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Brine in Geothermal Energy Systems

A special issue of Energies (ISSN 1996-1073). This special issue belongs to the section "H: Geo-Energy".

Deadline for manuscript submissions: closed (28 February 2022) | Viewed by 6127

Special Issue Editor


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Guest Editor
Department of Chemistry and Bioscience, Section of Chemical Engineering, Aalborg University, 6700 Esbjerg, Denmark
Interests: water; brine; geochemistry; hydrates; hydrothermal liquefaction

Special Issue Information

Dear Colleagues,

Since the beginning of the 20th century, geothermal energy has been used to apply heat to produce electrical power and district heating. The rapid growth of the world’s energy use together with concerns about climate change have put a new focus on possibilities for geothermal energy as a renewable energy source.

However, scaling problems have limited the growth of new geothermal plants. Typically, high-saline water from heat reservoirs from about 1500 m or more below ground is pumped to the geothermal plant. Through a heat exchanger, district heating systems benefit from the heat and are often scaled up with the help of heat pumps. An electricity power unit can use high-temperature brine. If the salinity in the brine is high, a SaltPower unit can improve the sustainability of the installation.

The scaling problems principally arise in reinjection wells. Often, they are a result of the oxidation of Fe(II) from the brine. Another possibility is a decrease in permeability due to the interaction between the reinjected brine and the reservoir, resulting in the loosening of small clay-containing cements that decrease the amounts of connected porosities in the sandstone reservoir. In other cases, lead can precipitate in the reinjection well. In addition, silicates often cause scaling problems.

These problems seem to increase if the geothermal plant stops operating during summer time. Starting it up again often results in a decrease in permeability. An injection of chemicals can often help the situation. This Special Issue of the international journal Energies (Energies is an SSCI and SCIE journal with a 2019 IF = 2.702) aims to cover all aspects of “Brines in Geothermal Energy Systems”. Potential topics include, but are not limited to:

  • the origin of brine in a reservoir;
  • interactions between brine and the solid formation;
  • porosity and permeability changes;
  • aspects of the flow of brine in a reservoir and the interaction of reinjected brine with original brine in the reservoir;
  • pumping issues;
  • precipitation of brine compounds in the geothermal plant or its production and reinjection wells; and
  • chemicals for the treatment of scaling and scale inhibitors.

Papers selected for this Special Issue will be subject to a rigorous peer-review procedure with the aim of the rapid and wide dissemination of research results, developments, and applications.

I invite you to submit an original research paper or a review article to this Special Issue. I look forward to receiving your research.

Prof. Dr. Erik Gydesen Søgaard
Guest Editor

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Keywords

  • identification of brine compounds from geothermal reservoirs
  • changes in brine content with temperature
  • scaling of brine compounds as a function of temperature, pressure, or flow
  • brine in interaction with formation brine
  • brine in interaction with a solid heat reservoir
  • solutions to scaling problems
  • chemicals in the geothermal industry
  • SaltPower

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Published Papers (3 papers)

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Research

15 pages, 25677 KiB  
Article
Impact of Reservoir Heterogeneity on Diluted Geothermal Brine Reinjection
by Jacquelin E. Cobos and Erik G. Søgaard
Energies 2022, 15(9), 3321; https://doi.org/10.3390/en15093321 - 2 May 2022
Cited by 1 | Viewed by 1846
Abstract
Many geothermal plants have been shut down due to reinjection problems with the heat-depleted brine. In Denmark, only one out of three plants that extract heat from a geothermal fluid distributed to the district heating system is still working. In general, the large [...] Read more.
Many geothermal plants have been shut down due to reinjection problems with the heat-depleted brine. In Denmark, only one out of three plants that extract heat from a geothermal fluid distributed to the district heating system is still working. In general, the large salinity of heat-depleted geothermal brines can be used to produce electricity with the help of turbines and generators through an osmotic power unit known as a SaltPower plant. Harnessing more energy out of the reinjection of geothermal brines is feasible without compromising the overall reservoir assurance when the iron is kept under control. This study is an attempt to determine the feasibility of the reinjection of a diluted geothermal brine with ethylenediaminetetraacetic acid (EDTA) into homogeneous and heterogeneous sandstone rocks. The results from the coreflooding experiments show an improvement in the rock properties both in porosity and permeability for homogeneous and heterogeneous rocks. EDTA not only avoids the precipitation of Fe(III) oxides inside the porous media but can also be used for scale removal and matrix acidizing in geothermal reservoirs. Full article
(This article belongs to the Special Issue Brine in Geothermal Energy Systems)
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11 pages, 717 KiB  
Article
Microcalorimetric Study of Carbonating Produced Water as a Promising CO2 Storage and Enhanced Oil Recovery Method
by Jacquelin E. Cobos, Yassin Kissami, Issam Abdolkareem Alkutaini and Erik G. Søgaard
Energies 2022, 15(8), 2888; https://doi.org/10.3390/en15082888 - 14 Apr 2022
Cited by 4 | Viewed by 1595
Abstract
Carbonated produced water injection (CPWI) might be considered an efficient alternative to handle the largest waste stream while enhancing the oil recovery and storing carbon dioxide (CO2) underground. This study was an attempt to get a deeper understanding of the oil [...] Read more.
Carbonated produced water injection (CPWI) might be considered an efficient alternative to handle the largest waste stream while enhancing the oil recovery and storing carbon dioxide (CO2) underground. This study was an attempt to get a deeper understanding of the oil recovery process through synergy between spontaneous imbibition and isothermal titration calorimetry (ITC) experiments. The results from the spontaneous imbibition experiments showed 7% to 11% additional oil recovery in comparison with plain produced water. Rock–fluid and fluid–fluid interactions, evaluated by isothermal titration calorimetry (ITC) experiments, confirmed that the CPW interactions with oil+EFB+chalk and oil+EFB systems are much more exothermic than those with plain PW in those systems. The synergy between spontaneous imbibition and ITC experiments provides an improved understanding of carbonated water injection in carbonate reservoirs. Full article
(This article belongs to the Special Issue Brine in Geothermal Energy Systems)
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16 pages, 9039 KiB  
Article
A Geothermal Plant from a Time-Scale Perspective
by Jacquelin E. Cobos, Christen Knudby and Erik G. Søgaard
Energies 2021, 14(19), 6096; https://doi.org/10.3390/en14196096 - 24 Sep 2021
Cited by 5 | Viewed by 2122
Abstract
In recent years, geothermal energy use from low-temperature sandstone reservoirs has sharply increased. Nonetheless, the injection of heat-depleted geothermal fluids has not been an easy task because of well/formation damage and operational/economic issues. Sønderborg geothermal plant is a case example of heat-mining from [...] Read more.
In recent years, geothermal energy use from low-temperature sandstone reservoirs has sharply increased. Nonetheless, the injection of heat-depleted geothermal fluids has not been an easy task because of well/formation damage and operational/economic issues. Sønderborg geothermal plant is a case example of heat-mining from a low-temperature reservoir. It is in the northeast of Sønderborg towards Augustenborg Fjord. The present work takes into consideration the regional and local geology of the Sønderborg area, construction of the wells, field experience and water chemistry. The main issues of the geothermal plant appear to be related to the construction of the wells and reinjection of the heat-depleted brine. Our water chemistry analysis and PHREEQC simulations indicate that geothermal brine was saturated with respect to carbonate and barite minerals. The excess of Ca2+ and SO42− ions could have led to the formation and precipitation of carbonate and sulfate scales. Moreover, the increment of iron concentration over time could suggest the ingress of oxygen and pitting corrosion due to the presence of halide ions. Full article
(This article belongs to the Special Issue Brine in Geothermal Energy Systems)
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