Deposits in utilized Icelandic high-temperature systems
The most common scales in 7 utilized Icelandic high-temperature geothermal systems are calcite, amorphous silica, magnesium silicates, iron silicates, aluminium silicates and metal sulphides. They are mostly controlled by adjustment of temperature and pressure although chemical inhibition may be pre...
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2019-01-01
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Online Access: | https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_07003.pdf |
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doaj-390389c4159b45ee94006b696f2a6d7a2021-02-02T06:44:38ZengEDP SciencesE3S Web of Conferences2267-12422019-01-01980700310.1051/e3sconf/20199807003e3sconf_wri-162018_07003Deposits in utilized Icelandic high-temperature systemsÁrmannsson Halldór0ÍSOR, Iceland GeosurveyThe most common scales in 7 utilized Icelandic high-temperature geothermal systems are calcite, amorphous silica, magnesium silicates, iron silicates, aluminium silicates and metal sulphides. They are mostly controlled by adjustment of temperature and pressure although chemical inhibition may be preferred due to production capacity. Reaming of wells by drilling and physical removal from surface equippment or acid cleaning may be needed.https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_07003.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Ármannsson Halldór |
spellingShingle |
Ármannsson Halldór Deposits in utilized Icelandic high-temperature systems E3S Web of Conferences |
author_facet |
Ármannsson Halldór |
author_sort |
Ármannsson Halldór |
title |
Deposits in utilized Icelandic high-temperature systems |
title_short |
Deposits in utilized Icelandic high-temperature systems |
title_full |
Deposits in utilized Icelandic high-temperature systems |
title_fullStr |
Deposits in utilized Icelandic high-temperature systems |
title_full_unstemmed |
Deposits in utilized Icelandic high-temperature systems |
title_sort |
deposits in utilized icelandic high-temperature systems |
publisher |
EDP Sciences |
series |
E3S Web of Conferences |
issn |
2267-1242 |
publishDate |
2019-01-01 |
description |
The most common scales in 7 utilized Icelandic high-temperature geothermal systems are calcite, amorphous silica, magnesium silicates, iron silicates, aluminium silicates and metal sulphides. They are mostly controlled by adjustment of temperature and pressure although chemical inhibition may be preferred due to production capacity. Reaming of wells by drilling and physical removal from surface equippment or acid cleaning may be needed. |
url |
https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_07003.pdf |
work_keys_str_mv |
AT armannssonhalldor depositsinutilizedicelandichightemperaturesystems |
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1724300653442891776 |