![]() ·Table of Contents ·Civil Engineering | Fabrication of a piezoelectric impact hammer and its application to the measurements of in-situ wave velocities of ConcreteJ. -H. Tong, T. -T. Wu, C.-K. LeeInstitute of Applied Mechanics, National Taiwan University, Taipei, TAIWAN e-mail: wutt@spring.iam.ntu.edu.tw Contact |
Recently, Wu and Fang [7] proposed a method for determining the elastic wave velocities of a concrete specimen using transient elastic waves. In the method, the Rayleigh wave velocity is determined based on the cross correlation of the surface responses and the longitudinal wave velocity is determined by measuring the wave-front arrival of the skimming longitudinal wave. The proposed method is based on the measurements of horizontally polarized surface responses. The longitudinal wave-front can be identified from the surface response directly. In the above-mentioned method, a hand held steel ball impactor was used to generate the elastic waves. However, due to the difficulty in controlling the impact force and the time origin, the averaging method, which is commonly adopted in ultrasonics to improve the signal to noise ratio, cannot be applied. In addition, on lacking the information of the impact time origin, the application of the point-source/point-receiver technique to the imaging of crack in concrete has some limitations.
To reduce the noise level in the stress wave measurements on concrete, Popovics et al. [8] used a DC-powered solenoid with a spring-loaded steel shaft as the stress wave source and thus reduced the noise level by averaging the repeated impact signals. However, a quantitative report of the noise level reduction has not been included. In addition, the time origin of the impact is still hard to find. On the other hand, the wave-guide concept has been applied to design a high speed piezoelectric driven system for application in the printer industry by Chang and Wang [9,10]. Later, the mechanism was improved by Lee and Wu [11], which add an on-line load cell to detect the impact force for micro-impact applications such as the study of the mechanical properties of amorphous carbon under high rate indentation. The high speed piezoelectric hammer has also been applied recently to the structural modal testing of small metallic structure to give precise impact timing and positioning by Lee et al. [12]. To the best of the authors' knowledge, application of the wave-guide based piezoelectric hammer to the NDE of concrete structure has not been reported.
In this paper, a piezoelectric impact hammer is designed and fabricated for applications in the nondestructive evaluation of concrete structures. To obtain a large enough impact force, special design in the holding fixture of the impact hammer is utilized. With an on-line sensor, the impact time origin resolution can be controlled in the range of sub-microsecond. To demonstrate the accuracy of the newly fabricated impact device, measurements of the longitudinal and Rayleigh wave velocities of a concrete specimen were conducted. Due to the stable impact generation of the piezoelectric impact hammer, the experimental results showed that the accuracy of the wave velocity measurement is enhanced significantly through signal averaging.
Fig 1: The assembly of the piezoelectric impact hammer.
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It is worth noting that the capacitance of the PZT stack is as high as 5.4 mF and the driving voltage is 150 V, therefore, to generate the large enough power to drive the impact hammer, a high voltage pulse generator is needed. In this study, a 150 V voltage pulse generator, which is composed of a capacitor bank and an N channel MOSFET, is used in this study. In addition, a gated circuit was designed to gate the impact signal from the on-line piezoelectric sensor and to send a trigger signal synchronous with the impact time origin.
To overcome the above-mentioned difficulties, an on-line piezoelectric sensor was utilized to determine the precise time origin of the impact at the specimen surface. The upper trace shown in Fig. 2 is the signal detected by the on-line piezoelectric sensor for a particular impact on a concrete specimen. Three separated pulses are found in the signal. Pulse 1 is the first received signal by the on-line sensor for wave transmitting from the wave-guide and arriving at the sensor. Pulse 2 denotes the back propagation wave induced by the impact of the flying head on the testing surface. Pulse 3 is generated by the impact between the bounced back flying head and the wave-guide.
Fig 2: Signal from the on-line piezoelectric sensor (upper trace), gated region (middle trace) and the time reference (lower trace).
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To reduce the error from in-situ applications, the time reference of this impact device must be deduced from the true impact signal, pulse 2, which is induced by the flying head hitting the specimen. A gated circuit was designed to catch the signal from the on-line piezoelectric sensor and send a synchronous pulse out as the time reference of the measuring system (Fig.2). With this circuit, the accuracy of time reference of the impact can be improved to the range of sub-microsecond.
The time reference mentioned above was utilized to average the repeated signals to enhance the S/N ratio. However, some application of the impact hammer, such as crack depth evaluation, needs not only an accurate time reference but also the true impact time origin. To obtain the impact time origin, calibration experiment on a steel block was conducted, as shown in Fig. 3. A 9 V battery was used as the voltage source to give the impact time origin. As the flying head hits the steel surface, a circuit loop is formed and this gives a step signal with a very short rise time (about 0.02 ms). The experimental result (Fig. 4) showed that the time delay between the time reference and the 9V-step signal is about 7.2 ms.
Fig 3: Arrangement of the calibration experiment.
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Fig 4: Experimental result of the calibration experiment.
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4.1 Longitudinal wave velocity measurement
Analysis made by Wu and Fang [7] has shown that for elastic wave generation by a point source in a half space, the amplitude of the tangential component of the skimming longitudinal wave is four to five times larger than that of the normal component. In addition, it gives a much clear displacement jump at the wave-front arrival. For this reason, a pair of horizontal polarized conical PZT transducers were employed is this paper to measure the wave-front arrival of the surface skimming longitudinal wave.
4.2 Rayleigh wave velocity measurement
Fig 5: Relative position of the impact source and receivers.
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| (1) |
If the signals h1(t) and h2(t) are similar with a time delay Dt, the maximum of z(t) occurs at Dt. In other words, the time delay between h1(t) and h2(t) can be determined by finding the corresponding time at which z(t) is a maximum.
5.1 Longitudinal wave measurement
In determine the longitudinal wave-front arrival using a hand held impactor [7], to enhance the resolution of the delay time measurement, the recorded signal was enlarged and processed by a linear phase finite impulse response filter. Shown in Fig. 6 are the measured signals by the two horizontally polarized conical transducers. The distance of the impact source to the first receiver was kept at the value of r1=7 cm. The distance between the first receiver and the second receiver was kept at a constant distance 10 cm. The signals showed that there are a lot of noises riding on top of the elastic wave signals, and hence to determine the true arrival of the longitudinal wave-front, special care is needed to ensure a reliable measurement. Although the hand held impactor method can give a measurement of the longitudinal wave-front arrival with reasonable accuracy, it is relative time consuming and is not practical for in-situ measurement.
Fig 6: Received displacement signals of the longitudinal wave measurement using a hand-held impactor.
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Fig 7: Averaged (40 times) displacement signals of the longitudinal wave measurements.
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| 1st | 2nd | 3rd | 4th | Average |
| 4000 | 3960 | 3960 | 3976 | 3974 |
| 0.65% | -0.35% | -0.35% | 0.05% | |
| Standard deviation = 0.47% | ||||
| Table 1: Four different measurements of the longitudinal wave velocities at the same location of the concrete specimen. | ||||
5.2 Rayleigh wave measurement
Figs. 8 and 9 shows the Rayleigh wave signals generated by a hand held impactor and the piezoelectric impact hammer (20 times averaging), respectively. Significant improvement on the signal to noise ratio has been achieved. The signals after the peaks of the Rayleigh waves have been removed before conducting the cross correlation of the two signals. Table 2 is the result for four different measurements of the Rayleigh wave velocities at the same location of the concrete specimen. The average Rayleigh wave velocity is 2178 m/s and the standard deviation of the four measurements is 0.08%.
Fig 8: Received displacement signals of the Rayleigh wave measurement using a hand-held impactor.
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Fig 9: Averaged (20times) displacement signals of the Rayleigh wave measurement
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| 1st | 2nd | 3rd | 4th | Average |
| 2140 | 2140 | 2137 | 2137 | 2139 |
| 0.08% | 0.08% | -0.08% | -0.08% | |
| Standard deviation = 0.08% | ||||
| Table 2: Four different measurements of the Rayleigh wave velocities at the same location of the concrete specimen. | ||||
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