Zobrazeno 1 - 10
of 33
pro vyhledávání: '"Hrefna Kristmannsdóttir"'
Publikováno v:
Water-Rock Interaction ISBN: 9780203734049
Water-Rock Interaction
Water-Rock Interaction
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01449eb90f43925b015a6c604ef5891d
https://doi.org/10.1201/9780203734049-49
https://doi.org/10.1201/9780203734049-49
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
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
Autor:
Gabrielle Stockmann, Carl-Magnus Mörth, Hreinn Hjartarson, Arny E. Sveinbjörnsdottir, Hrefna Kristmannsdóttir, Erik Sturkell, Margareta Andrén, Heike Siegmund, Ingrid Kockum, Alasdair Skelton, Sigurjón Jónsson, Helga Rakel Guðrúnardóttir
Publikováno v:
Nature Geoscience. 7:752-756
Precursor events to earthquakes are rarely reproduced. Measurement of groundwater chemistry in Iceland between 2008 and 2013 reveals distinct changes prior to two consecutive >M5 earthquakes.
Autor:
Stefán Arnórsson, Jan Heinemeier, Hrefna Kristmannsdóttir, Árný E. Sveinbjörnsdóttir, Ríkey Kjartansdóttir, Andri Stefánsson
Publikováno v:
Stefansson, A, Sveinbjornsdottir, A E, Heinemeier, J, Arnorsson, S, Kjartansdottir, R & Kristmannsdottir, H 2016, ' Mantle CO 2 degassing through the Icelandic crust : Evidence from carbon isotopes in groundwater ', Geochimica et Cosmochimica Acta, vol. 191, pp. 300-319 . https://doi.org/10.1016/j.gca.2016.06.038
Carbon isotopes of groundwater in Iceland were studied in order to determine the source and reactions of carbon at divergent plate boundaries not associated with active volcanic systems. All the waters were of meteoric origin, with temperatures of 1-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a28bf23573b93d7c89a839ab2b0c873f
https://pure.au.dk/portal/da/publications/mantle-co2-degassing-through-the-icelandic-crust(bcbf268e-617e-4674-b3e2-512c6b33f4e0).html
https://pure.au.dk/portal/da/publications/mantle-co2-degassing-through-the-icelandic-crust(bcbf268e-617e-4674-b3e2-512c6b33f4e0).html
Publikováno v:
Applied Geochemistry. 27:1146-1152
The geothermal field at Hofsstadir northern Snaefellsnes peninsula, Iceland produces low-temperature geothermal water with about 5.4‰ salinity. The fluid temperature is 87 °C, near the reservoir temperature of 90 °C as assessed from mineral solut
Publikováno v:
Aquatic Ecology. 38:115-128
Lake Myvatn, northern Iceland is unique in that almost all the inflow is supplied through the groundwater by artesian springs. Hardly any surface water is encountered in the area which is covered by young and porous lava fields and transected by faul
Publikováno v:
Geothermics. 32:451-461
Geothermal energy is a clean and sustainable energy source, but its development still has some impact on the environment. The positive and negative aspects of this environmental impact have to be considered prior to any decision to develop a geotherm
Autor:
Hrefna Kristmannsdóttir, Arny E. Sveinbjörnsdottir, P Torsander, Bernard Dupré, Árni Snorrason, Sigurdur R. Gislason, J Ólafsson, S Castet
Publikováno v:
Chemical Geology. 190:181-205
The October 1996 eruption within the Vatnajokull Glacier, Iceland, provides a unique opportunity to study the net effect of volcanic eruptions on atmospheric and oceanic CO2. Volatile elements dissolved in the meltwater that enclosed the eruption sit
Publikováno v:
Clays and Clay Minerals. 50:174-185
A study of the mineralogy, chemical composition and structure of poorly-crystalline saponite precipitated from a submarine hot spring in Eyjafjordur, northern Iceland is reported. Special emphasis was placed on the microstructures of the minerals and
Autor:
Hrefna Kristmannsdóttir, Halldór Ármannsson, Hreinn Hjartarson, Magnús Ólafsson, Magnús Á. Sigurgeirsson
Publikováno v:
Geothermics. 29:525-538
Sulfur gas (H 2 S and SO 2 ) emissions from geothermal fields in Iceland have been studied as part of a project, aimed at enhancing environmental research concerning effects of geothermal development. Short-term measurements of the gases have been ca