Understanding amorphous silica scaling under well-constrained conditions inside geothermal pipelines

Amorphous silica is a common precipitate in modern and ancient hot springs and in geothermal power plants, yet the corresponding precipitation rates and mechanisms are still highly debated, primarily due to the plethora of parameters that can affect the reactions in natural waters. Here, we report t...

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Published in:Geothermics
Main Authors: van den Heuvel, D., Gunnlaugsson, E., Gunnarsson, I., Stawski, T., Peacock, C., Benning, L.
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_3444892
https://gfzpublic.gfz-potsdam.de/pubman/item/item_3444892_3/component/file_5000170/3444892.pdf
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_3444892 2023-05-15T16:51:07+02:00 Understanding amorphous silica scaling under well-constrained conditions inside geothermal pipelines van den Heuvel, D. Gunnlaugsson, E. Gunnarsson, I. Stawski, T. Peacock, C. Benning, L. 2018 application/pdf https://gfzpublic.gfz-potsdam.de/pubman/item/item_3444892 https://gfzpublic.gfz-potsdam.de/pubman/item/item_3444892_3/component/file_5000170/3444892.pdf eng eng info:eu-repo/semantics/altIdentifier/doi/10.1016/j.geothermics.2018.07.006 https://gfzpublic.gfz-potsdam.de/pubman/item/item_3444892 https://gfzpublic.gfz-potsdam.de/pubman/item/item_3444892_3/component/file_5000170/3444892.pdf info:eu-repo/semantics/openAccess Geothermics info:eu-repo/semantics/article 2018 ftgfzpotsdam https://doi.org/10.1016/j.geothermics.2018.07.006 2022-09-14T05:56:28Z Amorphous silica is a common precipitate in modern and ancient hot springs and in geothermal power plants, yet the corresponding precipitation rates and mechanisms are still highly debated, primarily due to the plethora of parameters that can affect the reactions in natural waters. Here, we report the results from a first ever industrial-scale time-resolved (1 day to 10 weeks) study of silica precipitation conducted at the Hellisheiði geothermal power plant (SW-Iceland). We show that such in-work pipelines of a geothermal power plant are ideal environments to investigate silica precipitation because the physicochemical conditions are well constrained and constantly monitored. Our results document that amorphous silica forms via two distinct precipitation modes: (1) the fast deposition of continuous botryoidal silica layers and (2) the growth of 3D fan- or ridge-shaped silica aggregates. The continuous layers grow by heterogeneous nucleation and subsequent surface controlled growth by monomer addition. In contrary, the 3D aggregates form through homogeneous nucleation of silica nano- and microparticles in solution, followed by deposition and cementation on the surface of the botryoidal layer. From the time-resolved data, silica precipitation rates of over 1 g m−2 day-1 are derived. Over time, this deposition of silica on pipelines and fluid handling equipment is detrimental to geothermal power production. Our data does not only help improve our understanding of silica precipitation from geothermal fluids, but the determined silica precipitation mechanisms and rates help improve mitigation strategies against silica scaling inside in-work geothermal power plants. Article in Journal/Newspaper Iceland GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Geothermics 76 231 241
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Amorphous silica is a common precipitate in modern and ancient hot springs and in geothermal power plants, yet the corresponding precipitation rates and mechanisms are still highly debated, primarily due to the plethora of parameters that can affect the reactions in natural waters. Here, we report the results from a first ever industrial-scale time-resolved (1 day to 10 weeks) study of silica precipitation conducted at the Hellisheiði geothermal power plant (SW-Iceland). We show that such in-work pipelines of a geothermal power plant are ideal environments to investigate silica precipitation because the physicochemical conditions are well constrained and constantly monitored. Our results document that amorphous silica forms via two distinct precipitation modes: (1) the fast deposition of continuous botryoidal silica layers and (2) the growth of 3D fan- or ridge-shaped silica aggregates. The continuous layers grow by heterogeneous nucleation and subsequent surface controlled growth by monomer addition. In contrary, the 3D aggregates form through homogeneous nucleation of silica nano- and microparticles in solution, followed by deposition and cementation on the surface of the botryoidal layer. From the time-resolved data, silica precipitation rates of over 1 g m−2 day-1 are derived. Over time, this deposition of silica on pipelines and fluid handling equipment is detrimental to geothermal power production. Our data does not only help improve our understanding of silica precipitation from geothermal fluids, but the determined silica precipitation mechanisms and rates help improve mitigation strategies against silica scaling inside in-work geothermal power plants.
format Article in Journal/Newspaper
author van den Heuvel, D.
Gunnlaugsson, E.
Gunnarsson, I.
Stawski, T.
Peacock, C.
Benning, L.
spellingShingle van den Heuvel, D.
Gunnlaugsson, E.
Gunnarsson, I.
Stawski, T.
Peacock, C.
Benning, L.
Understanding amorphous silica scaling under well-constrained conditions inside geothermal pipelines
author_facet van den Heuvel, D.
Gunnlaugsson, E.
Gunnarsson, I.
Stawski, T.
Peacock, C.
Benning, L.
author_sort van den Heuvel, D.
title Understanding amorphous silica scaling under well-constrained conditions inside geothermal pipelines
title_short Understanding amorphous silica scaling under well-constrained conditions inside geothermal pipelines
title_full Understanding amorphous silica scaling under well-constrained conditions inside geothermal pipelines
title_fullStr Understanding amorphous silica scaling under well-constrained conditions inside geothermal pipelines
title_full_unstemmed Understanding amorphous silica scaling under well-constrained conditions inside geothermal pipelines
title_sort understanding amorphous silica scaling under well-constrained conditions inside geothermal pipelines
publishDate 2018
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_3444892
https://gfzpublic.gfz-potsdam.de/pubman/item/item_3444892_3/component/file_5000170/3444892.pdf
genre Iceland
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op_source Geothermics
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.geothermics.2018.07.006
https://gfzpublic.gfz-potsdam.de/pubman/item/item_3444892
https://gfzpublic.gfz-potsdam.de/pubman/item/item_3444892_3/component/file_5000170/3444892.pdf
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1016/j.geothermics.2018.07.006
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