摘 要: | This paper reviews the opportunities for microgravity and Earth-based measurements of the thermal conductivityλ(t, L) of4He confined in cylindrical geometries of radiusL with axial heat flow at temperatures near the bulk superfluid-transition lineT
λ
(P) (t is the reduced temperatureT/T
λ
−1). It provides an evaluation of existing data forL=1 μm nearT
λ
at saturated vapor pressure (SVP), and uses these to derive a scaling function for the resistivityR(t, L)=1/λ(t, L). The purpose of future measurements over a wide range ofL and of the pressureP will be to test the applicability of this function. In the present paper the scaling function is used to assess quantitatively
the effect of gravity on potential Earth-based measurements. It is found that the gravity effect forR is particularly severe belowT
λ
. For typical three-mm-high samples at SVP, values ofL significantly larger than 8 μm can only be investigated fully in micro-gravity. At higher pressures the gravity effect is
larger. At 30 bar, three-mm samples withL≳4 μm require microgravity for measurements belowT
λ
(P). Modern thermometry has sufficient resolution to permit quantitative measurements in micro-gravity of the anticipated finite-size
effect for values ofL as large as 50 μm.
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