set up, Europe should see a 270% increase in geothermal energy consumption between 2019 and 2024.

What if France were to rely part­ly on geo­ther­mal ener­gy to achieve car­bon neu­tra­li­ty ? Last Februa­ry, the govern­ment pre­sen­ted an action plan to acce­le­rate its deploy­ment. The objec­tive : “to pro­duce enough heat in 15 to 20 years to save 100 TWh/year of gas, i.e. more than Rus­sian gas imports before 2022.” The mul­ti-annual ener­gy pro­gramme aims to increase geo­ther­mal heat pro­duc­tion faci­li­ties by a fac­tor of 2 or more bet­ween 2016 and 2028.

Geo­ther­mal ener­gy relies on the heat in the sub­soil1 : it is cap­tu­red and used in the form of elec­tri­ci­ty or heat. Let’s take a look at heat pro­duc­tion, the govern­ment’s objective.

Geothermal energy to produce heat

At a depth of more than 200 metres, low-ener­gy deep geo­ther­mal ener­gy – such as the Dog­ger aqui­fer in the Île-de-France region – consists of pum­ping and then rein­jec­ting water from aqui­fers, under­ground reser­voirs. It is hea­ted by the natu­ral decay of radio­ac­tive ele­ments in the sub­soil. High-ener­gy deep geo­ther­mal ener­gy, as in Soultz-sous-Forêts in Alsace, exploits the water natu­ral­ly contai­ned in frac­tu­red rocks. These sites are loca­ted in active vol­ca­nic zones or in col­lapse trenches (par­ti­cu­lar geo­lo­gi­cal structures).

At a depth of less than 200 metres, sur­face geo­ther­mal ener­gy exploits the iner­tia of the ground, which is almost unaf­fec­ted by varia­tions in atmos­phe­ric tem­pe­ra­ture : it remains constant at around 10–15°C in main­land France. The use of a geo­ther­mal heat pump (PACg) is neces­sa­ry : it exploits the tem­pe­ra­ture dif­fe­rence bet­ween the sur­face and the sub­soil. Heat is reco­ve­red by pum­ping (and then re-injec­ting) ground­wa­ter or by cir­cu­la­ting a heat trans­fer fluid through a pipe in the hot ground.

Geothermal energy in France

In France, the heat pro­du­ced by deep geo­ther­mal ener­gy is main­ly used to sup­ply urban hea­ting net­works (cur­rent­ly 59) and is used in indus­trial pro­cesses (2 TWh in total) or to heat green­houses. “With an ambi­tious deploy­ment plan, it would be pos­sible to pro­duce around ten TWh of addi­tio­nal heat within 20 years,” adds Mikaël Phi­lippe, head of BRGM’s Geo­ther­mal and Ener­gy Sto­rage unit. It is par­ti­cu­lar­ly inter­es­ting for sup­plying large conur­ba­tions : it requires the ins­tal­la­tion of a hea­ting net­work and a power sta­tion near­by, with a sur­face area of around 2 000 m2. “There are many untap­ped aqui­fers with very inter­es­ting resources,” says Mikaël Phi­lippe. “We are star­ting new explo­ra­tion and research pro­grammes to bet­ter assess their poten­tial.” These basins are loca­ted to the west of Paris, in south-eas­tern France and in the Aqui­taine basin. The limit ? “Exploi­ta­tion of the resource is only pos­sible if it is appro­priate to the need : the aqui­fer must be loca­ted near a high­ly popu­la­ted area,” replies Mikaël Philippe.

Ano­ther poten­tial to be deve­lo­ped is sur­face geo­ther­mal ener­gy. It accounts for most of the geo­ther­mal heat pro­du­ced in France today (4.8 TWh). “We esti­mate the poten­tial to be rea­ched within 20 years at 100 TWh, which is 10 times more than with deep geo­ther­mal ener­gy,” says Mikaël Phi­lippe. The major advan­tage ? It is avai­lable over almost the entire French ter­ri­to­ry, unlike deep geo­ther­mal ener­gy. “Sur­face geo­ther­mal ener­gy is par­ti­cu­lar­ly inter­es­ting in areas with scat­te­red, mode­ra­te­ly dense hou­sing,” adds Mikaël Phi­lippe. “Its rever­si­bi­li­ty to pro­duce cold, thanks to PACg, is a real asset in the context of cli­mate change.”

What are the limits of geothermal energy ?

Howe­ver, a very small pro­por­tion of heat consump­tion is sup­plied by geo­ther­mal ener­gy in France : in 2021, it will amount to 1% of final consump­tion2. Why ? “It is lit­tle known by the gene­ral public, and local autho­ri­ties,” des­cribes Mikaël Phi­lippe. “There are also very few drilling com­pa­nies in the coun­try. With the help of seve­ral orga­ni­sa­tions, we are wor­king to remove these obs­tacles.” The invest­ment costs are also high, even if the State sup­ports its deploy­ment through various schemes (Fonds Cha­leur, MaPri­me­Re­nov’, Coup de pouce chauf­fage). For a single-fami­ly home, Ademe esti­mates3 that the cost (exclu­ding sub­si­dies) of a PACg is €2,731 per year (inclu­ding ins­tal­la­tion), com­pa­red with €2,236 for a gas boi­ler or €4,429 for elec­tric hea­ting. Howe­ver, the cal­cu­la­tion is dif­ferent if the increase in the price of elec­tri­ci­ty, gas and wood is taken into account : geo­ther­mal ener­gy becomes the solu­tion with the lowest ope­ra­ting cost. For col­lec­tive and ter­tia­ry buil­dings, sur­face geo­ther­mal ener­gy is cur­rent­ly the most expen­sive solution.

In 2021, geo­ther­mal ener­gy accoun­ted for 1% of final heat consumption.

What about inter­na­tio­nal­ly ? Eve­ryone has in mind the images of power sta­tions sur­roun­ded by steam in Ice­land. By fee­ding a tur­bine, geo­ther­mal heat (above 110°C) is used here to pro­duce heat and elec­tri­ci­ty in coge­ne­ra­tion. In 2013, 29% of Ice­land’s elec­tri­ci­ty was pro­du­ced using this tech­nique and 45% of buil­dings were hea­ted4. But Ice­land is a model : world­wide in 2022, only 0.37% of the heat consu­med is of geo­ther­mal ori­gin5. French heat pro­duc­tion amounts to 6.7 TWh, com­pa­red to 82.1 TWh on a Euro­pean scale6 and 26,000 TWh on a glo­bal scale7. For elec­tri­ci­ty, the Uni­ted States has the lar­gest pro­duc­tion capa­ci­ty (2.5 TWh), fol­lo­wed by Indo­ne­sia and the Phi­lip­pines8. In France, elec­tri­ci­ty pro­duc­tion is essen­tial­ly limi­ted to the Bouillante plant in Gua­de­loupe (112 GWh/year) and the Soultz-sous-Forêts plant in Alsace (12 GWh/year).

“In France, we are seeing an acce­le­ra­tion in heat pro­duc­tion pro­jects, par­ti­cu­lar­ly for ter­tia­ry buil­dings and hea­ting net­works,” says Mikaël Phi­lippe. Accor­ding to the Inter­na­tio­nal Ener­gy Agen­cy, Chi­na and Tur­key are res­pon­sible for most of the growth in geo­ther­mal heat pro­duc­tion in recent years. In its pro­jec­tions, the agen­cy esti­mates that Chi­nese growth should conti­nue, but also notes that Europe is one of the most active mar­kets : the conti­nent should record a 270% increase in geo­ther­mal ener­gy consump­tion bet­ween 2019 and 2024.

EARTHQUAKES RELATED TO DEEP GEOTHERMAL ENERGY

Deep geo­ther­mal exploi­ta­tion is often accom­pa­nied by ear­th­quakes. “This is a well-known phe­no­me­non, and ope­ra­tors are obli­ged to moni­tor this seis­mi­ci­ty,” reports Jérôme Vergne, a phy­si­cist at the School and Obser­va­to­ry of Earth Sciences in Stras­bourg. The ear­th­quakes mea­su­red are very often below magni­tude 1.5 and are not felt by the popu­la­tion. “In some spe­ci­fic cases, a few ear­th­quakes of a higher magni­tude occur : for example, bet­ween 2019 and 2021, three ear­th­quakes of magni­tude 3 to 3.9 were recor­ded during the pre­pa­ra­tion phase of the Ven­den­heim very deep site, in the north of the Stras­bourg Euro­me­tro­po­lis,” says Jérôme Vergne.

Most of the seis­mic acti­vi­ty is gene­ra­ted during the hydrau­lic sti­mu­la­tion phases : a mix­ture of water and addi­tives is injec­ted under pres­sure to improve the cir­cu­la­tion of geo­ther­mal fluids in the reser­voirs. “These reser­voirs are natu­ral­ly per­meable due to pre-exis­ting cracks and faults, natu­ral frac­tures along which ear­th­quakes can occur,” explains Jérôme Vergne. Injec­ting water modi­fies the pres­sures on these frac­tures and can gene­rate seis­mic rup­tures. These are cal­led indu­ced ear­th­quakes. Some­times lar­ger ear­th­quakes are recor­ded, such as the Pohang ear­th­quake (South Korea) in 2017 with a magni­tude of 5.4 (the lar­gest asso­cia­ted with a geo­ther­mal pro­ject). “In this case, geo­ther­mal ener­gy did not induce an unpre­ce­den­ted ear­th­quake, but rather a trig­ge­red ear­th­quake,” com­ments Jérôme Vergne. Geo­ther­mal exploi­ta­tion acce­le­ra­ted the occur­rence of an ear­th­quake that would have taken place natu­ral­ly later, it was the last straw.  A pre­ven­tion sys­tem – cal­led “traf­fic lights” – is put in place for each high-ener­gy deep geo­ther­mal pro­ject. In Ill­kirch-Graf­fens­ta­den and Ven­den­heim, it pro­vides for the switch to rein­for­ced vigi­lance as soon as an ear­th­quake of magni­tude 1.5 is recor­ded, and a gra­dual stop for any ear­th­quake rea­ching magni­tude 2.

Anaïs Marechal 
1Web­site consul­ted on 30/03/2023 : www​.geo​ther​mies​.fr
2Minis­try of Ener­gy Tran­si­tion, 2 Februa­ry 2023, Geo­ther­mal ener­gy : an action plan to acce­le­rate.
3Ademe, Coûts des éner­gies renou­ve­lables et de récu­pé­ra­tion en France, édi­tion 2022.
4Web­site consul­ted on 31/03/2023 : https://​nea​.is/​g​e​o​t​h​e​r​m​a​l​/​t​h​e​-​r​e​s​o​urce/
5IEA (2019d), World Ener­gy Sta­tis­tics and Balances 2018 (data­base), www​.iea​.org/​s​t​a​t​i​s​tics/; IEA (for­th­co­ming), World Ener­gy Out­look 2019.
6Web­site acces­sed on 30/03/2023 : www​.geo​ther​mies​.fr
7IEA (2019), Rene­wables 2019, IEA, Paris https://​www​.iea​.org/​r​e​p​o​r​t​s​/​r​e​n​e​w​a​b​l​e​s​-2019, License : CC BY 4.0
8Web­site acces­sed on 30/03/2023 : www​.geo​ther​mies​.fr

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