Materials for Geothermal Steam Utilization at Higher Temperatures and Pressure

ABSTRACT Materials used in high temperature/pressure geothermal steam can be subjected to corrosion due to the aggressiveness of the geothermal fluid and non-condensable gasses such as hydrogen sulfide (H 2 S) and carbon dioxide (CO 2 ), chloride ions (Cl -) and hydrogen fluoride (HF). Icelandic Dee...

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Main Authors: Ingolfur O Thorbjornsson, Sigrun N Karlsdottir, Ásbjörn Einarsson, Kolbrun R Ragnarsdottir
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1075.3447
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1075.3447 2023-05-15T16:48:10+02:00 Materials for Geothermal Steam Utilization at Higher Temperatures and Pressure Ingolfur O Thorbjornsson Sigrun N Karlsdottir Ásbjörn Einarsson Kolbrun R Ragnarsdottir The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1075.3447 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1075.3447 Metadata may be used without restrictions as long as the oai identifier remains attached to it. https://pangea.stanford.edu/ERE/db/WGC/papers/WGC/2015/27045.pdf text ftciteseerx 2020-04-26T00:29:18Z ABSTRACT Materials used in high temperature/pressure geothermal steam can be subjected to corrosion due to the aggressiveness of the geothermal fluid and non-condensable gasses such as hydrogen sulfide (H 2 S) and carbon dioxide (CO 2 ), chloride ions (Cl -) and hydrogen fluoride (HF). Icelandic Deep Drilling well (IDDP-1) in the Krafla area in NA Iceland gave well head temperature of 452°C at 140 bar pressure flowing 12 ks/s of superheated steam. This well alone could produce 25-35 MWe, but due to extreme conditions it is not currently operational. This paper focus on learnings from the material testing performed during the lifetime of the well and reveal several promising material choices for utilizing geothermal steam in extreme conditions like in IDDP1. Work is now ongoing in designing the next Icelandic Deep Drilling (IDDP-2) well in Iceland and expectations are to get 400-500°C steam with well head pressure over 100 bar. This will put several constrains on materials normally suitable for high temperature geothermal steam and calls for redesigning of materials, both down hole and above surface. Safety issues will be considered and direct or indirect use of the steam for electricity production will be discussed. Materials are evaluated based on research from the first IDDP well and possible changes in chemical composition of the geothermal fluid and gas contents are discussed. Text Iceland Unknown Krafla ENVELOPE(-16.747,-16.747,65.713,65.713)
institution Open Polar
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description ABSTRACT Materials used in high temperature/pressure geothermal steam can be subjected to corrosion due to the aggressiveness of the geothermal fluid and non-condensable gasses such as hydrogen sulfide (H 2 S) and carbon dioxide (CO 2 ), chloride ions (Cl -) and hydrogen fluoride (HF). Icelandic Deep Drilling well (IDDP-1) in the Krafla area in NA Iceland gave well head temperature of 452°C at 140 bar pressure flowing 12 ks/s of superheated steam. This well alone could produce 25-35 MWe, but due to extreme conditions it is not currently operational. This paper focus on learnings from the material testing performed during the lifetime of the well and reveal several promising material choices for utilizing geothermal steam in extreme conditions like in IDDP1. Work is now ongoing in designing the next Icelandic Deep Drilling (IDDP-2) well in Iceland and expectations are to get 400-500°C steam with well head pressure over 100 bar. This will put several constrains on materials normally suitable for high temperature geothermal steam and calls for redesigning of materials, both down hole and above surface. Safety issues will be considered and direct or indirect use of the steam for electricity production will be discussed. Materials are evaluated based on research from the first IDDP well and possible changes in chemical composition of the geothermal fluid and gas contents are discussed.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Ingolfur O Thorbjornsson
Sigrun N Karlsdottir
Ásbjörn Einarsson
Kolbrun R Ragnarsdottir
spellingShingle Ingolfur O Thorbjornsson
Sigrun N Karlsdottir
Ásbjörn Einarsson
Kolbrun R Ragnarsdottir
Materials for Geothermal Steam Utilization at Higher Temperatures and Pressure
author_facet Ingolfur O Thorbjornsson
Sigrun N Karlsdottir
Ásbjörn Einarsson
Kolbrun R Ragnarsdottir
author_sort Ingolfur O Thorbjornsson
title Materials for Geothermal Steam Utilization at Higher Temperatures and Pressure
title_short Materials for Geothermal Steam Utilization at Higher Temperatures and Pressure
title_full Materials for Geothermal Steam Utilization at Higher Temperatures and Pressure
title_fullStr Materials for Geothermal Steam Utilization at Higher Temperatures and Pressure
title_full_unstemmed Materials for Geothermal Steam Utilization at Higher Temperatures and Pressure
title_sort materials for geothermal steam utilization at higher temperatures and pressure
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1075.3447
long_lat ENVELOPE(-16.747,-16.747,65.713,65.713)
geographic Krafla
geographic_facet Krafla
genre Iceland
genre_facet Iceland
op_source https://pangea.stanford.edu/ERE/db/WGC/papers/WGC/2015/27045.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1075.3447
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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