Skip to content
  • Submit

  • Category

  • Sort by

  • Per page

Found 9972 publications. Showing page 349 of 399:

Publication  
Year  
Category

The alamar blue assay in the context of safety testing of nanomaterials

The Alamar Blue (AB) assay is widely used to investigate cytotoxicity, cell proliferation and cellular metabolic activity within different fields of toxicology. The use of the assay with nanomaterials (NMs) entails specific aspects including the potential interference of NMs with the test. The procedure of the AB assay applied for testing NMs is described in detail and step-by-step, from NM preparation, cell exposure, inclusion of interference controls, to the analysis and interpretation of the results. Provided that the proper procedure is followed, and relevant controls are included, the AB assay is a reliable and high throughput test to evaluate the cytotoxicity/proliferation/metabolic response of cells exposed to NMs.

2022

The AMAP 2021 assessment

Eckhardt, Sabine; Flanner, Mark; Kupiainen, Kaarle

2020

The ANALYST project: Strengthening the integrated approach of holistic impact assessments for Safe and Sustainable by design plastic value chain

Longhin, Eleonora Marta; Murugadoss, Sivakumar; Olsen, Ann-Karin Hardie; SenGupta, Tanima; Rundén-Pran, Elise; El Yamani, Naouale; Dusinska, Maria; Lago, Ana; Ferreira, G.

2025

The ArcRisk mercury (Hg) case study. NILU F

Sundseth, K.; Pacyna, J.M.; Banel, A.; Pacyna, E.G.

2014

The ArcRisk mercury (Hg) case study.

Sundseth, K.; Pacyna, J.M.; Banel, A.; Pacyna, E.G.

2014

The Arctic tundra and its soil-dwelling springtails (Collembola) reflect nitrogen and contaminants biotransported by seabirds

Kristiansen, Silje Marie; Leinaas, Hans Petter; Herzke, Dorte; Hylland, Ketil; Gabrielsen, Geir W.; Harju, Mikael; Borgå, Katrine

2019

The ASSET intercomparison of stratosphere and lower mesosphere humidity analyses.

Thornton, H. E.; Jackson, D. R.; Bekki, S.; Bormann, N.; Errera, Q.; Geer, A. J.; Lahoz, W. A.,, Rharmili, S.

2009

The Assimilation of Envisat data (ASSET) project.

Lahoz, W.A.; Geer, A.J.; Bekki, S.; Bormann, N.; Ceccherini, S.; Elbern, H.; Errera, Q.; Eskes, H.J.; Fonteyn, D.; Jackson, D.R.; Khattatov, B.; Marchand, M.; Massart, S.; Peuch, V.-H.; Rharmili, S.; Ridolfi, M.; Segers, A.; Talagrand, O.; Thornton, H.E.; Vik, A.F.; von Clarmann, T.

2007

The ASTAR 2007 April 14 haze layer: The radiative effect of an aged and internally mixed aerosol in the Arctic. NILU PP

Engvall, A.-C.; Ström, J.; Tunved, P.; Krejci, R.; Schlager, H.; Minikin, A.

2008

The Atlantic Multidecadal Variability phase-dependence of teleconnection between the North Atlantic Oscillation in February and the Tibetan Plateau in March

The Tibetan Plateau (TP), referred to as the “Asian water tower,” contains one of the largest land ice masses on Earth. The local glacier shrinkage and frozen-water storage are strongly affected by variations in surface air temperature over the TP (TPSAT), especially in springtime. This study reveals that the relationship between the February North Atlantic Oscillation (NAO) and March TPSAT is unstable with time and regulated by the phase of the Atlantic multidecadal variability (AMV). The significant out-of-phase connection occurs only during the warm phase of AMV (AMV+). The results show that during the AMV+, the negative phase of the NAO persists from February to March, and is accompanied by a quasi-stationary Rossby wave train trapped along a northward-shifted subtropical westerly jet stream across Eurasia, inducing an anomalous adiabatic descent that warms the TP. However, during the cold phase of the AMV, the negative NAO cannot persist into March. The Rossby wave train propagates along the well-separated polar and subtropical westerly jets, and the NAO–TPSAT connection is broken. Further investigation suggests that the enhanced synoptic eddy and low-frequency flow (SELF) interaction over the North Atlantic in February and March during the AMV+, caused by the southward-shifted storm track, helps maintain the NAO pattern via positive eddy feedback. This study provides a new detailed perspective on the decadal variability of the North Atlantic–TP connection in late winter to early spring.

2021

The Atmosphere Above Ny-Ålesund: Climate and Global Warming, Ozone and Surface UV Radiation

Maturilli, Marion; Hanssen-Bauer, Inger; Neuber, Roland; Rex, Markus; Edvardsen, Kåre

2019

The atmospheric fate of 1,2-dibromo-4-(1,2-dibromoethyl)cyclohexane (TBECH): spatial patterns, seasonal variability, and deposition to Canadian coastal regions

Brominated flame retardants (BFRs) that are gradually being phased out are being replaced by emerging BFRs. Here, we report the concentration of the α- and β-isomers of 1,2-dibromo-4-(1,2-dibromoethyl)cyclohexane (TBECH; also known as DBE-DBCH) in over 300 air, water, and precipitation samples collected between 2019 and 2022 using active air and deposition sampling as well as networks of passive air and water samplers. The sampling region includes Canada's most populated cities and areas along the St. Lawrence River and Estuary, Quebec, as well as around the Salish Sea, British Columbia. TBECH was detected in over 60 % of air samples at levels comparable to those of 2,2′,4,4′-tetrabromodiphenyl ether (BDE-47). Concentrations of TBECH and BDE-47 were typically higher in urban areas, with stronger correlations with population density during warmer deployments. Uniform α-  β-TBECH ratios across space, time, and environmental media indicate the highly similar atmospheric fate of the two isomers. Although TBECH air concentrations were strongly related to temperature in urban Toronto and a remote site on the east coast, the lack of such dependence at a remote site on the west coast can be explained by the small seasonal temperature range and summertime air mass transport from the Pacific Ocean. Despite there being no evidence that TBECH has been produced, or imported for use, in Canada, it is now one of the most abundant gaseous BFRs in the Canadian atmosphere. The recorded spatial and temporal variability of TBECH suggest that its emissions are not constrained to specific locations but are generally tied to the presence of humans. The most likely explanation for its environmental occurrence in Canada is the release from imported consumer products containing TBECH. Chiral analysis suggests that despite its urban origin, at least some fraction of TBECH has experienced enantioselective processing, i.e., has volatilized from reservoirs where it has undergone microbial transformations. Microbial processes in urban soils and in marine waters may have divergent enantioselectivity.

2023

The Atmospheric Fate of TBECH: Spatial Patterns, Seasonal Variability, and Deposition to Canadian Coastal Regions

Oh, Jenny; Zhan, Faqiang; Li, Yuening; Shunthirasingham, Chubashini; Lei, Ying Duan; Dalpé-Castilloux, Abigaëlle; Lu, Zhe; Lee, Kelsey; Gobas, Frank; Eckhardt, Sabine; Alexandrou, Nick; Hung, Hayley; Wania, Frank

2023

The BEEP Stavanger Workshop: Mesocosm exposures.

Sundt, R.C.; Pampanin, D.M.; Larsen, B.K.; Brede, C.; Herzke, D.; Bjørnstad, A.; Andersen, O.K.

2006

Publication
Year
Category