CONDENSATION OF SUPERSATURATED He4 VAPOR IN A CLOUD CHAMBER

1960 ◽  
Vol 38 (3) ◽  
pp. 335-345 ◽  
Author(s):  
M. H. Edwards ◽  
W. C. Woodbury

The critical supercooling, ΔTc, required to produce visible condensation in pressure-limited adiabatic expansions of presumably ion-free saturated He4 vapor has been measured in a small glass cloud chamber. The transient gas temperatures were measured during expansions by using a carbon resistance thermometer in a Wheatstone bridge. An oscilloscope was used in place of a galvanometer, and its trace was photographed during expansions. Low-amplitude temperature oscillations in the gas, which might not normally have been detected, were frequently observed in the early stages of this work. These oscillations either appeared spontaneously ("Taconis Resonances"), or could be shock-excited by an expansion. These oscillations were subsequently eliminated. Condensation thresholds were then measured using starting temperatures from 4.2 to 1.7 °K. ΔTc dropped from about 50 to 60 mdeg above the λ point to less than 20 mdeg below the λ point. The critical supersaturations required to produce condensation were thus always less than 105%. The supersaturations were calculated without making the usual, but highly implausible, assumption that the expanding gas is ideal. Assuming that the condensation nuclei are embryonic droplets arising accidentally from density fluctuations in the supersaturated vapor, the critical droplet radius is found to be about 10−6 cm above 2.5 °K, although the theoretical treatment here is not rigorous.

1966 ◽  
Vol 21 (9) ◽  
pp. 1348-1351
Author(s):  
A. Lodding

A theoretical treatment is given of the recently discovered thermotransport effect in pure liquid metals. The isotope effect is related to the diffusive mass flow by a proportionality factor familiar from electrotransport. The mass flow is given primarily by the temperature dependence of the mean size or amount of density fluctuations in the liquid. Very little activation energy is required for diffusive motion, which takes place by cooperative position adjustments of neighbor atoms. The mean displacement length of the diffusing cluster is by an order of magnitude smaller than the effective cluster diameter. The liquid model suggested is coherent with models based on evidence from other experimental methods.


1957 ◽  
Vol 38 (7) ◽  
pp. 391-394
Author(s):  
George L. Mason

A resistance-thermometer system is described which permits simultaneous and continuous recording of air temperatures at a number of separated points. Unbalance current in a Wheatstone bridge network is used as the measure of temperature, and is recorded by a multichannel light-beam oscillograph. The lag coefficient of the system is approximately 0.1 second.


1993 ◽  
Vol 412 ◽  
pp. L51 ◽  
Author(s):  
Stephane Courteau ◽  
S. M. Faber ◽  
Alan Dressler ◽  
Jeffrey A. Willick

2019 ◽  
Author(s):  
Steven K. Krueger

Abstract. In a laboratory cloud chamber that is undergoing Rayleigh-Bénard convection, supersaturation is produced by isobaric mixing. When aerosols (cloud condensation nuclei) are injected into the chamber at a constant rate, and the rate of droplet activation is balanced by the rate of droplet loss, an equilibrium droplet size distribution (DSD) can be achieved. We derived analytic equilibrium DSDs and PDFs of droplet radius and squared radius for conditions that could occur in such a turbulent cloud chamber when there is uniform supersaturation. The loss rate due to fall out that we used assumes that (1) the droplets are well-mixed by turbulence, (2) when a droplet becomes sufficiently close to the lower boundary, the droplet’s terminal velocity determines its probability of fall out per unit time, and (3) a droplet’s terminal velocity follows Stokes’ Law (so it is proportional to its radius squared). Given the chamber height, the analytic PDF is determined by the mean supersaturation alone. From the expression for the PDF of the radius, we obtained analytic expressions for the first five moments of the radius, including moments for truncated DSDs. We used statistics from a set of measured DSDs to check for consistency with the analytic PDF. We found consistency between the theoretical and measured moments, but only when the truncation radius of the measured DSDs was taken into account. This consistency allows us to infer the mean supersaturations that would produce the measured PDFs in the absence of supersaturation fluctuations. We found that accounting for the truncation radius of the measured DSDs is particularly important when comparing the theoretical and measured relative dispersions of the droplet radius. We also included some additional quantities derived from the analytic DSD: droplet sedimentation flux, precipitation flux, and condensation rate.


1969 ◽  
Vol 24 (10) ◽  
pp. 1226-1234 ◽  
Author(s):  
E. Nebrich ◽  
H. Mohrmann

Saturated ethanol vapour in an atmosphere of nitrogen was expanded in a cloud chamber. The condensation arising thereby was shown by light scattering. At the same time the temperature curve occurring after the expansion was measured by means of a resistance thermometer.Experiments with twenty different expansion ratios (from E=1,083 to E= 1,324) were carried out at room temperature. The expansions were polytropic at n = 1,24.Supersaturations were obtained at about 1,3 and 1,5 regardless of E and never attained the critical value of 2,1. Nevertheless a condensation was shown every time, although nuclei were not present. The cloud vanished shortly after its appearence, long before the initial temperature could be reached again. The formation as well as start and finish of the evaporation of this “subcritical fog” can be traced exactly in the registered temperature curves. The simultaneous light scatteringand temperature measurement make a stronger interpretation of the temperature curves recorded by STACHORSKA also possible.


2002 ◽  
Vol 58 (3) ◽  
pp. 361-371 ◽  
Author(s):  
Ida M. Berstad ◽  
Joyce Lundberg ◽  
Stein-Erik Lauritzen ◽  
Henriette C. Linge

AbstractA stalagmite from northern Norway is dated with 12 thermal ionization mass spectrometry U-Th dates, and at least four separate growth periods are identified that correspond with marine isotope stages 9, 11, 13, and probably 15. The calcite is tested for isotopic equilibrium with the Hendy test. Oxygen isotope measurements on 231 subsamples on a vertical transect are used as a paleotemperature proxy. The detailed isotopic record from MIS 9 show apparent similarities to a Holocene record from the same cave, both in the climatic evolution and the overall temperatures: both show temperature oscillations changing from high-frequency, low-amplitude cycles in the beginning of the interglacial period to lower frequency, higher amplitude cycles in the later part of the interglacial period. The isotope record from MIS 11 shows a distinct isotopic event toward heavier values. The isotopic record together with the porous, humus-rich calcite are interpreted as indicating a warmer than present interglacial period with several episodes of heavy rainfall.


2020 ◽  
Vol 20 (13) ◽  
pp. 7895-7909
Author(s):  
Steven K. Krueger

Abstract. In a laboratory cloud chamber that is undergoing Rayleigh–Bénard convection, supersaturation is produced by isobaric mixing. When aerosols (cloud condensation nuclei) are injected into the chamber at a constant rate, and the rate of droplet activation is balanced by the rate of droplet loss, an equilibrium droplet size distribution (DSD) can be achieved. We derived analytic equilibrium DSDs and probability density functions (PDFs) of droplet radius and squared radius for conditions that could occur in such a turbulent cloud chamber when there is uniform supersaturation. We neglected the effects of droplet curvature and solute on the droplet growth rate. The loss rate due to fallout that we used assumes that (1) the droplets are well-mixed by turbulence, (2) when a droplet becomes sufficiently close to the lower boundary, the droplet's terminal velocity determines its probability of fallout per unit time, and (3) a droplet's terminal velocity follows Stokes' law (so it is proportional to its radius squared). Given the chamber height, the analytic PDF is determined by the mean supersaturation alone. From the expression for the PDF of the radius, we obtained analytic expressions for the first five moments of the radius, including moments for truncated DSDs. We used statistics from a set of measured DSDs to check for consistency with the analytic PDF. We found consistency between the theoretical and measured moments, but only when the truncation radius of the measured DSDs was taken into account. This consistency allows us to infer the mean supersaturations that would produce the measured PDFs in the absence of supersaturation fluctuations. We found that accounting for the truncation radius of the measured DSDs is particularly important when comparing the theoretical and measured relative dispersions of the droplet radius. We also included some additional quantities derived from the analytic DSD: droplet sedimentation flux, precipitation flux, and condensation rate.


Author(s):  
Feng Tsai ◽  
J. M. Cowley

Reflection electron microscopy (REM) has been used to study surface defects such as surface steps, dislocations emerging on crystal surfaces, and surface reconstructions. However, only a few REM studies have been reported about the planar defects emerging on surfaces. The interaction of planar defects with surfaces may be of considerable practical importance but so far there seems to be only one relatively simple theoretical treatment of the REM contrast and very little experimental evidence to support its predications. Recently, intersections of both 90° and 180° ferroelectric domain boundaries with BaTiO3 crystal surfaces have been investigated by Tsai and Cowley with REM.The REM observations of several planar defects, such as stacking faults and domain boundaries have been continued by the present authors. All REM observations are performed on a JEM-2000FX transmission electron microscope. The sample preparations may be seen somewhere else. In REM, the incident electron beam strikes the surface of a crystal with a small glancing angle.


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