Voorbeelden van buoyancy

• I rise, gaining buoyancy as air fills my lungs.

• The weight of the cargo affected the buoyancy of the vehicle.

• The ball's buoyancy pulled him back up to the surface.

• Book publishers reported buoyancy in the 24+ age group market.

• The trend has been driven by buoyancy in stock market prices.

• Buoyancy in New York also helped the FTSE 100 index.

• Europe's economy has drawn much of its buoyancy from growing exports.

• She was normally subdued, but today she radiated buoyancy.

• This catchy track has a happy buoyancy.

• His buoyancy had not been punctured by any of these events.

• This gradient, established and maintained by the surface buoyancy flux through the process of turbulent convection, is what draws fluid in from the external reservoir.

• At a certain depth, the heaters are turned on, and the robot ascends due to its now positive buoyancy, resulting from its reduced density.

• The results obtained by using that formula were compared with the total static buoyancy force exerted on the caudal fluid column.

• The function of lipids within the intramolluscan stages is speculative and suggested functions are buoyancy, energy reserves, metabolic waste products, and others.

• The detached amphibolitized oceanic crust may then return to shallow depths as a result of its positive buoyancy against the denser surrounding mantle.

• The magnetic mechanism predominates over the buoyancy mechanism in fluid layers about 1 mm thick.

• It also shows the hot fluid moving around the circumference of the cylinder under the influence of the non-axial component of buoyancy force.

• This will no longer hold if buoyancy effects are sufficiently strong to create a gravity tongue, such as in the reference flow discussed above.

• This may be followed by a (previously investigated) purely inertial phase, wherein the buoyancy force of the intruding fluid is balanced by the inertial force.

• Lithospheric buoyancy and collisional orogenesis: subduction of oceanic plateaus, continental margins, island arcs, spreading ridges, and seamounts.

• However, in both numerical and laboratory experiments, the phenomenon of buoyancy spreading due to localized baroclinic vortices is clearly observed.

• The fluid will be accelerated by buoyancy forces alone and balancedessentially by viscous shear forces.

• The buoyancy falls essentially to zero at a height of 704m and goes negative at a height of about 1400.

• In the foregoing equations for two-layer flows with surface buoyancy flux, it is equation (14) which governs the dynamics of the system.

• The limited horizontal extent of the forcing results in a buoyancy gradient across the sill and an associated circulation.