| dc.contributor |
Jarðhitaskóli Háskóla Sameinuðu þjóðanna |
is |
| dc.contributor.author |
Li Yuanyuan |
is |
| dc.date.accessioned |
2020-06-30T17:44:51Z |
|
| dc.date.available |
2020-06-30T17:44:51Z |
|
| dc.date.issued |
2011 |
|
| dc.identifier.issn |
1670-7427 |
|
| dc.identifier.uri |
http://hdl.handle.net/10802/23809 |
|
| dc.description |
Í: Geothermal training in Iceland 2010, bls. 295-318 |
is |
| dc.description |
Myndefni: kort, gröf. |
is |
| dc.description.abstract |
The Reykir low-temperature geothermal area at Reykjabraut is on the edge of the Vatnsdalur extinct central volcano. Eight deep geothermal wells have been drilled in the area, with a depth of 234 to 1676 m. Wells RR-05 and RR-12 are the major production wells. Based on the consideration of fluid and mineral compositions, geothermometers, mineral-solution equilibrium, mixing, isotopes, and water-rock interaction, this paper mainly describes the chemical characteristics of the thermal fluids, their origins, and the recharge and discharge of fluids. Finally, the process of water-rock interaction was modelled with PHREEQC. Some of the results were compared to the nearby Laugarbakki field in order to discuss different formation conditions of geothermal fluids. |
is |
| dc.format.extent |
1 rafrænt gagn (22 bls.) |
is |
| dc.language.iso |
en |
|
| dc.publisher |
United Nations University |
is |
| dc.publisher |
Orkustofnun |
is |
| dc.relation.ispartofseries |
United Nations University., UNU Geothermal Training Programme, Iceland. Report ; 2010 : 17 |
|
| dc.relation.uri |
http://www.os.is/gogn/unu-gtp-report/UNU-GTP-2010-17.pdf |
|
| dc.subject |
Jarðhiti |
is |
| dc.subject |
Jarðefnafræði |
is |
| dc.subject |
Reykir við Reykjabraut |
is |
| dc.subject |
Laugarbakki |
is |
| dc.title |
Chemical characteristics and the formation conditions of geothermal fluids in Reykir at Reykjabraut, N-Iceland |
en |
| dc.title.alternative |
Geothermal training in Iceland |
en |
| dc.type |
Bók |
is |
| dc.identifier.gegnir |
991010606909706886 |
|
