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. 2023 Jul 28;62(31):12381–12406. doi: 10.1021/acs.iecr.3c01720

A Dual-Path Pulse-Echo Instrument for Liquid-Phase Speed of Sound and Measurements on p-Xylene and Four Halogenated-Olefin Refrigerants [R1234yf, R1234ze(E), R1233zd(E), and R1336mzz(Z)]

Mark O McLinden 1,*, Richard A Perkins 1
PMCID: PMC10416216  PMID: 37576937

Abstract

graphic file with name ie3c01720_0020.jpg

We describe an instrument to measure the speed of sound in liquids based on the dual-path, pulse-echo technique; it covers a temperature range of 228.15–423.15 K, with pressures of up to 93 MPa. It differs from similar instruments in the method of mounting the quartz-crystal transducer, a path-length ratio of 2.5:1, and automated data-collection protocols. The path-length difference was calibrated with measurements on high-purity propane. The performance of the instrument was verified by comparison with recent literature data on p-xylene. We present new liquid-phase measurements for the halogenated-olefin refrigerants 2,3,3,3-tetrafluoroprop-1-ene [R1234yf], trans-1,3,3,3-tetrafluoroprop-1-ene [R1234ze(E)], trans-1-chloro-3,3,3-trifluoroprop-1-ene [R1233zd(E)], and cis-1,1,1,4,4,4-hexafluorobut-2-ene [R1336mzz(Z)]. These measurements cover a combined temperature range of 230 to 420 K, with pressures of up to 50 MPa; these data are compared to literature data (where available) and multiproperty equations of state. The average relative expanded uncertainty in the speed of sound ranged from 0.035 to 0.088% for the different fluids.

1. Introduction

We describe an apparatus to measure the speed of sound based on the dual-path pulse-echo technique. Our instrument is intended for fluid property measurements of chemicals of industrial interest. It operates over a temperature range of 228.15–423.15 K, with pressures of up to 93 MPa. We describe the instrument in some detail, describe calibration measurements with propane and water, and report measurements on p-xylene as well as four “new” halogenated-olefin refrigerants that have very low values of the global warming potential (GWP).

Speed of sound is a thermodynamic property that is important for numerous applications, such as flow metering with ultrasonic flow meters or critical flow venturis. Speed of sound is more generally applicable for its use in developing multiproperty equations of state (EOS). Heat capacity is a useful input in fitting an EOS, and speed of sound w is related to isochoric heat capacity CV through

1. 1

where p is pressure and ρ is density. But in contrast to the difficult measurement of the heat flows and small temperature differences involved in a calorimetric determination of heat capacity, the measurement of the speed of sound involves the measurement of a characteristic length and a time or frequency, both of which can be measured with very low uncertainties.

Modern EOS are often expressed in terms of the Helmholtz free energy, and the speed of sound provides information on the first and second derivatives of the Helmholtz free energy

1. 2

where the dimensionless Helmholtz energy α = A/RT is a function of the dimensionless density δ = ρ/ρcrit and dimensionless inverse temperature τ = Tcrit/T; α0 and αr are the ideal-gas and residual contributions to α, R is the molar gas constant, and M is the molar mass. Lemmon and Jacobsen1 provide a description of the Helmholtz-form EOS as well as additional thermodynamic relationships along the lines of eqs 1 and 2.

Vapor-phase speed-of-sound data at low pressures can yield the ideal-gas heat capacity, which is related to α0. At higher pressures and in the liquid phase, speed-of-sound data provide information on the slope and curvature of the Helmholtz energy. Trusler and Lemmon2 demonstrate how the entire liquid-phase EOS could be based on speed-of-sound data together with single datums for density and heat capacity at a reference temperature and pressure. Thus, speed of sound is a very valuable supplement to other types of data, such as density and vapor pressure, in defining an EOS.

Techniques for measuring speed of sound can be broadly divided into (1) resonator techniques, where the frequency of a standing wave in a cavity of simple geometry (e.g., a sphere or cylinder) is measured;36 (2) optical techniques, such as dynamic light scattering, where the frequency shift of Brillouin peaks is measured;7,8 and (3) time-of-flight techniques, which involve timing an ultrasonic burst as it traverses a defined path length.9,10 Time-of-flight techniques are most applicable to dense fluids. The instrument described here complements the spherical acoustic resonator at NIST (Perkins and McLinden11), which has been used to measure the vapor-phase speed of sound of numerous fluids.1215

2. Description of Experimental Apparatus

2.1. Measuring Principle

The dual-path, pulse-echo-type instrument was first introduced by Kortbeek et al.16 In such an instrument, a piezoelectric transducer is located within a sample volume filled with the test fluid. A function generator excites the transducer (e.g., a quartz crystal) with a sinusoidal burst; ultrasonic pulses are thus emitted from each face of the crystal, which travel through the fluid sample, reflect off of planar surfaces at each end of the sample volume, and return to the transducer, which also serves as the detector. The experiment is schematically represented in Figure 1.

Figure 1.

Figure 1

Principle of the dual-path pulse-echo experiment.

The difference in the arrival times of the echo signals gives the speed of sound by

2.1. 3

where w is the speed of sound, L1 and L2 are the path lengths, Δt is the measured time difference, and δtd is a correction accounting for diffraction effects, as described in section 2.7. The differential nature of this technique cancels the end effects and improves the accuracy. This “single-burst method” has been described by Ball and Trusler,17 among others. An alternative method employing two burst signals separated by a Δt chosen to result in cancellation of the first burst traversing the long path with the second burst traversing the short path was the method originally proposed by Kortbeek et al.16 and has been adopted by others.10,18 We chose the single-burst method because it was much simpler to automate the data acquisition process. Furthermore, it allows for the off-line analysis of the data (as opposed to needing to determine the Δt in real time as a single-burst experiment is carried out).

2.2. Description of Instrument: Pulse-Echo Cell

A quartz crystal with a diameter of 24 mm, thickness of 0.36 mm, and resonant frequency of 8.00 MHz served as the ultrasonic transducer. The quartz crystal was “X-cut,” which means that its thickness expands and contracts when a voltage is applied to electrodes on opposite faces of the crystal. The electrodes were 10 mm in diameter and consisted of gold films plated onto the faces of the crystal; the electrical leads were connected to a keyhole extension of each electrode that extended to the edge of the crystal. The crystal was excited with a 10-cycle sinusoidal burst from an arbitrary function generator. The fluid path lengths on the opposite faces of the crystal were 30 mm and 12 mm (ratio of 2.5:1); the separations of the crystal and the reflectors were maintained by tubular spacers fabricated of a machinable ceramic (Macor, Corning Inc. Certain trade names and products are given to adequately document the experimental equipment and procedures. This does not constitute a recommendation or endorsement of these products by the National Institute of Standards and Technology nor does it imply that the products are necessarily the best available for the purpose.)

The crystal, spacers, and reflectors were assembled into a “stack” that was then inserted into a close-fitting support tube; these components were held in place with springs located at the ends of the support tube. Figure 2 gives a schematic diagram of the measuring cell (along with the pressure vessel and thermostat described in section 2.3), and Figure 3 shows an exploded view of the components. With this design, the individual components are of simple geometries, simplifying the fabrication of, for example, planar faces for the reflectors and parallel ends for the spacers. Our measuring cell was fabricated primarily of brass, which was chosen for ease of fabrication in prototype testing. A more corrosion-resistant cell made of stainless steel is planned. (Corrosion resistance is important because if the faces of the reflectors were to corrode during measurements the path lengths would be continually changing.)

Figure 2.

Figure 2

Schematic of the measuring cell and pressure vessel.

Figure 3.

Figure 3

Exploded view of the measuring cell showing the components.

The electrical connections to the crystal were made with spring-loaded pins contacting the keyhole extensions of the electrodes. These pins were located in holes drilled into the (electrically insulated) ceramic spacers. One of these pins connected to the reflector and then on to the support tube and pressure vessel, which was at electrical ground. The signal wire from the electrical feedthrough connected to the other pin; see Figure S1 in the Supporting Information.

The electrical feedthrough passed the signal to/from the crystal and served as a pressure seal into the pressure vessel; it also isolated the signal wire from the fluid of the thermostatting bath. This was accomplished with a custom-made assembly; this is shown in Figure S2 of the Supporting Information. The main portion of the feedthrough consisted of a coaxial assembly of the signal wire, PTFE sleeving (serving as the dielectric), and a 3.2-mm-diameter stainless steel tube (serving as the outer ground). The pressure seal of the signal wire was effected by a polyimide ferrule replacing the usual stainless-steel ferrule of a standard high-pressure fitting (High Pressure Equipment Company, 1/16 in. taper seal); the stainless tubing was brazed into the high-pressure nut to effect a seal against the bath fluid. At the top end of the feedthrough (which was above the level of the bath fluid), a standard SMA-coax fitting was modified to connect to the stainless tubing rather than the braid of the usual coaxial cable. This feedthrough maintained the coaxial electrical characteristics of the signal cable until it was inside the pressure vessel, and we observed substantially lower noise with this assembly compared to that of the twisted-pair connections that we used in early prototype testing.

An inductor, consisting of turns of PTFE-insulated wire wound around a 3.2 mm o.d. stainless-steel post, was in series with the signal wire inside the pressure vessel. The number of turns was adjusted to obtain an impedance of 50 Ω for the transducer/measuring cell assembly, thus matching the impedance of the oscilloscope and coax cable.

An electrical schematic is shown in Figure 4: A high-speed switch connected the crystal to the function generator during the input sinusoidal burst, and then, after a delay of 6 μs, it switched the crystal to the input of a three-stage amplifier (5× per stage for a total of 125×), which then fed into a digital storage oscilloscope (Keysight model DSO-X 4022A). Note that any noise was also amplified; the purpose of the 125× amplifier was to bring weak signals into the range of the oscilloscope. The echo signals were recorded for off-line analysis.

Figure 4.

Figure 4

Electrical schematic of the dual-path pulse-echo instrument.

A key feature of the pulse-echo technique is the unequal path lengths L1 and L2, and most authors have employed a path-length ratio of 1.5:1.10 Here, we chose a path-length ratio of 2.5:1. The larger ratio yields a longer time difference and, thus, greater time resolution for the arrival time of the two pulses for a given sample volume. It also allows a longer time for the short-path echo to damp out before the arrival of the long-path echo; this is a particular advantage for measurements on fluids, where damping is low. On the other hand, for fluids or conditions with significant damping, the long-path echo can be very weak with the 2.5:1 ratio. Thus, there is no single optimum path-length ratio.

There is the possibility of an overlap of echoes. The sound burst traverses the fluid sample and is reflected back to the crystal; the noninteger path-length ratio ensures that the reflected signals are well separated upon arriving back at the crystal. This time difference is the primary measurement of the experiment. A portion of the sound energy, however, is transmitted into the body of the reflector, bounces off the back face of the reflector, and is re-emitted into the fluid. Depending on the path lengths and fluid speed of sound relative to the reflector lengths and speed of sound in the reflector material, there is a range of fluid speeds of sound where the re-emitted short-path signal can overlap with the long-path echo. The magnitude of any overlap can be reduced in two ways. First, one wants to maximize the fraction of the sound energy that is reflected. This is done by maximizing the mismatch in acoustic impedance between the fluid sample and reflector material, which implies a reflector made of a very dense and stiff material, and most metals are adequate in this regard. The second way to minimize overlap is to have a coned (rather than flat) back surface of the reflector, thus scattering the sound burst transmitted into the reflector; this has been discussed by numerous authors.10,17,19 With these two considerations, we were not able to observe any signal returning from the back side of the reflector and consider the uncertainty arising from any potental overlap to be negligible.

2.3. Description of the Instrument: Thermostat and Pressure Measuring System

The measuring cell holding the crystal and fluid sample was contained in a commercial stainless-steel pressure vessel rated to 93 MPa (High Pressure Equipment Company, model GC-1); see Figure S3 in the Supporting Information. This, in turn, was held in a thermostated oil bath operating from −45 to 150 °C (228.15 to 423.15 K). A schematic of the measuring cell and pressure vessel in the thermostat is shown as Figure 2. A photograph of the thermostated bath is shown in the Supporting Information as Figure S4. A photograph of the instruments (which were located in the adjacent room) is shown as Figure S5.

The temperature of the oil bath was measured with a long-stem 25 Ω standard platinum resistance thermometer (SPRT); the temperature-sensing portion of the SPRT was located immediately adjacent to the pressure vessel, as indicated in Figure 2. The resistance of the SPRT was ratioed to a standard resistor with an AC resistance bridge. The 25 Ω reference resistor for the bridge was thermostated at 37.0 ± 0.1 °C in a small enclosure. The SPRT, standard resistor, and resistance bridge were calibrated as a system on ITS-90 over the range of 234.316 to 505.078 K with fixed-point cells (mercury triple point, water triple point, and indium and tin freezing points). The standard uncertainty in the fixed-point/SPRT/resistor/bridge system was estimated as 3 mK. The short-term (minute-to-minute) variations in the oil-bath temperature were 2 mK or less. No long-term (hour-to-hour) variation was observed. The temperature gradients in the oil bath were less than 3 mK over the region of the pressure vessel. Any uncertainty associated with measuring the bath temperature (as opposed to having the SPRT in the pressure vessel) is included in the 3 mK uncertainty associated with the bath gradients. The combined standard (k = 1) uncertainty in the temperature measurement, including the effects of the SPRT, standard resistor, resistance bridge, calibration standards, stability of the oil bath, and temperature gradients in the oil bath, was 5 mK.

The pressure was measured with a vibrating-quartz-crystal pressure transducer with a maximum pressure of 138 MPa. The transducer was held at room temperature and was calibrated by the manufacturer with piston gages; this calibration included a temperature-compensation term. The zero of the transducer was checked regularly (while the system was evacuated between samples), and readings were corrected for any drift in the zero. The standard uncertainty in pressure was 26 × 10–6p + 0.007 MPa.

The pressure manifold for sample handling and pressure measurement is shown in Figure 5. It was built up from 1/8 in. high-pressure, coned-and-threaded-type valves and fittings rated to a pressure of 204 MPa. The design provided considerable flexibility in loading samples, and fluid ports on the top and bottom of the measuring cell allowed for flushing of the system between samples. During the course of an experiment, the sample was loaded from the right-hand side of the manifold, and the general “flow” of sample was toward the waste bottle on the left-hand side. The entire system was flushed with solvent and evacuated between samples, but there was the possibility of trapping nonvolatile samples or sample residues in the dead volumes formed by the safety rupture disk and the pressure transducer. These were both on the “downstream” side of the manifold so that any trapped sample that might diffuse out was carried toward the waste bottle as the pressure was adjusted during the course of measurements.

Figure 5.

Figure 5

Schematic of the pressure/filling manifold; red lines indicate valve ports that are always interconnected.

A manual, piston/cylinder-type pump could be used to pressurize the sample. (However, as described in section 2.6, this pump was not typically required for a measurement sequence.) The total volume of fluid sample, including the filling manifold and pressure transducer (but not the manual pump), was 30 mL.

The pressure manifold was operated at room temperature for most of the measurements reported here. The measurements on p-xylene, however, required heating the manifold to 40 °C to avoid freezing of the sample at a high pressure. This was done by wrapping tubing around the valves and pressure transducer through which water from a thermostated bath was circulated; insulation was then wrapped around the water tubing.

2.4. Typical Echoes

The description of the experiment presented above implied a single ultrasonic burst. In fact, we continuously excited the crystal with sinusoidal bursts at a frequency of 100 Hz (i.e., bursts of 10 sinusoids separated by 10 ms). The crystal was driven with a signal of 2.0 V peak to peak; higher voltages were found to overdrive the switch (although the received echo signals appeared normal and undistorted). The periodic excitation of the crystal enabled the averaging of the signal and other signal processing by the oscilloscope. We typically averaged 256 echo signals, although the oscilloscope would allow averaging of up to 10 000.

Figure 6(a) shows a screen shot of the oscilloscope for propane at T = 285 K, p = 35 MPa, and w = 1164 m·s–1. The input burst is shown in green on the left at t = 0 μs. A transient associated with switching the signal from the function generator to the oscilloscope is observed at t ≈ 6 μs. The echo signals are shown in yellow, and multiple echoes are observed. (Note the different voltage scales for the green and yellow traces.) The short-path echo arrives at t ≈ 21 μs, and the long-path echo arrives at t ≈ 52 μs. The bursts traversing the short path two and three times are seen at t ≈ 41 μs and at t ≈ 62 μs; these echoes have distorted shapes resulting from reflections off of both faces of the crystal and resulting interference. The strongest echo is seen at t ≈ 72 μs, corresponding to 3.5 times the arrival time of the short-path echo; we consistently observe this echo, and it is sometimes the strongest echo for highly compressed liquid states. We cannot associate this echo with any particular mode and surmise that it arises from constructive interference. It does not enter into the analysis, but it does present a slight complication for data recording, as discussed in section 2.5. All of the echoes have damped back down to noise level at t ≈ 1000 μs, well before the next burst is generated at t = 10 ms.

Figure 6.

Figure 6

Oscilloscope screen shots showing representative echo signals for propane at T = 285 K, p = 35 MPa, and w = 1164 m·s–1: (a) signal for t = (0–270) ms; each division represents 30 μs; (b) phase envelopes for short-path, 2 × short-path, and long-path echos, where each division represents 3.9 μs and the time scale is offset by 22.40 ms; (c) short-path echo, where each division represents 500 ns and the time scale is offset by 20.92 μs; (d) long-path echo where each division represents 500 ns and the time scale is offset by 51.77 μs.

Figure 6(b) shows the phase envelopes of the short-path, 2× short-path, and long-path echoes; these are the data of interest for the analysis. Figure 6(c,d) show zoomed-in images of the short-path and long-path echoes, respectively; they are virtually identical in shape, but with the long-path echo slightly attenuated compared to the short-path echo. Note that the maximum signal occurs on the 12th oscillation, although the input burst consisted of only 10 cycles. Note that these screen shots are an average of 64 echo signals taken over 0.64 s, which reduces the noise; this averaging was carried out by the oscilloscope itself. An example of much weaker echo signals is shown as Figure S6 in the Supporting Information.

2.5. Recording of Echo Signals

We used our control program (described in section 2.6) together with the signal-processing capabilities of the oscilloscope to automate the detection and recording of the echo signals. In brief, the oscilloscope operated on the portion of the signal displayed on its screen, and we adjusted the time and voltage scales of the oscilloscope multiple times to identify the short-path and long-path echoes and recorded them in a file for off-line analysis.

When the control program triggered a measurement, a time offset was used to push the input burst and switch transient off the left side of the screen; the maximum signal in the resulting window was found, and the voltage was rescaled accordingly. The average voltage was also computed, and this was used to adjust the voltage offset or zero. The maximum signal could be either the short-path echo at techo_short or the unidentified echo (discussed in section 2.4) at ∼3.5 × techo_short; resetting the window time scale to 0.4 times the time to the maximum signal then revealed either the short-path echo or a signal at noise level (in which case, the first signal was the short-path echo). Having identified the time to the short-path echo, the maximum signal in the time interval (2.3 × techo_short < t < 2.8 × techo_short) was the long-path echo at techo_long. The time scale was adjusted to place techo_short at the 10% position and techo_long at the 90% position in the window (i.e., the data shown in Figure 6(b)); the averaging was reset to 256, and 16 000 data points were written to the output file. The window was reset to span 10 μs (80 cycles) centered first around techo_short and then techo_long to separately record 16 000 data points for each of the echoes (i.e., the data shown in Figure 6(c,d)). (This final step was implemented after we saw that for fluid speeds of sound less than about 600 m·s–1 not enough points were being recorded for the actual echo signals; i.e., most of the 16 000 data points recorded the noise between the echoes. This separate recording was not done for all of the fluids reported here.)

2.6. Measurement Sequence

The sample was loaded into the measuring cell in one of two ways. For fluids with a room-temperature vapor pressure of more than a few kPa (including all of the fluids measured in this work), the fluid sample was loaded directly from the sample cylinder into the evacuated measuring cell. The sample cylinder was heated to increase the vapor pressure. This avoided any possibility of contamination that a pump might introduce.

For fluids with very low vapor pressures (such as the lubricants reported in ref (20)), the fluid sample was loaded into a manual piston-type pump and degassed by pulling a vacuum on the head space of the pump. The sample was then pushed into the measuring cell (which had been evacuated), the pump was valved off, the oil bath was set to the first set-point temperature, and the experimental run begun.

The entire experiment was controlled by a computer running a custom control program written in Visual Basic 6. The pressure of the fluid sample and the temperature of the oil bath were scanned every 30 s. The approach to equilibrium conditions was determined by monitoring three quantities: (1) the difference in the average bath temperature computed over the previous eight scans compared to the set-point temperature; (2) the standard deviation of the previous eight temperature scans; and (3) the rate of change of pressure with time, computed with a linear fit of the previous eight pressure readings. When all three of these were within preset tolerances, a “converged” flag was set in the control program, and an additional equilibration time of 30 min was allowed before starting the measurements. A single measurement set comprised recording three sets of echo signals and the four temperature and pressure readings made at the start and end of the set and between the recordings of the echoes. Four such sets, spaced 10 min apart, were recorded before moving to the next (T, p) state point. These raw data were analyzed with a separate program (described in section 2.8) to generate the (T, p, and w) data points.

When measurements at the first (T, p) state point were completed, the temperature was increased by (5 or 10) K, and since the cell was liquid-filled, this increased the pressure. Measurements continued along this pseudoisochore (line of approximately constant density) until either the desired maximum temperature or maximum pressure was reached. The bath was then cooled to a temperature (10 to 20) K above the initial temperature of the isochore, and the total quantity of sample in the measuring cell was reduced by venting sample into a waste bottle to achieve a starting pressure for the next isochore of approximately 1 MPa or slightly above the saturation pressure, whichever was greater. The next isochore then commenced. This process was repeated to cover the liquid surface of the fluid sample, within the operating limits of the instrument. Since the thermostatic bath was under computer control, an entire isochore could be carried out automatically; manual adjustment of the fluid charge was required only between isochores.

Replicate isochores were regularly measured by cooling the bath to a near-ambient temperature and adding a small amount of additional sample to again completely fill the system with liquid. These repeat isochores served to check the stability of the pulse-echo system and to check for any possible degradation in the fluid sample.

Some of the measurements on p-xylene were carried out along isotherms. The procedures were the same except that the pump was also partially filled along with the measuring cell. The pump was then used to adjust the pressure between points along an isotherm.

2.7. Diffraction Correction

The time difference was corrected for diffraction effects; these are due to a phase advance of the actual sound wave compared to a perfect plane wave.21 The electrodes on the quartz crystal cover only the central region (0 ≤ rb) of the crystal. Application of a voltage to the electrodes causes the thickness of the crystal to increase in the region between the electrodes. Since the quartz is stiff, there must also be some increase in the crystal thickness for some radial distance outside of the electrodes. This is obviously a simplification, and other functional forms for the vibration amplitude have been considered; for example, Meier9 considered four models for the deformation of the crystal, namely, a (1) piston source, (2) simply supported source, (3) clamped source, and (4) Gaussian source. The simplest model for the diffraction correction is based on a piston source that has a uniform amplitude of vibration in the active region of the electrodes. Meier et al. demonstrated that there were only small differences of less than 0.001% in the speed of sound between the diffraction corrections from each of these source models. We will base our diffraction correction on the piston source (uniform amplitude) model.

The development of the piston source model was originally described by Williams22 in 1951. The model is further discussed by Trusler21 as a diffraction correction for pulse-echo measurements of the speed of sound in fluids. The model assumes that the sound source is a plane that oscillates uniformly over its entire cylindrical surface with radius b. The sound is detected by a cylindrical surface of the same radius b that is located a distance z from the source and is centered on the same axis as the source. The detector response is proportional to the average acoustic pressure over its surface. The average acoustic pressure is given by

2.7. 4

where

2.7. 5

z is the distance and θ is the angle normal to the transducer, and

2.7. 6

A is the amplitude, ϕ is the phase advance in radians due to diffraction, and f is the frequency of the tone burst. For path lengths greater than several times the source radius (which is to say about 20 mm for our system),

2.7. 7

where

2.7. 8

Equations 7 and 8 were evaluated for our transducer with complex numerical integration in Mathematica.23 These results are shown in Figure 7 along with a simple power law fit given by

2.7. 9

which well represents eqs 7 and 8.

Figure 7.

Figure 7

Diffraction phase advance calculated with eqs 7 and 8 (solid line); the dotted line shows a simple power law representation (eq 9), which represents these results with a correlation coefficient of R2 = 0.9977.

The diffraction correction is applied to the measured differential time between the return tone bursts along the short path and the long path. The time shift due to the diffraction correction is given by

2.7. 10

with ϕ calculated from eq 9 and with S from eq 8 for each path length (i.e., z is set to 2Ls or 2Ll). From the above equations, it is seen that the diffraction correction becomes smaller as the frequency increases. The characteristics of our instrument are summarized in Table 1, which indicates that the diffraction correction ranges from 3.9 ppm for the long path at w = 200 m·s–1 to 207 ppm for the short path at w = 2000 m·s–1. But we are concerned with the difference in δtd between the short and long paths, which ranges from 2.5 ppm (0.0025%) at w = 200 m·s–1 to 88 ppm (0.0088%) at w = 2000 m·s–1. Although the diffraction correction is very small, it is non-negligible at low speeds of sound and long path lengths.

Table 1. Diffraction Correction Parameters for Our Transducer (f = 8 MHz with b = 5 mm) at Several Representative Values for Liquid Speeds of Sound.

Speed of Sound: w = 200 m·s–1 w = 800 m·s–1 w = 2000 m·s–1
  L = 2 × Ls = 24 mm
S 0.024 0.096 0.240
ϕ 0.0355 0.0756 0.125
Δt/μs 120 30 12
δtd/μs 0.000706 0.00150 0.00249
  L = 2 × Ll = 60 mm
S 0.060 0.240 0.600
ϕ 0.0585 0.125 0.205
Δt/μs 300 75 30
δtd/μs 0.00116 0.00248 0.00408

2.8. Data Analysis

The experimental data were written to a file for off-line analysis as described in section 2.6. The file was first parsed to identify and separate the echo, temperature, and pressure data.

All of the echo data are depicted in the top panel of Figure 8. The basic idea of the analysis is to find a “best” superimposition of the short-path and long-path echo signals V by adjusting the amplitude ratio A and Δt according to

2.8. 11

Figure 8.

Figure 8

Schema for the analysis of the echo data: (top) phase envelope for the 16 000 recorded data points; (second from top) approximate superposition of the short-path (red) and long-path (green) signals; (second from bottom) determination of the Δt giving the minimum variance for the superposition; and (bottom) final superposition. Data shown are for propane at T = 250.004 K, p = 6.403 MPa.

This general approach was developed by Ball and Trusler.17 Signal processing carried out by the oscilloscope provided the times to the maxima in the short-path and long-path echoes, from which an initial estimate of the Δt was obtained. An approximate superposition of the two echoes using this initial estimate is shown in the second panel. Here the attenuation of the long-path signal (green) relative to the short-path signal (red) can be clearly seen. A slight mismatch in the time overlap is also present although less apparent. A regression for A and Δt is carried out over ±12 cycles from the peak amplitude (±1.5 μs for our 8.00 MHz frequency); the variance in the fit for each cycle is plotted versus Δt as shown in the third panel of Figure 8. A parabola is fitted to the variance, and the minimum in this parabola defines the optimal Δt. Note that this approach allows a resolution in Δt that is smaller than that of the sample period. The final superposition with optimal Δt and A is shown in the bottom panel of Figure 8. With strong signals, the superposition is nearly perfect—while Figure 8 seems to show only the green of the long-path echo, a few pixels of red from the short-path signal are seen.

Figure 8 depicts the situation with strong echo signals (the data shown are for propane well away from the critical point). Figure S6 in the Supporting Information depicts signals that are much weaker and also with substantial attenuation; the same process successfully finds the optimal superposition. We note, however, that occasionally with weak signals the Δt is in error by one or two cycles (0.125 or 0.25 μs); these can be detected (and the points discarded) by manually examining the superposition plots. The case of weak signals emphasizes the advantage of basing the Δt on a superposition of the entire echo signal rather than attempting to find the difference between the rising edge of the echoes—the “time zero” of the long-path signal would be very difficult to ascertain in the case of weak echoes. The Δt obtained from this superposition was then adjusted by the diffraction correction of eqs 9 and 10.

This analysis contrasts with the analysis carried out by others using the dual-path pulse echo technique. We are not applying any sort of Fourier transform21 or Hilbert transform24 to deal with noisy data. Rather, we obtained signals with a good signal/noise ratio by averaging 256 echo signals; this was done with a few simple commands on the digital oscilloscope. The off-line analysis presented here contrasts with the real-time determination of the Δt obtained with the double-pulse method, a technique that requires sophisticated signal processing at the time of the measurement, often by a human operator as done by Meier.10 The present single-pulse method is much easier to automate, and the off-line analysis permits a closer examination of the data in cases of weak signals. The continuously rising or falling signal is advantageous in the present analysis: if the signal were to reach a steady-state amplitude, then the superposition would be much harder to identify, and the Δt could easily be in error by an integer number of cycles.

Our analysis could be improved for weak signals. We averaged 256 echo signals for the present measurements, but averaging a larger number of echoes could improve the signal-to-noise ratio and we have averaged as many as 4096 echoes for some subsequent measurements. A Fourier transform can function as a digital bandpass filter. We applied both of these techniques to mixtures of carbon dioxide and R1132a, which have very weak signals.25 An analog bandpass filter might also be helpful, but we were not able to locate a suitable commercial unit.

The temperature data were recorded as raw resistance ratios from the AC resistance bridge; these were converted to resistance, and then the SPRT calibration on ITS-90 was applied to obtain the temperature of the oil bath. Similarly, the signals from the pressure transducer were recorded as the vibration periods of the pressure and temperature crystals in the transducer, and calibration equations were applied to obtain the pressure. Four measurements of temperature and pressure were recorded for each set of three echo measurements, and the average of these four was assigned as the (T, p) for the three echo measurements.

3. Results

Measurements of the speed of sound of seven fluids were carried out. The path-length difference was calibrated with measurements on propane; measurements on water were used to confirm the calibration. Verification of the instrument was carried out on p-xylene by comparing our results to literature data. Finally, data for four “new” halogenated-olefin refrigerants are reported; the literature data for these fluids are very limited, and thus, comparisons are made primarily to reference-quality equations of state.

3.1. Experimental Samples

The experimental samples are detailed in Table 2. For all of the fluids, the samples were used as received, except that they were degassed with multiple cycles of freezing the sample, evacuating the vapor space, and thawing. The pressure over the frozen material on the final freeze–pump–thaw cycle was 1 × 10–4 Pa or lower. We also carried out our own analysis of the refrigerant samples by gas chromatography/mass spectrometry (carried out according to the protocols of Bruno and Svoronos26,27).

Table 2. Sample Information.

Name IUPAC Name Source Initial Purity/Mol Frac. Purification Method Final Purity/Mol Frac. Analysis Method
propane propane Scott 0.99999 degassing 0.99999 GC/MSa
water water b >0.99999 b >0.99999 resistivity
p-xylene p-xylene Sigma-Aldrich 0.997 degassing 0.997 none
R1234yf 2,3,3,3-tetrafluoroprop-1-ene Honeywell 0.9996 degassing 0.9996 GC/MS
R1234ze(E) trans-2,3,3,3-tetrafluoroprop-1-ene Honeywell 0.99993 degassing 0.99993 GC/MS/IRc
R1233zd(E) trans-1-chloro-3,3,3-trifluoroprop-1-pene Honeywell 0.99985 degassing 0.99985 GC/MS
R1336mzz(Z) cis-1,1,1,4,4,4-hexafluorobut-2-ene Chemours 0.9999 degassing 0.9999 GC/QToF-MSd
a

Gas chromatography/mass spectrometry.

b

The water sample was obtained from a commercial ultrapure laboratory water system that consisted of two ion-exchange stages, ultraviolet light dosing (to photo-oxidize organics), a third ion-exchange stage, and an ultrafiltration membrane; the resistivity of this water was 18.2 MΩ·cm.

c

Gas chromatography/mass spectrometry/infrared spectroscopy.

d

Gas chromatography/quadrupole time-of-flight mass spectroscopy.

3.2. Calibration of Path-Length Difference with Propane

The path-length difference was calibrated with measurements on propane spanning the operating range of temperature and pressure by taking the propane speed of sound as a known quantity and inverting eq 3 to obtain ΔL for each measurement

3.2. 12

where the propane speed of sound was calculated with the equation of state (EOS) of Lemmon et al.28 Note that the diffraction correction δtd to the measured transit time must also be included. These data were fitted to an emprical function representing the temperature and pressure variation of the path-length difference

3.2. 13

where ΔL is in mm, T is in K, and p is in MPa and the parameters are ΔL293 = 17.9546 mm, a1 = 7.843 × 10–6, a2 = 8.499 × 10–9, and a3 = −8.38 × 10–6. These parameters were obtained strictly from fitting the propane data, and while we did not expect any systematic temperature and pressure effects associated with our mounting of the crystal, such effects would be accounted for, in contrast with parameters developed from the material properties.

The propane EOS of Lemmon et al. was fitted to a wide range of data, including vapor pressure, p–ρ–T, saturation densities, isochoric and isobaric heat capacities, enthalpy of vaporization, second and third virial coefficients, and speed of sound. It fits the speed-of-sound data of Meier and Kabelac18 within 0.06% over their entire temperature and pressure range (240 to 420 K, with pressures of up to 100 MPa), with an RMS deviation of 0.013%. Thus, our instrument is, in effect, calibrated to the speed of sound data of Meier and Kabelac, who estimated the expanded uncertainty in their measurements to be 0.019 to 0.022%. Details of the Meier and Kabelac instrument are given by Meier;9 their path-length difference was based on a combination of material properties of their quartz transducer and stainless-steel measuring cell and calibrations carried out with water at p = 0.10 MPa over a temperature range of 1 to 95 °C. Propane was selected here as the calibration fluid largely because of the excellent data of Meier and Kabelac (which covered temperature and pressure ranges similar to those of our instrument) and the EOS of Lemmon et al.; furthermore, the availability of high-purity propane minimizes sample purity effects.

Figure 9 presents the path-length difference obtained from 1319 data points on propane measured along 10 isochores spanning a temperature range of (230 to 420) K with pressures to 52 MPa. The path-length correlation of eq 13 is shown for p = 0 and 60 MPa. The RMS deviation between the experimental points and eq 13 is 0.0021 mm, or 0.012%. The propane data are presented in the Supporting Information, including a comparison of our data with the data of Meier and Kabelac18 as Figures S7 and S8. Also shown in Figure 9 are similar results for water (discussed in section 3.4).

Figure 9.

Figure 9

Propane calibration of the path-length difference; ●, propane data; −■–, eq 13 with p = 0; −▲–, eq 13 with p = 60 MPa; and *, water data.

3.3. Direct Measurement of Path-Length Difference

The path-length difference was also determined directly by measuring the lengths of the ceramic spacers before assembly. This was done with digital micrometers; the resolution of the micrometer used for the short-path spacer was 0.001 mm, and the one for the long-path spacer was 0.0025 mm. The calibration of the micrometers was checked with gage blocks immediately prior to measuring the spacers. Six to eight measurements were made of each spacer with average values and standard deviations of Lshort = 12.0096 mm, σ = 0.0066 mm and Llong = 29.9585 mm, σ = 0.0069 mm or (LlongLshort) = 17.949 mm at T = 293 K. This value is 0.0056 mm or 0.031% smaller than the path-length difference determined by the propane calibration. The standard deviation in this determination was 0.04%, with a somewhat larger uncertainty. This is a larger uncertainty than the path-length calibration with propane (as discussed in section 4.3), and thus, the calibrated path-length difference was used in the analysis. Nevertheless, this direct measurement served as a powerful consistency check.

3.4. Verification of Path-Length Difference with Water

The calibration of the path-length difference was repeated with water. These measurements were carried out on isochores over a temperature range of (275 to 420) K, with pressures of up to 68 MPa. For measurements at low temperatures along the first isochore (T = 275 to 320 K, p to 16.8 MPa), the results are seen to be consistent with the propane data and eq 13 as shown in Figure 9; the RMS deviation with eq 13 was 0.0039 mm or 0.022%. At higher temperatures and for subsequent isochores, however, the results were not repeatable, even at low temperatures or with a fresh sample.

The cell was disassembled, and we found that the ceramic spacers had been attacked by water; the surface appeared powdery. The spacers were swollen and had to be hammered out of the support tube. The quartz crystal, brass reflectors, and brass support tube, on the other hand, showed no visible degradation. It was not possible to determine when the spacers were attacked, and thus, we did not use the water data in calibrating the path lengths. Nevertheless, the low-temperature water data confirm the propane calibration.

We should note that the water measurements were the last ones carried out in the present work because we were concerned about the potential corrosivity of water at high temperatures. This is the reason that we measured propane first. After repairs, subsequent measurements with this instrument required a full repetition of the path-length calibration (which was different than the one reported here), as discussed by Rowane et al.29

3.5. Verification Measurements with p-Xylene

p-Xylene was chosen for verification measurements so that we could compare with the recent high-accuracy data of Al Ghafri et al.30 Our measurements began with isotherms at T = (373.7, 422.8, and 323.5) K; these measurements were limited to a pressure of 20 MPa to avoid freezing of the sample in the room-temperature manifold. We then heated the manifold, as described in section 2.3, and loaded a fresh sample of p-xylene. The isotherm at T = 323.5 K was repeated but with pressures of up to 43.1 MPa. The liquid phase was then measured along 11 isochores covering an overall (T, p) range of (288.1 K, 0.065 MPa) to (423.2 K, 53.7 MPa).

The measured data are summarized in Figure 10 and reported in Table 3. The most recent equation of state available for p-xylene, that of Zhou et al.,31 was developed with only limited speed-of-sound data, and its uncertainty in the speed of sound is estimated to be 0.3%. Thus, we compare to an empirical fit of the present data; we adopt the same implicit equation used by Al Ghafri et al.,30 namely,

3.5. 14
3.5. 15

where p0 = 0.1 MPa, T0 = 286.4 K is the triple point of p-xylene, w0,T is the speed of sound at p0, and the coefficients are listed in Table 4.

Figure 10.

Figure 10

Measured points for p-xylene; Δ, present results, measurements along isotherms; ◇, present results, measurements along isochores; ○, Al Ghafri et al.30

Table 3. Experimental Liquid-Phase Speeds of Sound, w, for p-Xylene, with the Combined Expanded (k = 2) Relative Uncertainty in the Speed of Sound, Uc, Also Given along with Relative Deviations from the Empirical Fit to the Data (Equations 14 and 15)a,b.

T (K) P (MPa) W (m·s–1) Uc (k = 2) (%) 100(w/wfit – 1)
373.657 5.567 1053.42 0.038 –0.071
373.657 2.096 1028.64 0.039 –0.083
373.657 10.297 1085.31 0.037 –0.062
373.657 14.943 1114.79 0.036 –0.058
373.657 20.015 1145.20 0.035 –0.055
       
422.819 1.934 851.85 0.048 –0.062
422.818 5.097 880.82 0.045 –0.061
422.819 10.008 922.22 0.042 –0.060
422.819 15.148 961.81 0.040 –0.061
422.818 20.102 997.06 0.038 –0.063
       
373.566 5.088 1050.49 0.038 –0.064
323.520 2.074 1218.73 0.035 –0.015
323.520 5.173 1236.45 0.034 –0.013
323.521 10.089 1263.47 0.034 –0.009
323.520 15.068 1289.56 0.034 –0.009
323.520 20.059 1314.60 0.033 –0.009
       
288.105 0.193 1353.53 0.033 –0.004
293.099 5.121 1357.32 0.033 –0.005
298.114 10.045 1361.30 0.033 0.000
303.105 14.897 1365.23 0.033 0.005
308.106 19.706 1369.10 0.033 0.008
313.122 24.482 1372.93 0.033 0.009
318.107 29.176 1376.67 0.033 0.008
323.125 33.839 1380.33 0.033 0.006
328.113 38.419 1383.89 0.033 0.005
333.111 42.938 1387.33 0.033 0.005
338.126 47.351 1390.43 0.033 0.006
       
323.526 2.131 1219.18 0.035 –0.004
323.524 5.138 1236.36 0.035 –0.003
323.526 10.156 1263.86 0.034 –0.005
323.525 15.284 1290.69 0.034 –0.006
323.527 20.136 1314.97 0.033 –0.007
323.526 25.306 1339.82 0.033 –0.008
323.526 30.208 1362.47 0.033 –0.010
323.527 35.192 1384.69 0.033 –0.012
323.526 40.338 1406.86 0.033 –0.014
323.527 43.121 1418.63 0.033 –0.008
       
288.105 0.514 1354.98 0.033 –0.017
293.099 5.467 1358.84 0.033 –0.019
298.114 10.394 1362.78 0.033 –0.016
303.105 15.243 1366.64 0.033 –0.012
308.106 20.054 1370.46 0.033 –0.011
313.122 24.829 1374.25 0.033 –0.011
318.108 29.522 1377.96 0.033 –0.012
323.127 34.194 1381.64 0.033 –0.012
328.113 38.783 1385.24 0.033 –0.012
333.112 43.330 1388.78 0.033 –0.011
338.127 47.837 1392.28 0.033 –0.007
343.115 49.951 1386.07 0.033 –0.002
348.129 51.039 1375.73 0.033 0.000
       
303.103 0.145 1290.58 0.034 0.013
308.104 4.751 1294.89 0.034 0.009
313.119 9.345 1299.28 0.034 0.008
318.106 13.864 1303.59 0.034 0.008
323.125 18.369 1307.86 0.033 0.007
328.113 22.798 1312.04 0.033 0.006
333.111 27.193 1316.15 0.033 0.003
338.127 31.541 1320.15 0.033 0.003
343.115 35.827 1324.07 0.033 0.001
348.129 40.091 1327.96 0.033 0.001
353.128 44.302 1331.78 0.033 0.002
358.140 48.478 1335.54 0.033 0.004
       
318.104 0.331 1230.52 0.034 0.014
323.123 4.656 1235.36 0.034 0.010
328.110 8.921 1240.17 0.034 0.009
333.109 13.153 1244.90 0.034 0.009
338.126 17.348 1249.50 0.034 0.008
343.115 21.484 1254.02 0.034 0.006
348.128 25.604 1258.49 0.034 0.003
353.128 29.675 1262.87 0.034 0.000
358.140 33.716 1267.19 0.034 –0.002
363.155 37.719 1271.43 0.033 –0.003
368.133 41.651 1275.54 0.033 –0.002
373.167 45.589 1279.63 0.033 –0.001
378.156 49.458 1283.64 0.033 0.003
       
333.109 0.265 1170.63 0.035 0.015
338.123 4.287 1175.87 0.035 0.013
343.112 8.268 1181.10 0.035 0.013
348.126 12.237 1186.27 0.035 0.011
353.126 16.157 1191.32 0.035 0.009
358.138 20.050 1196.28 0.034 0.005
363.153 23.911 1201.14 0.034 0.002
368.132 27.706 1205.85 0.034 –0.001
373.167 31.509 1210.53 0.034 –0.004
378.156 35.238 1215.07 0.034 –0.005
383.175 38.958 1219.55 0.034 –0.004
388.181 42.631 1223.93 0.034 –0.003
393.183 46.269 1228.24 0.034 –0.001
398.191 49.865 1232.42 0.034 0.003
       
348.121 0.524 1114.17 0.036 0.014
353.122 4.274 1119.85 0.036 0.015
358.135 8.011 1125.50 0.036 0.016
363.150 11.718 1131.03 0.036 0.015
368.129 15.368 1136.40 0.035 0.012
373.165 19.025 1141.71 0.035 0.008
378.154 22.638 1146.95 0.035 0.003
383.173 26.220 1151.99 0.035 –0.001
388.180 29.762 1156.94 0.035 –0.003
393.182 33.270 1161.78 0.035 –0.005
398.191 36.755 1166.55 0.034 –0.004
403.194 40.202 1171.21 0.034 –0.003
408.202 43.623 1175.79 0.034 –0.003
413.209 47.019 1180.31 0.034 –0.001
418.209 50.385 1184.77 0.034 0.000
423.215 53.729 1189.18 0.034 –0.002
       
363.146 0.122 1054.28 0.038 0.003
368.125 3.588 1060.34 0.038 0.009
373.161 7.079 1066.42 0.037 0.012
378.150 10.512 1072.31 0.037 0.012
383.170 13.932 1078.06 0.037 0.011
388.176 17.318 1083.68 0.036 0.009
393.179 20.674 1089.17 0.036 0.006
398.187 24.010 1094.55 0.036 0.003
403.191 27.316 1099.81 0.036 0.002
408.200 30.599 1104.97 0.035 0.001
413.207 33.856 1110.04 0.035 0.001
418.208 37.086 1115.02 0.035 0.002
423.215 40.299 1119.96 0.035 0.004
       
378.147 0.838 1003.71 0.040 0.004
383.168 4.100 1010.13 0.039 0.012
388.175 7.341 1016.46 0.039 0.016
393.177 10.553 1022.62 0.038 0.017
398.186 13.746 1028.63 0.038 0.016
403.190 16.913 1034.50 0.038 0.014
408.200 20.062 1040.25 0.037 0.012
413.207 23.190 1045.89 0.037 0.010
418.207 26.294 1051.43 0.037 0.010
423.215 29.386 1056.90 0.036 0.012
       
393.176 0.195 943.46 0.042 0.009
398.185 3.214 950.34 0.042 0.019
403.189 6.215 957.08 0.041 0.025
408.199 9.192 963.58 0.040 0.028
413.206 12.154 969.96 0.040 0.028
418.207 15.096 976.20 0.039 0.028
423.215 18.026 982.34 0.039 0.030
       
408.198 0.138 888.35 0.046 0.034
413.205 2.928 895.52 0.045 0.043
418.206 5.706 902.59 0.044 0.051
423.215 8.486 909.57 0.043 0.055
       
288.103 0.065 1353.04 0.033 0.007
293.098 4.921 1356.50 0.033 0.007
298.114 9.839 1360.39 0.033 0.007
303.104 14.686 1364.27 0.033 0.009
308.105 19.475 1368.06 0.033 0.011
313.120 24.231 1371.83 0.033 0.012
318.107 28.910 1375.53 0.033 0.012
323.125 33.569 1379.20 0.033 0.011
328.112 38.145 1382.79 0.033 0.011
333.111 42.563 1385.81 0.033 0.011
338.126 43.961 1376.15 0.033 0.017
a

The listed data are averaged from 12 measured echo-delay times (4 sets of 3 replicates each); see Supporting Information for unaveraged data. The data are listed in the order measured; blank lines separate isotherms and isochores.

b

The standard (k = 1) uncertainties in T and p are 0.005 K and (26 × 10–6p + 0.016 MPa), respectively.

Table 4. Coefficients to the Empirical Fit of the p-Xylene Data (Equations 14 and 15).

a10 –0.50585 a11 1.57213 a12 –1.29872 a13 0.425685
a20 2.41506 × 10–4   a21 –3.93517 × 10–4   a22 3.34927 × 10–4   a23 0.0
a30 –6.82551 × 10–7   a31 1.84037 × 10–6   a32 1.15418 × 10–6   a33 0.0
b0 3.20442 × 103   b1 –2.71050 × 103   b2 1.11379 × 103   b3 –2.47322 × 102

Deviations of the measured data from eqs 14 and 15 are shown in Figure 11. Our data are seen to be self-consistent and well-fit by eqs 14 and 15 except for the two isotherms at T = (373.7 and 422.8) K, which are systematically lower by 0.058 to 0.069%. The RMS deviation of all of the data from eqs 14 and 15 is 0.022%; it is 0.015% dropping the two isotherms. Replicates of the T = (288 to 338) K isochore measured at the beginning and end of the testing showed a systematic difference of up to 0.021%, indicating a possible slight degradation of the sample.

Figure 11.

Figure 11

Deviations between the measured speed of sound for p-xylene and the fit of the present data (eq 14); ○, Al Ghafri et al.;30 Δ, □, present results for measurements along isotherms; replicates of the isochore starting at T = 288 K are indicated by ×, +, and ○ in blue (measured in that order); and other symbols indicate measurements along isochores.

Al Ghafri et al.30 measured along isotherms from T = (306 to 447) K, with pressures to 66 MPa; this is the only literature source covering a wide range of temperature and pressure. Their data are shown in Figures 10 and 11; they are quite self-consistent but are systematically lower than our data by an average of 0.077%. The NIST TDE database32 lists 57 additional sources of literature data for the liquid-phase speed of sound, but all report data only at atmospheric pressure (mostly at near-ambient temperatures) or for the saturated liquid and only three of these sources report more than six data points. As the present paper is not intended to review the literature on p-xylene, we will not consider these other sources further.

Al Ghafri et al.30 estimate their expanded uncertainty in speed of sound to range from 0.023 to 0.104%, and thus, our data and the data of Al Ghafri et al. are consistent within mutual uncertainties. (Our uncertainties are discussed in section 4.) It is instructive to discuss the differences and similarities in our two instruments: We both employ the dual-path pulse-echo technique with a single ultrasonic burst. We have a path-length difference of 18 mm with a 2.5:1 ratio, while the Al Ghafri et al. instrument has a path-length difference of 10 mm with a 1.5:1 ratio. We employ a quartz crystal with a resonant frequency of 8.00 MHz versus a piezoelectric element at 5.00 MHz. Our reflectors extend to the edges of the fluid volume while those of Al Ghafri et al. are of a “post-type” design that sits away from the edges of the fluid volume.

Our calibration procedures differ from those of Al Ghafri et al.30 As discussed in section 3.2, we calibrated with propane over a range of temperatures and pressure. Al Ghafri et al. calibrated with water at (T = 306.1 K, p = 0.1 MPa) and calculated the path-length difference as a function of T and p by use of the material properties of their Invar-36 spacers. They did carry out verification measurements on water at temperatures of up to 421 K and pressures of up to 60 MPa.

Our p-xylene sample had an overall purity of 99.7% according to the supplier’s certificate of analysis, with impurities of 0.18% m-xylene and 0.07% ethylbenzene (specified as “GC area percentage”, which we take as approximately equivalent to a molar basis). These impurities are chemically similar to those of p-xylene and have speeds of sound that differ by less than 1%. Calculating the liquid-phase speed of sound (over the range of T and p of our measurements) with the equations of state of Zhou et al.31 for each of the pure fluids and mixing coefficients given by Bell and Lemmon33 (as implemented in the REFPROP database34) gives speeds of sound for our sample that are 0.006 to 0.010% lower than for pure p-xylene.

The p-xylene sample of Al Ghafri et al.30 had an overall purity of 99.8%, with a water content of 0.01% (mass basis) according to the supplier’s certificate of analysis; other impurities were not listed but would likely contribute a systematic effect similar to the impurities in our sample. Calculating the p-xylene/water mixture with REFPROP yields a speed of sound 0.050 to 0.067% lower than that of pure p-xylene. It must be noted that there are no mixture data for p-xylene/water, and this calculation assumed mixing coefficients of octane/water. There is considerable uncertainty in the effect of a small water impurity on the speed of sound, but this result suggests that a significant fraction of the systematic difference between our data and the data of Al Ghafri et al. could be due to sample purity effects.

Given the differences in our instruments, procedures, and samples, our agreement with the data of Al Ghafri et al.30 is quite remarkable; this result serves to verify both of our instruments and indicates the robustness of the pulse-echo technique.

3.6. Speed of Sound of Halogenated-Olefin Refrigerants

Four “new” halogenated-olefin refrigerants were measured. These fluids have very low values of the global warming potential (GWP) due to the presence of a carbon–carbon double bond. They have been developed and recently commercialized as replacements for high-GWP hydrofluorocarbon (HFC) and hydrochlorofluorocarbon (HCFC) refrigerants currently in use. Some of these fluids are also used as solvents or foam-blowing agents. Table 5 lists some of the basic properties of these fluids, including the normal-boiling-point and critical-point temperatures and the global warming potential relative to CO2 on a 100-year integration time horizon (GWP100).35

Table 5. Characteristics of the Halogenated-Olefin Refrigerants Measured Here.

Name TNBP/K Tcrit/K GWP100 ASHRAE Safety Class
R1234yf 243.7 367.9 <1 A2L
R1234ze(E) 254.2 382.5 <1 A2L
R1233zd(E) 291.4 439.6 1 A1
R1336mzz(Z) 306.5 444.4 2 A1

Also listed in Table 5 is the safety classification under ANSI/ASHRAE Standard 34;36 the rating is divided into a toxicity part (A or B) and a flammability part (1, 2L, 2, or 3). A toxicity rating of “A” designates “lower toxicity” as indicated by an occupational exposure limit of 400 ppm (parts per million) or higher on a volume basis in air; all four fluids studied here have received an “A” rating. A flammability rating of “1” indicates “no flame propagation” in the ASTM E-681 test;37 a rating of “2L” indicates marginal flammability, defined as a heat of combustion of less than 19 MJ/kg, a lower flammability limit of greater than 0.10 kg·m–3, and a maximum burning velocity of less than 10 cm·s–1. Ratings of “2” and “3” indicate higher flammability. The fluids studied here are rated 1 or 2L. The R numbers used here as shorthand notation are also specified by ANSI/ASHRAE Standard 34. ISO Standard 81738 is substantially the same in both the designation and safety classification of these fluids.

Only very limited literature data for the liquid-phase speed of sound are available for these fluids, so we compare primarily to recent reference equations of state. For the refrigerants measured here, we provided the present data to the EOS developers of three of these EOS, who used our data in their fitting, and thus such comparisons cannot independently verify the measurements—they can only indicate their internal consistency. However, the ability of an EOS to fit the present speed-of-sound data as well as other data types (including vapor pressure, p–ρ–T, vapor-phase speed of sound, and heat capacity data), all nearly within experimental uncertainties (as will be shown below), strongly suggests that all of the data are thermodynamically consistent, as discussed by Lemmon and Jacobsen.1

3.6.1. R1234yf-2,3,3,3-Tetrafluoroprop-1-ene

R1234yf, also known as HFO-1234yf (“HFO” = “hydrofluoroolefin”), was developed as a replacement for R134a (1,1,1,2-tetrafluoroethane) in automotive air-conditioning systems,39 and it now accounts for the majority of new automotive systems. It is also a component in at least 29 refrigerant blends classified by ANSI/ASHRAE Standard 34.36

Measurements of the speed of sound of R1234yf were carried out along 19 isochores at temperatures from (235 to 380) K, with pressures of up to 50 MPa. The measured points are shown in Figure 12 and reported in Table 6. The initial set of four isochores was measured to a maximum (T, p) of 370 K and 50.3 MPa; upon venting the sample at the conclusion of these tests, a few milligrams of polymer was collected. Earlier testing indicated the possibility of polymerization at high pressures,40 and the second series of isochores (which comprises the main data set) was limited to a maximum pressure ranging from 15.9 MPa for the highest-density (i.e., lowest temperature) isochore to 7.1 MPa for the lowest-density isochore, which extended to T = 370 K. Upon completion of this series of isochores, the same sample was then measured along two additional isochores (referred to as series 3) up to (T = 370 K, p = 25.8 MPa) and (T = 380 K, p = 17.4 MPa); each of these tests was followed by a replicate of the isochore (measured in the second series) that extended from (T = 290 K, p = 1.0 MPa) to (T = 310 K, p = 11 MPa). Upon flushing the cell with acetone following these tests, less than 1 mg of residue was collected, indicating very limited or no polymerization.

Figure 12.

Figure 12

Measured speed-of-sound data for R1234yf; ▲, present work (series 1); ◆, present work (series 2); *, present work (series 3); □, Lago et al.;43 and ○, Yoshitake.42 The critical point is indicated by a red ⊗.

Table 6. Experimental Speeds of Sound, w, for R1234yf (2,3,3,3-Tetrafluoroprop-1-ene), with the Combined Expanded (k = 2) Relative Uncertainty in the Speed of Sound, Uc, Also Given along with Relative Deviations from the Equation of State of Lemmon and Akasaka41a,b.
T (K) P (MPa) W (m·s–1) Uc (k = 2) (%) 100(w/wEOS – 1)
260.090 0.641 617.92 0.055 0.034
265.117 0.638 595.66 0.058 0.067
270.098 1.895 585.39 0.059 0.059
275.100 5.020 592.64 0.056 0.033
280.107 8.149 599.84 0.054 0.015
290.111 14.430 614.11 0.050 –0.012
300.105 20.638 627.61 0.047 –0.016
310.108 26.784 640.41 0.045 –0.011
320.146 32.869 652.60 0.043 –0.001
330.159 38.879 664.28 0.041 0.006
       
280.103 1.080 533.39 0.071 0.058
285.089 3.892 541.30 0.067 0.035
290.106 6.728 549.09 0.063 0.014
295.105 9.540 556.58 0.060 0.001
300.105 12.350 563.88 0.057 –0.008
310.109 17.923 577.75 0.053 –0.010
320.133 23.485 591.08 0.050 –0.004
330.123 28.982 603.71 0.047 0.003
340.118 34.401 615.63 0.045 0.017
350.119 39.760 627.01 0.043 0.028
360.126 45.057 637.89 0.042 0.035
370.138 50.278 648.27 0.040 0.037
       
300.100 0.715 437.61 0.109 –0.016
305.118 0.821 415.20 0.123 –0.059
310.104 0.938 392.78 0.140 –0.108
315.115 1.068 370.05 0.161 –0.162
320.127 2.166 365.95 0.161 –0.116
330.125 5.839 384.76 0.130 –0.025
340.116 9.517 401.52 0.108 –0.009
350.135 13.197 416.80 0.094 0.003
360.143 16.855 430.86 0.083 0.019
       
319.979 1.289 349.60 0.185 –0.174
324.983 3.063 359.82 0.163 –0.071
329.992 4.846 369.35 0.146 –0.023
334.981 6.621 378.20 0.132 –0.010
339.983 8.403 386.62 0.121 –0.007
344.992 10.185 394.64 0.111 0.000
349.990 11.966 402.33 0.103 0.004
355.010 13.754 409.76 0.095 0.007
359.996 15.527 416.85 0.089 0.015
       
235.010 0.637 729.97 0.043 –0.050
240.002 0.734 708.26 0.045 –0.023
245.003 4.676 714.03 0.044 –0.032
250.005 8.663 720.22 0.043 –0.036
254.995 12.624 726.36 0.042 –0.035
259.990 16.592 732.57 0.041 –0.033
       
250.001 1.049 666.04 0.049 0.004
254.996 4.746 672.67 0.047 –0.012
259.990 8.460 679.43 0.046 –0.024
264.997 12.253 686.64 0.044 –0.038
269.992 15.942 693.26 0.043 –0.032
       
259.988 1.012 621.58 0.054 0.031
264.995 4.401 628.57 0.052 0.007
269.992 7.791 635.56 0.050 –0.010
274.996 11.181 642.49 0.048 –0.019
280.000 14.563 649.33 0.047 –0.023
       
269.990 1.011 577.43 0.061 0.049
274.995 4.113 584.90 0.058 0.022
280.000 7.177 591.96 0.056 0.009
285.002 10.248 598.98 0.053 –0.005
290.020 13.339 606.04 0.051 –0.011
       
279.999 1.014 533.15 0.071 0.059
285.001 3.836 541.08 0.067 0.034
290.004 6.660 548.85 0.063 0.016
294.999 9.483 556.46 0.060 0.004
300.000 12.305 563.88 0.057 –0.003
       
290.002 1.002 488.16 0.085 0.045
294.998 3.566 496.79 0.079 0.030
300.003 6.159 505.32 0.074 0.007
305.000 8.776 513.87 0.069 –0.002
310.001 11.331 521.56 0.065 0.000
       
289.998 1.065 488.94 0.085 0.042
294.995 3.618 497.39 0.079 0.030
299.997 6.182 505.63 0.073 0.015
304.996 8.743 513.59 0.069 0.006
309.999 11.304 521.30 0.065 0.000
       
299.996 1.063 443.13 0.105 0.000
304.996 3.365 452.31 0.096 0.005
310.002 5.680 461.14 0.089 –0.001
314.994 7.997 469.68 0.082 –0.001
320.002 10.294 477.62 0.077 –0.002
       
309.996 1.242 398.58 0.134 –0.061
314.993 3.278 408.13 0.121 –0.023
320.003 5.328 417.23 0.110 –0.007
325.008 7.377 425.86 0.101 –0.001
329.998 9.417 434.05 0.093 0.004
       
320.001 1.356 351.05 0.183 –0.112
325.006 3.135 361.18 0.161 –0.027
330.014 4.921 370.57 0.144 –0.010
335.002 6.722 379.65 0.130 –0.016
340.006 8.495 387.97 0.119 0.025
       
330.012 1.732 306.16 0.256 –0.207
335.000 3.267 316.98 0.221 –0.016
340.007 4.814 327.03 0.193 0.106
345.011 6.373 336.21 0.172 0.084
350.008 7.969 345.18 0.153 –0.019
       
289.995 1.008 488.27 0.085 0.044
294.990 3.578 496.95 0.079 0.028
299.991 6.155 505.37 0.074 0.016
       
309.992 1.278 399.22 0.133 –0.054
319.997 5.380 418.02 0.109 0.001
329.995 9.489 434.97 0.093 0.008
340.005 13.584 450.38 0.081 0.017
350.007 17.663 464.70 0.073 0.029
359.997 21.713 478.08 0.066 0.050
369.991 25.751 490.77 0.061 0.068
       
289.991 0.994 488.14 0.085 0.052
294.989 3.557 496.76 0.079 0.038
299.991 6.128 505.12 0.074 0.025
304.991 8.697 513.20 0.069 0.015
309.993 11.264 521.00 0.066 0.010
       
329.995 1.753 307.02 0.255 –0.132
340.003 4.867 328.07 0.192 0.100
350.006 7.987 345.96 0.153 0.117
359.996 11.113 361.70 0.127 0.023
369.991 14.242 376.38 0.109 0.019
380.020 17.378 390.06 0.095 0.027
       
289.992 1.010 488.35 0.085 0.054
294.990 3.561 496.83 0.079 0.042
299.987 6.117 505.04 0.074 0.029
304.990 8.666 512.92 0.069 0.022
309.993 11.224 520.64 0.066 0.016
a

The listed data are averaged from 12 measured echo-delay times (4 sets of 3 replicates each); see Supporting Information for unaveraged data. The data are listed in the order measured; blank lines separate measured isochores.

b

The standard (k = 1) uncertainties in T and p are 0.005 K and (26 × 10–6·p + 0.016 MPa), respectively.

The measured data are compared to the EOS of Lemmon and Akasaka41 in Figure 13; the present data were included in the fitting of this EOS. Figure 13(a) plots the deviations of the present data versus temperature, and there are no obvious trends except for a somewhat larger scatter at higher temperatures. (Note that the figure plots the deviations of all of the replicate measurements, which are tabulated in the Supporting Information, while Table 6 reports only average values.) The overall RMS deviation is 0.056%, which is not surprising given that these data were included in the EOS fitting. Figure 13(b) plots deviations versus pressure, and series 1 and 3 show small (less than 0.068%), but systematically increasing, deviations as the pressure is increased. Five replicates of the isochore extending from (T = 290.0 K, p = 1.0 MPa) to (T = 310.0 K, p = 11 MPa) were measured during the course of series 2 and 3; the speed of sound systematically increased by a maximum of 0.0087% between the middle and end of series 2 and 0.024% between series 2 and the end of series 3. These results indicate that the sample was stable, except for a slight degradation when it was taken to the higher pressures of series 3.

Figure 13.

Figure 13

Deviations between data for R1234yf and the EOS of Lemmon and Akasaka;41 ▲, present work (series 1); ◆, present work (series 2); *, present work (series 3); □, Lago et al.;43 and ○, Yoshitake.42 (a) Deviations versus temperature and (b) deviations versus pressure (most of the data of Lago et al. would be off-scale and are not shown).

Figure 12 also shows the measured points of Yoshitake42 and Lago et al.,43 and these data are compared to the equation of state in Figure 13. (Note that ref (42) does not tabulate the measured data; Yositake provided these data directly to E. Lemmon of NIST for his EOS fitting.) Yositake measured to a maximum pressure of 22 MPa, and the data of Lago et al. extend to 6.1 MPa; nevertheless, there is considerable overlap in the measured temperature and pressure ranges of the three data sets. The data of Yoshitake are generally consistent with the EOS and the present data with a systematic bias of −0.152%; the RMS deviation to the EOS is 0.166%. The data of Lago et al., on the other hand, are systematically higher than the present data with an RMS deviation of 1.153% and maximum deviation of 2.516% at (T = 360.0 K, p = 5.0 MPa).

3.6.2. R1234ze(E)—trans-1,3,3,3-Tetrafluoroprop-1-ene

R1234ze(E) or HFO-1234ze(E) has been approved by the Significant New Alternatives Program (SNAP) of the U.S. Environmental Protection Agency44 for use in chillers, as a foam-blowing agent for polyurethane foams, and as an aerosol propellant. R1234ze(E) was measured along 14 isochores covering a temperature range of 230 to 420 K, with pressures of up to 37 MPa. The measured points are displayed in Figure 14 and reported in Table 7. Also shown are the liquid-phase data of Lago et al.,43 who measured R1234ze(E) along five isotherms from 260 to 360 K with pressures of up to 10 MPa.

Figure 14.

Figure 14

Measured points for R1234ze(E); ○, data of Lago et al.;43 other symbols indicate the measured isochores of the present work; replicates of the isochore starting at T = 290 K are indicated by ×, +, ○, and Δ in red (measured in that order). The critical point is indicated by a red ⊗.

Table 7. Experimental Speeds of Sound, w, for R1234ze(E) (trans-1,3,3,3-Tetrafluoroprop-1-ene) and the Combined Expanded (k = 2) Relative Uncertainty in the Speed of Sound, Uc, Given along with Relative Deviations from the Equation of State of Thol and Lemmon45a,b.
T (K) P (MPa) W (m·s–1) Uc (k = 2) (%) 100(w/wEOS – 1)
230.002 1.805 847.82 0.037 0.277
235.012 6.881 853.01 0.037 0.374
240.003 12.028 858.85 0.036 0.445
245.005 17.145 864.67 0.036 0.497
250.006 22.154 870.10 0.036 0.529
254.998 27.124 875.51 0.035 0.545
259.993 32.041 880.81 0.035 0.552
264.997 36.619 884.72 0.035 0.548
       
245.003 1.182 775.98 0.040 0.032
250.007 5.761 782.25 0.039 0.114
254.998 10.323 788.57 0.039 0.170
259.991 14.852 794.77 0.038 0.205
264.997 19.343 800.79 0.038 0.225
269.994 23.820 806.84 0.037 0.234
274.997 28.251 812.71 0.037 0.236
280.001 32.627 818.38 0.036 0.233
280.000 32.381 817.18 0.036 0.230
285.003 36.704 822.70 0.036 0.223
       
259.989 1.156 708.39 0.044 –0.171
264.995 5.196 715.06 0.043 –0.113
269.993 9.253 721.91 0.042 –0.076
274.996 13.299 728.68 0.041 –0.055
280.001 17.324 735.32 0.040 –0.046
285.003 21.311 741.75 0.040 –0.045
290.020 25.289 748.09 0.039 –0.048
295.000 29.203 754.21 0.038 –0.054
300.001 33.114 760.26 0.038 –0.060
       
274.993 0.898 639.06 0.051 –0.375
279.999 4.509 646.83 0.049 –0.336
285.000 8.093 654.31 0.048 –0.317
290.019 11.680 661.66 0.046 –0.310
294.999 15.217 668.73 0.045 –0.308
300.001 18.747 675.61 0.044 –0.312
305.015 22.268 682.33 0.043 –0.315
310.002 25.743 688.82 0.042 –0.318
315.013 29.216 695.18 0.041 –0.319
       
290.015 0.982 572.03 0.062 –0.621
294.997 4.109 580.28 0.059 –0.592
299.999 7.253 588.39 0.056 –0.574
305.014 10.390 596.19 0.054 –0.562
310.002 13.502 603.73 0.052 –0.553
315.012 16.618 611.09 0.050 –0.546
319.989 19.688 618.09 0.048 –0.539
324.995 22.761 624.94 0.047 –0.531
330.003 25.816 631.57 0.046 –0.526
334.988 28.795 637.70 0.045 –0.520
       
290.014 0.944 571.63 0.062 –0.628
294.994 4.096 580.17 0.059 –0.592
299.995 7.242 588.31 0.056 –0.574
305.010 10.355 595.92 0.054 –0.562
309.998 13.457 603.39 0.052 –0.554
315.010 16.569 610.72 0.050 –0.546
319.987 19.641 617.76 0.048 –0.539
324.992 22.709 624.58 0.047 –0.532
330.000 25.760 631.20 0.046 –0.527
334.987 28.739 637.33 0.045 –0.522
       
305.009 1.027 503.60 0.079 –1.029
309.995 3.735 512.66 0.074 –0.935
315.008 6.454 521.38 0.070 –0.858
319.987 9.153 529.70 0.066 –0.799
324.991 11.840 537.55 0.063 –0.755
330.001 14.544 545.32 0.060 –0.724
334.987 17.175 552.35 0.057 –0.702
339.993 19.815 559.28 0.055 –0.685
344.996 22.457 566.10 0.053 –0.675
349.994 25.085 572.73 0.051 –0.669
       
319.983 1.220 434.73 0.108 –1.548
324.988 3.522 444.60 0.100 –1.271
329.997 5.829 453.94 0.092 –1.074
334.985 8.099 462.43 0.086 –0.942
339.991 10.397 470.82 0.081 –0.855
344.996 12.681 478.77 0.076 –0.799
349.994 14.956 486.37 0.072 –0.771
355.015 17.243 493.80 0.068 –0.758
359.999 19.492 500.79 0.065 –0.757
365.017 21.752 507.64 0.062 –0.760
       
334.981 1.596 365.02 0.164 –1.955
339.988 3.498 375.73 0.147 –1.428
344.992 5.402 385.62 0.133 –1.100
349.990 7.311 394.92 0.122 –0.909
355.012 9.227 403.71 0.112 –0.805
359.999 11.128 411.99 0.103 –0.760
365.017 13.040 419.93 0.096 –0.751
370.011 14.940 427.50 0.090 –0.762
375.012 16.836 434.75 0.084 –0.784
380.024 18.733 441.77 0.080 –0.808
       
290.010 0.987 572.11 0.062 –0.621
294.990 4.125 580.45 0.059 –0.591
299.993 7.261 588.49 0.056 –0.572
305.008 10.401 596.32 0.054 –0.560
309.994 13.507 603.81 0.052 –0.551
315.006 16.616 611.10 0.050 –0.543
319.984 19.688 618.13 0.048 –0.535
324.988 22.759 624.95 0.047 –0.530
329.996 25.809 631.55 0.046 –0.525
334.984 28.790 637.67 0.045 –0.520
       
349.991 2.014 289.93 0.299 –2.015
355.013 3.504 301.63 0.256 –1.204
359.998 4.997 312.10 0.223 –0.809
365.016 6.511 321.87 0.196 –0.636
370.009 8.024 330.90 0.175 –0.598
375.012 9.546 339.54 0.158 –0.593
380.023 11.071 347.63 0.144 –0.653
385.014 12.589 355.45 0.132 –0.672
390.042 14.118 363.02 0.121 –0.690
395.039 15.639 369.99 0.113 –0.781
       
370.004 5.068 266.62 0.325 –0.448
375.008 6.337 276.38 0.279 –0.415
380.020 7.616 285.78 0.243 –0.352
385.011 8.895 294.24 0.215 –0.460
390.041 10.189 302.49 0.192 –0.517
395.039 11.476 310.22 0.174 –0.590
400.047 12.770 317.49 0.159 –0.710
405.054 14.063 324.76 0.146 –0.714
410.052 15.354 331.36 0.135 –0.827
       
395.036 7.969 241.00 0.334 0.350
400.044 8.987 248.17 0.293 –0.145
405.053 10.011 255.60 0.260 –0.340
410.052 11.036 262.98 0.233 –0.393
415.069 12.067 269.54 0.211 –0.626
420.072 13.099 276.34 0.192 –0.643
       
290.007 0.972 571.98 0.062 –0.620
294.987 4.102 580.26 0.059 –0.590
299.990 7.250 588.40 0.056 –0.573
305.004 10.400 596.32 0.054 –0.560
309.991 13.492 603.71 0.052 –0.550
315.002 16.613 611.10 0.050 –0.542
319.980 19.679 618.07 0.048 –0.537
324.986 22.751 624.90 0.047 –0.531
329.994 25.805 631.52 0.046 –0.525
334.981 28.789 637.67 0.045 –0.522
a

The listed data are averaged from 12 measured echo-delay times (4 sets of 3 replicates each); see Supporting Information for unaveraged data. The data are listed in the order measured; blank lines separate measured isochores.

b

The standard (k = 1) uncertainties in T and p are 0.005 K and (26 × 10–6p + 0.016 MPa), respectively.

Deviations of the present measurements from the EOS of Thol and Lemmon45 are shown in Figure 15; the RMS deviation is 0.68%, with an average deviation (bias) of −0.50%. The deviations range from −2.07 to +0.67%. Systematic deviations are observed for the individual isochores. The deviations are very smooth with temperature for the initial isochores. Significant scatter is observed only for the three isochores at the highest temperatures; these isochores were closer to the critical point, where the speed of sound was lower, the fluid was much more compressible, and the echo signals were much weaker. Four replicates of the isochore extending from (T = 290 K, p = 1.0 MPa) to (T = 335 K, p = 29 MPa) were measured, including one at the end of the testing; the speed of sound varied over a total range of 0.005% for replicate (T, p) state points, except at T = 290 K, where the total range was slightly higher at 0.013%. These results indicate the stability and repeatability of the pulse-echo system and negligible degradation of the fluid sample.

Figure 15.

Figure 15

Deviations between data for R1234ze(E) and the EOS of Thol and Lemmon;45 ○, Lago et al.43 Other symbols indicate the measured isochores of the present work and are the same as in Figure 14.

The data of Lago et al.43 were included in the EOS fit of Thol and Lemmon,45 and these data are fitted well (deviations of less than 0.17%) for T = (260 to 335) K, but the isotherm at 360 K shows deviations of up to 1.84%; the overall RMS deviation is 0.48%. At temperatures of 260 to 310 K, the data of Lago et al. are consistent with the present data, but at T = 360 K, p = 10 MPa, they are systematically higher by 2.62%. Similar deviations with our data were observed for the Lago et al. data for R1234yf. Lago et al. report a purity “assay” for their sample of 99.5% (mass basis) but details on the impurities were not provided, and thus the effect of impurities on the measured speed of sound cannot be determined.

3.6.3. R1233zd(E)—trans-1-Chloro-3,3,3-trifluoroprop-1-ene

R1233zd(E) or HCFO-1233zd(E) (“HCFO” = “hydrochlorofluoroolefin”) contains chlorine and has a small, but nonzero, ozone depletion potential (ODP) of 0.00024–0.00034.44 It has been SNAP-approved44 for use in centrifugal-type chillers, as a foam-blowing agent for polyurethane foams, as a cleaning solvent, and as a fire-suppression agent. R1233zd(E) was measured at temperatures from (230 to 420) K, with pressures of up to 25.6 MPa. Measurements were carried out along 22 isochores, including 4 replicates of the isochore extending from (T = 300 K, p = 0.9 MPa) to (T = 325 K, p = 18.7 MPa). The measured points are displayed in Figure 16.

Figure 16.

Figure 16

Measured points for R1233zd(E) and *, data of Lago et al.19 Other symbols indicate the isochores measured in the present work. Replicates of the isochore starting at T = 300 K are indicated by × , + , ○, and Δ in red (measured in that order). The critical point of 438.86 K, 3.358 MPa is off the scale of the plot.

Deviations of the present measurements from the EOS of Akaska and Lemmon46 are shown in Figure 17 and reported in Table 8. The EOS was fitted to these data. The RMS deviation is 0.054%, with a range of −0.189 to +0.122%. The deviations show a small systematic deviation with the temperature and increasing scatter at higher temperatures. The replicate isochores show a total range of 0.050% compared to the EOS. The final two replicates measured in the latter half of the testing were systematically 0.024% higher compared to the first replicate. While this is well within the uncertainty of the measurements (see section 4), we observed smaller differences for replicate measurements on other fluids, thus this difference could indicate a possible slight thermal degradation of the sample as the measurements progressed.

Figure 17.

Figure 17

Deviations between the present data for R1233zd(E) and the EOS of Akasaka and Lemmon.46 *, Data of Lago et al.19 Other symbols indicate the measured isochores and are the same as in Figure 16.

Table 8. Experimental Speeds of Sound, w, for R1233zd(E) (trans-1-Chloro-3,3,3-trifluoroprop-1-ene), with the Combined Expanded (k = 2) Relative Uncertainty in the Speed of Sound, Uc, Given along with Relative Deviations from the Equation of State of Akasaka and Lemmon46a,b.
T (K) P (MPa) W (m·s–1) Uc (k = 2) (%) 100(w/wEOS – 1)
229.999 1.036 970.99 0.035 –0.025
235.011 6.670 975.48 0.034 –0.047
240.001 12.266 980.12 0.034 –0.051
245.002 17.859 984.91 0.034 –0.041
250.004 23.418 989.74 0.034 –0.020
       
240.000 1.016 929.25 0.035 –0.060
245.003 6.402 934.58 0.035 –0.065
250.006 11.749 939.92 0.035 –0.055
254.996 17.092 945.40 0.035 –0.036
259.991 22.289 950.41 0.034 –0.005
       
250.002 1.018 888.18 0.036 –0.066
254.997 6.009 893.60 0.036 –0.060
259.991 10.962 898.98 0.036 –0.044
264.996 15.882 904.29 0.035 –0.020
269.992 20.762 909.57 0.035 0.011
274.996 25.613 914.80 0.035 0.048
       
259.988 1.008 847.69 0.038 –0.047
264.995 5.702 853.49 0.037 –0.041
269.992 10.366 859.26 0.037 –0.024
274.996 15.008 864.99 0.036 –0.001
280.000 19.622 870.65 0.036 0.029
285.002 24.192 876.19 0.036 0.064
       
269.990 0.978 807.48 0.039 –0.022
274.994 5.348 813.49 0.038 –0.018
280.000 9.715 819.54 0.038 –0.005
285.001 14.055 825.51 0.037 0.016
290.019 18.383 831.41 0.037 0.043
294.999 22.635 837.09 0.037 0.076
       
279.997 0.966 767.78 0.041 0.007
285.000 5.086 774.31 0.040 0.003
290.018 9.191 780.73 0.039 0.012
294.999 13.240 786.97 0.039 0.029
300.000 17.281 793.11 0.038 0.052
305.014 21.304 799.11 0.038 0.081
       
290.016 0.135 722.65 0.044 0.035
294.996 3.925 729.48 0.043 0.022
299.999 7.725 736.27 0.042 0.023
305.014 11.514 742.89 0.041 0.031
310.001 15.258 749.32 0.040 0.049
315.012 18.995 755.60 0.039 0.074
       
299.997 0.945 689.34 0.047 0.045
305.012 4.532 696.52 0.045 0.029
309.999 8.085 703.49 0.044 0.026
315.011 11.663 710.45 0.043 0.030
319.989 15.192 717.17 0.042 0.047
324.994 18.697 723.60 0.041 0.071
       
299.994 0.972 689.38 0.046 0.021
305.011 4.569 696.66 0.045 0.011
309.996 8.135 703.72 0.044 0.009
315.009 11.684 710.51 0.043 0.017
319.986 15.203 717.15 0.042 0.033
324.991 18.698 723.52 0.041 0.059
       
309.996 0.943 650.36 0.051 0.038
315.008 4.261 657.77 0.049 0.018
319.987 7.551 664.96 0.047 0.010
324.990 10.850 672.02 0.046 0.013
330.000 14.120 678.78 0.044 0.027
334.986 17.345 685.24 0.043 0.048
       
319.984 0.903 611.20 0.056 0.034
324.989 3.994 619.12 0.053 0.009
329.998 7.080 626.79 0.051 –0.001
334.986 10.109 633.92 0.049 0.000
339.991 13.140 640.87 0.048 0.008
344.995 16.157 647.63 0.046 0.026
       
329.996 1.155 574.60 0.062 0.018
334.984 3.984 582.58 0.059 –0.005
339.990 6.814 590.25 0.056 –0.018
344.994 9.647 597.76 0.054 –0.021
349.992 12.459 604.95 0.052 –0.011
355.013 15.270 611.92 0.050 0.007
       
339.987 0.985 533.73 0.072 –0.004
344.992 3.593 542.40 0.067 0.019
349.991 6.187 550.40 0.064 0.008
355.012 8.793 557.90 0.060 –0.044
359.998 11.371 565.32 0.058 –0.036
365.015 13.949 572.55 0.055 –0.004
       
349.988 0.584 488.94 0.086 –0.036
355.010 1.410 479.10 0.089 –0.041
359.996 3.686 487.77 0.083 –0.067
365.015 5.976 496.29 0.077 –0.046
370.008 8.250 504.10 0.073 –0.075
375.010 10.538 511.85 0.069 –0.076
       
299.989 0.917 689.16 0.047 0.046
305.006 4.481 696.21 0.045 0.033
309.993 8.021 703.12 0.044 0.032
315.004 11.566 709.92 0.043 0.040
319.983 15.067 716.48 0.042 0.057
324.987 18.566 722.89 0.041 0.080
       
359.996 0.972 453.06 0.102 –0.043
365.014 3.122 461.95 0.094 –0.074
370.008 5.264 470.67 0.087 –0.038
375.010 7.413 479.13 0.081 0.015
380.022 9.558 486.46 0.076 –0.077
385.011 11.689 493.96 0.072 –0.052
390.040 13.831 501.11 0.068 –0.050
       
370.003 1.195 414.41 0.125 –0.071
375.006 3.136 423.65 0.113 –0.094
380.019 5.084 432.90 0.104 –0.002
385.011 7.023 440.82 0.096 –0.101
390.040 8.970 449.37 0.089 0.034
395.038 10.905 456.68 0.084 –0.024
400.044 12.843 463.75 0.079 –0.068
       
380.015 1.176 369.80 0.165 –0.189
385.007 2.027 364.11 0.167 –0.095
390.037 3.700 373.82 0.150 –0.038
395.035 5.368 382.54 0.136 –0.102
400.044 7.044 391.16 0.124 –0.080
405.054 8.720 399.29 0.114 –0.068
410.051 10.389 407.03 0.106 –0.049
       
390.002 1.618 332.75 0.213 –0.155
394.999 3.140 342.91 0.188 –0.045
400.009 4.675 352.43 0.167 0.002
405.019 6.213 361.31 0.151 0.023
410.017 7.755 369.76 0.137 0.033
415.034 9.309 377.67 0.126 –0.017
420.037 10.856 385.08 0.116 –0.078
       
400.006 1.995 292.98 0.293 –0.071
405.015 3.322 303.52 0.253 0.117
410.015 4.657 312.94 0.222 0.103
415.033 6.005 322.01 0.197 0.122
420.037 7.355 330.51 0.177 0.106
       
299.986 0.956 689.62 0.047 0.069
305.000 4.539 696.79 0.045 0.054
309.989 8.080 703.68 0.044 0.052
315.001 11.604 710.32 0.043 0.060
319.977 15.110 716.90 0.042 0.076
324.984 18.616 723.34 0.041 0.099
314.999 11.602 710.35 0.043 0.066
324.983 18.590 723.19 0.041 0.100
       
299.985 0.892 689.14 0.047 0.069
309.988 8.010 703.20 0.044 0.051
305.001 4.456 696.20 0.045 0.056
a

The listed data are averaged from 12 measured echo-delay times (4 sets of 3 replicates each); see Supporting Information for unaveraged data. The data are listed in the order measured; blank lines separate measured isochores.

b

The standard (k = 1) uncertainties in T and p are 0.005 K and (26 × 10–6p + 0.016 MPa), respectively.

Lago et al.19 measured R1233zd(E) along six isotherms from 273 to 353 K with pressures of up to 35 MPa, as shown in Figure 16. The Lago et al. data are consistently lower than the present data and the EOS of Akaska and Lemmon46 as shown in Figure 17; the average deviation is −0.383%.

3.6.4. R1336mzz(Z)—cis-1,1,1,4,4,4-Hexafluorobut-2-ene

R1336mzz(Z) is of interest as a refrigerant in chillers and as a working fluid in organic Rankine-cycle power systems. It has also been SNAP approved44 as a foam-blowing agent and cleaning solvent. R1336mzz(Z) (also known as HFO-1336mzz(Z)) is a component of the azeotropic mixture with trans-1,2-dichloroethene, which is designated as R514A in ANSI/ASHRAE Standard 34;36 this blend has been commercialized for use in centrifugal-type refrigeration compressors.

Here, we report speed-of-sound measurements for R1336mzz(Z) at temperatures from (230 to 420) K, with pressures of up to 46 MPa. The measurements were carried out along 15 isochores, including 4 replicates of the isochore extending from (T = 290 K, p = 0.9 MPa) to (T = 350 K, p = 42.9 MPa). The measured points are displayed in Figure 18 and reported in Table 9.

Figure 18.

Figure 18

Measured points for R1336mzz(Z). Different symbols indicate the measured isochores. Replicates of the isochore starting at T = 290 K are indicated by × , + , ○, and Δ in red (measured in that order). The critical point of 444.5 K, 2.903 MPa is off the scale of the plot.

Table 9. Experimental Speeds of Sound, w, for R1336mzz(Z) (cis-1,1,1,4,4,4-Hexafluorobut-2-ene), with the Combined Expanded (k = 2) Relative Uncertainty in the Speed of Sound, Uc, Also Given along with Relative Deviations from the Equation of State of McLinden and Akasaka15a,b.
T (K) P (MPa) W (m·s–1) Uc (k = 2) (%) 100(w/wEOS – 1)
230.001 0.690 890.80 0.036 –0.033
235.011 6.133 895.90 0.035 –0.015
240.003 11.557 901.15 0.035 –0.006
245.011 16.982 906.51 0.035 0.000
250.008 22.349 911.84 0.035 0.005
255.000 27.667 917.13 0.034 0.009
259.991 32.983 922.55 0.034 0.013
264.998 38.176 927.57 0.034 0.019
       
245.008 1.010 832.01 0.037 –0.025
250.007 6.001 837.95 0.037 –0.020
254.997 10.946 843.83 0.036 –0.015
259.991 15.845 849.60 0.036 –0.011
264.998 20.691 855.19 0.036 –0.008
269.994 25.507 860.77 0.035 –0.007
274.997 30.284 866.25 0.035 –0.006
280.002 35.027 871.66 0.035 –0.005
285.003 39.722 876.95 0.035 –0.003
290.021 44.391 882.16 0.034 –0.001
         
259.987 0.901 773.45 0.039 –0.010
264.995 5.359 779.58 0.039 –0.010
269.993 9.820 785.85 0.038 –0.012
274.996 14.257 792.04 0.037 –0.012
280.002 18.657 798.09 0.037 –0.014
285.003 23.020 803.99 0.037 –0.017
290.022 27.366 809.81 0.036 –0.020
295.001 31.638 815.43 0.036 –0.024
300.003 35.903 821.00 0.036 –0.025
305.017 40.140 826.46 0.035 –0.025
310.003 44.320 831.80 0.035 –0.022
       
274.993 0.674 715.73 0.042 0.001
279.998 4.721 722.55 0.041 –0.003
285.001 8.744 729.24 0.040 –0.005
290.019 12.752 735.79 0.040 –0.010
294.999 16.677 741.98 0.039 –0.018
300.001 20.612 748.17 0.038 –0.025
305.016 24.544 754.28 0.038 –0.032
310.003 28.423 760.22 0.037 –0.038
315.015 32.292 766.05 0.037 –0.040
319.991 36.101 771.69 0.037 –0.042
324.996 39.899 777.24 0.036 –0.040
330.003 43.670 782.67 0.036 –0.035
       
290.015 0.889 662.22 0.046 0.008
294.995 4.513 669.38 0.044 0.004
299.998 8.136 676.40 0.043 –0.002
305.013 11.751 683.25 0.042 –0.010
309.999 15.324 689.89 0.042 –0.020
315.013 18.901 696.42 0.041 –0.028
319.990 22.419 702.67 0.040 –0.036
324.996 25.937 708.82 0.039 –0.042
330.003 29.430 714.81 0.039 –0.046
334.988 32.848 720.44 0.038 –0.048
339.993 36.281 726.10 0.038 –0.048
       
290.013 0.799 661.60 0.046 0.009
294.994 4.420 668.78 0.044 0.007
299.996 8.044 675.82 0.043 –0.001
305.011 11.658 682.70 0.042 –0.009
309.998 15.228 689.33 0.042 –0.019
315.010 18.798 695.84 0.041 –0.027
319.988 22.316 702.11 0.040 –0.035
324.994 25.829 708.26 0.039 –0.041
330.001 29.322 714.26 0.039 –0.045
334.988 32.737 719.89 0.038 –0.047
339.994 36.162 725.52 0.038 –0.047
344.998 39.569 731.06 0.037 –0.046
349.994 42.948 736.46 0.037 –0.043
       
305.008 0.774 607.69 0.051 0.010
309.995 4.014 615.20 0.049 0.009
315.008 7.255 622.52 0.048 0.005
319.985 10.473 629.65 0.046 –0.004
324.990 13.691 636.60 0.045 –0.014
329.999 16.885 643.29 0.044 –0.022
334.986 20.007 649.50 0.043 –0.032
339.992 23.149 655.74 0.042 –0.039
344.997 26.279 661.86 0.041 –0.045
349.994 29.390 667.84 0.041 –0.048
355.016 32.494 673.69 0.040 –0.049
360.000 35.557 679.36 0.040 –0.049
365.018 38.617 684.91 0.039 –0.047
370.011 41.647 690.34 0.039 –0.042
375.013 44.656 695.63 0.038 –0.036
       
319.980 0.866 555.63 0.059 0.019
324.986 3.756 563.45 0.056 0.024
329.995 6.644 571.05 0.054 0.023
334.982 9.488 578.17 0.052 0.013
339.988 12.349 585.23 0.050 0.003
344.993 15.196 592.07 0.049 –0.008
349.991 18.022 598.66 0.047 –0.017
355.012 20.849 605.11 0.046 –0.026
359.998 23.645 611.36 0.045 –0.032
365.016 26.444 617.48 0.044 –0.036
370.010 29.215 623.42 0.043 –0.037
375.013 31.980 629.24 0.042 –0.037
380.024 34.723 634.88 0.042 –0.034
385.014 37.440 640.35 0.041 –0.032
390.043 40.164 645.76 0.040 –0.027
395.040 42.854 651.01 0.040 –0.021
400.047 45.534 656.16 0.039 –0.014
       
334.976 0.903 503.45 0.070 0.027
339.983 3.459 511.60 0.066 0.038
344.988 6.011 519.44 0.063 0.039
349.986 8.552 526.97 0.060 0.033
355.008 11.097 534.26 0.058 0.024
359.994 13.616 541.26 0.055 0.014
365.012 16.141 548.06 0.053 0.003
370.006 18.645 554.63 0.052 –0.006
375.009 21.136 560.96 0.050 –0.013
380.021 23.625 567.27 0.049 –0.002
385.012 26.090 573.17 0.048 –0.021
390.041 28.574 579.14 0.046 –0.020
395.039 31.008 584.79 0.045 –0.017
400.047 33.444 590.36 0.045 –0.014
405.055 35.871 595.83 0.044 –0.008
410.053 38.283 601.17 0.043 –0.002
415.070 40.695 606.44 0.042 0.006
420.073 43.086 611.57 0.042 0.016
       
290.007 0.841 662.08 0.046 0.033
294.988 4.444 669.12 0.044 0.031
299.990 8.064 676.14 0.043 0.025
305.006 11.675 682.99 0.042 0.017
309.992 15.247 689.63 0.042 0.007
315.004 18.819 696.16 0.041 –0.002
319.982 22.342 702.45 0.040 –0.010
324.986 25.860 708.61 0.039 –0.016
329.994 29.353 714.61 0.039 –0.020
334.982 32.769 720.24 0.038 –0.023
339.986 36.195 725.86 0.038 –0.024
344.991 39.587 731.33 0.037 –0.022
349.989 42.900 736.44 0.037 –0.018
       
349.988 0.989 451.60 0.087 0.021
355.010 3.232 460.37 0.081 0.104
359.995 5.457 468.15 0.076 0.055
365.013 7.692 476.00 0.072 0.079
370.006 9.916 483.41 0.068 0.068
375.009 12.137 490.42 0.065 0.029
380.020 14.355 497.39 0.062 0.032
385.011 16.553 504.08 0.060 0.039
390.040 18.764 510.43 0.058 0.005
395.038 20.952 517.16 0.056 0.095
400.045 23.136 523.02 0.054 0.050
405.054 25.316 528.73 0.052 0.005
410.052 27.482 534.50 0.051 0.006
415.070 29.651 540.09 0.050 –0.007
420.072 31.808 545.71 0.048 0.014
       
365.004 0.867 396.29 0.116 0.029
369.999 2.778 404.95 0.107 0.042
375.002 4.698 413.34 0.099 0.066
380.015 6.619 421.23 0.092 0.054
385.006 8.531 428.90 0.086 0.072
390.036 10.453 435.85 0.081 –0.014
395.034 12.362 443.06 0.077 0.028
400.042 14.273 449.83 0.073 0.020
405.052 16.182 456.57 0.069 0.056
410.050 18.083 462.79 0.067 0.027
415.069 19.987 468.91 0.064 0.013
420.072 21.883 475.13 0.061 0.060
       
380.013 1.047 343.10 0.162 0.006
385.005 2.664 352.08 0.146 0.040
390.034 4.300 360.80 0.133 0.092
395.033 5.930 368.75 0.122 0.053
400.041 7.565 376.40 0.113 0.025
405.051 9.202 383.58 0.105 –0.039
410.050 10.838 390.90 0.098 0.010
415.068 12.483 397.86 0.092 0.020
420.072 14.116 404.49 0.087 0.033
       
394.998 1.269 288.13 0.250 0.072
400.007 2.607 297.47 0.219 0.100
405.017 3.953 306.20 0.194 0.092
410.016 5.305 314.36 0.174 0.043
415.035 6.669 322.32 0.158 0.047
420.038 8.032 329.88 0.144 0.052
       
290.006 0.858 662.20 0.046 0.033
294.988 4.472 669.31 0.044 0.031
299.989 8.097 676.34 0.043 0.022
305.004 11.707 683.18 0.042 0.014
309.991 15.254 689.68 0.041 0.007
315.003 18.816 696.14 0.041 –0.001
319.981 22.331 702.40 0.040 –0.008
324.986 25.839 708.51 0.039 –0.015
329.993 29.326 714.48 0.039 –0.020
334.980 32.736 720.08 0.038 –0.023
339.986 36.158 725.69 0.038 –0.024
344.990 39.534 731.08 0.037 –0.021
349.987 42.803 735.99 0.037 –0.017
a

The listed data are averaged from 12 measured echo-delay times (4 sets of 3 replicates each); see Supporting Information for unaveraged data. The data are listed in the order measured; blank lines separate measured isochores.

b

The standard (k = 1) uncertainties in T and p are 0.005 K and (26 × 10–6p + 0.016 MPa), respectively.

Deviations of the present measurements from the EOS of McLinden and Akasaka15 are shown in Figure 19. The present data were included in the fitting of this EOS, which was also fitted to the vapor pressure, p–ρ–T, saturated liquid density, heat capacity, and vapor-phase speed-of-sound data. The RMS deviation to the EOS is 0.033%, with an average offset of −0.0005%. The overall range of the deviations is −0.049 to +0.104%. The individual isochores show smooth and systematic deviation patterns except for larger scatter for the higher-temperature isochores; these could arise from small systematic errors in the present measurements, small inconsistencies between the different data types used in the EOS fitting, or small defects in the form of the EOS, such that it was not able to simultaneously fit the different data types. The final replicate of the T = (290 to 350) K isochore was systematically 0.025% higher than the first replicate, indicating possible slight degradation of the sample as the measurements progressed. There are no literature data for comparison.

Figure 19.

Figure 19

Deviations between present data for R1336mzz(Z) and the EOS of McLinden and Akasaka.15 Different symbols indicate the measured isochores and are the same as in Figure 18.

4. Uncertainty of the Measurements

The measurement of the speed of sound essentially reduces to the measurement of geometry (i.e., the difference in the path lengths) and time (i.e., the difference in the arrival time of the short-path and long-path echoes). Both geometry and time can be measured with extremely low uncertainties, and the potential for low uncertainties is one of the major advantages of measuring the speed of sound over other quantities (such as heat capacity) that would yield similar thermodynamic information for the purposes of fitting an equation of state. But other factors increase the uncertainties in the measurement and must be considered carefully. These can be grouped into uncertainties resulting from the analysis of the echo signals; determination of the geometry (i.e., the calibration and stability of the path length difference); correction for diffraction and dispersion effects; the determination of the thermodynamic (T, p, x) state point; and effects related to the purity and stability of the fluid sample. In this discussion, we consider standard (k = 1) uncertainties and apply a coverage factor when combining the individual uncertainty components to arrive at a combined expanded uncertainty.

4.1. Uncertainty of the Measured Echo Signals

The echo signals were detected and recorded with a digital storage oscilloscope. The time bases of the oscilloscope and function generator were synchronized to a 10 MHz rubidium frequency standard (Stanford Research Systems DG645) with a relative short-time stability of 1 × 10–10 and long-term stability of 5 × 10–10 per year. The uncertainty in the speed of sound is directly proportional to this uncertainty, so the uncertainty from timing was negligible.

An additional uncertainty is associated with the determination of the Δt between the two echoes. The time delay for the 12 replicate echo measurements carried out at each (T, p) state point was typically consistent within a few parts in 106. Occasionally (most often near the critical point), a larger variance was observed; this occurred because the data analysis algorithm superimposed the short-path and long-path echoes, and this could be in error by one or two cycles (i.e., 0.125 or 0.250 μs) with echo signals that were weak or noisy or where low damping in the fluid resulted in prolonged resonance of the crystal. State points with a large variance were manually examined, and faulty replicates were discarded. This effect was observed at speeds of sound lower than about 600 m·s–1, i.e., near the critical point, but only for propane, R1234yf, and R1234ze(E) for which 11 to 19% of the echoes were suspect. These three fluids were the first ones measured. No such problems were observed for p-xylene, R1233zd(E), or R1336mzz(Z), for which we separately recorded the short-path and long-path echoes, as described in section 2.5; for these fluids, the speed of sound was as low as 292 m·s–1. The estimated relative uncertainty associated with the determination of the time difference (after discarding suspect signals) was estimated to be 0.001%.

4.2. Path-Length Difference

As discussed in section 3.2, the path-length difference was calibrated as a function of the temperature and pressure with measurements on propane. The propane equation of state28 was fitted to the liquid-phase speed-of-sound data of Meier and Kabelac,18 and thus, the uncertainty in the path-length calibration is dependent on the uncertainties in the Meier and Kabelac18 data. Their data have an estimated expanded relative uncertainty of 0.019–0.022%, including purity effects. The propane EOS28 fits these data with an RMS deviation of 0.013%. The RMS deviation of our propane data from the path-length correlation (eq 13) was 0.0035%. Combining these three effects in quadrature yields a standard uncertainty of 0.017% due to the propane calibration.

Related to the uncertainty in the calibration of the path-length difference is the mechanical stability of the overall assembly comprising the crystal, spacers, and reflectors. Repeated measurements on propane taken over the course of 25 months revealed average differences of less than 0.005% as reported by Rowane et al.,29 and we take 0.005% as the standard uncertainty associated with the mechanical stability of the path lengths.

Any corrosion of the reflector faces, especially corrosion that affected one reflector more than the other, would alter the effective path length difference. We did not observe any corrosion on our brass reflectors upon disassembly after the completion of all of the tests reported here, and we consider any uncertainty associated with corrosion to be negligible.

4.3. Diffraction Correction

The time difference was corrected for diffraction effects, as discussed in section 2.7. Meier9 reported a difference of 0.001% among the different models used to calculate this correction for his (similar) pulse-echo instrument, and we take 0.001% as the uncertainty in this correction.

4.4. Possible Dispersion Effects

Dispersion can present problems; it occurs when the vibration period of the ultrasonic pulse is short relative to the relaxation time of the molecule’s internal degrees of freedom, resulting in a measured speed of sound that is not equal to the thermodynamic value. Dispersion was observed, for example, by El Hawary et al.48 for their measurements on isopentane, characterized by a significant damping of the echo signal.

Dispersion is more common with higher operating frequencies. Our frequency of 8 MHz is near the upper end of the pulse-echo instruments; lower frequencies would result in a longer pulse duration and the possibility of overlap between the short- and long-path echoes and the attendant need for longer path lengths. Thus, there is a design compromise, and we opted for a compact cell.

We did not observe any evidence of dispersion in the present measurements and considered the effects of dispersion to be negligible.

4.5. State-Point Uncertainty

The uncertainty in the temperature measurement system (SPRT and its calibration, resistance bridge, and standard resistor) was estimated to be 3 mK. The SPRT was calibrated with fixed-point cells on ITS-90. The uncertainty in the temperature of the fluid sample also included the effects of temperature gradients and short-term variations in the thermostat bath, and we estimated the total temperature uncertainty to be 5 mK. The uncertainty in the pressure measurement arose from the calibration of the transducers, their repeatability and zero (vacuum) drift, and the uncertainty in the hydrostatic head correction. We estimated the standard uncertainty in the pressure transducer to be (26 × 10–6p + 7 kPa), based on the uncertainties of the piston-gage pressure standards used for the calibration and the fit of the transducer coefficients to the piston-gage calibration points. The observed vacuum drift of the transducer adds (in quadrature) an additional 7 kPa. We estimate the uncertainty in the hydrostatic head correction to be 10% of the correction. The standard deviations in the observed temperature and pressure readings taken before, during, and after recording the echo signals were added to these uncertainty estimates as a type A uncertainty.

The effect of these state-point uncertainties on the speed of sound is given by

4.5. 16

where the derivatives are estimated from the equation of state for the fluid being measured. The temperature effect was relatively constant from 0.008 to 0.011 m·s–1; the pressure effect ranged from 0.013 to 0.093 m·s–1 and increased as the critical point was approached.

4.6. Sample Purity and Stability

The state point also depends on the composition of the sample. This includes not only impurities in the fluid sample but also contamination that might be introduced by the system and possible decomposition of the sample during the course of the testing. This uncertainty component varied from fluid to fluid. The impurities in the propane and water samples were negligible. But, as noted in section 3.4, the water measurements resulted in corrosion and the sample removed following the first series of tests was discolored, but any corrosion was assumed to occur only at high temperatures and such points were not included in the analysis. Degradation of the p-xylene was observed upon measurement of replicate isochores at the level of 0.021%; also, as noted in section 3.5, impurities in the p-xylene sample resulted in a systematic error in the speed of sound of 0.006 to 0.010%. Replicate measurements of the refrigerants indicated stability effects of 0.013 to 0.025%. All of these were the maximum differences among replicates, which we take as expanded uncertainties with a coverage factor of 3. This effect was added as a linear function of the time that the sample was in the instrument. We had insufficient knowledge of impurities in the refrigerant samples to estimate this effect with any certainty, and we assign a conservative standard uncertainty of 0.005%. These effects are summarized in Table 10.

Table 10. Summary of Errors and Resulting Uncertainty in the Speed of Sound.

    Range of Uncertainties in Speed of Sound/(m·s–1, unless Indicated)
Source Magnitude of Error (k = 1) p-xylene R1234yf R1234ze(E) R1233zd(E) R1336mzz(Z)
State Point
Temperature 0.005 Ka 0.008 to 0.010 0.010to 0.011 0.009 to 0.010 0.008 to 0.011 0.010 to 0.010
Pressure 26 × 10–6p + 10 kPaa 0.014 to 0.036 0.023to 0.088 0.016 to 0.093 0.013 to 0.083 0.017 to 0.074
Path-Length Difference
ΔL (Tp) 0.017% 0.145 to 0.241 0.045 to 0.124 0.039 to 0.150 0.050 to 0.168 0.050 to 0.158
ΔL (t) (stability) 0.005% 0.043 to 0.071 0.013 to 0.037 0.012 to 0.044 0.015 to 0.049 0.014 to 0.046
Fitting of and Corrections to Echo Data
Δt 0.001% 0.009 to 0.014 0.003 to 0.007 0.002 to 0.009 0.003 to 0.010 0.003 to 0.009
Diffraction 0.001% 0.009 to 0.014 0.003 to 0.007 0.002 to 0.009 0.003 to 0.010 0.003 to 0.009
Sample Purity and Stability
Sample impurities (Varies with fluid) (0.006 to 0.010)% 0.005% 0.005% 0.005% 0.005%
Sample instability (Varies with fluid) 0.007% 0.008% 0.004% 0.008% 0.008%
Combined and Expanded Uncertainties
Relative combined expanded (k = 2.2) uncertainty (0.033 to 0.048)% (0.040 to 0.256)% (0.035 to 0.334)% (0.034 to 0.293)% (0.034 to 0.250)%
Average relative combined expanded (k = 2.2) uncertainty 0.035% 0.088% 0.086% 0.068% 0.055%
a

Plus Type A uncertainty arising from standard deviation of multiple temperature or pressure readings

4.7. Summary of Uncertainties

The relative combined expanded standard uncertainty Uc,i for a given measurement i, expressed as a percentage, is given by

4.7. 17

where the summation is over the individual uncertainty components discussed in sections 4.1 through 4.6 and 2.20 is a coverage factor corresponding to a 95% confidence interval, based on 12 echo signals measured at each state point. A tabulation of the individual uncertainty components for each measured point is given in the Supporting Information, and a summary of the uncertainties for each of the fluids is given in Table 10. The average Uc ranged from 0.035 to 0.088% for the different fluids and increased as the critical point was approached; we measured the refrigerants as close to the critical point as the signal strength allowed, and these had the highest uncertainties. All of the measurements on p-xylene (Tcrit = 616.2 K) were well below the critical point, and this fluid had the lowest average uncertainty.

5. Discussion and Conclusions

A dual-path, pulse-echo apparatus has been developed at NIST for measurement of the liquid-phase speed of sound. It operates over a temperature range of 228.15 to 423.15 K, with pressures of up to 93 MPa. While it implements a standard and well-proven technique, our instrument has several unique features. We employ a 2.5:1 ratio of path lengths compared to the more typical 1.5:1 ratio; the larger ratio gives a greater time resolution and allows a longer time for the short-path echo to damp out before the arrival of the long-path echo. The quartz crystal transducer is clamped between ceramic spacers. This simple mounting arrangement has proven to be reliable and yielded repeatable time-of-flight measurements. This mounting method, together with the design of the electrical contacts, results in a smaller sample volume compared with some other designs. The electrical feed through is a custom design.

The echo signals were automatically detected and recorded with custom instrument control software; this made extensive use of the signal processing capabilities of our modern digital oscilloscope. We averaged many echo signals (typically 256), again using the capability of the oscilloscope, and this reduced the noise in the signal and allowed a simple fitting of the data to evaluate the time delay; other authors using a single echo often require a fast Fourier transform (FFT) analysis to deal with a noisy signal. Our data analysis was done entirely off-line, and this simplified the automation of the instrument compared to the double-pulse/cancellation-of-echoes method.

We calibrated the path lengths of the instrument with measurements on propane. This calibration was nearly identical to the one based on a direct measurement of the spacer lengths at room temperature. The propane calibration also compared closely with a calibration (over a more limited range of temperatures) with water. We verified the overall performance of the instrument by comparing to recent, high-accuracy measurements on p-xylene. The average expanded combined uncertainty in the speed of sound for this instrument ranged from 0.035 to 0.088% for the different fluids based on a detailed analysis.

This instrument was used to determine the liquid-phase speed of sound of four “new” low-GWP refrigerants over a combined temperature and pressure range of (230 to 430) K with pressures of up to 50 MPa. There are very limited liquid-phase speed-of-sound data reported in the literature for these fluids, and the present data are the first reported for R1336mzz(Z). These data were used in developing high-accuracy, wide-ranging equations of state for three of the fluids.

Acknowledgments

We gratefully acknowledge Robert Gomez and Michael Rybowiak of NIST for fabricating the instrument described here. We found the habilitation thesis of Karsten Meier9 of Helmut-Schmidt-Universität to be a very helpful textbook on the pulse-echo technique. We appreciate helpful discussions with Martin Trusler of Imperial College London as we developed this instrument. We carried out the measurements on p-xylene in cooperation with Saif Al Ghafri of the University of Western Australia during his visit to NIST. Robin Wegge of Ruhr-Universität Bochum assisted with the setup and automation of the instrument during his visit to NIST. Finally, we thank Honeywell and Chemours for the donation of the refrigerant samples. This work was funded by the National Institute of Standards and Technology and was carried out in the normal course of our duties as research staff.

Supporting Information Available

The Supporting Information is available free of charge at https://pubs.acs.org/doi/10.1021/acs.iecr.3c01720.

  • Additional figures showing details of the instrument and an example of weak echo signals (PDF)

  • All measured values from which the average values reported in the tables in the main text were calculated and details on the uncertainties for each measured point. (TXT)

Author Contributions

Contribution of the National Institute of Standards and Technology. Not subject to copyright in the United States.

The authors declare no competing financial interest.

Supplementary Material

ie3c01720_si_001.pdf (7.2MB, pdf)
ie3c01720_si_002.zip (136.1KB, zip)

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Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Data Citations

  1. Diky V.; Muzny C.; Smolyanitsky A.; Bazyleva A.; Chirico R.; Magee J.; Paulechka Y.; Kazakov A.; Townsend S.; Lemmon E.; Frenkel M.; Kroenlein K.. ThermoData Engine (TDE). NIST Standard Reference Database 103b, version 10.1 (Pure Compounds, Binary Mixtures, Ternary Mixtures, and Chemical Reactions), Standard Reference Data Program; National Institute of Standards and Technology: Gaithersburg, MD, 2016.

Supplementary Materials

ie3c01720_si_001.pdf (7.2MB, pdf)
ie3c01720_si_002.zip (136.1KB, zip)

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