130 research outputs found
Applicability of Boussinesq approximation in a turbulent fluid with constant properties
The equations of motion describing buoyant fluids are often simplified using
a set of approximations proposed by J. Boussinesq one century ago. To resume,
they consist in assuming constant fluid properties, incompressibility and
conservation of calories during heat transport. Assuming fulfilment of the
first requirement (constant fluid properties), we derive a set of 4 criteria
for assessing the validity of the two other requirements in turbulent
Rayleigh-B\'enard convection. The first criterion simply
results from the incompressibility condition in the thermal boundary layer
( and are the thermal expansion coefficient and the
temperature difference driving the flow). The 3 other criteria are proportional
or quadratic with the density stratification or, equivalently with the
temperature difference resulting from the adiabatic gradient across the cell
. Numerical evaluations with air, water and cryogenic helium show
that most laboratory experiments are free from such Boussinesq violation as
long as the first criterion is fulfilled. In ultra high Rayleigh numbers
() experiments in He, one of the stratification criteria, scaling
with , could be violated. This criterion garanties that
pressure fluctuations have a negligible influence both on the density variation
and on the heat transfer equation through compression/expansion cycles.
Extrapolation to higher suggests that strong violation of Boussinesq
approximation could occur in atmospheric convection.Comment: Submitted to Phys.Fluids (oct 2007
Energy cascade and the four-fifths law in superfluid turbulence
The 4/5-law of turbulence, which characterizes the energy cascade from large
to small-sized eddies at high Reynolds numbers in classical fluids, is verified
experimentally in a superfluid 4He wind tunnel, operated down to 1.56 K and up
to R_lambda ~ 1640. The result is corroborated by high-resolution simulations
of Landau-Tisza's two-fluid model down to 1.15 K, corresponding to a residual
normal fluid concentration below 3 % but with a lower Reynolds number of order
R_lambda ~ 100. Although the K\'arm\'an-Howarth equation (including a viscous
term) is not valid \emph{a priori} in a superfluid, it is found that it
provides an empirical description of the deviation from the ideal 4/5-law at
small scales and allows us to identify an effective viscosity for the
superfluid, whose value matches the kinematic viscosity of the normal fluid
regardless of its concentration.Comment: 6 pages, 7 figure
Investigation of intermittency in superfluid turbulence
International audienceThis paper reports new experimental and simulation velocity data for superfluid steady turbulence above 1 K. We present values for the scaling exponent of the absolute value of velocity-increment structure functions. In both experiments and simulations, they evidence that intermittency occurs in superfluid flows in a quite comparable way to classical turbulence. In particular, the deviation from Kolmogorov 1941 keeps the same strength as we cross the superfluid transition. To the best of our knowledge, this is the first confirmation of the superfluid 4He experimental results from Maurer et al. EPL 1998 and the first numerical evidence of intermittency in superfluid turbulence
Evidence of a boundary layer instability at very high Rayleigh number
In 1997, a Rayleigh-B\'enard experiment evidenced a significant increase of
the heat transport efficiency for Rayleigh numbers larger than and interpreted this observation as the signature of the Kraichnan's
``Ultime Regime'' of convection. According to Kraichnan's 1962 prediction, the
flow boundary layers above the cold and hot plates -in which most of the fluid
temperature drop is localized- become unstable for large enough and this
instability boosts the heat transport compared to the other turbulent regimes.
Using the same convection cell as in the 1997 experiment, we show that the
reported heat transport increase is accompanied with enhanced temperature
fluctuations of the bottom plate, which was heated at constant power levels.
Indeed, for , the bottom plate fluctuations can simply be
accounted from those in the bulk of the flow. In particular, they share the
same spectral density at low frequencies, as if the bottom plate was following
the slow temperature fluctuations of the bulk, modulo a constant temperature
drop across the bottom boundary layer. Conversely, to account for the plate's
temperature fluctuations at higher , we no-longuer can ignore the
fluctuations of the temperature drop across the boundary layer. The negative
skewness of fluctuations at high supports the picture of a boundary layer
instability. These observations provide new evidence that the transition
reported in 1997 corresponds to the triggering of the Ultimate Regime of
convection.Comment: Submitted for publicatio
Comment on "Turbulent heat transport near critical points: Non-Boussinesq effects" (cond-mat/0601398)
In a recent preprint (cond-mat/0601398), D. Funfschilling and G. Ahlers
describe a new effect, that they interpret as non-Boussinesq, in a convection
cell working with ethane, near its critical point. They argue that such an
effect could have spoiled the Chavanne {\it et al.} (Phys. Rev. Lett. {\bf 79}
3648, 1997) results, and not the Niemela {\it et al.} (Nature, {\bf 404}, 837,
2000) ones, which would explain the differences between these two experiments.
We show that:-i)Restricting the Chavanne's data to situations as far from the
critical point than the Niemela's one, the same discrepancy remains.-ii)The
helium data of Chavanne show no indication of the effect observed by D.
Funfschilling and G. Ahlers.Comment: comment on cond-mat/060139
Thixotropic behaviour of paving grade bitumens under dynamic shear
A material exhibits a thixotropic behaviour if its apparent viscosity decreases in time under stress, and if it progressively recovers its initial viscosity when the stress is released. Methods for characterizing thixotropy for fluids are relatively well known, the situation is more difficult for viscoelastic materials. For bituminous binders, it corresponds to a decrease of material stiffness under cyclic loading by modification of its internal structure and to a recovery of this stiffness after rest. This property has been highlighted by simple shear tests, carried out using a controlled stress rheometer. An experimental procedure has been defined for studying the thixotropic behaviour of binders in dynamic mode. Then, it has allowed describing the corresponding curves of complex modulus versus the set stress and the rest period at different conditioning times of samples. This study has also permitted to demonstrate that stiffness variations are linked to re-arrangement of molecular structure and not to cracks formation and healing. Finally, based on specific indicators, it has been possible to compare different bituminous binders in order to estimate the ability of materials to restore their internal structures
Vorticity scattering measurements in a superfluid inertial round jet
International audienceThe aim of this proceeding paper is twofold. First, we present a newly developed cryogenic testing facility where a steady high Reynolds liquid helium inertial round jet flow is generated allowing to address classical turbulence issues, such as statistical intermittency, and quantum turbulence when the facility is operating in superfluid helium. Secondly we present the first spatial Fourier vorticity modes measurements made both above and below the superfluid transition at different nozzle velocities. These preliminary results were obtained by probing the vorticity flow-field with the ultrasonic scattering technique
Prandtl and Rayleigh numbers dependences in Rayleigh Bénard convection
International audienceUsing low-temperature gaseous helium close to the critical point, we investigate the Prandtl-number dependence of the effective heat conductivity (Nusselt number) for a 1/2 aspect ratio Rayleigh-Bénard cell. Very weak dependence is observed in the range 0.7 < Pr < 21; 2 × 10^8 < Ra < 2 × 10^10: the absolute value of the average logarithmic slope δ = (∂ln Nu/∂ln Pr)Ra is smaller than 0.03. A bimodality of Nu, with 7% difference between the two sets of data, is observed, which could explain some discrepancies between precise previous experiments in this range
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