Method for Onset Time Detection of Acoustic Emission Based on Histogram Distance
20230130080 · 2023-04-27
Inventors
- Zhensheng Yang (Shanghai, CN)
- Handong Xu (Shanghai, CN)
- Haoda Li (Shanghai, CN)
- Bangping Gu (Shanghai, CN)
- Junliang He (Shanghai, CN)
Cpc classification
G01N29/36
PHYSICS
G06F17/18
PHYSICS
G01N29/449
PHYSICS
International classification
G01N29/44
PHYSICS
G01N29/36
PHYSICS
Abstract
The present invention discloses a method for onset time detection of acoustic emission signals based on histogram distance. The method comprises the following steps: acquiring an acoustic emission signal; dividing the signal into two intervals with a sliding point k as the demarcation point; obtaining the relative frequency histograms of two adjacent intervals; obtaining histogram distance of the relative frequency histograms of two adjacent intervals; moving the sliding point k to the next element to obtain two new intervals and generating new histograms of the two new intervals and calculating the histogram distance of two new intervals; searching for the point which gives the maximum value of the histogram distances, and the corresponding time to this point is regarded as the onset time.
Claims
1. A method for onset time detection of acoustic emission signals based on histogram distance, comprising the following steps: (1) acquiring a signal: acquiring an acoustic emission signal that contains n elements with a sampling frequency in accordance with Shannon sampling theorem; that is, acquiring the acoustic emission signal with a sampling frequency not less than twice the highest frequency of the acquired signal; (2) dividing a signal: dividing the acquired signal that contains n elements into two intervals by a sliding point k at each time; marking the two intervals wherein the former interval is marked as Interval A and the latter interval is marked as Interval B; fitting the Interval A to the former interval from the 1st to kth element, and fitting the Interval B to the latter interval from (k + 1)th to nth element; (3) obtaining the relative frequency histogram of the Interval A and the Interval B: (3.1) defining the histogram: let y be a measurement and have one of b bins contained in an ordinal set, Y = {y.sub.1, ...y.sub.i, ...,y.sub.b} , where i = 1,2, ...,b , and y.sub.i < y.sub.t+1; considering a signal X = {x.sub.1,x.sub.2,...,x.sub.j, ... x.sub.m} containing m elements, where j = 1,2, ... m, and x.sub.j falls within one of the bins of Y; defining the histogram of the signal X by the relationship:
Description
BRIEF DESCRIPTION OF THE DRAWINGS
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EMBODIMENTS
[0032] Illustrations presented herein are not meant to be actual views of any particular material, component, or system but are merely idealized representations that are employed to describe embodiments of the disclosure.
[0033] The following description provides specific details, such as the dividing process and calculation process, to provide a thorough description of embodiments of the disclosure. However, a person of ordinary skill in the art will understand that the embodiments of the disclosure may not be practiced without employing these specific details. Only those process acts and calculations necessary to understand the embodiments of the disclosure are described in detail below. A person of ordinary skill in the art will understand that some process components (e.g., acoustic emission, histogram, probability, and the like) are inherently disclosed herein and would be in accord with the disclosure.
[0034] As used herein, the term “acoustic emission” (AE) means and includes the propagation of acoustic (elastic) waves that occur when a material undergoes either reversible or irreversible changes in internal structure that are the result of stresses in the material. Acoustic emissions may result from, for example, crack formation, plastic deformation, corrosion, or change of geological shape.
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[0036] The type of signal of acquiring signal 1 shown in
[0037] The present invention discloses a method for onset time detection of acoustic emission signals based on histogram distance, which is characterized in that it comprises the following steps: [0038] (1) acquiring a signal: acquiring an acoustic emission signal with the sampling frequency in accordance with Shannon sampling theorem; that is, acquiring the acoustic emission signal with a sampling frequency not less than twice the highest frequency of the acquired signal; [0039] (2) dividing a signal: dividing the acquired signal that contains n elements into two intervals by a sliding point k at each time; marking the two intervals wherein the former interval is marked as Interval A and the latter interval is marked as Interval B; fitting the Interval A to the former interval from the 1st to kth element, and fitting the Interval B to the latter interval from (k + 1)th to nth element; [0040] (3) obtaining the relative frequency histogram of the Interval A and the Interval B: [0041] (4) obtaining the histogram distance between the relative frequency histograms of the Interval A and the Interval B: [0042] (5) determining the onset time: according to the definition of d.sub.B (h.sup.A,h.sup.B ), the sliding point k with a maximum value of the histogram distance is regarded as the onset time.
Step 3 Comprises the Following Steps
[0043] (3.1) defining the histogram: let y be a measurement and have one of b bins contained in an ordinal set, Y = {y.sub.1, ... y.sub.i, ..., y.sub.b} , where i = 1,2, ..., b , and y.sub.i < y.sub.i+1 . Consider a signal X = {x.sub.1,x.sub.2,...,x.sub.j, ...x.sub.m} containing m elements, where j = 1,2, ... m, and x.sub.j falls within one of the bins of Y. The histogram of the signal X is defined by the relationship:
where h.sup.x is defined as the histogram of the signal X, b is the total number of bins of the histogram in the signal X, and
is the value of the ith bin of the histogram of the signal X and is defined by the relationship:
[0044] (3.2) calculating the relative frequency histograms of two intervals A and B: the relative frequency histograms of said intervals A and B is defined by the relationship,
wherein
and
are the probability of elements that fall within the ith bin of said histogram, k.sub.A is the total number of elements of the interval A and k.sub.B is the total number of elements of the interval B;
Step 4 Comprises the Following Steps
[0045] (4.1) the histogram distance is defined by the relationship:
where d.sub.B(h.sup.A,h.sup.B) is the histogram distance between the histograms h.sup.A and h.sup.B, B(h.sup.A,h.sup.B) is the Bhattacharyya coefficient between the histograms h.sup.A and h.sup.B and defined by the relationship:
[0046] (4.2) moving the sliding point k: after calculating the histogram distance of the Interval A and the Interval B, moving the sliding point k to the next element to obtain new intervals, generating new histograms of two new intervals and calculating the histogram distance of two new intervals; moving the sliding point k from the first element to the nth element and moving one element at each time;
[0047] The present invention is tested through two typical experiments. The experiment data are AE signals generated by the pencil-lead break (PLB) experiment and seismic P-phase data.
[0048] Pencil-lead break (PLB) (Hsu-nielsen source acoustic emission data on a concrete block, Data in brief, 2019.) , also known as Hsu-Nielsen source, is an artificial method of generating AE signals. The PLB data in this invention represent AE signals transmitted and received by conducting the PLB experiment on a concrete specimen. The PLB test consists of breaking pencil-lead in three different locations. The generated stress waves were captured by ten piezoelectric AE sensors and converted into electrical signals. The signals were digitized according to a specified sampling rate and expressed in voltage amplitudes. The data are presented for each PLB and channel. The geometry and mixture design of the concrete specimen, sensor types, sensor locations, and PLB locations are shown in
[0049] Seismic P-phase data were gathered from the Incorporated Research Institutions for Seismology (IRIS). Data points within 5 minutes before and after the arrival of P phases are selected. Vertical component data is used as the strongest component in P phases. A total of 300 recordings with various SNRS are extracted in the dataset. The sampling rate was 100 Hz, which satisfies Shannon sampling theorem.
[0050] Methods based on Akaike information criterion (AIC) have been shown to provide accurate results for detecting the onset time. The comparison with the AIC-based method is an excellent choice to evaluate the applicability of the present inventions. AIC assumes the time series can be divided into locally stationary segments, each segment is modeled as an autoregressive process, and that intervals before and after the onset time can be split into two different stationary time series. For a fixed order auto-regressive process, the corresponding time to the point at which the AIC is minimized is the onset time. The AIC used here is defined by the relationship ( Strategies for reliable automatic onset time picking of acoustic emissions and of ultrasound signals in concrete, Ultrasonics, 2005 ) :
where the index w of R.sub.w denotes that not the whole time series is taken but only the chosen window containing the onset, and T.sub.w is the last sample of the curtate time series, t.sub.w ranges through all samples of R.sub.w and var denotes the variance function. The term R.sub.w (t.sub.w,1) means that the variance function is only calculated from the current value of t.sub.w while R.sub.w(1+t.sub.w,T.sub.w) means that all samples ranging from 1+t.sub.w to T.sub.w are taken.
[0051] The invention discloses a method for onset time detection of acoustic emission signals based on histogram distance which determines the onset time accurately. The experimental verification is as follows:
[0052] (1) Pencil-lead break test: pencil-lead break (PLB) is an artificial method of generating AE signals and is commonly used for calibration and simulation. These tests consisted of breaking a 0.3-mm-diameter pencil lead approximately 3 ± 0.5 mm from its tip by pressing it against the surface of the specimen. HB pencil leads were broken at three different points on the surface of the concrete beam. The energy released by PLB was collected by ten piezoelectric AE sensors with an operating frequency range of 200 - 850 kHz. The original signals were amplified using 26 dB gain. The sampling rate was 1 MHz with a threshold of 31 dB, which satisfies Shannon sampling theorem. The PLB tests generated a hundred sets of AE data. Through the above steps, the results obtained are compared with the onset time that are detected manually. The manual detection results, defined as those determined by the experienced analyst in daily analysis, have been empirically assumed as being the correct ones.
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[0054] Methods based on Akaike information criterion (AIC) are conventional methods for detecting onset time of signals. The present invention is compared with the AIC-based methods.
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[0056] (2) Seismic P-phase detection test: The digital seismic waveform data were gathered from the Incorporated Research Institutions for Seismology (IRIS). Data points within 5 minutes before and after the arrival of P phases are selected. Vertical component data is used as the strongest component in P phases. A total of 300 recordings are extracted from the dataset. The sampling rate was 100 Hz, which satisfies the Shannon sampling theorem. This dataset has a diversity of waveform characteristics. Through the above five steps, the results obtained are compared with the onset time detected manually.
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[0059] All seismic data were downloaded through the IRIS Wilber 3 system (https://ds.iris.edu/wilber3/) or IRIS Web Services (https://service.iris.edu/), including the following seismic networks:(1) the II (GSN; Scripps Institution of Oceanography, 1986); (2) the IU (GSN; Albuquerque, 1988); (3) the CU (USGS, Albuquerque, 2006).
[0060] In the above two verification experiments, PLB is the most commonly used acoustic emission related detection and verification approach, and acoustic emission technology is widely used in the field of nondestructive testing. Seismic P-phase detection is the basis of seismic signal post-processing and source location, which is of great significance in the field of geology. The present invention has experienced many verification experiments and has high reliability. Compared with the conventional method, the present invention shows the characteristics of high accuracy. The present invention has experienced verification with various SNR signals, especially for the identification of low SNR signals. In summary, the present invention has high practicability and is suitable for process monitoring, seismology and other fields.
[0061] While the present invention has been particularly shown and described with reference to exemplary embodiments thereof, it is evident that many alternatives, modifications and variations will be apparent to those skilled in the art. It will be understood by those skilled in the art that various changes in form and details may be made therein without departing from the spirit and scope of the invention as defined by the appended claims.
[0062] In addition, since the present invention can be embodied in various forms, and should not be construed as being limited to the embodiments set forth herein. Rather, these embodiments are provided so that this disclosure will be thorough and complete and will fully convey the concept of the invention to those skilled in the art, and the present disclosure will only be defined by the appended claims.