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  1. Regions with low or medium surface heat flow in stable cratonic areas, such as in eastern Canada, have received little attention for geothermal energy. In the presence of a high heat-producing basement overlai...

    Authors: Hejuan Liu, Bernard Giroux, Lyal B. Harris, Steve M. Quenette and John Mansour
    Citation: Geothermal Energy 2018 6:30
  2. Laboratory studies designed to provide the strength of rocks are typically performed on either dry- or water-saturated rock samples. To better understand the mechanical behaviour of rocks in a geothermal conte...

    Authors: Michael J. Heap, Thierry Reuschlé, Alexandra R. L. Kushnir and Patrick Baud
    Citation: Geothermal Energy 2018 6:29
  3. Hydraulic stimulation treatments are standard techniques to access geologic resources which cannot economically be exploited with conventional methods. Fluid injection into unproductive formations may increase...

    Authors: Hannes Hofmann, Günter Zimmermann, Arno Zang and Ki-Bok Min
    Citation: Geothermal Energy 2018 6:27

    The Correction to this article has been published in Geothermal Energy 2019 7:1

  4. This paper examines the social, cultural and political factors that favor or disrupt deep geothermal energy projects in Alsace. The research was conducted in the Risk Governance package of the H2020 DESTRESS p...

    Authors: Philippe Chavot, Christine Heimlich, Anne Masseran, Yeny Serrano, Jean Zoungrana and Cyrille Bodin
    Citation: Geothermal Energy 2018 6:26
  5. After publication of the article (Glaas et al. 2018), it has been brought to our attention that there are some errors. The authors have listed them below.

    Authors: C. Glaas, A. Genter, J. F. Girard, P. Patrier and J. Vidal
    Citation: Geothermal Energy 2018 6:25

    The original article was published in Geothermal Energy 2018 6:14

  6. Hydraulic stimulation treatments required to produce deep geothermal reservoirs present the risk of generating induced seismicity. Understanding the processes that operate during the stimulation phase is criti...

    Authors: Guillem Piris, Albert Griera, Enrique Gomez-Rivas, Ignasi Herms, Mark W. McClure and Jack H. Norbeck
    Citation: Geothermal Energy 2018 6:24
  7. The Upper Rhine Graben (URG) is a highly favorable location for deep geothermal energy utilization. One of the main reservoir horizons is the lower Triassic Buntsandstein formation. While quantification of the...

    Authors: Robert Egert, Robin Seithel, Thomas Kohl and Ingrid Stober
    Citation: Geothermal Energy 2018 6:23
  8. Coda wave interferometry (CWI) is a high-resolution technique that aims at tracking small changes in a diffusive medium from the time correlation of seismic waveforms. CWI has been widely used in recent years ...

    Authors: Jérôme Azzola, Luke Griffiths, Jean Schmittbuhl, Dimitri Zigone, Vincent Magnenet, Frédéric Masson, Michael Heap and Patrick Baud
    Citation: Geothermal Energy 2018 6:21
  9. This article presents the study of the mass redistribution associated with the geothermal energy exploitation of the Soultz-sous-Forêts and Rittershoffen plants by microgravity monitoring in the period 2014–20...

    Authors: Nolwenn Portier, Jacques Hinderer, Umberto Riccardi, Gilbert Ferhat, Marta Calvo, Yassine Abdelfettah and Jean-Daniel Bernard
    Citation: Geothermal Energy 2018 6:19
  10. Reduction or prevention of scaling is commonly achieved by injecting scaling inhibitors into the geothermal circuit. Inhibitor-efficiency tests can be carried out in static or dynamic experiment set-ups allowi...

    Authors: Joerg Zotzmann, Alexandra Vetter and Simona Regenspurg
    Citation: Geothermal Energy 2018 6:18
  11. A wider exploitation of deep geothermal reservoir requires the development of Enhanced Geothermal System technology. In this context, drilling and stimulation of high-enthalpy geothermal wells raise technical ...

    Authors: M. Peter-Borie, A. Loschetter, I. A. Merciu, G. Kampfer and O. Sigurdsson
    Citation: Geothermal Energy 2018 6:17
  12. Geothermal energy exploitation in the Upper Rhine Graben currently targets high-temperature anomalies in the crystalline Paleozoic basement at depths up to 5 km. However, at certain locations (e.g. Rittershoff...

    Authors: Alexandra R. L. Kushnir, Michael J. Heap, Patrick Baud, H. Albert Gilg, Thierry Reuschlé, Catherine Lerouge, Chrystel Dezayes and Philippe Duringer
    Citation: Geothermal Energy 2018 6:16
  13. Two deep wells were drilled at Rittershoffen (Alsace, France) to produce high-temperature fluids to supply heat to a biorefinery. The GRT-2 production well was drilled to a depth of 3196 m MD and was deviated ...

    Authors: C. Glaas, A. Genter, J. F. Girard, P. Patrier and J. Vidal
    Citation: Geothermal Energy 2018 6:14

    The Correction to this article has been published in Geothermal Energy 2018 6:25

  14. New and old magnetic and gravimetric data acquired in the frame of a geothermal project have been processed in N. Vosges and the adjacent Rhinegraben in order to identify the nature and tectonic framework of t...

    Authors: J. B. Edel, V. Maurer, E. Dalmais, A. Genter, A. Richard, O. Letourneau and R. Hehn
    Citation: Geothermal Energy 2018 6:13
  15. The classical methodology to perform and analyze thermal response test (TRT) is unsuccessful when advection contributes to heat transfer in the ground, due to the presence of a groundwater flow. In this study,...

    Authors: Adriana Angelotti, Franco Ly and Andrea Zille
    Citation: Geothermal Energy 2018 6:12
  16. Knowledge of the strength and elastic modulus of a reservoir rock is important for the optimisation of a particular geothermal resource. The reservoir rock for many geothermal projects in the Upper Rhine Grabe...

    Authors: Marlène C. Villeneuve, Michael J. Heap, Alexandra R. L. Kushnir, Tao Qin, Patrick Baud, Guanglei Zhou and Tao Xu
    Citation: Geothermal Energy 2018 6:11
  17. In the present study, CFD-based parametric analysis is carried out to optimise the parameters affecting the temperature drop and heat transfer rate achieved from earth air tunnel heat exchanger (EATHE) system....

    Authors: Kamal Kumar Agrawal, Mayank Bhardwaj, Rohit Misra, Ghanshyam Das Agrawal and Vikas Bansal
    Citation: Geothermal Energy 2018 6:10
  18. Earthquakes, despite being a mostly natural phenomenon, may also be induced by a wide range of anthropogenic activities such as mining, fluid injection and extraction, hydraulic fracturing and geothermal reser...

    Authors: Konstantinos G. Megalooikonomou, Stefano Parolai and Massimiliano Pittore
    Citation: Geothermal Energy 2018 6:8
  19. The present work investigates the influence of crack opening rates on the development of four important calcite vein morphologies, namely fibrous, elongate-blocky, partially open, and euhedral, as a result of ...

    Authors: Nishant Prajapati, Michael Selzer, Britta Nestler, Benjamin Busch and Christoph Hilgers
    Citation: Geothermal Energy 2018 6:7
  20. The thermal structure of continental crust is a critical factor for geothermal exploration, hydrocarbon maturation and crustal strength, and yet our understanding of it is limited by our incomplete knowledge o...

    Authors: Alexandre Lemenager, Craig O’Neill, Siqi Zhang and Morgan Evans
    Citation: Geothermal Energy 2018 6:6
  21. The lateral and vertical temperature distribution in Oman is so far only poorly understood, particularly in the area between Muscat and the Batinah coast, which is the area of this study and which is composed ...

    Authors: Felina Schütz, Gerd Winterleitner and Ernst Huenges
    Citation: Geothermal Energy 2018 6:5
  22. Geologic mapping, a magnetotelluric survey, well data, and earlier reports are integrated to guide further development of the Fang geothermal system. The Fang Hot Springs originally flowed ~ 20 l s−1 of 90–99 °C ...

    Authors: Spencer H. Wood, Pichet Kaewsomwang and Fongsaward Suvagonda Singharajwarapan
    Citation: Geothermal Energy 2018 6:3
  23. The Taupo Volcanic Zone (TVZ) hosts 23 geothermal fields, seven of which are currently utilised for power generation. Ngatamariki geothermal field (NGF) is one of the latest geothermal power generation develop...

    Authors: J. L. Cant, P. A. Siratovich, J. W. Cole, M. C. Villeneuve and B. M. Kennedy
    Citation: Geothermal Energy 2018 6:2
  24. A 1912-m exploration corehole was drilled along the axis of the eastern Snake River Plain, Idaho. Two temperature logs run on the corehole display an obvious inflection point at about 960 m. Such behavior is i...

    Authors: Thomas E. Lachmar, Thomas G. Freeman, Christopher J. Sant, Jeffrey R. Walker, Joseph F. Batir, John W. Shervais, James P. Evans, Dennis L. Nielson and David D. Blackwell
    Citation: Geothermal Energy 2017 5:28
  25. Geothermal projects in the Upper Rhine Graben aim to harness thermal anomalies that have arisen due to hydrothermal circulation within the granitic basement and the overlying Permo-Triassic sedimentary units. ...

    Authors: Michael J. Heap, Alexandra R. L. Kushnir, H. Albert Gilg, Fabian B. Wadsworth, Thierry Reuschlé and Patrick Baud
    Citation: Geothermal Energy 2017 5:26
  26. Leaching tests with synthetic brines (25 g/L NaCl) between 25 °C and 90 °C were performed under oxic and anoxic conditions over 7 days on two pyrite-bearing siliciclastic rocks from the Lower Jurassic Hettangi...

    Authors: Daniel Richard Müller and Simona Regenspurg
    Citation: Geothermal Energy 2017 5:25
  27. Minimizing exploration risk in deep geothermics is of great economic importance. Especially, knowledge about temperature and permeability of the reservoir is essential. We test the potential of an outcrop anal...

    Authors: Johanna F. Bauer, Michael Krumbholz, Silke Meier and David C. Tanner
    Citation: Geothermal Energy 2017 5:24
  28. After publication of the article (Orywall et al. 2017), it has been brought to our attention that there are a number of errors. The authors have listed them below.

    Authors: Pia Orywall, Kirsten Drüppel, Dietmar Kuhn, Thomas Kohl, Michael Zimmermann and Elisabeth Eiche
    Citation: Geothermal Energy 2017 5:23

    The original article was published in Geothermal Energy 2017 5:20

  29. This paper aims to predict ground temperature variation with depth for time variant ambient air temperature and solar radiation data for Jamshedpur, India. Finite difference method has been used to discretise ...

    Authors: Raviranjan Kumar Singh and Ram Vinoy Sharma
    Citation: Geothermal Energy 2017 5:22
  30. It is commonly known that heat extraction and decompression can lead to mineral precipitation and reservoir clogging in geothermal systems. In the Upper Rhine Graben, the precipitating minerals are mainly bari...

    Authors: Pia Orywall, Kirsten Drüppel, Dietmar Kuhn, Thomas Kohl, Michael Zimmermann and Elisabeth Eiche
    Citation: Geothermal Energy 2017 5:20

    The Correction to this article has been published in Geothermal Energy 2017 5:23

  31. To simulate the growth of geological veins, it is necessary to model the crystal shape anisotropy. Two different models, classical and natural models, which incorporate the surface energy anisotropy into the obje...

    Authors: Oleg Tschukin, Alexander Silberzahn, Michael Selzer, Prince G. K. Amos, Daniel Schneider and Britta Nestler
    Citation: Geothermal Energy 2017 5:19
  32. Earth’s crust offers a vast resource of heat that can be used and converted into energy both for electricity and heating/cooling purposes. The utilization of this geothermal energy can make an important contri...

    Authors: Simona Regenspurg and Thorsten Schäfer
    Citation: Geothermal Energy 2017 5:18
  33. The aim of this study is to compare between single flash, dual flash, and binary power plants in terms of the power generated, their performance, and the related cost. The results from the comparison are used ...

    Authors: M. El Haj Assad, E. Bani-Hani and M. Khalil
    Citation: Geothermal Energy 2017 5:17
  34. Supercritical geothermal systems are very high-temperature geothermal systems that are located at depths near or below the brittle–ductile transition zone in the crust where the reservoir fluid is assumed to b...

    Authors: Thomas Reinsch, Patrick Dobson, Hiroshi Asanuma, Ernst Huenges, Flavio Poletto and Bernard Sanjuan
    Citation: Geothermal Energy 2017 5:16
  35. In this paper, a conceptual model has been developed for NW Sabalan geothermal field using exploration indicators. These indicators include the data and results of subsurface and surface investigations compris...

    Authors: Mirmahdi Seyedrahimi-Niaraq, Faramarz Doulati Ardejani, Younes Noorollahi and Soheil Porkhial
    Citation: Geothermal Energy 2017 5:14
  36. The determination of reservoir temperatures represents a major task when exploring geothermal systems. Since the uncertainties of classical solute geothermometry are still preventing reliable reservoir tempera...

    Authors: Fabian Nitschke, Sebastian Held, Ignacio Villalon, Thomas Neumann and Thomas Kohl
    Citation: Geothermal Energy 2017 5:12
  37. Decreasing production rates and massive precipitation of native copper (Cu(0)) were observed in the production well at the geothermal research facility Groß Schönebeck (Germany). The Cu precipitates filling up...

    Authors: Simona Regenspurg, Ives Geigenmüller, Harald Milsch and Michael Kühn
    Citation: Geothermal Energy 2017 5:11
  38. In this study, we report results of the analysis of a particularly interesting scaling sample from the geothermal plant in Neustadt-Glewe in northern Germany, which contained 19% Galena (PbS) and 81% of a hete...

    Authors: Frank Heberling, Dieter Schild, Detlev Degering and Thorsten Schäfer
    Citation: Geothermal Energy 2017 5:9

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