Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Morgan Tranter"'
Autor:
Christopher Otto, Svenja Steding, Morgan Tranter, Torsten Gorka, Mária Hámor-Vidó, Wioleta Basa, Krzysztof Kapusta, István Kalmár, Thomas Kempka
Publikováno v:
Advances in Geosciences
In the context of a potential utilisation of coal resources located in the Mecsek mountain area in Southern Hungary, an assessment of groundwater pollution resulting from a potential water-borne contaminant pool remaining in in situ coal conversion r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d1517fcf91522dd8118cf037ffe9c9a8
https://adgeo.copernicus.org/articles/58/55/2022/
https://adgeo.copernicus.org/articles/58/55/2022/
Autor:
Thomas Kempka, Svenja Steding, Morgan Tranter, Christopher Otto, Torsten Gorka, Mária Hámor-Vidó, Wioleta Basa, Krzysztof Kapusta, István Kalmár
In the context of a potential utilisation of coal resources located in the Mecsek mountain area in Southern Hungary (Püspöki et al.. 2012), an assessment of groundwater pollution resulting from a potential water-borne contaminant pool remaining in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::272b63239e7662482f1b4f349c3599b2
https://doi.org/10.5194/egusphere-egu22-11204
https://doi.org/10.5194/egusphere-egu22-11204
Autor:
Morgan Tranter, Svenja Steding, Christopher Otto, Konstantina Pyrgaki, Mansour Hedayatzadeh, Vasilis Sarhosis, Nikolaos Koukouzas, Georgios Louloudis, Christos Roumpos, Thomas Kempka
Publikováno v:
Advances in Geosciences
Comprehensive risk assessments for subsurface utilisation projects such as in-situ coal conversion, deep geothermal energy, geological storage, and waste disposal are implemented to a limited extent in common practice. The impacts of subsurface proce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::875ef6426fd47d726554bd5660087723
https://doi.org/10.5194/egusphere-egu22-10115
https://doi.org/10.5194/egusphere-egu22-10115
Publikováno v:
Minerals, Vol 11, Iss 1198, p 1198 (2021)
Minerals
Volume 11
Issue 11
Minerals
Volume 11
Issue 11
Barite scalings are a common cause of permanent formation damage to deep geothermal reservoirs. Well injectivity can be impaired because the ooling of saline fluids reduces the solubility of barite, and the continuous re-injection of supersaturated f
Publikováno v:
Goldschmidt2021 abstracts.
Deep hydrothermal systems in fractured media are a potential source of geothermal energy. A key problem prevails as a consequence of utilisation that the geochemical system is perturbed and scaling may build up over time. Barite stands out as one of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f71158f291b85af183034bef7e3df0e7
https://doi.org/10.5194/egusphere-egu2020-417
https://doi.org/10.5194/egusphere-egu2020-417
Publikováno v:
Water
Volume 12
Issue 11
Water, Vol 12, Iss 3078, p 3078 (2020)
Volume 12
Issue 11
Water, Vol 12, Iss 3078, p 3078 (2020)
Barite scales in geothermal installations are a highly unwanted effect of circulating deep saline fluids. They build up in the reservoir if supersaturated fluids are re-injected, leading to irreversible loss of injectivity. A model is presented for c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::21252023e8ce46c4395d815affe9549a
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5004236_1/component/file_5004279/5004236.pdf
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5004236_1/component/file_5004279/5004236.pdf
Publikováno v:
Geothermics
Barite stands out as one of the most ubiquitous scaling agents in deep geothermal systems, responsible for irreversible efficiency loss. Due to complex parameter interplay, it is imperative to utilise numerical simulations to investigate temporal and
Publikováno v:
Grundwasser. 22:55-62
A significant proportion of the global water supply is ensured by karst aquifers. However, these are often highly vulnerable to contamination. A storm water tank located in the rural karst catchment area of the Gallusquelle spring (Swabian Alb, south