The purpose of the present invention is to detect water ingress in the intermediate layer of a measurement object, having a cylindrical sandwich structure, such as that shown in
Generally, these measurement objects comprise an outermost solid material layer 510
The method may alternatively be applied to characterize only parts of the described sandwich structure, such as the outermost layer 510 and possibly the intermediate layer 511. The method might also be applied for cases in which either the outermost layer 510 or internal layers 512 are covered with coatings, or are corroded. In the latter case, several measurements will be utilized to smear out the presumed random nature of the corrosion topology, cf. Sec. 3.4, block 1040.
The following description refers mainly to
Now the operator enables the function generator 110 (using a button), via the control PC 180, to transmit an electrical wide-band pulse, such as the one in Error! Reference source not found, to the power amplifier 120. The wide-band pulse should at least cover a frequency band, referring to −3 dB, of
where c is the sound velocity of the outermost layer 110, and d1 and d2 are respectively the maximum and minimum allowed thicknesses of the outermost layer 510 to be characterized.
Hence, f1 and f2 represent the fundamental half-wave resonances associated with d1 and d2. Preferably, the upper frequency limit should embrace multiple harmonics.
The wide-band pulse is input at the power amplifier (PA) 120, while the DAQ 170 is triggered to start digitizing and storing the electrical signal at its input. The PA 120 preferably amplifies the input wide-band pulse (
The HF part of the transmitting matching filter 131 minimizes the impedance mismatch between the PA 120 and the transmitting HF part of the transceiver 141, so as to maximize the electrical power input at the transmitting HF part of the transceiver 141.
The HF transmitting part of the transceiver 141 transforms the input electrical pulse to mechanical vibrations. The mechanical vibrations generate a sound wave that propagates through the coupling medium, which may either be a waveguide or a gas, to the measurement object 150. In case of a waveguide, it should preferably have a circular geometry, consist of some solid material, and possess acoustic impedance between that of the active transceiver clement 141 and the outermost layer 510 (
The sound waves are partially reflected at the outermost layer of the measurement object 150, causing a primary echo. The primary echo travels back through the waveguide, and into the HF receiving part of the transceiver 141. The primary echo is also received at the low-frequency (LF) part of the transceiver 140, but considerably reduced, and considered negligible upon reception.
The HF receiving part of the transceiver 141 is excited by the primary echo to vibrate mechanically, and converts these mechanical vibrations to an electrical HF signal, which is input at the preamplifier 160.
The preamplifier 160 amplifies the input electrical HF signal to a level similar to the input range of the DAQ 170. Possibly, the preamplifier 170 may have embedded a switching circuit that disables the preamplifier output, if—for some reason—the DAQ saturates.
The DAQ 170 digitizes and stores the received HF signal as a reference measurement data result, comprising the primary echo (
Next, the transceiver 140 and 141 is moved to a region of the measurement object 150 that is suspected to contain a wet intermediate layer 511, preferably at a position directly below the presumed dry position. The measurement procedure described in Sec. 3.1 is then repeated, and the received signal is taken to be a measurement data set corresponding to a possible wet region.
An example of a resonance tail due to a wetted intermediate layer 511 is shown in
To be able to characterize the internal layer, it is required that the water column reaches the internal layer. Moreover, it is required that the thickness of the intermediate layer be greater than τcw/2, where τ and cw are respectively the time duration of the secondary echo inclusive tail, and sound velocity of the fresh water contained in the intermediate layer.
Upon reception of the above HF signal, the function generator 110 is triggered to transmit another electrical wide-band pulse, similar to the one in
where c is the sound velocity of the internal layer 512, and d1 and d2 are respectively the maximum and minimum allowed thicknesses of the internal layer 512 to be characterized,
Hence, f1 and f2 represent the fundamental half-wave resonances associated with d1 and d2 for the internal layer 512. Preferably, the upper frequency limit should embrace multiple harmonics. The present wide-band pulse will be referred to as wide-band LF pulse.
The wide-band LF pulse is input at the PA 120, which preferably amplifies the wide-band LF pulse linearly to a level slightly less than the maximum input level of the transmitting LF part of the transceiver 140.
The LF part of the transmitting matching filter 130 minimizes the impedance mismatch between the PA 120 and the transmitting LF part of the transceiver 140, so as to maximize the electrical power input at the transmitting LF part of the transceiver 140.
The LF transmitting part of the transceiver 140 converts the input electrical pulse to mechanical vibrations. These mechanical vibrations cause sound waves to propagate through the coupling medium to the outermost layer of the measurement object 150.
The sound waves are partially transmitted through the outermost layer of the measurement object 150, proceeding though the intermediate layer (
The secondary echo propagates back through the intermediate layer 511 (
The secondary echo proceeds through the waveguide, into the LF receiving part of the transceiver 140.
The receiving LF part of the transceiver 140 is excited by the secondary echo to vibrate mechanically, and these mechanical vibrations are converted to an electrical LF signal. The electrical LF signal is then input at the preamplifier 160.
The preamplifier 160 amplifies the input electrical LF signal to a level similar to the input range of the DAQ 170.
The DAQ 170 digitizes and stores the received LF signal, comprising the secondary echo.
The set of real numbers corresponding to voltages from the DAQ unit 170.
Speed of sound of outer layer, c
Speed of sound of wet intermediate layer 511, cw
Length of time window for spectral estimation, N
Expected width of primary echo without resonance tail, W
Spectral estimation methods
Choice of window functions (e.g. Hanning, Bartley)
Sampling frequency, Fs
Frequency interval used in transceiver
a Expected outer layer 510 thickness
The thickness of the intermediate layer 511, l Maximum allowed lag of secondary peak from its theoretical arrival, k
Number of datasets in reference memory, M
Inputs: time signal, spectral estimation technique, N, Fs
The power content in the time-frequency domain is estimated, using any standard technique, such as the sliding Fourier transform, or the Wigner distribution. The time of the maximum energy is identified, from this and N the start time of the tail is found,
Time-frequency analysis is processing intensive and can be switched off.
Outputs: matrix of power, vector of times (in units of sampling interval), vector of frequencies (in Hz), start of tail time
Inputs: time vector, expected width of primary echo
Finds the time corresponding to the largest pulse energy, and uses expected width of primary echo to find the start and stop of the echo
Outputs: start and stop times of echo
Inputs: cw, l, k, time vector, start and stop times of primary echo
The rough peak location of the secondary echo is found from
where τ0 is the time of arrival of the primary echo (which is found as the midpoint between the start time and end time of the echo), l is the thickness of the intermediate layer 511. The nearest local maximum in the signal energy is deemed to be the time of arrival of the secondary echo. If that local maximum falls outside the range given by k, the start and end of secondary echo are left empty.
Outputs: start and stop times of secondary echo
Inputs: start and stop times of secondary echo
If the inputs are empty, abort the calculation of internal layer 512 thickness because no echo could be identified.
Outputs: whether secondary echo was found
Inputs: time vector, spectral estimation method, start and stop times for analysis, window functions, N, Fs
The frequency power content of the time signal is estimated using any standard technique, from periodogram based methods to parametric methods, for example using the Yule-Walker model. The estimation is performed in two windows, one comprising the tail only (starting at end of echo lasting to end of echo+N), and one comprising the echo and its tail, starting at the time start of echo−N lasting to end of echo+N.
Outputs: power vector tail, vector with frequencies (in Hz) corresponding to the power values, power vector echo, vector with frequencies (in Hz) corresponding to the power values
Inputs: frequency vector from Time-frequency analysis and/or Spectral estimation, power matrix and/or power vector tail, frequency interval used in transceiver, start of tail time in time-frequency vector
Either one or both of the following:
Outputs: index into time and frequency vectors corresponding to the resonance frequency
Inputs: frequency vector tail, frequency vector echo, power vector tails power vector echo
An elaborate procedure is required to achieve a reliable determination of harmonic orders belonging to frequencies. The procedure is detailed in 971-979 below.
Outputs: harmonic orders, resonance frequencies
Inputs: c, resonance frequencies, harmonic orders
The layer thickness is computed from
where fres is the resonance frequency. If the wide band pulse produced by the transceiver 140 and 141 covers several harmonic orders of the resonance frequency, a more reliable method for thickness computation calculates
where now n is the integer indicating the harmonic order <·> indicates averaging.
Display results.
Outputs: thickness estimates
Inputs: time-frequency power matrix, vector of frequencies, start of tail time
The characteristic decay time of the resonance in the tail is found.
Outputs: the decay time of the resonance frequency
Inputs: power vector tail, power vector echo, index of resonance frequency
Reads the values in the power vectors
Outputs, power at resonance frequency in tail, power at resonance frequency in echo
Inputs: power of resonance frequency in tail, power vector echo, decay time, reference power of resonance frequency in tail, reference power vector echo, reference decay time
Reference variables are vectors comprising several previous realisations, the exact to number determined by the input variable M (see above under Input parameters)
Initalisation of comparison: one or more data sets are recorded at location(s) known to be dry. The readings are analysed using the above steps, and the power spectrum in echo, decay time of resonance frequency in the tails, and lastly the maximum power of the resonance frequency in the tail, are stored. All the features are classified as “dry”.
The new data comprising the power of resonance frequencies in tail, power vector echo, and the decay time, are compared with their respective reference values in the following manner:
Outputs: division spectra, difference powers, difference decay times
Inputs: division spectra, difference powers, difference decay times, power vector tail, resonance frequency, previous result (wet/dry), M
For each of the comparisons one must determine whether they are consistent with wet or dry conditions This is done in the following manner:
A simple majority voting is then used to classify the measurement as indicating either “dry” or “wet” conditions
According to the decision, the power vector tail, the power vector echo, and decay time are stored as a reference in either the “wet” or “dry” class, If the number of stored references is equal to M, the currently obtained results replace the oldest reference.
Output: display result, new reference values,
The original time vector is stored.
All display functions in the flow chart imply storage.
Inputs: power vector echo, power vector tail, bispectrum vector
Finds local maxima in the bispectrum vector and the power vector tail. Finds local minima in the power vector echo.
The union of the three sets is the list of potential harmonic frequency candidates.
Outputs: harmonic frequency candidates
Inputs: harmonic frequency candidates, power vector echo, power vector tail, bispectrum vector, filter size
The ensuing weight vector gives weight to large peaks/deep minima in the respective power vectors, but penalises each weight if it is far from frequencies in the other sets. Weights are real numbers between 0 and 1.
Outputs: weights assigned to each harmonic frequency candidate
Inputs: weights, harmonic frequency candidates
Sorts the weights vector, and uses the sort indices to rearrange the harmonic frequency candidates so that they are listed in decreasing weighted order.
Outputs: sorted harmonic frequency candidates
Inputs: sorted harmonic frequency candidates, weights, frequency weights threshold
Each frequency set is denoted Fn.
Outputs: frequency sets {F1, F2, . . . , FN}
975 Loop Through n=1, . . . ,N
Input: Frequency sets {F1, F2, . . . , FN}, integer tolerance, expected maximum thickness, frequency interval used in transceiver
The harmonic sets for one frequency list Fi is computed as follows: initially a n×n matrix with filled with all possible ratios of frequencies is found,
The matrix M′ is used to build a larger matrix M by concatenating kM′, k=1,2, . . . ,kmax as follows:
The integer kmax is computed from the maximum allowed thickness, a user input.
The next step is to round all elements in M to their nearest integer, and compare the difference between the integer values and the frequency ratios in M. An element is deemed an integer if this difference is less than a user specified threshold, typically 0.1, and a matrix N where all non-integer elements in M equal zero if found. The rows in N identify the harmonic sets: for a given Nij element the value corresponds to the harmonic order of frequency fj in the frequency list.
Output: Set of integer matrices {N1, N2, . . . , NN}.
Input: Set of integer matrices {N1, N2, . . . , Nn}, expected maximum thickness) frequency interval used in transceiver
The harmonic order matrices Nn are significantly reduced by removing rows containing a value above the max order kmax. All duplicate rows are removed, and rows giving a thickness above the user input maximum value are removed,
Outputs: Set of reduced integer matrices {N1, N2, . . . , Nn}
Input: Set of reduced integer matrices (N1, N2, . . . , Nn}.
For each Nn, the harmonic set with the largest number of unique frequencies are recorded. The numbers are stored in a vector Φ.
Output: Vector Φ of maximum number of unique sets.
Input: Vector Φ of maximum number of unique sets, number of frequencies in each frequency set, set of reduced integer matrices (N1, N2, . . . , Nn}.
The aim is to find the optimum subset of the original frequency list. Each subset is associated with a number of unique harmonics stored in Φ. In addition, each subset has a number of frequencies.
The optimal subset is found by finding the highest ratio of Φ divided by the number of frequencies in the list, neglecting the trivial case for only a single frequency. In this process we have accomplished both a rejection of frequencies, and obtained harmonic sets.
Output: Indices to optimal subset of frequencies, set of harmonics.
Upon positive detection of liquid in the intermediate layer 511, the transceiver 140 and 141 is moved upwards in steps of, say 10 mm, towards elevated regions of the measurement object 150. Meanwhile, the procedures described in Secs. 3.1 to 3.4 are repeatedly performed, to determine at which level the liquid surface occurs.
Number | Date | Country | Kind |
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2007 4644 | Sep 2007 | NO | national |
Number | Date | Country | |
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60971684 | Sep 2007 | US |