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We present componentry and granulometry data for eight outcroppings of the fall deposit (four on plume axis and four off plume axis).
However, there are important differences amongst models in terms of local properties along the plume axis, particularly for the strong plume.
The stoichiometric KNbO3 films with K/Nb molar ratio of 0.98 were obtained by locating the substrate at an oblique angle of 3 12° from the plume axis.
The novelty of this arrangement is the ability to place by computer-control the substrate synchronously in front of the plume axis compensating the plume deflection effect.
The central axis of deposition is ~ 063° Az; the lateral margins of the fall deposit are massive to unbedded whereas deposits underlying the plume axis feature complex bedding relationships.
Applying Kuo and Hayes's (1991) analytical method, the suspended-sediment concentration and ambient flow velocity measured along plume axis were used to obtain the hydraulic parameters of turbidity plume dispersion.
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The ash sample E4 (EYJA) was collected on 18 May 2010 along the plume dispersal axis at 7.5 km north from the vent as it sedimented from the ash cloud.
The simulation results show that generally, an inclined high-speed gas jet and coal plume are formed along the axis followed by an expansion and recirculation near the wall, resulting in the higher temperature and lower O2 at the lower part of the chamber.
It is found that cross winds significantly reduce the air volume flow rate that is delivered by the up-wind fans, while winds along the longitudinal axis cause increased hot plume air recirculation along the sides of the ACHE bank.
The downward velocities cause oscillation of the fire plume and the flames around the vertical axis.
The results show that in a thermally stratified environment, the axial temperature and velocity of a fire plume decrease more quickly along the vertical axis than in uniform environment, and in some cases the fire plume ceases to rise.
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