Opin vísindi
Opin vísindi er varðveislusafn vísindaefnis og doktorsritgerða í opnum aðgangi á vegum íslenskra háskóla og Landsbókasafns Íslands - Háskólabókasafns.
Opinn aðgangur að rannsóknaniðurstöðum er í samræmi við 10. gr. laga nr. 3/2003 um opinberan stuðning við vísindarannsóknir sem og kröfur innlendra og erlendra rannsóknasjóða. Markmiðið með opnum aðgangi er að niðurstöður rannsókna séu aðgengilegar sem flestum óhindrað og án endurgjalds á rafrænu formi. Vistun í varðveislusafninu er varanleg og ætlað að tryggja aðgang að vísindaefni íslenskra háskóla í opnum aðgangi um ókomna tíð. Varðveislusafnið Opin vísindi er tengt við rannsóknagáttina IRIS og rannsóknaniðurstöður í opnum aðgangi sem eru skráðar í IRIS eru um leið vistaðar og gerðar aðgengilegar til framtíðar í varðveislusafninu. Með því að safna þessu efni saman í eitt safn verður aðgangur að því einfaldur og þægilegur fyrir alla sem vilja kynna sér það og geta þannig notið þess öfluga vísindastarfs sem fram fer í háskólum landsins.
Varðveislusafnið er OpenAIRE / OpenAIREplus samhæft og samrýmist kröfum sem gerðar eru um birtingu rannsóknaniðurstaðna úr verkefnum sem styrkt eru úr evrópsku rannsóknaáætlununum FP7 og H2020.
Varðveislusafnið notar opna hugbúnaðinn DSpace.
Opinn aðgangur að rannsóknaniðurstöðum er í samræmi við 10. gr. laga nr. 3/2003 um opinberan stuðning við vísindarannsóknir sem og kröfur innlendra og erlendra rannsóknasjóða. Markmiðið með opnum aðgangi er að niðurstöður rannsókna séu aðgengilegar sem flestum óhindrað og án endurgjalds á rafrænu formi. Vistun í varðveislusafninu er varanleg og ætlað að tryggja aðgang að vísindaefni íslenskra háskóla í opnum aðgangi um ókomna tíð. Varðveislusafnið Opin vísindi er tengt við rannsóknagáttina IRIS og rannsóknaniðurstöður í opnum aðgangi sem eru skráðar í IRIS eru um leið vistaðar og gerðar aðgengilegar til framtíðar í varðveislusafninu. Með því að safna þessu efni saman í eitt safn verður aðgangur að því einfaldur og þægilegur fyrir alla sem vilja kynna sér það og geta þannig notið þess öfluga vísindastarfs sem fram fer í háskólum landsins.
Varðveislusafnið er OpenAIRE / OpenAIREplus samhæft og samrýmist kröfum sem gerðar eru um birtingu rannsóknaniðurstaðna úr verkefnum sem styrkt eru úr evrópsku rannsóknaáætlununum FP7 og H2020.
Varðveislusafnið notar opna hugbúnaðinn DSpace.
Flokkar í Opnum vísindum
Veldu flokk til að skoða.
- University of Iceland
- University of Akureyri
- Bifröst University
- Hólar University College
- Reykjavík University
- IRIS
- Agricultural University of Iceland
- National and University Library of Iceland
- Iceland University of the Arts
Nýlega bætt við
Online communication and adolescent health. Exploring adolescent mental and physical health and online communication in the early 21st century: Longitudinal and cross-sectional perspectives
(University of Iceland, School of Education, Faculty of Health Promotion, Sport and Leisure Studies, 2025-09) Birgisson, Ottar; Erlingur Jóhannsson, G. Sunna Gestsdóttir; Deild heilsueflingar, íþrótta og tómstunda (HÍ); Faculty of Health Promotion, Sport & Leisure Studies (UI); Menntavísindasvið (HÍ); School of Education (UI)
In this thesis, I investigate the evolving relationship between online communication and
adolescent mental and physical health, focusing on changes over time. The main aim
was to assess how online communication relates to mental health outcomes (depression,
anxiety, self-esteem, and body image) and physical health, measured as
cardiorespiratory fitness (CRF). Additionally, how these relationships have changed in
the early 21st century, during a period of significant transformations in online
communication, was explored.
Three datasets collected from Icelandic adolescents were used. 1) A cohort born in
1988 assessed in 2003 at age 15 (n = 385), 2) a cohort born in 1999 assessed in 2015
at age 15 (n = 302), and 3) the cohort born in 1999 followed up in 2017 at age 17
(n = 236). Measurements included self-reported online communication frequency,
validated questionnaires assessing mental health, and objective CRF measurements
using a maximal cycle ergometer test. Socioeconomic status (SES) was estimated based
on parental education and living arrangements. Statistical analyses included descriptive
statistics, multiple regression, analysis of variance, structural equation modeling, and
mixed-effects models.
Results showed that depressive symptoms increased among adolescent females
between 2003 and 2015 while remaining stable for males. Anxiety levels and self-
esteem did not change significantly for either sex. Body image improved slightly for
males but was stable for females. By 2015, a significant relationship was found between
online communication and an increase in depressive and anxiety symptoms in females
but not in males. CRF declined from 2003 to 2015, and a negative association between
CRF and mental health outcomes was observed. Lastly, online communication had a
negative association with mental health and CRF at the age of 15, and that this
relationship persisted until the age of 17, regardless of sex and SES.
The findings highlight the complex dynamics of online communication and its impact
on adolescent mental and physical health. Increased online communication appears to
be linked to poorer mental health outcomes particularly for females, possibly mediated
by social comparison. Declining CRF underscores the importance of promoting
physical fitness alongside mental health interventions. To address these challenges,
interventions should integrate both digital literacy and physical activity strategies. This
study contributes to a deeper understanding of adolescent well-being in the digital age
and provides a foundation for targeted interventions.
Tourist safety on adventure trips: Guide competencies and risk management strategies in the Arctic
(University of Iceland, School of Engineering and Natural Sciences, Faculty of Life and Environmental Sciences, 2025-09) Hild, Barbara Olga; Gunnar Þór Jóhannesson; Líf- og umhverfisvísindadeild (HÍ); Faculty of Life and Environmental Sciences (UI); Verkfræði- og náttúruvísindasvið (HÍ); School of Engineering and Natural Science (UI)
Improving modelling of crustal deformation in relation to magmatic and geothermal processes
(University of Iceland, School of Engineering and Natural Sciences, Faculty of Earth Sciences, 2025-09) Lanzi, Chiara; Freysteinn Sigmundsson; Jarðvísindadeild (HÍ); Faculty of Earth Sciences (UI); Verkfræði- og náttúruvísindi (HÍ); School of Engineering and Natural Sciences (UI)
Understanding small crustal deformation signals is important for improving volcano monitoring and hazard mitigation. Spatial and temporal ground displacement patterns were mapped with Global Navigation Satellite System (GNSS) geodesy and Interferometric analysis of Synthetic Aperture Radar (InSAR) images, allowing detection of millimeter- to centimeter-scale deformation. Geodetic modelling, through inversion or forward modelling, was used to infer deformation source parameters and increase understanding of volcanic, geothermal and tectonic processes. In summer 2018, a change in the pattern of ground deformation at the Krafla caldera coincided with increased pressure in a monitoring well. This occurred at a similar time as re-injection of water, in relation to geothermal utilization, was modified. The difference between GNSS and InSAR velocity fields from 2015–2018 and 2018–2020 reveals an inflation pattern with horizontal motion up to 8–10 mm/yr. Geodetic inversion shows that the difference velocity field can be fit with a 2.1–2.5 km deep point-source, near the magma-hydrothermal interface. The observations are broadly explained by local variations in intra-caldera crustal elasticity and pressure increase at ~2.2 km depth, consistent with the well data. The study also examined how local elastic and viscoelastic crustal and mantle properties at volcanoes located at divergent plate boundaries influence deformation by regional processes like plate spreading, using a Finite Element Method model to simulate local rheological anomalies beneath calderas and rifts. This approach helps explaining the observed decades-long subsidence at Krafla (1989–2018) and Askja (1985–2021). The results show that extensional forces and rheological anomalies can drive volcanic subsidence. At Krafla, this account for much of observed 2015-2018 subsidence, but only 20–30% at Askja. Finally, the ~40-60 mm subsidence during the 2021 Fagradalsfjall eruption was analyzed and evaluated how changes in deformation relate to changes in eruption rate, geochemistry of eruptive products, and eruptive style. Surface lava loading within 1-2 km significantly contributed to the subsidence. After removing this effect, geodetic inversion locates a 12–14 km deep sill source with volume contraction of 2127 Mm3. This research highlights the need to consider complex geological settings when interpreting small ground deformation signals, as multiple interacting processes may produce observed deformation.
Basalt lava degassing: mechanism and characterisation
(University of Iceland, School of Engineering and Natural Sciences, Faculty of Earth Sciences, 2025-05) Levillayer, Nicolas; Olgeir Sigmarsson; Jarðvísindadeild (HÍ); Faculty of Earth Sciences (UI); Verkfræði- og náttúruvísindasvið (HÍ); School of Engineering and Natural Sciences (UI)
The volcanic gas composition emitted during basaltic eruptions is relatively well understood,
but the emissions from cooling lava fields have been less studied, along with their
environmental impacts. The study investigated the gas emission from crystallising lava, as
well as the internal structure of lava and associated segregation veins. Gas samples were
collected from the eruptive crater, cooling vents, and solidifying lava in Fagradalsfjall. The
gas emissions were found rich in sulphur and sulphide-forming elements at the eruptive
crater, while post-eruptive gas is richer in halogens, especially chlorine at the crystallising
lava and fluorine at the cooling vent. Estimates of emissions from crystallising lava show
significant release of metals that form chlorides. The relationship between emission and
fractional crystallisation, along with segregation melt formation during lava solidification,
was examined. The first minerals to from are anhydrous, forming a fully crystallised
framework after 40-50% crystallisation. In the residual melt, volatile elements saturate and
form a volume-rich gas phase. The gas presses the melt through the crystal framework,
forming segregation veins. Chemical analyses of these veins reveal whether the gas phase
escaped into the atmosphere or solidified with the melt. The similar compositions of
segregation veins and gas from solidifying lava indicate a relationship between the internal
lava evolution and lava degassing. Overall, the results show that gas emissions from lava are
distinct from emissions at the vent but correlate well with the fractional emission of basalt
melt, both in terms of origin and nature. The environmental impacts of heavy metal gas
emissions from basalt lava are a worthy subject for future research.
Ágripabók: 25. ráðstefna Þjóðarspegilsins
(University of Iceland, School of Social Sciences, Social Science Research Institute, 2024-11) Háskóli Íslands, Félagsvísindastofnun; Félagsvísindastofnun (HÍ); Social Science Research Institute (UI); Félagsvísindasvið (HÍ); School of Social Sciences (UI)