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31.
A new Monte Carlo method for calculating ground-state properties of liquid 4He is described. It is shown that Bose-Einstein condensation (BEC) implies delocalization of the wave function. It is shown that there is no general connection between the static structure factor and BEC. It is suggested that the observed connection in liquid 4He is due to the creation of spaces in the liquid structure, which are required so that the wave function can delocalize, in the presence of the hard-core interactions. It is shown that this suggestion is quantitatively consistent with observations on liquid 4He. 相似文献
32.
We study the flow of yield stress fluids over a rotating surface when both the viscoelastic solid behavior below a critical
deformation (γ
c) and liquid properties beyond γ
c can play a significant role. We review the detailed characteristics of the flow in the solid regime in the specific case
of a pure elongational strain (large height to radius ratio). We, in particular, show that there exists a critical rotation
velocity (ω
c) associated with the transition from the solid to the liquid regime. We then consider the specific case of lubricational
regime (small height to radius ratio) in the liquid regime. In that case we describe the different possible evolutions of
the equilibrium shape of the material as a function of the rotation velocity (ω), from which we extrapolate the transient shape evolutions as ω increases. We show that for a sufficiently large rotation velocity the sample separates into two parts, one remaining at
rest around the rotation axis, the other going on moving radially. These predictions are then compared with systematic spin-coating
tests under increasing rotation velocity ramps followed by a plateau at ω
f with typical yield stress fluids. It appears that there exists a critical velocity below which the material undergoes a limited
elongation and beyond which it starts to spread significantly over the solid surface. For a larger ω
f value the sample forms a thick peripheral roll, leaving behind it a thin layer of fluid at rest relatively to the disc. These
characteristics are in qualitative agreement with the theoretical predictions. Beyond a sufficiently large ω
f value this roll eventually spreads radially in the form of thin fingers. Moreover, in agreement with the theory in the lubricational
regime, the different curves of deformation vs ω fall along a master curve when the rotation velocity is scaled by ω
c for different accelerations, different sample radii, or different material yield stress. The final thickness of the deposit
seems to be mainly governed by the displacement of the roll, the characteristics of which take their origin in the initial
stage of the spreading, including the solid–liquid transition. 相似文献
33.
Structural Similarity and Transition from Newtonian to Non-Newtonian Behavior for Clay-Water Suspensions 总被引:1,自引:0,他引:1
Coussot P 《Physical review letters》1995,74(20):3971-3974