Progress of Geothermal Development in Algeria

Hakim Saibi, Sachio Ehara, Yasuhiro Fujimitsu, Jun Nishijima

Research output: Contribution to journalArticle

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Abstract

There are more than 240 thermal springs in Algeria. The geothermal energy in Algeria is generally of a low enthalpy type. The total heat discharge from the main springs and existing wells is approximately 642 MWt. Three geothermal zones have been delineated according to some geological and thermal considerations: 1) The Tlemcenian dolomites in the northwestern part of Algeria, 2) carbonate formations in the northeastern part of Algeria and 3) the sandstone Albian reservoir in the Sahara (south of Algeria). The northeastern part of Algeria is geothermally very interesting. Application of gas geothermometery to northeastern Algerian gases suggests that the reservoir temperature is around 198˚C. Two conceptual geothermal models are presented, concerning the northern and southern part of Algeria. The principal utilizations of the hot water are balneology and space and greenhouse heating. Eight hot springs are used as public thermal resorts for medical purposes.

Original languageEnglish
Pages (from-to)383-397
Number of pages15
JournalJournal of the Geothermal Research Society of Japan
Volume28
Issue number4
DOIs
Publication statusPublished - 2006

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Algeria
thermal spring
geothermal energy
enthalpy
gas
dolomite
sandstone
heating
well
carbonate
temperature
greenhouses
sandstones
gases
carbonates
heat
hot water
public

All Science Journal Classification (ASJC) codes

  • Geophysics

Cite this

Progress of Geothermal Development in Algeria. / Saibi, Hakim; Ehara, Sachio; Fujimitsu, Yasuhiro; Nishijima, Jun.

In: Journal of the Geothermal Research Society of Japan, Vol. 28, No. 4, 2006, p. 383-397.

Research output: Contribution to journalArticle

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