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CONDUCTION

the “ Guard-Ring” method, hut it is generally rather difficult to determine the effective area of the ring. There is little difficulty in measuring the time of flow, provided that it is not too short. The measurement of the temperature gradient in the plate generally presents the greatest difficulties. If the plate is thin, it is necessary to measure the thickness with great care, and it is necessary to assume that the temperatures of the surfaces are the same as those of the media with which they are in contact, since there is no room to insert thermometers in the plate itself. This assumption does not present serious errors in the case of bad conductors, such as glass or wood, but has given rise to large mistakes in the case of metals. The conductivities of thin slices of crystals have been measured by Lees by pressing them between plane amalgamated surfaces of metal. This gives very good contact, and the conductivity of the metal being more than 100 times that of the crystal, the temperature of the surface is determinate. In applying the plate method to the determination of the conductivity of iron, Hall has recently succeeded in overcoming this difficulty by coating the plate thickly with copper on both sides, and deducing the difference of temperatijre between the two surfaces of junction of the iron and the copper from the thermo-electric force observed by means of a number of fine copper wires attached to the copper coatings at different points of the disc. The advantage of the thermo-junction for this purpose is that the distance between the surfaces of which the temperaturedifference is measured, is very exactly defined. The disadvantage is that the thermo-electric force is very small, about ten-millionths of a volt per degree, so that a small accidental disturbance may produce a serious error with a difference of temperature of only 1° between the junctions. The chief uncertainty in applying this method appears to have arisen from variations of temperature at different parts of the surface, due to inequalities in the heating or cooling effect of the stream of water flowing over the surfaces. Uniformity of temperature could only be secured by using a high velocity of flow, or violent stirring. Neither of these methods could be applied in this experiment. The temperatures indicated by the different pairs of wires differed by as much as 10 per cent., but the mean of the whole would probably give a fair average. The heat transmitted was measured by observing the flow of water (about 20 gm./sec.), and the rise of temperature (about 0‘5° C.) in one of the streams. The results appear to be entitled to considerable weight on account of the directness of the method, and the full consideration of possible errors. They were as follows:— Cast-iron, & = 0*1490 C.G.S. at 30° C., temp. coef. -0*00075. Pure iron, &=0*1530 at 30° C., temp. coef. -0*0003. The discs were 10 cms. in diam., and nearly 2 cms. thick, plated with copper to a thickness of 2 mm. The cast-iron contained about 3*5 per cent, of carbon, 1*4 per cent, of silicon, and 0*5 per cent, of manganese. 7. Tube Method.—If the inside of a glass tube is exposed to steam, and the outside to a rapid current of water, or vice versd, the temperatures of the surfaces of the glass may be taken to be very approximately equal to those of the water and steam, which may be easily observed. If the thickness of the glass is small compared with the diameter of the tube, say one-tenth, equation (1) may be applied with sufficient approximation, the area A being taken as the mean between the internal and external surfaces. It is necessary that the thickness x should be approximately uniform. Its mean value may be determined most satisfactorily from the weight and the density. The heat Q transmitted in a given time T may be deduced from an observation of the rise of temperature of the water, and the amount which passes in the interval. This is one of the simplest of all methods in practice, but it involves the measurement of several different quantities, some of which are difficult to observe accurately. The employment of the tube form evades one of the chief difficulties of the plate method, namely, the uncertainty of the flow at the boundary of the area considered. Unfortunately the method cannot be applied to good conductors, like the metals, because the difference of temperature between the surfaces may be five or ten times less than that between the water and steam in contact with them, even if the water is energetically stirred. 8. Cylinder Method.—A variation of the tube method, which can be applied to metals and good conductors, depends on the employment of a thick cylinder with a small axial hole in place of a thin tube. The actual temperature of the metal itself can then be observed by inserting thermometers or thermo-couples at measured distances from the centre. This method has been applied by Callendar and Nicolson {Brit. Assoc. Report, 1897), to cylinders of cast-iron and mild steel, 5 inches in diam. and 2 feet long, with one-inch axial holes. The surface of the central hole was heated by steam under pressure, and the total flow of heat was determined by observing the amount of steam condensed in a given time. The outside of the cylinder was cooled by water

OF

HEAT

circulating in a spiral screw thread in a very narrow space with high velocity under a pressure of 120 R> per square inch. A very uniform surface temperature was thus obtained. The lines of flow in this method are radial. The isothermal surfaces are coaxial cylinders. The areas of successive surfaces vary as their radii, hence the rate of transmission QjA T varies inversely as the radius r, and is Q^lirrlT, if l is the length of the cylinder, and § the total heat, calculated from the condensation of steam observed in a time T. The outward gradient is ddjdr, and is negative if the central hole is heated. We have therefore the simple equation— -kd6ldr=Ql2irrlT. (2) If k is constant the solution is evidently, 0 = a log r + b, where a= — <2/2 irklT, and b and k are determined from the known values of the temperatures observed at any two distances from the axis. This gives an average value of the conductivity over the range, but it is better to observe the temperatures at three distances, and to assume k to be a linear function of the temperature, in which case the solution of the equation is still very simple, namely— d+ e92l2=a log r + b, (3) where e is the temperature-coefficient of the conductivity. The chief difficulty in this method lay in determining the effective distances of the bulbs of the thermometers from the axis of the cylinder, and in ensuring uniformity of flow of heat along different radii. For these reasons the temperature-coefficient of the conductivity could not be determined satisfactorily on this particular form of apparatus, but the mean results were probably trustworthy to 1 or 2 per cent. They refer to a temperature of about 60° C., and were— Cast-iron, 0*109; mild steel, 0*119, C.G.S. These are much smaller than Hall’s results. The cast-iron contained nearly 3 per cent, each of silicon and graphite, and 1 per cent, each of phosphorus and manganese. The steel contained less than 1 per cent, of foreign materials. The low value for the cast-iron was confirmed by two entirely different methods given below. 9. Forbes's Bar Method.—Observation of the steady distribution of temperature along a bar heated at one end was very early employed by Fourier, Despretz, and others for the comparison of conductivities. It is the most convenient method in the case of good conductors on account of the great facilities which it permits for the measurement of the temperature gradient at different points, but it has the disadvantage that the results depend almost entirely on a knowledge of the external heat loss or emissivity, or, in comparative experiments, on the assumption that it is the same in different cases. The method of Forbes (in which the conductivity is deduced from the steady distribution of temperature on the assumption that the rate of loss of heat at each point of the bar is the same as that observed in an auxiliary experiment in which a short bar of the same kind is set to cool under conditions which are supposed to be identical), is too well known to require detailed description, but a consideration of its weak points is very instructive, and the results have been most remarkably misunderstood and misquoted. The method gives directly, not k, but kjc. Tait repeated Forbes’s experiments, using one of the same iron bars, and endeavoured to correct his results for the variation of the specific heat c. Mitchell, under Tait’s direction, repeated the experiments with the same bar nickel-plated, correcting the thermometers for stem-exposure, and also varying the conditions by cooling one end, so as to obtain a steeper gradient. The results of Forbes, Tait, and Mitchell, on the same bar, and Mitchell’s two results by different methods, are quoted by Landoldt and Bornstein as if they referred to different metals. This is not very surprising, if the values in the following table are compared:— Table I. Thermal Conductivity of Forbes's Iron Bar D (1*25 Inches Square). C.G.S. Units. Temp. Cent. 0° 100° 200°

Uncorreeted for Variation of c. Forbes. Tait.
 * 207
 * 157
 * 136


 * 231
 * 198
 * 176

Mitchell: Cooled. •197 •178 •160

•178 •190 •181

Corrected for Variation of c. Forbes. Tait. •213 •168 •152

•238 •212 •196

Mitchell: Cooled. •203 •190 •178

T84 •197 •210

The variation of c is uncertain. The values credited to Forbes are those given by Everett on Balfour Stewart’s authority. Tait gives different figures. The values given in the column headed “cooled” are those found by Mitchell with one end of the bar cooled. The discrepancies are chiefly due to the error of the