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Campus development
Lund University's four campuses offer attractive academic environments that clearly reflect the University's identity. Research and learning are at the core, while the campuses also provide inviting spaces for social interaction, relaxation and recreation – all within a safe and inclusive setting. The University's campuses are continuously developed to meet the needs of a changing society. The pro
https://www.lunduniversity.lu.se/about-university/university-glance/mission-vision-and-values/campus-development - 2026-05-05
Special Area Study (SAS) courses
Nominated exchange students can apply for so-called 'Special Area Study' (SAS) courses in a wide range of subjects across eight out of nine faculties at Lund University. These courses are a wonderful opportunity for you to learn more about subjects outside your major. The course offerings include courses mostly focusing on one discipline as well as interdisciplinary courses tackling contemporary s
Middle East research
We conduct research that enhances our understanding of the major issues in the Middle East. The goal is to promote democracy, peace and sustainable development in this dynamic yet unstable region. The Middle East and North Africa (MENA) is a geopolitical region that has experienced significant economic and political change in recent decades. According to the UN, the region’s population is expected
https://www.lunduniversity.lu.se/research-and-innovation/focus-areas/strategic-research-areas/middle-east-research - 2026-05-05
Kulturkriminologi - Masterprogram
Innovative Geophysical Surveys for Contaminated Site Ground Condition Characterisation, Albertslund, Denmark
On the Application of Surface Wave Surveys for Seismic Site Response Evaluation
Popular Abstract in English The work presented here is about methods that will enable more precise estimates of soil and rock parameters related to seismic hazard mapping, in particular when resources are limited. This will allow for evaluating the seismic risk in countries where earthquakes are frequent and large budgets are not available. Particularly, the study of ground response due to the ene
Palynology of Oligocene to middle Miocene sediments from ODP leg 159, site 959 offshore Ivory Coast, equatorial West Africa
Populärvetenskaplig sammanfattning: Tiden mellan 33,9–5,3 miljoner år sedan är indelad i perioderna Oligocen och Miocen. Denna tid karaktäriseras av ett oscillerande klimat som var knutet till de primära så kallade Milankovitchcyklerna – excentricitet hos Jordens bana kring solen, jordaxelns lutning och dess precession – men magnituden hos oscillationerna var mycket varierande. Dinoflagellater äThe Oligocene and Miocene are characterized by a number of climate oscillations, following the primary Milankovitch cycles but varying in magnitude. Dinoflagellates are sensitive environmental indicators as well as biostratigraphic markers, but their use as the former has mainly been restricted to higher latitudes. This palynological study is made on samples belonging to the Oligocene-Miocene inte
Resistivity imaging as a tool in shallow site investigation - A case study
Antibiotic Prophylaxis With Trimethoprim/Sulfamethoxazole Instead of Cloxacillin/Cefotaxime Increases Inguinal Surgical Site Infection Rate After Lower Extremity Revascularization
Folkhälsovetenskap - Masterprogram
The importance of site isolation and phase cooperation in propane ammoxidation on rutile-type vanadia catalysts
Effects of tamoxifen and estradiol on estrogen binding sites in the urogenital tract: an experimental study in the rabbit
Archaeology in Modernity, Two World Heritage Sites in Scandinavia as Cultural Identity?
Energy efficiency at building sites: barriers and drivers
Supplying Production Instruction Knowledge to the Construction Sites
Is street art site-specific?
Interfacial defective Ti3+ on Ti/TiO2 as visible-light responsive sites with promoted charge transfer and photocatalytic performance
The effects of site preparation on carbon fluxes at two clear-cuts in southern Sweden
Popular science The carbon balance of the forest ecosystems is determined by the uptake and release of carbon. Forests take up carbon dioxide (CO2) by photosynthesis and release by respiration. One part of the assimilated carbon is respired back to the atmosphere by vegetation. The other part is respired by soil microbes which decompose organic material in soil. The microbial respiration is contro
