Method of wave form segmentation and characterization of the segmented interval thereof

• US 20040102710A1
• Filed: 10/16/2003
• Published: 05/27/2004
• Est. Priority Date: 11/13/2001
• Status: Abandoned Application

• Current Assignee: Jungkuk Kim
• Original Assignee: Jungkuk Kim
• Inventors: Kim, Jungkuk
• Application Number:
  US10/451,700
• Publication Number:
  US 20040102710A1
• Time in Patent Office: Days
• US Class Current: 600/509
• CPC Class Codes: G06F 17/17 Function evaluation by approximation methods, e.g. inter- or extrapolation, smoothing, least mean square method G06F17/18 takes precedence ; interpolation for numerical control G05B19/18
• CPC Class Codes: G06F 2218/08 Feature extraction

Abstract

The present invention discloses a method of partitioning a waveform for characterization with a slope-inversion point and a slope-transition point by utilizing a slope-tracing waveform, which can be utilized for the application to the physiological signal of a living body.

Claims

1. A method of partitioning a sampled signal waveform into several sections each of which includes a multiple of samples with a tracing waveform, comprising steps of:

(a) updating the functional value of said tracing waveform at an (n+1)-th sample with the amplitude of said signal waveform at an (n+1)-th sample if the functional value of said tracing waveform at an n-th sample is smaller than the amplitude of said signal waveform at an (n+1)-th sample;

(b) comparing the functional value of said tracing waveform at an n-th sample with that at an (n−

1)-th sample of said tracing waveform if the functional value of said tracing waveform at an n-th sample is greater than or equal to the amplitude of said signal waveform at an (n+1)-th sample;

(c) either maintaining the functional value of said tracing waveform at an (n+1)-th sample with that at an n-th sample of said tracing waveform in case when the functional value of said tracing waveform at consecutively foregoing samples including an n-th, an (n−

1)-th, an (n−

2)-th, . . . , has been kept constant wherein the number of samples is less than a predefined number k, or updating the functional value of said tracing waveform at an (n+1)-th sample by subtracting the functional value of said tracing waveform at the n-th sample with an average slope between the n-th sample and the (n−

k)-th sample that is regarded as a slope-inversion point in the case when the number of samples is more than or equal to said predefined number k at the step of (b);

(d) updating the functional value of said tracing waveform at an (n+1)-th sample by subtracting a first slope from the functional value of said tracing waveform at an n-th sample if the value of said tracing waveform at an n-th sample is different from that at an (n−

1)-th sample and the number of samples including the n-th, (n−

1)-th, an (n−

2)-th, . . . of which the value has been decreasing with the same slope (said “

first slope”

) is less than a predefined number L, or by subtracting a second slope from the functional value of said tracing waveform at an n-th sample if the number of samples decreasing with said first slope is greater than or equal to said predefined number L and the average slope (“

a second slope”

) between the n-th sample and the (n−

L)-th sample is steeper than said first slope multiplied by a predefined rate (X %), or by subtracting a first slope multiplied by said predefined rate (X %) from the functional value of said tracing waveform at an n-th sample if said second slope is less steep than said first slope multiplied by said predefined rate (X %) at step of (b); and

(e) regarding the (n+1)-th sample as a slope-transition point and regarding the interval between said slop-changing point and said slope-inversion point as a single section if the functional value of said tracing waveform at an (n+1)-th sample is lees than or equal to the value of said signal waveform at an (n+1)-th sample and thereby the two waveforms intersect.

3. The method as set forth in claim 1 or claim 2 further comprising steps of:

subtracting the amplitude of said signal waveform at slope-transition point from the amplitude of said signal waveform at each sample in said partitioned section and summing the values of subtraction at each sample for the calculation of the area of said partitioned section.

4. The method as set forth in claim 1 or claim 2 wherein the interval between the left slope-transition point and the right slope-transition point with respect to said slope-inversion point as a center is defined as a single section, further comprising steps of:

calculating the area of the left and right part of the waveform in said partitioned section; and

characterizing said partitioned section by summing the calculated area of the left and right part of the waveform.

5. The method as set forth in claim 1 or claim 2 wherein the interval between the left slope-transition point and the right slope-transition point with respect to said slope-inversion point as a center is defined as a single section, further comprising steps of:

calculating the area of the left and right part of the waveform in said partitioned section; and

characterizing said partitioned section by coupling a pair of the calculated area of the left and right part of the waveform.

6. The method as set forth in claim 1 or claim 2 further comprising a step of characterizing the waveform of the partitioned section by calculating the difference in amplitude of the signal waveform at each samples in the partitioned section.

7. The method as set forth in claim 1 or claim 2 further comprising a step of calculating the difference in amplitude in said partitioned section by subtracting the amplitude of a slope-transition point from that of a slope-inversion point.

8. The method as set forth in claim 1 or claim 2 wherein the interval between the left slope-transition point and the right slope-transition point with respect to a slope-inversion point as a center is regarded as a single section, further comprising a step of characterizing said section by subtracting the amplitude of the slope-inversion point from that of each slope-transition point and summing the subtracted value.

9. The method as set forth in claim 1 or claim 2 wherein the interval between the left slope-transition point and the right slope-transition point with respect to a slope-inversion point as a center is regarded as a single section, further comprising a step of characterizing said section by subtracting the amplitude of the slope-inversion point from that of each slope-transition point and coupling a pair of the subtracted value.

10. The method as set forth in claim 1 or claim 2 further comprising a step of defining a time interval by calculating a time difference between the initial point and the final point of said partitioned section determined by said slop-changing point and said slope-inversion point.

11. The method as set forth in claim 1 or claim 2 wherein a section is defined as an interval between the left slope-transition point and the right slope-transition point with respect to a slope-inversion point as a center, further comprising a step of characterizing the time interval of said section by calculating the time difference between the initial and final points and summing the values.

12. The method as set forth in claim 1 or claim 2 wherein a section is defined as an interval between the left slope-transition point and the right slope-transition point with respect to a slope-inversion point as a center, further comprising a step of characterizing the time interval of said section by calculating the time difference between the initial and final points and coupling a pair of said values.

13. The method as set forth in claim 1 or claim 2 wherein the amplitude of the slope-inversion point and of the left and right slope-transition points is detected, further comprising steps of:

selecting a slope-transition point among the two whose amplitude is more similar to that of said slope-inversion points; and

amending said partitioned section by selecting a sample of said signal waveform as another slope-transition point whose amplitude is the most similar to that of the selected slop-changing point and whose position is the most close to the mirror location of said selected slope-transition point with respect to said slope-inversion point if the difference in amplitude between the left and right slope-transition points exist by less than a predetermined amount (Y %).

2. A method of partitioning a sampled signal waveform into several sections each of which includes a multiple of samples with a tracing waveform, comprising steps of:

(a) updating the functional value at an (n+1)-th sample of said tracing waveform with the amplitude of said signal waveform an (n+1)-th sample if the functional value of said tracing waveform at an n-th sample is larger than the amplitude of said signal waveform at an (n+1)-th sample;

(b) comparing the functional value of said tracing waveform at an n-th sample with that at an (n−

1)-th sample of said tracing waveform if the functional value of said tracing waveform at an n-th sample is smaller than or equal to the amplitude of said signal waveform at an (n+1)-th sample;

(c) either maintaining the functional value of said tracing waveform at an (n+1)-th sample with that at an n-th sample in case when the functional value of said tracing waveform at consecutively foregoing samples including an n-th, an (n−

1)-th, an (n−

2)-th, . . . , has been kept constant wherein the number of times is less than a predefined number k, or updating the functional value of said tracing waveform at an (n+1)-th sample with an (n+1)-th sample by adding the functional value of said tracing waveform at the n-th sample with an average slope between the n-th sample and the (n−

k)-th sample which is regarded as a slope-inversion point in case when the number of samples is more than or equal to said predefined number at the step of (b);

(d) updating the functional value of said tracing waveform at an (n+1)-th sample by adding a first slope from the functional value of said tracing waveform at an n-th sample if the value of said tracing waveform at an n-th sample is different from that at an (n−

1)-th sample and the number of samples including the n-th, (n−

1)-th, an (n−

2)-th, of which the value has been increasing with the same slop (said “

first slope”

) is less than a predefined number L, or by adding a second slope from the functional value of said tracing waveform at an n-th sample if the number of samples increasing with said first slope is greater than or equal to said predefined number L and the average slope (“

a second slope”

) between the n-th sample and the (n−

L)-th sample is steeper than said first slope multiplied by a predefined rate (X %), or by adding a first slope multiplied by said predefined rate (X %) from the functional value of said tracing waveform at an n-th sample if said second slope is less steep than said first slope multiplied by said predefined rate (X %) at step of (b); and

(e) regarding the (n+1)-th sample as a slope-transition point and regarding the interval between said slop-changing point and said slope-inversion point as a single section if the functional value of said tracing waveform at an (n+1)-th sample is greater than or equal to the value of said signal waveform at an (n+1)-th sample and thereby the two waveforms intersect.