Assessing the sources of inorganic carbon in surface-, soil- and non-thermal groundwater in Iceland by δ13C and 14C

Autor: Árný E. Sveinbjörnsdóttir, Rósa Ólafsdóttir, Andri Stefánsson, Stefán Arnórsson, Jan Heinemeier, Eydis Salome Eiriksdottir

Publikováno v: Sveinbjörnsdóttir, Á E, Stefánsson, A, Heinemeier, J, Arnórsson, S, Eiríksdóttir, E S & Ólafsdóttir, R 2020, ' Assessing the sources of inorganic carbon in surface-, soil-and non-thermal groundwater in Iceland by δ 13 C and 14 C ', Geochimica et Cosmochimica Acta, vol. 279, pp. 165-188 . https://doi.org/10.1016/j.gca.2020.03.021

Chemical weathering and associated atmospheric CO2 uptake by surface water and transport of dissolved inorganic carbon (DIC) by rivers to the ocean and subsequent carbonate deposition has been suggested to play a major role in long-time climate chang

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c4238f824c06e3696e3a966020afc246
https://doi.org/10.1016/j.gca.2020.03.021

Isotope (δD, δ18O, 3H, δ13C, 14C) and chemical (B, Cl) Constrains on water origin, mixing, water-rock interaction and age of low-temperature geothermal water

Autor: Jan Heinemaier, Hrefna Kristmannsdóttir, Stefán Arnórsson, Árný E. Sveinbjörnsdóttir, Andri Stefánsson

Publikováno v: Stefánsson, A, Arnórsson, S, Sveinbjörnsdóttir, Á E, Heinemeier, J & Kristmannsdóttir, H 2019, ' Isotope (δD, δ 18 O, 3 H, δ 13 C, 14 C) and chemical (B, Cl) Constrains on water origin, mixing, water-rock interaction and age of low-temperature geothermal water ', Applied Geochemistry, vol. 108, no. September, 104380 . https://doi.org/10.1016/j.apgeochem.2019.104380

The isotope (δD, δ18O, 3H, δ13C, 14C) and chemical (B, Cl) compositions of cold (streams, rivers, soil- and groundwater) and low-temperature geothermal water from northern Iceland were investigated in order to delineate the origin, mixing, water-r

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8537760d329b7e0b6b9d24b365d7d878
https://pure.au.dk/portal/da/publications/isotope-d-18o-3h-13c-14c-and-chemical-b-cl-constrains-on-water-origin-mixing-waterrock-interaction-and-age-of-lowtemperature-geothermal-water(1249f96b-e2b8-4748-91a6-8ecfd336bdd0).html

Surface water chemistry at Torfajökull, Iceland—Quantification of boiling, mixing, oxidation and water–rock interaction and reconstruction of reservoir fluid composition

Autor: Stefán Arnórsson, Andri Stefánsson, Julia K. Björke

Publikováno v: Geothermics. 58:75-86

The surface geothermal water chemistry and alteration mineralogy associated with rhyolitic rocks at Torfajokull central volcano, Iceland was studied. The geothermal waters ranged in pH and temperature from 2.33 to 9.77 and 6–98 °C, respectively, a

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3134f76a82d7df79fc9b852d6e64a90f
https://doi.org/10.1016/j.geothermics.2015.09.007

Hydrogeology of the Krafla geothermal system, northeast Iceland

Autor: Stefán Arnórsson, Niels Giroud, Dennis K. Bird, E. C. Pope

Publikováno v: Geofluids. 16:175-197

The Krafla geothermal system is located in Iceland's northeastern neovolcanic zone, within the Krafla central volcanic complex. Geothermal fluids are superheated steam closest to the magma heat source, two-phase at higher depths, and sub-boiling at t

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::4d6e614dc02e90c19b0285c39929e942
https://doi.org/10.1111/gfl.12142

Stable isotopes of hydrothermal minerals as tracers for geothermal fluids in Iceland

Autor: E. C. Pope, Stefán Arnórsson, Dennis K. Bird

Publikováno v: Geothermics. 49:99-110

The Reykjanes and Krafla geothermal systems, located within the active rift zone of Iceland, are both potential venues for exploitation of deep supercritical fluids by the Iceland Deep Drilling Project (IDDP). An essential aspect of properly characte

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::887b041990ff60b459b9992e28390c28
https://doi.org/10.1016/j.geothermics.2013.05.005