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Macro- and micro-electrochemical properties of clad and core surfaces of a modified AA4xxx/AA3xxx brazing sheet material, before and after brazing, have been evaluated and compared.
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Discrete samples for paleo- and rock magnetic measurements were taken sequentially from the half-split core surfaces using plastic cubes of 7 cm3 each.
A relatively lower indium signal in InN x microcones is probably due to nonuniform radial distribution of In and N in the micron-size cone with more N expected from core surface attachment of N in vapor.
In the process of spontaneous imbibition, low salinity water penetrated into the porous media and altered the wettability of core surface by desorption of ions which were attached to the core surface.
Animation of the geographical distribution of the core surface radial component of the sub-centennial constituent.
As the core flow is plausibly in the TG balance over a large area of the core surface, a majority of the non-geostrophic SV should not originate from the advection of radial MF by the ageostrophic flow.
Fig. 4 Time Latitude plots of the core surface radial component of the sub-centennial constituent for selected longitudes.
Fig. 5 Latitude-azimuthal-speed power plot of the core surface radial component of the sub-centennial constituent.
Fig. 2 Time Longitude plots of the core surface radial component of the sub-centennial constituent for selected middle-high latitudes.
Movement direction is highlighted by straight line segments Fig. 3 Time Longitude plots of the core surface radial component of the sub-centennial constituent for selected low-middle latitudes.
This paper studied core geometry of convex cross-section shape to increase neutron leakage from core surface in case of core compaction.
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