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DSC - polymer thermal analysis - Raw and processed data and image
The .txt files contains the raw differential scanning calorimetry (DSC) data for the P(DMAA-co-MABP) copolymer foil, measured using a DSC 3 system. The experiment was conducted... -
Physical oceanography, nutrients, and δ¹⁸O measured on water bottle samples d...
Extremely low summer sea-ice coverage in the Arctic Ocean in 2007 allowed extensive sampling and a wide quasi-synoptic hydrographic and d18O dataset could be collected in the... -
Replication Data for: Temperature dependence of the mutation rate towards ant...
Environmental conditions can influence mutation rates in bacteria. Fever is a common response to infection that alters the growth conditions of infecting bacteria. Here we... -
Southern Ocean moored time series (south of 60°S) (OCEAN ICE D1.1)
This mooring timeseries compilation contains temperature, salinity, current velocity measured from a wide range of marine instrument in the Southern Ocean (90°S-60°S) since... -
Role of powders and coatings - preliminary data
New dataset see relations. Provided data: Folder: Catalyst state and conversion - XAS -XAS: Columns within the files: 1) Energy (DCM_2Pitch) 2) Detector before sample (Ioni1) 3)... -
Replication Data for: Temperature affects the impact of anthropogenic light o...
These data form the basis for the paper titled 'Temperature affects the impact of anthropogenic light on bat activity' by Sander WJ Buddendorf, Marcel E Visser and Kamiel... -
An updated synthesis of ocean total alkalinity and dissolved inorganic carbon...
Since 2004, the Service facility SNAPO-CO2 (Service National d’Analyse des Paramètres Océaniques du CO2) housed by the LOCEAN laboratory (Paris, France) has been in charge for... -
A synthesis of ocean total alkalinity and dissolved inorganic carbon measurem...
Since 2004, the Service facility SNAPO-CO2 (Service National d’Analyse des Paramètres Océaniques du CO2) housed by the LOCEAN laboratory (Paris, France) has been in charge for... -
Input files for the 2-D cases of the ASPECT models of a mantle plume and csv ...
In order to understand the difference between high temperature drop across the mantle's basal thermal boundary layer and much lower plume excess temperatures we evaluated... -
Measurements of wind, temperature, pressure and humidity during the ascending...
Altitude (geopotential) is calculated from measured atmospheric static pressure, where the offset in the original data due to the reference pressure at departure was corrected... -
Measurements of wind, temperature, pressure and humidity during the ascending...
Altitude (geopotential) is calculated from measured atmospheric static pressure, where the offset in the original data due to the reference pressure at departure was corrected... -
Measurements of wind, temperature, pressure and humidity during the descendin...
Altitude (geopotential) is calculated from measured atmospheric static pressure, where the offset in the original data due to the reference pressure at departure was corrected... -
Measurements of wind, temperature, pressure and humidity during the ascending...
Altitude (geopotential) is calculated from measured atmospheric static pressure, where the offset in the original data due to the reference pressure at departure was corrected... -
Measurements of wind, temperature, pressure and humidity during the descendin...
Altitude (geopotential) is calculated from measured atmospheric static pressure, where the offset in the original data due to the reference pressure at departure was corrected... -
Measurements of wind, temperature, pressure and humidity during the ascending...
Altitude (geopotential) is calculated from measured atmospheric static pressure, where the offset in the original data due to the reference pressure at departure was corrected... -
Measurements of wind, temperature, pressure and humidity during the descendin...
Altitude (geopotential) is calculated from measured atmospheric static pressure, where the offset in the original data due to the reference pressure at departure was corrected... -
Measurements of wind, temperature, pressure and humidity during the ascending...
Altitude (geopotential) is calculated from measured atmospheric static pressure, where the offset in the original data due to the reference pressure at departure was corrected... -
Measurements of wind, temperature, pressure and humidity during the ascending...
Altitude (geopotential) is calculated from measured atmospheric static pressure, where the offset in the original data due to the reference pressure at departure was corrected... -
Measurements of wind, temperature, pressure and humidity during the descendin...
Altitude (geopotential) is calculated from measured atmospheric static pressure, where the offset in the original data due to the reference pressure at departure was corrected... -
Measurements of wind, temperature, pressure and humidity during the ascending...
Altitude (geopotential) is calculated from measured atmospheric static pressure, where the offset in the original data due to the reference pressure at departure was corrected...