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'y'L‘v _-N! ‘52; ,,.""2‘ ”r n ..~.;. 1"].‘4; L I B R‘A R Y Michigan State ~ University THE?“ This is to certify that the thesis entitled Coupling Between Pressure and Temperature Waves in Liquid Helium presented by Garold F. Fritz has been accepted towards fulfillment of the requirements for & degree in Physics . QQQQJQ Major professor 0469 V manna-v ' 4 Ill“ & SII' ‘ - ‘um ‘. ABSTRACT COUPLING BETWEEN PRESSURE AND TEMPERATURE WAVES IN LIQUID HELIUM By Garold F. Fritz When the thermal eXpansion coefficient (1 is retained in the linearized hydrodynamic equations of the two-fluid model of superfluid liquid helium, pressure and temperature waves are not independent. Thus a periodically varying temperature source produces not only temperature waves in ' and p ', 1 2 which prOpagate at the velocity of first and second sound, liquid helium, but also two pressure waves, p respectively. Similarly a vibrating diaphragm produces not only pressure waves but also two temperature waves, T1' and T2', which also prepagate at the velocity of first and second sound, respectively. Lifshitz has shown that the amplitudes of these cross-modes should be prOportional to CL . This thesis is an investigation of this coupling by observing and studying the two pressure waves p1' and p2 produced by a heater and the temperature wave T2 produced by a capacitor micrOphone. The temperature dependence of the amplitude of these waves has been studied using both pulse and standing wave techniques in the tempera- ture range from 1.2 K to the ).-point. Good agreement with theory has resulted only for the p1 mode. COUPLING BETWEEN PRESSURE AND TEMPERATURE WAVES IN LIQUID HELIUM By Garold anrritz A THESIS Submitted to Michigan State University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Department of Physics 1970 I I I . £17 ‘4‘ -'\ I 1,. (. To Carol ii ACKNOWLEDGEMENTS This experiment was suggested by Professor G. L. Pollack. I would like to thank him for his guidance and encouragement during the course of my work and for his advice in the preparation of this thesis. I would also like to express my gratitude to Dr. T. H. Edwards for the use of his vacuum coating equipment and to Mr. Carl James Duthler and Mr. Charles W. Leming for their assist- ance in the laboratory. Also, I wish to thank my wife, Carol, for typing the manuscript. I am also indebted to the U. S. National Aeronautics and Space Administra- tion for support in the form of a three year fellowship. Finally I would like to acknowledge the financial support of the U. S. Atomic Energy Commission. 111 TABLE OF CONTENTS Page I. INTRODUCTION . . . . . . . . . . . . . . . . 1 II. THEORY . . . . . . . . . . . . . . . . . . . 5 A. First and Second Sound . . . . . . . . 7 B. Coupling Coefficients . . . . . . . . 10 C. Vibrating Solid Surface . . . . . . . 13 D. Fluctuating Temperature Source . . . . 15 E. Vibrating Porous Surface . . . . . . . 17 F. Energy Considerations . . . . . . . . 18 III. EXPERIMENTAL . . . . . . . . . . . . . . . . 21 A. Pressure Waves p1' and p ' Produced by a Heater . C O O O C O .2. O O O O O . 21 1. Pulse Technique . . . . . . . 29 2. Standing Wave Technique . . . . 35 B. Temperature Wave T2' Produced by a MicrOphone . . . . . . . . . . . . . . 41 l. Porous Diaphragm Second Sound Transducer . . . . . . . . 41 2. Apparatus and Procedure for Measuring T2' . . . . . . . . . 44 IV 0 RESULTS 0 O O O O Q 0 O C O O O O Q 0 O C O 49 A. Pressure Waves p1' and p ' Produced by a Heater . . . . . . . .2. . . . . . . 49 1. Output Amplitude Data From MicrOphone . . . 49 2. Temperature Amplitude To Produced by the Carbon Disk Transmitter . 57 3. Output Amplitude Data Corrected for Variation of To . . . . . . 64 B. Temperature Wave T ' Produced by a Microphone . . . .2. . . . . . . . . . 7O 1. Sensitivity of the Porous Dia- phragm Transducer . . . . . . . 7O 2. Measurement of T2' . . . . . . . 74 iv V. DISCUSSION AND CONCLUSIONS . . . . . . . . . . 78 A. Pressure Waves p ' and p ' Produced by 3 Heater . . . .1. . .2. . . . . . 78 B. Temperature Wave T ' Produced by a Microphone . . . . . . . . . . . . . 81 LIST or REFERENCES . . . . . . . . . . . . . . 88 Figure 10 ll 12 LIST OF FIGURES EXperimental chamber. Carbon disk transmitter. Biasing circuit for the capacitor micro- phone used as a receiver. Schematic diagram of the experimental chamber and electronics used in the pulse measurements of p1' and pe'. Relative voltage gain of the frequency selective amplifier versus normalized fre- quency for various Q values. Some typical oscillosc0pe traces obtained in the pulse measurements of p1' and p2'. A typical frequency response curve of a standing wave resonance of p2' at a temperature of 2.06 K. Some typical OSCillOBCOpe traces illus- trating the response of the cavity to a long tone burst driving current at the resonant p2' frequency. Biasing circuit for the capacitor micro- phone used as a transmitter. The pressure wave amplitudes p ' and p ' produced by the carbon disk trdnsmitte , plotted versus temperature. The p ' standing wave resonance amplitude plottgd versus temperature. The damping constant of p ' standing waves plotted versus temperatur . vi Page 23 24 27 30 32 34 38 4O 46 51 53 56 Figure 13 14 15 l6 17 18 A schematic diagram of the apparatus used to measure the second sound amplitude T2' produced by the carbon disk transmitter. The second sound amplitude T ' produced by the carbon disk transmitter, plottes versus temperature. A plot of the p ' data on Figure 10 divided by the 2' data on Figure 14. A plot of the p ' data on Figure 10 divided by the 32' data on Figure 14. The output voltage from the porous dia- phragm transducer used as a receiver of the second sound waves produced by the carbon disk transmitter, plotted versus tempera~ ture. The second sound amplitude T ' produced by the capacitor microphone, plotted versus temperature. vii Page 60 63 66 69 73 76 I. INTRODUCTION Liquid 4He cooled below 2.17 K, which is called the lambda temperature, exhibits a number of peculiar properties which have been successfully explained by the introduction of a two-fluid model.1’2’3 In this model it is assumed that the ordered motion of the elementary excitations in the liquid is associated with only part of the liquid. This part is called the normal component and is characterized by the normal density F%. The normal component has viscosity and its flow is described by a velocity field vn. The remaining part of the liquid, which is called the superfluid component, is characterized by the density F: = F5- F£ , where F>is the total density of the liquid. The superfluid component has no viscosity and performs an independent motion which is described by the velocity field v No explicit S. assumptions are made about the temperature dependence of 5% and F% except the following: P. 0 Ion P .___. p :1 atT:T>\:2.17K ps :1 .8120 atT:O. P p 2 With these assumptions a complete set of hydrodynamic equations can be derived for superfluid liquid helium.4’5 One consequence of these hydrodynamic equations is the exist- ence of two wave modes which prOpagate with different veloci- ties. One of these wave modes is ordinary sound or pressure variations which propagate with the velocity u1= Bbp/bp)s]%, where p is the pressure and S the specific entrOpy. In the other wave mode the temperature is the fluctuating thermo- dynamic quantity. This mode is called "second sound". The velocity of second sound is u2=[3T82/0)(F%/F%i]%, where C is the Specific heat. The velocity u2 is an order of mag- nitude lower than u1 and vanishes at T = T)p When terms containing the thermal expansion coefficient ((13 ~(1/pXPP/5T') are neglected, first and second sound are independent. In this approximation a vibrating dia- phragm would produce only pressure waves which prOpagate at u,; that is, pure first sound. Similarly a fluctuating temperature source would produce only temperature waves which prOpagate at u2; that is, pure second sound. When thermal expansion is taken into account pressure and temperature waves in liquid helium are coupled. In this case there exists both pressure and temperature fluc- tuations which prOpagate with each velocity u1 and u2. The original theoretical treatment of this coupling is due to LifshitzfS He has shown that the relative ampli- tudes of the pressure and temperature waves produced in liquid helium depend upon the boundary conditions at the transmitter. 3 The object of this eXperiment was to investigate this coupling by observing and studying the pressure waves pro- duced in liquid helium by a fluctuating temperature source and the temperature waves produced by a vibrating diaphragm. The amplitudes of the two pressure waves produced by a fluc- tuating temperature source are denoted by p1 and p2'. The subscripts 1 or 2 indicate that the wave prOpagates at u1 or u2, respectively. Similarly the two temperature waves produced by a vibrating diaphragm are denoted by T1"and I T2 . The pressure waves produced in liquid helium by a periodically heated resistor have been studied by other investigators. Jacucci and Signorelli7 have Optically ob- E served p2' by the Debye—Sears effect. Eynatten, et 3;. have also observed this wave mode with a magnetic micrOphone. Hofmann, g; 3;.9 have observed and studied both p1' and p2 . All of the above results agree neither with each other nor with the theoretical results calculated by Lifshitz.6 The results of the independent measurements of this investi- gation are in substantial but not total agreement with those of Hofmann, gt 3;.9 Historically the first attempt to observe second sound was made by Shalnikov and Sokolov who attempted to generate this wave with a piezoelectric crystal.1O They were unsuc- cessful. This negative result was, in fact, the motivation for the above mentioned investigations by Lifshitz.6 He showed that a much more effective method of producing second sound would be by periodic heating. When this was pointed 4 10 out second sound was soon observed and has been compre- hensively studied since that time."2 No successful attempts have been reported, since the work of Shalnikov and Sokolov, in which second sound pro- duced by a vibrating mechanical transducer has been observed. In the present investigation second sound, produced by a capacitor micrOphone, has been observed. A new type of second sound receiver whose active element is a metalized porous diaphragm has been used to observe this wave mode. I I . THEORY When dissipative terms are neglected, the complete set of hydrodynamic equations based on the two-fluid model of liquid helium can be determined from conditions imposed by the Galilean relativity principle and the necessary conservation laws.5 The derivation is similar to that for an ordinary fluid except that an additional relation, which takes into account the superfluid prOperties, must be included. Most often this additional relation is an equation of motion for the superfluid component. This choice, however, is not unique.11 When dissipative processes are considered, additional terms must be included in all the hydrodynamic equations except the continuity equation. There is considerable disagreement among the various authors on the prOper form of these terms.2 For the purpose of studying first and second sound the hydrodynamic equations constructed by Landau and Khalatnikov5 are the most useful. In our investigation the amplitude of the sound waves is small enough that only terms linear in the normal fluid and superfluid velocities, v and vs, need be retained. n In this case the hydrodynamic equations due to Landau and Khalatnikov take the following forms: 5 1.8.. 4—6.? :: O (1) ‘o ‘03: ,b2 = ), ‘ovni *.Wk 38 2311) bt bri brk brk bri 11‘ br owl-5 VG Pvn) +C2_V>~?n] (2) 4. B? A A .5 A a. AA bts 4V“: V[§3V-(J -pvn) + §4Vovn] (3) 2353?. +PS$R§I :lg—VgT (4) In Eq. (2) summation over the repeated indices is implied. The various symbols in these equations are as follows: A A j : mass flux = ngs 4 f%;; (5) {3: total liquid 4He density : (g +f% (6) ll superfluid density 505D u normal fluid density <: I _ superfluid velocity 4 (D II normal fluid velocity p : pressure r1 : i-th component of the position vector S : specific entrOpy fiL: free entrepy T temperature i<= thermal conductivity coefficient 77: ordinary viscosity of the normal fluid €1,€2,é3,£4 : coefficients of second viscosity 7 Equation 1 is, of course, the continuity equation representing conservation of mass. Equation 2 is the equation of motion of the fluid as a whole. Equation 3 is the equation of motion of the superfluid component. Finally Eq. 4 represents the balance of entropy. The coefficients of second viscosity represent energy losses associated with changes in density which occur rapidly in comparison with the relaxation time required for restora- tion of thermodynamic equilibrium. If all dissipative terms are neglected and use is made of the thermodynamic relation‘e: 1 d = - Sd’l‘ _.._...dp (7) H + P then Eqs. (1) - (4) take the following form: 1341+ I75?” (8) g+$p=o (9) his - SGT 4 _.F‘.J..$p = o (10) \O‘otS) +ps$mén=o (11) A. First and Second Sound Plane wave solutions in which all quantities are prOportional to exp [10(t—x/ui], will now be considered. If the symbols F“, p', T', and 8' represent the variation off), p, T, and S from their equilibrium values, Eqs. 8 - 11 become: up' — (vaE) + ,Onvn) = 0 (8a) u( Jag“) - p' .-= 0 (9a) upv8 4 SpT‘ - p' = 0 (10a) u(Sp' +ps') -5pvn=o (11a) It has been assumed that the fluid is stationary at equilibrium so that vn and v8 were not denoted with primes. In obtaining Eqs. 8a - 11a the expression for j in Eq. 5 has also been used. Eliminating J = Svs + F$vn from Eqs. 8a and 9a yields u2p' — p' = o (12) Solving Eq. 11a for S' and then substituting expressions for F)and Ff obtained from Eqs. 6 and Ea, respectively, gives the following result: 5 5 SP 3 __ _ 8 Similarly, solving Eq. 10a for T' and then substituting expressions for F>and p' obtained from Eqs. 6 and 9a, respectively, gives the following result: I _ u u __ uPn T " (Pave * ann) " “vs " sp 5 sp Eliminating (vn-vs) from Eqs. 13 and 14 then gives 2 210 uS'-S——8—T':O (15) 81 (14) In Eqs. 12 and 15 pressure and temperature will be used as the independent variables. The density and entrOpy will then be eliminated by writing: 9' = F—fjp' + Pi) 1" (16) br>q, ‘bT p S' = (b8 p' + (ES T' (17) 2>p T Y>T The thermal expansion coefficient<1.is defined as follows: as 1 (\OP\ (18) 1° \M/p Also the following thermodynamic relations can be shown to hold12: be _ (‘Ov __lz(\o1°) __ _g_.__ (19) bPT bT P ET P ’ p p and ‘05 C (w) 2—2— . (90) ‘oT T In Eq. 19, v : —l— is the specific volume and in Eq. 20, {3 CF) is the specific heat at constant pressure. Substituting Eqs. 16 - 20 into Eqs. 12 and 15 then gives: [112(BP ~1]p'- quQT' : O (21) 2>p T 2 C " Ltd. 13' '0' [u2—p— - 52£]T' :: O (22) and 10 The coupling, due to the thermal expansion coefficient, between pressure and temperature waves in liquid helium is apparent in Eqs. 20 and 21. If'a.is neglected in these two equations, pressure and temperature waves will be independent and will prOpagate with the respective velo- cities: a U1 :: (2P (2}) t 2 1-2-8— P81 C R. In Eqs. 23 and 24 no distinction has been made between (hp/hp)T and (hp/bps or between GP and CV because of the following thermodynamic relations12: a - “1“" pr Cv hp; C 2 p : + C1. T (‘08.) (26) cv op bp 8 A Thus in the approximation that (1-.- o, (hp/bp)T a: (hp/25mg p v B. Coupling Coefficients The coefficients needed to determine the relative amplitudes of the pressure and temperature waves produced by a given transmitter can now be calculated as follows: In a plane wave the velocities v8 and v and the variable n parts p' and T' of the pressure and temperature are 11 prOportional to each other. Upon introducing the prOpor- tionality factors a, b, and c according to6 vn : av8 (27) p' : bVq (28) T' : cv (29) s Equations 10a, 14, 21, and 22 can be written as follows: b - 8pc = up (30) a - 1 : SF) c (31) 1181 2 2 u 33-2— -1b-aupc:0 (32) 3P T 2 2 (lTu b - (u - T82 PS )0 = C (33) PCp CD pm There will be two sets of the coefficients a, b, and 0; one for the case when u : 111 and one for u : u2. When u : u1, Eqs. 30, 31, and 33 can be solved for a b and c‘. The results, to first order intl, are 2 2 u u a :: 1 4- up 1 2 (34) 1 Sf) u 2 - u 2 s 1 2 u 2 (ITS 1 b1 :pu1 1 4 C ‘9 2 2—) (35) u1 -u2 u 3 CLT 1 c1- 2 T . (36) 12 In Eqs. 35 and 36 the subscript has again been left off the specific heat C because no distinction is being made between the specific heat at constant volume and at constant pressure. Doing so would merely introduce terms of higher order in a.which have been neglected anyway. When u : u Eqs. 30, 31, and 32 can be solved for 29 a2, b2, and cg. These results, to first order in a,, are “ 2 2 Pg CLP L11 L12 a? = -— + 2 2 (37) Pn Sel u1 -u2 2 3 CLP u1 112 b = -—- ~ (38) 2 S u 2--u 3 1 2 u u 2n 2 C2 = ' 2 1 - SE é 2? (39) S S u1 --u2 In the approximation,<:.: 0, Eq. 34 gives the result, vngévs. Thus, as expected, in a first sound wave in this approximation the liquid vibrates as a whole in each volume element. For a second sound wave with. 0,: 0, Eq. 37 shows that vn’}: - (Fa/9+8. From this it follows that 3 2 Eve 4 ann: 0. Thus in a second sound wave in this approximation the superfluid and normal fluid components vibrate out of phase in such a way that the center of mass of each volume element remains stationary. The coefficients given by Eqs. 3h - 39 can now be used to analyze radiation of pressure and temperature waves from various types of transmitters. 13 C. Vibrating Solid Surface The first type of transmitter which will be considered is a plane solid surface lying in the y — 2 plane and vibrating in the x-direction with velocity given by u : uoexp(iUIQ. The superfluid velocity will consist of two components; one associated with waves which prOpagate at u1 and the other with waves which prOpagate at u2. Solutions in the form of plane waves will be sought. Thus v : v (1) + v (2) (40) s s s vs(1) : A1exp iUJt - —§_W (41) u i 1 2 - - V<>=AexP1wt-.—2<_ . (42) S 2 L ug- In general, the boundary conditions at a solid sur- face at rest in liquid helium require that the tangential component of the normal fluid velocity-$5 and the normal component of the mass flux-F : fgv; + F£3n vanish. Since only the normal fluid component is associated with the excitations in the liquid the heat flux will befDSTvn. The normal component of this heat flux at the surface must equal the heat flow into the surface due to thermal conduction. However, due to the high rate of heat transfer in liquid helium compared with that in a solid, the latter can be neglected. The boundary conditions then reduce 14 to the vanishing of the normal components of each velocity A A vS and vn. For the vibrating surface the normal components of R78 and RTn must then equal the velocity of the surface. From Eqs. 27, and 40-42 these boundary conditions give A + A = u (43) : u (44) a1A1 + a_A2 o 9 From Eqs. 43 and 44 it then follows that 1 - a2 A : _______ u (45) 1 a - a O 1 2 1 - a1 A2 : - no (46) a1 - 32 The amplitudes of the pressure and temperature waves pro- duced in the liquid helium by this vibrating surface are then given, from Eqs. 28, 29, 45 and 46, by b1(1-a2) p ' : b A : u (47) 1 1 1 a —a o 1 2 c (1-a ) T ' = C A : 1 2 u (48) 1 1 1 a -a o 1 2 ' b?(1-a1) p? : b?A? : - A -8 uo (49) 1 2 c2(1-a1) T?' I 02A? 2: - uo (50) 15 Substituting the expressions for the coefficients from Eqs. 34-39 into Eqs. 47-50 gives 2 p1':(pu1_ &)uo (51) S CLTu1 T1' = T 1.10 (52) 2 3 CL Tu p2' = (—30—2—4110 (53) CLTu2 T2' : C 110 (54) The velocity u2 is an order of magnitude smaller than u1 for the temperatures between 1.2 K and T)\which are of interest here. Thus in obtaining Eqs. 51-54 the 2 approximation (u12 - u22)§éu1 has been used. D. Fluctuating Temperature Source The second type of transmitter which will be consid— ered is a surface in the y-z plane whose temperature varies as T : To'expfliut). The boundary conditions in this case require that the normal component of the mass flux—F vanish at the surface and that the temperature of the liquid adjacent to the surface equal that of the surface. From Eqs. 27, 29 and 40—42 these boundary conditions give ps(A1+A2) + 90(81A1-a2A2) : O (55) _ 1 , 01A1 + 02A2 _ TO . (5C) 16 Solving Eqs. 55 and 56 for A1 and A2 yields a A : ps+2eq T' 1 o (57) °1(Ps+a281)'°2(%*a1pn) A = _ P848181 T I 2 c1(ps+a2%)-c2(g+a1pn) o (58) The amplitudes of the pressure and temperature waves produced in the liquid helium by this fluctuating tempera- ture plane are then given, from Eqs. 28, 29, 57, and 58 by b p1':b1A1= 1(gm2a) T ' (59) C1‘B*3291)-°2(%*a1%) O T '.-:c A -..-.- c‘(ps+a28‘) T ' (60) 1 1 1 c1(pg+a2RI)-c2(ps+a1%)0 b2\,-point22 3 and also to study second sound in He — 4He mixtures below 0.3 K.23 In these experiments the principle advantage of this type of transducer was that it was an efficient transmitter and receiver of second sound without introducing heating. A detailed study of these transducers has been made by Sherlock and Edwards.21 An experiment was devised to test the sensitivity of this transducer. The details of this experiment will be described in detail in Section IV-B below. The results were that, in addition to the above mentioned desirable prOperties, this transducer was also much more sensitive to second sound temperature fluctuations than the carbon resistance receiver described above. | T 2. Apparatus and Procedure for Neasurins 2 The investigation of the temperature waves produced by a vibrating diaphragm was carried out with the experi- mental chamber previously described (Figure 1) except that the regular capacitor micrOphone replaced the carbon disk as transmitter and the porous diaphragm transducer was the receiver. The biasing circuit shown in Figure 3 was also used with the porous diaphragm receiver in this experi- ment. 45 Even with the increased sensitivity of the porous diaphragm receiver the second sound waves produced by the micrOphone could only be observed with the standing wave technique. Again the amplitude of the fundamental resonance and the damping constant were measured as a function of temperature. The damping constant was deter- mined by measuring the width of the frequency response curve around each resonance. The alternate method of observing the decay of a long tone burst could not be used because the Q of the tuned amplifier had to be set at 50 or higher in order to make accurate measurements of the signal amplitude. The regular capacitor microphone transmitter was driven with 30 volt peak ac voltage. In addition a 1f0 volt dc bias voltage was applied in order to increase the output. The fact that this dc bias will increase the output can be seen as follows. Under the action of an applied force F : Fosin(00t) the diaphragm of the micro— phone will execute harmonic vibrations of frequencycu with 24 its velocity amplitude uO given by : u : O (86) where Zm is the mechanical impedance of the diaphragm and Z is the acoustic radiation impedance of the liquid r helium. The dc bias voltage was again applied through a large series resistor, as indicated in Figure 9, so that 46 R=2.0 M 0.22 , ——"WW\v " If C: 7 f -:_-.—- _i_ 2 5" OSCILLATOR __ ’- PVo= |80 volts MICROPHONE V ' 30 volts TRANSMITTER Figure 9 Biasing circuit for the capacitor microphone used as a transmitter. 47 charge could be assumed to be constant. The purpose of the 0.22}Lf capacitor in the circuit in Figure 9 is to block the dc voltage from the oscillator. The impedance of this capacitor is negligibly small compared to that of the micrOphone. The force between the aluminized side of the diaphragm and the back plate will be 2 2 F=__217_9—= ”TOO v2 (87) A A where Q is the charge, C the capacitance, A the area of o the diaphragm, and V the potential difference between the aluminized side of the diaphragm and the back plate. In this case V : VO+ V'sincdt so that ancoe 2 2 2 F : ——-— [VD-t 2VOV'sin(wt)+(V') sin (wt)] A 2 2 2W0 3 2 t F : ____9_[V?+_(_\_,_)_ + 2V V'sin(wt)- (V ) cos(2wt):l,(88) A O 2 O 2 2 o The term 1TC§(V')2/A is just a constant and therefore If v0: 0 then F :‘WCS(V')2/A - (’1TC (V')2/A)cos(2wt). the micrOphone will produce pressure and temperature waves whose frequency is double that of the driving voltage. This is physically clear because both the positive and negative half cycles of the driving voltage produce attrac- tion between the diaphragm and back plate. However, if V0 is several times larger than V' the coefficient of sin(UJt) in Eq. 88 will be much larger than that of cos(2cut). The microphone will then produce waves whose 48 frequency is equal to that of the driving voltage and whose amplitude is much larger than those produced when vozo. IV. RESULTS A. Pressure Waves p1' and p2' Produced by a Heater 1. Output Amplitude Data From MicrOphone In the pulse technique the amplitudes of the pressure pulses p1' and p2' (Figure 6) were measured as a function of temperature. The corrections to theaadata due to the attenuation of first and second sound were negligibly small. A plot of the data is shown in Figure 10. On Figure 10 the squares represent p1 pulse amplitude measure- ments and the circles p ' pulse amplitude measurements. Also included on this plot are data from the standing wave measurements of p2'. These are represented by the triangles. The ordinate of this graph is the amplitude of the ac output voltage of the micrOphone from the pulse experiments. As will be discussed below, the standing wave data have been reduced by a constant factor in order that they could be displayed on the same graph as the pulse data on Figure 10. Figure 11 shows a separate plot of the actual pg' standing wave resonance amplitude as a function of tempera- ture. These amplitudes are, of course, larger than the amplitudes of the p2' pulses. The damping constant of each resonance was measured both by measuring the width 49 50 Figure IO The pressure wave amplitudes p; and p'2 produced by the carbon disk transmit- ter, plotted versus temperature. 51 o. 8:2... 3: 823358. N._ 10¢ sow p... a 10m. m M. 10m_ ‘1 d A 100N( JO¢N 0mm 52 Figure II The p'zstanding wave resonance amp- litude plotted versus temperature. 53 __ 2.6a c: 3:25.“.sz Nu o.~ B B E N. a _ _ d _ _ _ a _ o as 100 10.. d a 3 12 w n a 3 1 ca m A L3 ( 1 o.» 1m.» _ _ _ _ _ _ _ _ 0+ 54 of the frequency response curve around each resonance and by the decay of a long tone burst driving signal at the resonant frequency. Figure 12 shows a plot of the damping constant k measured by both of these methods. The circles represent the experimental values of k obtained by measuring the width of the frequency response curve, (see Figure 7). In this case k =7T(f" - f') where f' and f" are the frequencies at which the amplitude is 1K/2'times its value at resonance. The squares represent the values of k obtained from the decay of a long tone burst driving signal as illustrated in Figure 8. The time it takes for the amplitude to decay to 1/e of its maximum is equal to 1/k. The resonance amplitude is directly preportional to the source output and inversely prOportional to the damping constant.24 Thus the amplitude data of Figure 11 must be corrected with the data of Figure 12 in order to obtain the temperature dependence of the source output from the standing wave measurements. The data represented by tri- angles in Figure 10 are the result of correcting the ampli- tude data of Figure 11 for the variation of the damping constant data in Figure 12 and then dividing by a constant factor. The values for the attenuation of second sound derived from the damping constant data of the standing wave measurements, (see Figure 12), are larger than the published values.25-27 This is not surprising, however, because 55 Figure 12 The damping constant of p'a standing waves plotted versus temperature. 56 l l I o (I_oos) «3 ¢ l0 .LNVLSNOO SNIdWVCI LG LG 2.0 2.2 TEMPERATURE (K) L4 |.2 Figure 12 57 in the standing wave experiments there are losses due to reflection and radiation in addition to absorption in the liquid. Experiments whose purpose it is to measure the attenuation of second sound are specifically designed to minimize the first two types of losses. In Figures 10 - 12 the solid lines are merely smooth curves drawn through the data points. In Figures 10 and 11 the units on the ordinate are microvolts and millivolts, respectively, because the capacitor microphone was not calibrated. The output voltage will be prOportional to the pressure wave amplitude. 2. Temperature Amplitude To Produced by the Carbon Disk Transmitter Before the experimental p ' and p ' data of Figure 10 can be compared with the theoretical expressions of Equations 63 and 64 the following must be considered: As previously indicated in Section II, the heat transport 1 2 is associated with the normal component and is given by ’ : i = pervn . (89) The units of Q are energy per square centimeter per second. An approximate relation between d and the amplitude of the temperature variation in a second sound wave will now be derived. Solving Eq. 14 for (vn-vs) and letting u = u2 gives SP ”231 -V : Vn S "32' . (90) 58 In the approximation that CL: 0 it was shown, in Section II, that for a second sound wave 2 T82 Pg , 1 2 C 1% <9) and j: PSVS + nVn = O o (92) Solving Eq. 92 for v8 and substituting this into Eq. 90 gives Ft ) Sf) v 1 + = T ' . (93) r1( F¥ nefg 2 Solving Eq. 93 for vn and using p 2 pa + 81 and Eq. 91 gives S Cu Vn : i T. : 2 T2' . (94) 'uZfia TS Substituting Eq. 94 into Eq. 89 then gives ° __ I Q, _pCu2T2 , (95) or T ' : Q . (96) 2 1° cue In the measurements of p" and p2' the input power to the carbon disk transmitter was constant. Therefore Q was constant. In the earlier analysis of the pressure waves produced by a fluctuating temperature source the 59 transmitter was considered to be a plane surface whose temperature varied as T = Toexp(icut). However, because the power input to the carbon disk transmitter was constant, and because of Eq. 96, To is itself a function of tempera— ture in this eXperiment. It is given, from Eqs. 66 and 96, by To = 6.430112. The theoretical expression of Eq. 96 was verified by doing the following experiment. In the experimental chamber of Figure 1 the capacitor micrOphone was replaced by a second carbon disk resistor identical to the trans- mitter. This resistor served as a receiver of the second sound wave T2' produced by the carbon disk transmitter. A schematic diagram of the experimental apparatus in this case is shown in Figure 13. A constant current I : 1.0 ma was maintained through the receiver R by means of a dry cell in series with a resistor R1 which was much larger than R. The temperature fluctuation T2' causes the resis- tance of the receiver to vary and this produces the output voltage dB 8 t: I“ T ' (97) 0 dT 2 The resistance of the receiver as a function of tempera- ture, dR/dT, was obtained by measuring the dc voltage across R due to the 1.0 ma dc current. This voltage was measured with a Leeds and Northrup type K—3 potentiometer. The result was that the average value of dR/dT from 1.2 K 6O eTo AMPLIFIER A CARBON DISK RECEIVER TONE BURST OSCILLATOR GENERATOR '—__—:' CARBON fDISK “'2‘: TRANSMITTER A\\\\\\\\\\‘X L\\\\\\\\\\\ Figure 13 A schematic diagram ot the apparatus used to measure the second sound amplitude Tg' produced by the carbon disk transmitter. 61 to TX was approximately 70 Q/K. Both the previously described pulse and standing wave methods were used to investigate the temperature dependence of T2'. The input power to the carbon disk transmitter was again 25 mW/cm2 which is the same as was used in the measurement of the pressure amplitudes p1' and p2' produced by this transmitter. The results of these measurements are shown in Figure 14. The solid line is the theoretical curve of Q436u2 with Q = 25 mW/cm2. The published measured values of density, specific heat,29'30 and velocity of second sound31”33 were used. The data represented by circles in Figure 14 are measurements of T2’ obtained by the pulse method and the squares represent standing wave measurements. Again, as in the standing wave measurements of p2', the amplitude of the fundamental T2' standing wave resonance, and the damping constant k were measured as a function of tempera- ture. The standing wave data on Figure 14 have been corrected for variation of the damping constant k and have been reduced by a constant factor so that they could be plotted on the same scale with the pulse data. ' from the pulse measure- The experimental values of T2 ments on Figure 14 were obtained from Eq. 97 and the measured values of eo and I(dR/dT). The scale on the right hand side of Figure 14 is labeled with the corresponding values of eo in microvolts. Good agreement is indicated between both the pulse and standing wave T2' data and the theoretical curve. 62 Figure l4 The second sound amplitude Tg' produced by the carbon disk . transmitter, plotted versus temperature. S e. 23:. Ax. mmahZm, the velocity amplitude of Eq. 102 would vary little with temperature. We do not have quantitative knowledge of the parameters of the microphone. Thus the relative amplitudes of Zm and 2 cannot be calculated. However some qualitative argu- r ments can be made which would indicate that the variation of 2m in this experiment is also small. Investigations by Kuhl, 23 31. 2 of the prOperties of capacitor microohones similar to the ones used in these investigations indicate that the resonant frequency, ujo, was 10 - 15 kHz or higher. The frequencies used in the standing wave measure- ments of T2' were in the range from 75 Hz to 190 Hz. It is therefore probably safe to assume that¢u<31¢ooin these measurements. At frequencies far from resonance it is also usually possible to neglect the mechanical resis- 24 tance, R. 84 In this case Eq. 103 gives 2mg iMwog/w. If it is also assumed that Zfii>zr then, from Eq. 102, u would be 0 prOportional to a). However, the resulting correction to the T2' data due to the variation of frequency in the standing wave measurements is still much too small to substantially reduce the discrepancy between the data and theory. A final consideration which might be the cause of the discrepancy between the T2' data and the theoretical expression of Eq. 54 is the fact that the porous diaphragm transducer will also be sensitive to pressure waves. This was already mentioned in Section IV-B-2 where it was pointed out that resonances of waves propagating at u1 were also observed in this experiment. The question is: Are these resonances of p1' of Eq. 51 or of T1' of Eq. 52 or both? Actually a better way to put the question is: What is the relative sensitivity of the porous diaphragm transducer to pressure and temperature waves? The same question is involved in the observation of resonances corresponding to waves prOpagating at u . 2 Could there be a significant contribution to the received signal due to the p2 waves of Eq. 53? Since Q.is very small, Eqs. 53 and 54 would indicate that pg', which is prOportional to C12, could be neglected in comparison to TQ', which is prOportional to 0.. However this may not be true if the porous diaphragm transducer is more sensi- tive to pressure waves than to temperature waves. 85 We have not been able to arrive at a definite quan- titative answer to these questions. However, certain results obtained in our investigations and also the results of the investigation by Sherlock and Edwards21 would seem to indicate that the porous diaphragm transducer is a more efficient receiver of temperature waves than of pressure waves. Recall the following two experiments which were per- formed in this investigation. First a regular capacitor microphone was used as the receiver in the experiment in which the transmitter was a periodically heated carbon disk resistor. In this case two pressure waves, one prOpagating at u1 and the other at u2, were observed. In a succeeding eXperiment, described in Section IV-B-l, the same carbon disk transmitter was used but the receiver was now the porous diaphragm transducer. In this case only waves prOpagating at u2 were observed. Moreover the output signal from this wave was two orders of magnitude larger than that from the u2 wave in the first eXperiment. In the first experiment the two waves were p1' and p2' of Eqs. 63 and 65 because the regular capacitor micro- phone is sensitive only to pressure waves. In the second experiment the received signal could be due to either ' or T ' of Eqs. 65 and 66 respectively. However, if 2 2 the contribution of p2 P to this signal were significant, then we should also have been able to observe p1 waves in this experiment. 86 The fact that we did not observe any waves prOpagating at u1 in the second eXperiment, but did observe very strong signals corresponding to waves prOpagating at u2, would indicate that the porous diaphragm transducer is a more efficient receiver of temperature waves than of pressure waves. This conclusion is also indicated from the work of Sherlock and Edwards.21 They used a configuration in which both transmitter and receiver were porous diaphragm transducers. They also observed only waves prOpagating at u2. These results indicate that the discrepancy between the T2' data and the theoretical expression of Eq. 54 is not due to a contribution from p2' of Eq. 53. However it is still not clear what the relative contributions of p1' and T1' of Eqs. 51 and 52 are to the u1 resonances which were observed. In this case T1' is prOportional to a.while p1' is not. Thus these resonances could still be due mainly to p1'. The fact that the amplitude of these resonances varied little with temperature would seem to indicate that this is the case sincepu1 in Eq. 51 is relatively independent of temperature compared to the corresponding coefficient in Eq. 52. 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