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Tree cores were analyzed at the Institute for Arctic and Alpine Research's Dendrochronology Lab, University of Colorado, Boulder.
After 5884 shots the coated cores were analyzed by means of SEM and energy-dispersive X-ray spectroscopy (EDS).
Nine cores were analyzed using a multi-proxy approach including a range of sedimentological parameters such as granulometry, micropaleontology (foraminifera), radiocarbon dating, and loss on ignition.
Two rejuvenation products were detected by the high-resolution industrial CT scans and the microstructure of the PA concrete cores were analyzed.
Suction and correlation coefficients beneath vortex cores were analyzed to identify the most unfavorable wind direction for saddle roofs, i.e. along the connection of the roof points with the highest elevations.
A total of 3,886 TMA cores were analyzed.
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The research poses special challenges because hydrates form under high pressure, caused by the weight of all the seawater or rock above them, and that pressure must be maintained when the sediment cores are analyzed.
After validating the numerical approach and introducing the computational model, sandwich-walled hollow cylinders with various graded aluminum foam cores are analyzed under air blast loading.
Multistep flow experiments on soil cores are analyzed using either mobile immobile or mobile mobile type 1D dual-porosity models, and a 3D numerical model that considers a local-scale distribution of fragments.
Using this concept, two types of SFR cores are analyzed; the proposed SFR type 1 core has new SFR fuel assemblies at the inner/mid core regions while the proposed SFR type 2 core has a B4C absorber sandwich in the middle of the active core region as well as new SFR fuel assemblies at the inner/mid core regions.
Finally, the size of mature granules and their cores was analyzed.
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