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Ultrasound techniques use the interaction of high-frequency sound waves with matter, in order to generate information about the physico-chemical properties. Such measurements have been established in numerous areas, like medicine, oceanography or material sciences. Therefore it became obvious to use ultrasound measurements to characterize also other systems, e.g. topical formulations. A number of publications could already demonstrate that ultrasound can be successfully used to measure the average particle size, the creaming, the crystallization and the aggregation in dispersed systems. Basic principles Ultrasound means acoustic signals in the frequency range from 10 kHz up to approx. 30 MHz. When such a sound wave propagates in a material it forces particles to oscillate. They oscillate around their equilibrium positions with a frequency equal to that of the ultrasonic wave. The movement can be parallel to the direction of propagation, so that the sound wave generates a compressional wave. If the movement is be perpendicular to the direction of propagation, a shear wave is generated (Figure 1).
An ultrasonic wave is characterized by its amplitude, frequency, wavelength, and attenuation coefficient. The first two are predetermined by the investigator whereas the latter two depend on the material through which the ultrasonic wave is passing. As the ultrasonic velocity is the product of wavelength and frequency, it is also characteristic of a particular material. Measurable parameters Ultrasound measurements make use of three different parameters:
The velocity of an ultrasonic wave through a material depends on its physical properties. For weakly attenuation materials a simple relationship can be derived:
where c is the ultrasonic velocity, Hence, the ultrasonic velocity increases with decreasing density and increasing resistance to deformation. Since differences in the elastic moduli of materials are greater than those in density, the ultrasonic velocity is more influenced by the former quantity than by the latter. Moreover, the ultrasonic velocity through a material depends strongly on the temperature. The velocity through water and electrolyte solution increase with increasing temperature whereas that through oil shows a negative temperature coefficient (Figure 2).
Experimental techniques Ultrasonic measurements can be performed using either pulsed or continuous wave ultrasound. Most commercial applications use pulse techniques because such instruments are easy to operate, the measurements are non-invasive, rapid, and can readily be automated. The simplest and most widely used technique to measure ultrasonic velocity is the so-called pulse-echo technique. Figure 3 displays schematically a typical experimental set-up.
A signal pulse propagates through a sample with the path length d and is reflected at the opposite wall of the cell producing an echo. Each echo travels a distance equal to twice the cell length d before it reaches again the transducer (Figure 6). By measuring the time delay between two echoes t the ultrasonic velocity c can be calculated according c = 2d/t.
Applications Determination of disperse phase volume fraction This application makes use of the fact that the ultrasonic properties of an emulsion or suspension vary significantly with varying disperse phase volume fraction. This implies, however, that a significant difference between the ultrasonic velocity of the continuous and the disperse phase exists at a certain measuring temperature (compare Figure 2). Such measurements for the determination of the disperse phase volume fraction can be evaluated using a simple mathematical equation, often referred to as the URICK equation, which relates the ultrasonic velocity c to
where The URICK equation, however, neglects scatter of ultrasound which takes place in most real systems. Thus, more precise evaluation needs sophisticated modifications of that simple relationship. Figure 6 illustrates the ultrasonic velocity through a typical water-in-oil emulsion in dependence from the oil content.
Determination of creaming in emulsions As the continuous and disperse phases have different densities, emulsions show phase separation. In an oil-in-water emulsion the droplets of the usually less dense oil phase move upwards under the influence of gravity and form a cream layer. In contrast, the water droplets in water-in-oil emulsions move downwards due to their higher density compared to the continuous oil phase. They form a sediment. Thus an initially (t = t0) uniformly dispersed emulsion separates with time (t = tx). The disperse phase volume fraction varies as a function of sample height and time. This can be measured easily by ultrasonic measurements when the velocity in a sample cell is determined as a function of height and time (Figure 7).
For sufficiently precise ultrasonic measurements it is always necessary to carefully control the temperature. In practice, deviations of less than 0.1 °C are intended. Moreover, the sample cells have to be calibrated, i.e. the cell length as a function of height has to be determined. This calibration preferentially uses the double-echo technique with water-filled sample cells. Since the ultrasonic velocity of water is known the cell length can be calculated from the time delay between the first and the second echo (Figure 8). Under such conditions ultrasonic measurements can be performed very precisely, i.e. the ultrasonic velocity (approximately 1500 m/s) can be measured easily with a precision of 1 m/s.
For serial investigations the method can be fully automated. The experimental set-up is given schematically in Figure 9. A carousel automatically positions up to 6 sample cells to the site of measurement. There, a transducer pair (transmitter and receiver) is vertically positioned by a stepper motor drive in 1 mm steps. The measurement uses the pulse-echo technique. Data are evaluated automatically with an EXCEL© based computer programme.
Figure 10 shows some typical results obtained with such an instrument. The samples used are HPMC-stabilized (Hydroxypropylmethylcellulose) hydro-dispersion gels. These systems display different shelf-lives in dependence of the substitution type of HPMC used: Hydro-dispersion gels with HPMC 2906 show no changes in disperse phase distribution within 4 weeks storage in a temperature cycling test (-5/+40 °C). Formulations using HPMC 2208 show first incidence of creaming after one week. This sign of instability becomes more and more obvious during the following weeks. Rapid creaming characterizes systems with HPMC 2910. These hydro-dispersion gels show almost complete phase separation after one week storage.
Particle sizing A further application prospect of ultrasonic measurement is the in situ particle size measurement. This field of application makes use of the fact that at a distinct phase volume fraction the ultrasonic velocity and attenuation varies with particle size and frequency (Figure 11).
Particle size distribution can be calculated from the raw data through complex mathematical algorithms when several physical constants of the system are known. References
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