CN114898278B - Non-contact rockfall protection dynamic response signal automatic identification and feedback method - Google Patents

Non-contact rockfall protection dynamic response signal automatic identification and feedback method Download PDF

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CN114898278B
CN114898278B CN202210653638.XA CN202210653638A CN114898278B CN 114898278 B CN114898278 B CN 114898278B CN 202210653638 A CN202210653638 A CN 202210653638A CN 114898278 B CN114898278 B CN 114898278B
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郭立平
余志祥
田永丁
廖林绪
张丽君
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Abstract

本发明涉及边坡落石灾害防护技术领域,涉及一种非接触式落石防护动态响应信号自动识别及反馈方法,其包括如下步骤:步骤(1):摄像机位布置及冲击过程高速视频录制;步骤(2):像素‑距离比例因子计算与校准;步骤(3):落石冲击运动轨迹自动识别;步骤(4):时域含噪信号频域分析及其能量分布;步骤(5):高斯函数与高斯小波族选择;步骤(6):信号伪频率确定与尺度参数选择;步骤(7):时域含噪信号与高斯小波的卷积运算;步骤(8):落石运动位移、速度、加速度信号反馈及其自洽性检查。本发明实现了非接触式落石防护动态响应信号的自动识别及实时反馈。

Figure 202210653638

The present invention relates to the technical field of slope rockfall disaster protection, and relates to a non-contact rockfall protection dynamic response signal automatic identification and feedback method, which includes the following steps: step (1): camera location arrangement and high-speed video recording during the impact process; step ( 2): Calculation and calibration of the pixel-distance scale factor; Step (3): Automatic recognition of rockfall impact trajectory; Step (4): Time domain noisy signal frequency domain analysis and its energy distribution; Step (5): Gaussian function and Gaussian wavelet family selection; step (6): signal pseudo-frequency determination and scale parameter selection; step (7): convolution operation of time-domain noisy signal and Gaussian wavelet; step (8): rockfall movement displacement, velocity, acceleration signal Feedback and its consistency check. The invention realizes the automatic identification and real-time feedback of the non-contact rockfall protection dynamic response signal.

Figure 202210653638

Description

非接触式落石防护动态响应信号自动识别及反馈方法Non-contact rockfall protection dynamic response signal automatic identification and feedback method

技术领域technical field

本发明涉及边坡落石灾害防护技术领域,具体地说,涉及一种非接触式落石防护动态响应信号自动识别及反馈方法。The invention relates to the technical field of slope rockfall disaster protection, in particular to a non-contact rockfall protection dynamic response signal automatic identification and feedback method.

背景技术Background technique

柔性防护网是一种常用于用于崩塌落石防护的强非线性结构,工作时易遭遇落石的连续冲击作用。一定冲击能量下,落石与拦截网片之间将发生多次碰撞、回弹过程,最终稳定于柔性网面。落石与防护网相互作用时,通过实时监测落石运动状态可以间接得到防护网变形、防护能级、冲击荷载等信息,为防护网系统抗冲击性能评价及工程设计提供关键数据支撑。但是,连续冲击作用下防护网物理特性与结构响应不断发生变化,落石运动信号为非线性、非稳态的瞬态脉冲信号。采用传统接触式有线设备测量落石防护动态响应信号时易发生设备损坏及信号不稳定现象。特别地,在噪声干扰条件下,实现落石运动数据信号的自动反馈与信息反馈均非常困难。The flexible protective net is a strong nonlinear structure commonly used for protection against landslides and rockfalls, and it is prone to continuous impacts from falling rocks during work. Under a certain impact energy, there will be multiple collisions and rebound processes between the falling rock and the intercepting mesh, and finally stabilize on the flexible mesh surface. When falling rocks interact with the protective net, the deformation of the protective net, protection energy level, impact load and other information can be indirectly obtained by monitoring the movement state of the falling rock in real time, providing key data support for the impact resistance performance evaluation and engineering design of the protective net system. However, the physical characteristics and structural response of the protective net are constantly changing under continuous impact, and the rockfall motion signal is a nonlinear and unsteady transient pulse signal. When traditional contact wired equipment is used to measure the dynamic response signal of rockfall protection, equipment damage and signal instability are prone to occur. In particular, under the condition of noise interference, it is very difficult to realize automatic feedback and information feedback of rockfall motion data signals.

发明内容Contents of the invention

本发明的内容是提供一种基于小波变换的非接触式落石防护动态响应信号自动识别及反馈方法,其能够克服现有技术的某种或某些缺陷。The content of the present invention is to provide a non-contact rockfall protection dynamic response signal automatic identification and feedback method based on wavelet transform, which can overcome some or some defects of the prior art.

根据本发明的非接触式落石防护动态响应信号自动识别及反馈方法,其包括如下步骤:According to the non-contact rockfall protection dynamic response signal automatic identification and feedback method of the present invention, it comprises the following steps:

步骤(1):摄像机位布置及冲击过程高速视频录制;Step (1): Camera placement and high-speed video recording during the impact process;

步骤(2):像素-距离比例因子计算与校准;Step (2): Calculation and calibration of pixel-distance scale factor;

步骤(3):落石冲击运动轨迹自动识别;Step (3): automatic recognition of rockfall impact trajectory;

步骤(4):时域含噪信号频域分析及其能量分布;Step (4): frequency domain analysis and energy distribution of noisy signal in time domain;

步骤(5):高斯函数与高斯小波族选择;Step (5): Gaussian function and Gaussian wavelet family selection;

步骤(6):信号伪频率确定与尺度参数选择;Step (6): signal pseudo-frequency determination and scale parameter selection;

步骤(7):时域含噪信号与高斯小波的卷积运算;Step (7): the convolution operation of the noise-containing signal in the time domain and the Gaussian wavelet;

步骤(8):落石运动位移、速度、加速度信号反馈及其自洽性检查。Step (8): Feedback of rockfall movement displacement, velocity, acceleration signal and its self-consistency check.

作为优选,步骤(1)中,根据柔性防护网安装位置架设2台高速摄像机,摄像机机位与录制目标之间因满足不同距离、不同角度要求;设置摄像机帧率,对冲击全过程进行录制;摄像机最小帧率应满足采样定理要求,最大帧率应当保证录制时间能够大于或等于冲击全过程时长。As a preference, in step (1), set up 2 high-speed cameras according to the installation position of the flexible protective net, because different distances and different angle requirements are satisfied between the camera position and the recording target; the frame rate of the camera is set, and the whole process of impact is recorded; The minimum frame rate of the camera should meet the requirements of the sampling theorem, and the maximum frame rate should ensure that the recording time can be greater than or equal to the duration of the entire impact process.

作为优选,步骤(2)中,选择高速视频画面中的不同目标物体,分别测量各个目标物体的实际特征长度;记录高速视频画面中选定目标物体所占的像素数量,根据视频画面像素与特征长度之间的一一对应关系计算像素-距离比例因子。As preferably, in step (2), select different target objects in the high-speed video picture, measure the actual characteristic length of each target object respectively; The one-to-one correspondence between the lengths computes the pixel-distance scale factor.

作为优选,步骤(3)中,在视频画面中标注落石轮廓,通过调节画面对比度、亮度选取落石运动捕捉的特征点;在冲击全过程中应保证落石特征点不被完全遮挡;结合运动分析技术实现对落石特征点的自动捕捉及落石运动轨迹的自动识别;通过步骤(2)中计算的像素-距离比例因子将落石运动过程的捕捉像素点转换为落石位移时域信号fM[tn],其中n=1,2,…,N。Preferably, in step (3), mark the rockfall outline in the video picture, and select the feature points captured by the rockfall motion by adjusting the picture contrast and brightness; in the whole process of impact, it should be ensured that the rockfall feature points are not completely blocked; combined with motion analysis technology Realize the automatic capture of rockfall feature points and automatic recognition of rockfall trajectory; through the pixel-distance scale factor calculated in step (2), the captured pixel points of rockfall motion process are converted into rockfall displacement time domain signal f M [t n ] , where n=1,2,...,N.

作为优选,步骤(4)中,对步骤(3)中获得的落石位移时域信号fM[tn]进行离散傅里叶变换,得到落石运动信号的傅里叶变换结果F(ωk):Preferably, in step (4), discrete Fourier transform is performed on the rockfall displacement time-domain signal f M [t n ] obtained in step (3), to obtain the Fourier transform result F(ω k ) of the rockfall motion signal :

Figure GDA0003947768790000021
Figure GDA0003947768790000021

其中ωk为信号的频率值;根据落石位移时域信号的离散傅里叶变换结果,可进一步获得信号的频域能量Efreqwhere ω k is the frequency value of the signal; according to the discrete Fourier transform result of the rockfall displacement time domain signal, the frequency domain energy E freq of the signal can be further obtained:

Figure GDA0003947768790000031
Figure GDA0003947768790000031

记录能量占比为0~90%及能量占比为0~99%的信号频段,该能量段的频率记为ω90及ω99The signal frequency bands with energy ratio of 0-90% and energy ratio of 0-99% are recorded, and the frequencies of the energy bands are denoted as ω 90 and ω 99 .

作为优选,步骤(5)中,高斯函数是概率统计与随机信号分析应用中最重要的函数之一,高斯函数g(t)的表达式为:As preferably, in step (5), the Gaussian function is one of the most important functions in the application of probability statistics and random signal analysis, and the expression of the Gaussian function g(t) is:

Figure GDA0003947768790000032
Figure GDA0003947768790000032

其中C、α为常数;高斯函数的傅里叶变换

Figure GDA0003947768790000033
仍然为高斯函数:Among them, C and α are constants; the Fourier transform of the Gaussian function
Figure GDA0003947768790000033
Still Gaussian:

Figure GDA0003947768790000034
Figure GDA0003947768790000034

高斯函数具有光滑的无穷阶导数,且高斯函数的n阶导数具备小波函数振荡、能量有限的特征,通过对高斯函数的n阶微分运算,可以生成n个高斯母小波:The Gaussian function has a smooth infinite order derivative, and the n-order derivative of the Gaussian function has the characteristics of wavelet function oscillation and limited energy. Through the n-order differential operation of the Gaussian function, n Gaussian mother wavelets can be generated:

Figure GDA0003947768790000035
Figure GDA0003947768790000035

对小波函数gn(t)做伸缩、平移变换可以得到一系列小波函数,称为小波函数族:A series of wavelet functions can be obtained by stretching and translating the wavelet function g n (t), which is called the wavelet function family:

Figure GDA0003947768790000036
Figure GDA0003947768790000036

其中gu,s(t)称为高斯小波函数族,s称为尺度参数、u称为平移参数。Among them, g u,s (t) is called the Gaussian wavelet function family, s is called the scale parameter, and u is called the translation parameter.

作为优选,步骤(6)中,小波尺度参数并不等同于工程中更容易理解的傅里叶频率;小波尺度参数s对应的信号频域特征采用伪频率fs表示,尺度参数与伪频率的对应关系可由下式换算:Preferably, in step (6), the wavelet scale parameter is not equal to the Fourier frequency that is easier to understand in engineering; the signal frequency domain feature corresponding to the wavelet scale parameter s is represented by a pseudo-frequency f s , and the scale parameter and pseudo-frequency The corresponding relationship can be converted by the following formula:

Figure GDA0003947768790000037
Figure GDA0003947768790000037

其中Δt=1/fsamp为时域信号的采样时间间隔,fsamp为采样频率,fc=ωc/2π为小波中心频率,对于时域冲击信号,更关注大于零的频率成分,选定小波变换中采用的母小波函数gn(t)后,母小波时间中心tc、角频率中心ωc可由下式计算:Where Δt=1/f samp is the sampling time interval of the time domain signal, f samp is the sampling frequency, f cc /2π is the center frequency of the wavelet, for the time domain impact signal, more attention is paid to the frequency components greater than zero, and the selected After the mother wavelet function g n (t) is adopted in the wavelet transform, the mother wavelet time center t c and angular frequency center ω c can be calculated by the following formula:

Figure GDA0003947768790000041
Figure GDA0003947768790000041

作为优选,步骤(7)中,对步骤(2)中获得的落石位移信号与步骤(5)中选择的高斯小波进行卷积运算,得到时域含噪信号的高斯小波变换结果GWT(u,s):As preferably, in step (7), convolution operation is performed on the rockfall displacement signal obtained in step (2) and the Gaussian wavelet selected in step (5), to obtain the Gaussian wavelet transform result GWT(u, s):

Figure GDA0003947768790000042
Figure GDA0003947768790000042

其中

Figure GDA0003947768790000043
Figure GDA0003947768790000044
为g(t)的复共轭;根据卷积运算的微分性质,高斯小波变换最终可以写为以下形式:in
Figure GDA0003947768790000043
Figure GDA0003947768790000044
is the complex conjugate of g(t); according to the differential nature of the convolution operation, the Gaussian wavelet transform can finally be written as the following form:

Figure GDA0003947768790000045
Figure GDA0003947768790000045

上式表明,选择高斯小波进行小波变换的表达式中显式地包含了含微分运算dn/dun与卷积运算f(u)*gs(u);由于高斯函数在实数域积分不为零性质,卷积运算解释为函数f在核函数gs(u)的加权平均平滑过程,不同阶数的高斯小波对应着对原始含噪信号的不同阶数微分计算;通过小波变换,同时实现对含噪振动信号f的光滑及其在尺度s上的n阶微分。The above formula shows that the expression of choosing Gaussian wavelet for wavelet transform explicitly includes differential operation d n /du n and convolution operation f(u)*g s (u); is the zero property, the convolution operation is interpreted as the weighted average smoothing process of the function f in the kernel function g s (u), different orders of Gaussian wavelets correspond to different order differential calculations for the original noisy signal; through wavelet transform, at the same time Realize the smoothing of the noisy vibration signal f and its nth order differential on the scale s.

作为优选,步骤(8)中,对于实际的时域振动信号,小波变换微分结果除了保证曲线形状与波峰波谷位置的准确性,还需要保证微分结果幅值的准确性;从步骤(7)发现,小波微分结果的幅值与小波尺度参数的sn相关,同时小波函数族的规范化处理也会影响微分运算的幅值结果;为了消除高斯小波变换过程对微分结果幅值的影响,引入幅值参数Amp,将含噪信号的小波微分运算定义为:As a preference, in step (8), for the actual time-domain vibration signal, the wavelet transform differential result needs to ensure the accuracy of the differential result amplitude in addition to the accuracy of the curve shape and the peak and valley positions; from step (7), it is found that , the amplitude of the wavelet differential result is related to the s n of the wavelet scale parameter, and the normalization of the wavelet function family will also affect the amplitude result of the differential operation; in order to eliminate the influence of the Gaussian wavelet transform process on the differential result amplitude, the amplitude The parameter A mp defines the wavelet differential operation of the noisy signal as:

Figure GDA0003947768790000051
Figure GDA0003947768790000051

数值微分过程将放大信号中噪声干扰的影响,逆向来看,数值积分过程对原始信号中的噪声干扰将起到抑制作用;因此通过对小波微分结果进行反向积分,对比与原始信号之间的重合程度,则可以用于衡量小波微分结果的准确性,积分结果与原始信号之间的重合程度越高,则可以认为微分后的结果越为准确可靠;由于小波变换前后两段时间序列具有相同的长度,采用欧氏距离评价含噪信号与小波近似微分的积分结果之间的重合程度,欧式距离计算如下:The numerical differentiation process will amplify the influence of noise interference in the signal, and in reverse, the numerical integration process will inhibit the noise interference in the original signal; The degree of coincidence can be used to measure the accuracy of the wavelet differential results. The higher the degree of coincidence between the integral result and the original signal, the more accurate and reliable the result after differentiation can be. Since the two time series before and after wavelet transformation have the same Euclidean distance is used to evaluate the coincidence degree between the noisy signal and the integral result of wavelet approximate differentiation. The Euclidean distance is calculated as follows:

Figure GDA0003947768790000052
Figure GDA0003947768790000052

其中j表示对原始时域信号小波微分结果的等距离抽样,m为采样信号离散点的个数,n为小波微分阶数;

Figure GDA0003947768790000053
为小波变换n阶微分结果
Figure GDA0003947768790000054
的数值积分,tk为求积节点,Ak为求积系数,亦称伴随节点tk的权;当n=0时,
Figure GDA0003947768790000055
为含噪信号
Figure GDA0003947768790000056
与高斯函数g0(t)的卷积平滑结果;Where j represents the equidistant sampling of the wavelet differential results of the original time domain signal, m is the number of discrete points of the sampled signal, and n is the wavelet differential order;
Figure GDA0003947768790000053
is the nth order differential result of wavelet transform
Figure GDA0003947768790000054
, t k is the product node, A k is the product coefficient, also known as the weight of the accompanying node t k ; when n=0,
Figure GDA0003947768790000055
is a noisy signal
Figure GDA0003947768790000056
Convolution smoothing result with Gaussian function g 0 (t);

Figure GDA0003947768790000057
Figure GDA0003947768790000057

幅值参数Amp的值可通过迭代求解得到,当n阶小波微分的一次积分与n-1阶小波微分之间的欧氏距离达到最小值EDmin,即曲线的重合程度最高时,幅值参数得到最优值;最后,通过含噪信号与高斯函数卷积运算反馈落石冲击位移信号;通过含噪信号与一阶高斯小波卷积运算反馈落石冲击速度信号;通过含噪信号与二阶高斯小波卷积运算反馈落石冲击加速度信号。The value of the amplitude parameter A mp can be obtained by iterative solution. When the Euclidean distance between the first integral of the n-order wavelet differential and the n-1 order wavelet differential reaches the minimum value ED min , that is, when the coincidence degree of the curves is the highest, the amplitude Finally, the rockfall impact displacement signal is fed back through the convolution operation of the noisy signal and the Gaussian function; the rockfall impact velocity signal is fed back through the noise signal and the first-order Gaussian wavelet convolution operation; the noise-containing signal and the second-order Gaussian The wavelet convolution operation feeds back the rockfall impact acceleration signal.

本发明的基于高斯小波变换的信号处理方法可应用于落石运动分析。该方法能够实现高速视频中冲击落石自动识别与自动捕捉。利用高斯函数具有无穷阶光滑导数的特性,采用高斯小波对落石捕捉信号进行小波变换,可实现含噪信号的任意阶近似微分计算,导数阶数取决于小波函数的性质。小波方法有效解决了落石捕捉信号的微分信息反馈过程对噪声干扰的高度敏感性问题。高斯小波变换相当于对信号卷积光滑与求导的过程,通过一次卷积运算即可反馈含噪落石位移信号的微分结果,获得接近真实的落石速度、加速度时程,实现了非接触式落石防护动态响应信号的自动识别及实时反馈。The signal processing method based on Gaussian wavelet transform of the present invention can be applied to rockfall movement analysis. This method can realize the automatic recognition and automatic capture of impact rockfall in high-speed video. Taking advantage of the characteristic of Gaussian function having infinite order smooth derivative, Gaussian wavelet is used to carry out wavelet transform on rockfall capture signal, which can realize arbitrary order approximate differential calculation of noisy signal, and the order of derivative depends on the nature of wavelet function. The wavelet method effectively solves the problem of high sensitivity to noise interference in the differential information feedback process of rockfall capture signals. The Gaussian wavelet transform is equivalent to the process of smoothing and deriving the signal convolution. Through a convolution operation, the differential result of the noisy rockfall displacement signal can be fed back, and the rockfall velocity and acceleration time history close to the real one can be obtained, realizing non-contact rockfall Automatic identification and real-time feedback of protection dynamic response signals.

附图说明Description of drawings

图1为实施例1中一种基于小波变换的非接触式落石防护动态响应信号自动识别及反馈方法的流程图;Fig. 1 is the flow chart of a kind of non-contact rockfall protection dynamic response signal automatic identification and feedback method based on wavelet transform in embodiment 1;

图2为实施例1中高速相机布置与落石运动捕捉原理图;Fig. 2 is the schematic diagram of high-speed camera layout and rockfall motion capture in embodiment 1;

图3为实施例1中高斯函数、一阶高斯小波、二阶高斯小波示意图;Fig. 3 is Gaussian function, first-order Gaussian wavelet, second-order Gaussian wavelet schematic diagram in embodiment 1;

图4为实施例1中落石运动捕捉时域信号及其频域分布示意图;Fig. 4 is the time domain signal and its frequency domain distribution schematic diagram of rockfall motion capture in embodiment 1;

图5为实施例1中高斯小波变换幅值参数迭代流程图;Fig. 5 is the iterative flowchart of Gaussian wavelet transform magnitude parameter in embodiment 1;

图6为实施例1中落石运动位移、速度、加速度信号反馈结果图。Fig. 6 is a graph showing the feedback results of rockfall motion displacement, velocity, and acceleration signals in Embodiment 1.

其中,1、落石,2、落石冲击平面,3、标尺,4、一号高速摄像机,5、二号高速摄像机,6、高斯函数,7、一阶高斯小波,8、二阶高斯小波,9、落石位移捕捉信号,10、落石位移信号频域分布,11、落石位移信号频域能量分布,12、小波方法反馈的落石位移,13、小波方法反馈的落石速度,14、小波方法反馈的落石加速度。Among them, 1. Rockfall, 2. Rockfall impact plane, 3. Ruler, 4. No. 1 high-speed camera, 5. No. 2 high-speed camera, 6. Gaussian function, 7. First-order Gaussian wavelet, 8. Second-order Gaussian wavelet, 9 , Rockfall displacement capture signal, 10. Frequency domain distribution of rockfall displacement signal, 11. Frequency domain energy distribution of rockfall displacement signal, 12. Rockfall displacement fed back by wavelet method, 13. Rockfall speed fed back by wavelet method, 14. Rockfall feedback fed by wavelet method acceleration.

具体实施方式detailed description

为进一步了解本发明的内容,结合附图和实施例对本发明作详细描述。应当理解的是,实施例仅仅是对本发明进行解释而并非限定。In order to further understand the content of the present invention, the present invention will be described in detail in conjunction with the accompanying drawings and embodiments. It should be understood that the examples are only for explaining the present invention and not for limiting it.

实施例1Example 1

如图1-6所示,本实施例提供了一种基于小波变换的非接触式落石防护动态响应信号自动识别及反馈方法:As shown in Figures 1-6, this embodiment provides a non-contact rockfall protection dynamic response signal automatic identification and feedback method based on wavelet transform:

一:摄像机位布置及冲击过程高速视频录制1: Camera placement and high-speed video recording of the impact process

根据落石1冲击运动轨迹范围架设两台高速摄像机,其中一号高速摄像机4录制方向与落石冲击平面2为垂直关系,距离为d1;二号高速摄像机5录制方向与落石冲击平面2为平行关系,距离为d2。两台摄像机帧率均为fsample,对冲击全过程进行录制。Set up two high-speed cameras according to the range of the impact trajectory of the rockfall 1, wherein the recording direction of the No. 1 high-speed camera 4 is perpendicular to the impact plane 2 of the rockfall, and the distance is d1 ; the recording direction of the No. 2 high-speed camera 5 is parallel to the impact plane 2 of the rockfall , the distance is d 2 . The frame rate of the two cameras is f sample , recording the whole process of impact.

二:像素-距离比例因子计算与校准Two: Calculation and calibration of pixel-distance scale factor

选择高速视频画面中的参考目标分别为落石1、冲击平面中的标尺3,分别测量落石1的直径l1、标尺3长度为l2。记录高速视频画面中落石1直径所占的像素数量为m1,标尺3长度所占的像素数量为m2。测试不同的参考目标,根据视频画面像素与特征长度之间的对应关系计算像素-距离比例因子计算值λ。当满足下式时,认为获得了像素比例因子的校准值[λ]。Select the reference targets in the high-speed video screen as rockfall 1 and scale 3 in the impact plane, and measure the diameter l 1 of rockfall 1 and the length of scale 3 as l 2 . The number of pixels occupied by the diameter of the falling rock 1 in the recorded high-speed video is m 1 , and the number of pixels occupied by the length of the scale 3 is m 2 . Test different reference targets, and calculate the pixel-distance scale factor calculation value λ according to the correspondence between video picture pixels and feature lengths. When the following expression is satisfied, it is considered that the calibration value [λ] of the pixel scale factor is obtained.

Figure GDA0003947768790000071
Figure GDA0003947768790000071

三:落石冲击运动轨迹自动识别Three: Automatic recognition of rockfall impact trajectory

在视频画面中标注落石轮廓,通过调节画面对比度、亮度选取落石运动捕捉的特征点。在冲击全过程中应保证落石特征点不被完全遮挡。结合运动分析技术实现对落石特征点的自动捕捉及落石运动轨迹的自动识别。通过像素-距离比例因子的校准值[λ]将落石运动过程的捕捉像素点转换为落石位移时域信号fM[tn],其中n为记录的位移数据点数,n=1,2,…,N。Mark the outline of the rockfall in the video screen, and select the feature points captured by the motion capture of the rockfall by adjusting the contrast and brightness of the screen. During the whole process of impact, it should be ensured that the feature points of falling rocks are not completely blocked. Combined with motion analysis technology, the automatic capture of rockfall feature points and the automatic identification of rockfall motion trajectories are realized. Through the calibration value [λ] of the pixel-distance scale factor, the captured pixel points of the rockfall movement process are converted into the rockfall displacement time domain signal f M [t n ], where n is the number of recorded displacement data points, n=1,2,… , N.

四:时域含噪信号频域分析及其能量分布Four: Time domain noise signal frequency domain analysis and its energy distribution

对落石位移捕捉信号9(fM[tn])进行离散傅里叶变换,得到落石位移信号频域分布10为F(ωk):Discrete Fourier transform is performed on the rockfall displacement capture signal 9(f M [t n ]), and the frequency domain distribution 10 of the rockfall displacement signal is obtained as F(ω k ):

Figure GDA0003947768790000072
Figure GDA0003947768790000072

其中ωk为信号的频率值。根据落石位移时域信号的离散傅里叶变换结果,可进一步获得落石位移信号频域能量分布11为EfreqWhere ω k is the frequency value of the signal. According to the discrete Fourier transform result of the rockfall displacement time domain signal, the frequency domain energy distribution of the rockfall displacement signal can be further obtained as E freq :

Figure GDA0003947768790000073
Figure GDA0003947768790000073

记录能量占比为0~90%及能量占比为0~99%的信号频段,该能量段的频率记为ω90及ω99The signal frequency bands with energy ratio of 0-90% and energy ratio of 0-99% are recorded, and the frequencies of the energy bands are denoted as ω 90 and ω 99 .

五:高斯函数与高斯小波族选择Five: Gaussian function and Gaussian wavelet family selection

高斯小波是由高斯函数6的无穷阶导数生成的一系列函数族,高斯函数g(t)的一般表达式可写为:The Gaussian wavelet is a family of functions generated by the infinite derivative of the Gaussian function6. The general expression of the Gaussian function g(t) can be written as:

Figure GDA0003947768790000081
Figure GDA0003947768790000081

其中C、α为常数。高斯函数的傅里叶变换

Figure GDA0003947768790000082
仍然为高斯函数6:Among them, C and α are constants. Fourier transform of Gaussian function
Figure GDA0003947768790000082
Still for the Gaussian function 6:

Figure GDA0003947768790000083
Figure GDA0003947768790000083

高斯函数6具有光滑的无穷阶导数,且高斯函数6的n阶导数(n为正整数)具备小波函数振荡、能量有限的特征,通过对高斯函数6的n阶微分运算,可以生成n个高斯母小波:The Gaussian function 6 has a smooth infinite derivative, and the n-order derivative of the Gaussian function 6 (n is a positive integer) has the characteristics of wavelet function oscillation and limited energy. Through the n-order differential operation of the Gaussian function 6, n Gaussian functions can be generated Mother wavelet:

Figure GDA0003947768790000084
Figure GDA0003947768790000084

对小波函数gn(t)做伸缩、平移变换可以得到一系列小波函数,称为小波函数族:A series of wavelet functions can be obtained by stretching and translating the wavelet function g n (t), which is called the wavelet function family:

Figure GDA0003947768790000085
Figure GDA0003947768790000085

其中gu,s(t)称为高斯小波函数族,s称为尺度参数、u称为平移参数。Among them, g u,s (t) is called the Gaussian wavelet function family, s is called the scale parameter, and u is called the translation parameter.

当求解含噪时域冲击信号的平滑结果时,选择高斯函数6;当求解含噪时域冲击信号的一阶导数(速度)时,选择一阶高斯小波7;当求解含噪时域冲击信号的二阶导数(加速度)时,选择二阶高斯小波8。When solving the smoothing result of the noisy time-domain shock signal, choose the Gaussian function 6; when solving the first-order derivative (velocity) of the noisy time-domain shock signal, choose the first-order Gaussian wavelet 7; when solving the noisy time-domain shock signal When the second-order derivative (acceleration) of , choose the second-order Gaussian wavelet8.

六:信号伪频率确定与尺度参数选择Six: Signal pseudo-frequency determination and scale parameter selection

小波尺度参数并不等同于工程中更容易理解的傅里叶频率。小波尺度参数s对应的信号频域特征可采用伪频率fs表示,尺度参数与伪频率的对应关系可由下式换算:The wavelet scale parameter is not equivalent to the Fourier frequency which is easier to understand in engineering. The frequency domain characteristics of the signal corresponding to the wavelet scale parameter s can be represented by the pseudo frequency f s , and the corresponding relationship between the scale parameter and the pseudo frequency can be converted by the following formula:

Figure GDA0003947768790000091
Figure GDA0003947768790000091

其中Δt=1/fsamp为时域信号的采样时间间隔,fsamp为采样频率,fc=ωc/2π为小波中心频率,对于时域冲击信号,更关注大于零的频率成分,选定小波变换中采用的母小波函数gn(t)后,母小波时间中心tc、角频率中心ωc可由下式计算:Where Δt=1/f samp is the sampling time interval of the time domain signal, f samp is the sampling frequency, f c =ω c /2π is the wavelet center frequency, for the time domain impact signal, more attention should be paid to the frequency components greater than zero, and the selected After the mother wavelet function g n (t) is adopted in the wavelet transform, the mother wavelet time center t c and angular frequency center ω c can be calculated by the following formula:

Figure GDA0003947768790000092
Figure GDA0003947768790000092

七:时域含噪信号与高斯小波的卷积运算Seven: Convolution operation of noisy signal in time domain and Gaussian wavelet

对落石位移信号与高斯小波进行卷积运算,得到时域含噪信号的高斯小波变换结果GWT(u,s):Convolute the rockfall displacement signal with the Gaussian wavelet to obtain the Gaussian wavelet transform result GWT(u,s) of the noisy signal in the time domain:

Figure GDA0003947768790000093
Figure GDA0003947768790000093

其中

Figure GDA0003947768790000094
Figure GDA0003947768790000095
为g(t)的复共轭。根据卷积运算的微分性质,高斯小波变换最终可以写为以下形式:in
Figure GDA0003947768790000094
Figure GDA0003947768790000095
is the complex conjugate of g(t). According to the differential nature of the convolution operation, the Gaussian wavelet transform can finally be written as the following form:

Figure GDA0003947768790000096
Figure GDA0003947768790000096

高斯小波变换的表达式中显式地包含了含微分运算dn/dun与卷积运算f(u)*gs(u)。由于高斯函数在实数域积分不为零性质,卷积运算可以解释为函数f在核函数gs(u)的加权平均平滑过程,不同阶数的高斯小波对应着对原始含噪信号的不同阶数微分计算。通过小波变换,可以同时实现对含噪振动信号f的光滑及其在尺度s上的n阶微分。The expression of Gaussian wavelet transform explicitly includes differential operation d n / du n and convolution operation f(u)*g s (u). Due to the non-zero property of the Gaussian function integral in the real number field, the convolution operation can be interpreted as a weighted average smoothing process of the function f in the kernel function g s (u), and different orders of Gaussian wavelets correspond to different orders of the original noisy signal Numeral differential calculations. Through the wavelet transform, the smoothing of the noisy vibration signal f and its n-order differential on the scale s can be realized simultaneously.

八:落石运动位移、速度、加速度信号反馈及其自洽性检查。Eight: Rockfall movement displacement, velocity, acceleration signal feedback and self-consistency inspection.

对于实际的时域冲击信号,小波变换微分结果除了保证曲线形状与波峰波谷位置的准确性,还需要保证微分结果幅值的准确性。小波微分结果的幅值与小波尺度参数的sn相关,同时小波函数族的规范化处理也会影响微分运算的幅值结果。为了消除高斯小波变换过程对微分结果幅值的影响,将含噪信号的小波微分运算定义为:For the actual time-domain impact signal, the differential result of wavelet transform needs to ensure the accuracy of the amplitude of the differential result in addition to the accuracy of the shape of the curve and the position of the peak and valley. The magnitude of the wavelet differential result is related to the s n of the wavelet scale parameter, and the normalization of the wavelet function family will also affect the magnitude of the differential operation. In order to eliminate the influence of the Gaussian wavelet transform process on the amplitude of the differential result, the wavelet differential operation of the noisy signal is defined as:

Figure GDA0003947768790000101
Figure GDA0003947768790000101

其中Amp为幅值参数。数值微分过程将放大信号中噪声干扰的影响,逆向来看,数值积分过程对原始信号中的噪声干扰将起到抑制作用。因此通过对小波微分结果进行反向积分,对比与原始信号之间的重合程度,则可以用于衡量小波微分结果的准确性,积分结果与原始信号之间的重合程度越高,则可以认为微分后的结果越为准确可靠。由于小波变换前后两段时间序列具有相同的长度,可以方便地采用欧氏距离评价含噪信号与小波近似微分的积分结果之间的重合程度,欧式距离计算如下Among them, A mp is the amplitude parameter. The numerical differentiation process will amplify the influence of noise interference in the signal, and in reverse, the numerical integration process will inhibit the noise interference in the original signal. Therefore, by performing reverse integration on the wavelet differential result and comparing the degree of coincidence with the original signal, it can be used to measure the accuracy of the wavelet differential result. The higher the degree of coincidence between the integration result and the original signal, the differential can be considered The results are more accurate and reliable. Since the two time series before and after the wavelet transform have the same length, it is convenient to use the Euclidean distance to evaluate the degree of coincidence between the noisy signal and the integral result of the wavelet approximate differential. The Euclidean distance is calculated as follows

Figure GDA0003947768790000102
Figure GDA0003947768790000102

其中j表示对原始时域信号小波微分结果的等距离抽样,m为采样信号离散点的个数,n为小波微分阶数。

Figure GDA0003947768790000103
为小波变换n阶微分结果
Figure GDA0003947768790000104
的数值积分,tk为求积节点,Ak为求积系数,亦称伴随节点tk的权。特别地,当n=0时,
Figure GDA0003947768790000105
为含噪信号
Figure GDA0003947768790000106
与高斯函数g0(t)的卷积平滑结果。Where j represents the equidistant sampling of the wavelet differential results of the original time domain signal, m is the number of discrete points of the sampled signal, and n is the wavelet differential order.
Figure GDA0003947768790000103
is the nth order differential result of wavelet transform
Figure GDA0003947768790000104
The numerical integration of , t k is the product node, and A k is the product coefficient, also known as the weight of the accompanying node t k . In particular, when n=0,
Figure GDA0003947768790000105
is a noisy signal
Figure GDA0003947768790000106
Convolution smoothing result with Gaussian function g 0 (t).

Figure GDA0003947768790000107
Figure GDA0003947768790000107

幅值参数Amp的值可通过迭代求解得到,如流程图5所示,当n阶小波微分的一次积分与n-1阶小波微分之间的欧氏距离达到最小值EDmin,即曲线的重合程度最高时,幅值参数Amp得到最优值。最后,分别获得小波方法反馈的落石位移12、小波方法反馈的落石速度13及小波方法反馈的落石加速度14。The value of the amplitude parameter A mp can be obtained by iterative solution, as shown in the flow chart 5, when the Euclidean distance between the first integral of the n-order wavelet differential and the n-1 order wavelet differential reaches the minimum value ED min , that is, the curve When the degree of coincidence is the highest, the amplitude parameter A mp gets the optimal value. Finally, the rockfall displacement 12 fed back by the wavelet method, the rockfall velocity 13 fed back by the wavelet method, and the rockfall acceleration 14 fed back by the wavelet method are respectively obtained.

本实施例利用高斯函数具有无穷阶光滑可导的性质,将落石高速视频捕捉信号与高斯小波族进行卷积,阐释了小波变换近似微分过程及其对抗噪声干扰的原理,建立了基于高斯小波变换理论的非接触式落石速度、加速度信息自动识别及反馈程序。通过引入幅值参数控制小波变换处理信号与真实信号间的匹配程度。根据时域捕捉信号能量分布的主要频段,对小波尺度参数进行了校准。发明的方法有效解决了落石捕捉信号的微分信息反馈过程对噪声干扰的高度敏感性问题,提高了冲击信号的信噪比水平,规避了传统接触式有线设备用于监测、记录高速落石防护动态响应信号的不稳定性及易损性难题。In this embodiment, the Gaussian function has the property of infinite order smoothness and derivability, and the high-speed video capture signal of falling rocks is convolved with the Gaussian wavelet family, and the approximate differential process of wavelet transform and the principle of anti-noise interference are explained. Theoretical non-contact rockfall speed, acceleration information automatic identification and feedback program. The degree of matching between the signal processed by wavelet transform and the real signal is controlled by introducing the amplitude parameter. The wavelet scale parameters are calibrated according to the main frequency bands in which the signal energy distribution is captured in the time domain. The invented method effectively solves the problem of high sensitivity to noise interference in the differential information feedback process of the rockfall capture signal, improves the signal-to-noise ratio level of the impact signal, and avoids the use of traditional contact wired equipment for monitoring and recording the dynamic response of high-speed rockfall protection Signal instability and vulnerability problems.

以上示意性的对本发明及其实施方式进行了描述,该描述没有限制性,附图中所示的也只是本发明的实施方式之一,实际的结构并不局限于此。所以,如果本领域的普通技术人员受其启示,在不脱离本发明创造宗旨的情况下,不经创造性的设计出与该技术方案相似的结构方式及实施例,均应属于本发明的保护范围。The above schematically describes the present invention and its implementation, which is not restrictive, and what is shown in the drawings is only one of the implementations of the present invention, and the actual structure is not limited thereto. Therefore, if a person of ordinary skill in the art is inspired by it, without departing from the inventive concept of the present invention, without creatively designing a structural mode and embodiment similar to the technical solution, it shall all belong to the protection scope of the present invention .

Claims (6)

1.非接触式落石防护动态响应信号自动识别及反馈方法,其特征在于:包括如下步骤:1. The non-contact rockfall protection dynamic response signal automatic identification and feedback method is characterized in that it includes the following steps: 步骤(1):摄像机位布置及冲击过程高速视频录制;Step (1): Camera placement and high-speed video recording during the impact process; 步骤(2):像素-距离比例因子计算与校准;Step (2): Calculation and calibration of pixel-distance scale factor; 步骤(2)中,选择高速视频画面中的不同目标物体,分别测量各个目标物体的实际特征长度;记录高速视频画面中选定目标物体所占的像素数量,根据视频画面像素与特征长度之间的一一对应关系计算像素-距离比例因子;In step (2), select different target objects in the high-speed video picture, and measure the actual characteristic length of each target object respectively; The one-to-one correspondence relationship calculates the pixel-distance scale factor; 步骤(3):落石冲击运动轨迹自动识别;Step (3): automatic recognition of rockfall impact trajectory; 步骤(4):落石位移时域信号频域分析及其能量分布;Step (4): frequency domain analysis of rockfall displacement time domain signal and its energy distribution; 步骤(5):高斯函数与高斯小波族选择;Step (5): Gaussian function and Gaussian wavelet family selection; 步骤(5)中,高斯函数是概率统计与随机信号分析应用中最重要的函数之一,高斯函数g(t)的表达式为:In step (5), the Gaussian function is one of the most important functions in the application of probability statistics and random signal analysis. The expression of the Gaussian function g(t) is:
Figure FDA0003947768780000011
Figure FDA0003947768780000011
其中C、α为常数;高斯函数的傅里叶变换
Figure FDA0003947768780000012
仍然为高斯函数:
Among them, C and α are constants; the Fourier transform of the Gaussian function
Figure FDA0003947768780000012
Still Gaussian:
Figure FDA0003947768780000013
Figure FDA0003947768780000013
高斯函数具有光滑的无穷阶导数,且高斯函数的n阶导数具备小波函数振荡、能量有限的特征,通过对高斯函数的n阶微分运算,生成n个高斯母小波:The Gaussian function has a smooth infinite order derivative, and the n-order derivative of the Gaussian function has the characteristics of wavelet function oscillation and limited energy. Through the n-order differential operation of the Gaussian function, n Gaussian mother wavelets are generated:
Figure FDA0003947768780000014
Figure FDA0003947768780000014
对小波函数gn(t)做伸缩、平移变换得到一系列小波函数,称为小波函数族:A series of wavelet functions are obtained by stretching and translating the wavelet function g n (t), which is called the wavelet function family:
Figure FDA0003947768780000015
Figure FDA0003947768780000015
其中gu,s(t)称为高斯小波函数族,s称为尺度参数、u称为平移参数;Among them, g u,s (t) is called the Gaussian wavelet function family, s is called the scale parameter, and u is called the translation parameter; 步骤(6):信号伪频率确定与尺度参数选择;Step (6): signal pseudo-frequency determination and scale parameter selection; 步骤(6)中,小波尺度参数并不等同于工程中更容易理解的傅里叶频率;小波尺度参数s对应的信号频域特征采用伪频率fs表示,尺度参数与伪频率的对应关系由下式换算:In step (6), the wavelet scale parameter is not equal to the Fourier frequency which is easier to understand in engineering; the frequency domain characteristics of the signal corresponding to the wavelet scale parameter s are represented by a pseudo-frequency f s , and the corresponding relationship between the scale parameter and the pseudo-frequency is given by The following conversion:
Figure FDA0003947768780000021
Figure FDA0003947768780000021
其中Δt=1/fsamp为时域信号的采样时间间隔,fsamp为采样频率,fc=ωc/2π为小波中心频率,对于时域冲击信号,更关注大于零的频率成分,选定小波变换中采用的母小波函数gn(t)后,母小波时间中心tc、角频率中心ωc由下式计算:Where Δt=1/f samp is the sampling time interval of the time domain signal, f samp is the sampling frequency, f cc /2π is the center frequency of the wavelet, for the time domain impact signal, more attention is paid to the frequency components greater than zero, and the selected After the mother wavelet function g n (t) is adopted in the wavelet transform, the mother wavelet time center t c and angular frequency center ω c are calculated by the following formula:
Figure FDA0003947768780000022
Figure FDA0003947768780000022
步骤(7):落石位移时域信号与高斯小波的卷积运算;Step (7): Convolution operation of rockfall displacement time domain signal and Gaussian wavelet; 步骤(8):落石运动位移、速度、加速度信号反馈及其自洽性检查。Step (8): Feedback of rockfall movement displacement, velocity, acceleration signal and its self-consistency check.
2.根据权利要求1所述的非接触式落石防护动态响应信号自动识别及反馈方法,其特征在于:步骤(1)中,根据柔性防护网安装位置架设2台高速摄像机,摄像机机位与录制目标之间因满足不同距离、不同角度要求;设置摄像机帧率,对冲击全过程进行录制;摄像机最小帧率应满足采样定理要求,最大帧率应当保证录制时间能够大于或等于冲击全过程时长。2. The non-contact rockfall protection dynamic response signal automatic identification and feedback method according to claim 1, characterized in that: in step (1), 2 high-speed cameras are set up according to the installation position of the flexible protective net, and the camera position and recording Due to different distances and different angles between targets; set the frame rate of the camera to record the whole impact process; the minimum frame rate of the camera should meet the requirements of the sampling theorem, and the maximum frame rate should ensure that the recording time can be greater than or equal to the duration of the entire impact process. 3.根据权利要求1所述的非接触式落石防护动态响应信号自动识别及反馈方法,其特征在于:步骤(3)中,在视频画面中标注落石轮廓,通过调节画面对比度、亮度选取落石运动捕捉的特征点;在冲击全过程中应保证落石特征点不被完全遮挡;结合运动分析技术实现对落石特征点的自动捕捉及落石运动轨迹的自动识别;通过步骤(2)中计算的像素-距离比例因子将落石运动过程的捕捉像素点转换为落石位移时域信号fM[tn],其中n=1,2,…,N。3. The non-contact rockfall protection dynamic response signal automatic identification and feedback method according to claim 1, characterized in that: in step (3), the rockfall contour is marked in the video picture, and the rockfall movement is selected by adjusting the picture contrast and brightness The captured feature points; in the whole process of impact, it should be ensured that the feature points of the rockfall are not completely blocked; combined with motion analysis technology, the automatic capture of the feature points of the rockfall and the automatic identification of the trajectory of the rockfall; through the pixels calculated in step (2)- The distance scale factor converts the captured pixel points in the rockfall movement process into the rockfall displacement time domain signal f M [t n ], where n=1,2,...,N. 4.根据权利要求3所述的非接触式落石防护动态响应信号自动识别及反馈方法,其特征在于:步骤(4)中,对步骤(3)中获得的落石位移时域信号fM[tn]进行离散傅里叶变换,得到落石位移时域信号的傅里叶变换结果F(ωk):4. The non-contact rockfall protection dynamic response signal automatic identification and feedback method according to claim 3, characterized in that: in step (4), the rockfall displacement time domain signal f M [t n ] to perform discrete Fourier transform to obtain the Fourier transform result F(ω k ) of the rockfall displacement time domain signal:
Figure FDA0003947768780000031
Figure FDA0003947768780000031
其中ωk为信号的频率值;根据落石位移时域信号的离散傅里叶变换结果,进一步获得信号的频域能量EfreqWhere ω k is the frequency value of the signal; according to the discrete Fourier transform result of the rockfall displacement time domain signal, the frequency domain energy E freq of the signal is further obtained:
Figure FDA0003947768780000032
Figure FDA0003947768780000032
记录能量占比为0~90%及能量占比为0~99%的信号频段,该能量段的频率记为ω90及ω99The signal frequency bands with energy ratio of 0-90% and energy ratio of 0-99% are recorded, and the frequencies of the energy bands are denoted as ω 90 and ω 99 .
5.根据权利要求1所述的非接触式落石防护动态响应信号自动识别及反馈方法,其特征在于:步骤(7)中,对步骤(2)中获得的落石位移时域信号与步骤(5)中选择的高斯小波进行卷积运算,得到落石位移时域信号的高斯小波变换结果GWT(u,s):5. The non-contact rockfall protection dynamic response signal automatic identification and feedback method according to claim 1, characterized in that: in the step (7), the time domain signal of the rockfall displacement obtained in the step (2) is compared with the step (5 ) to perform convolution operation on the Gaussian wavelet selected in ), and obtain the Gaussian wavelet transform result GWT(u,s) of the rockfall displacement time domain signal:
Figure FDA0003947768780000033
Figure FDA0003947768780000033
其中
Figure FDA0003947768780000034
Figure FDA0003947768780000035
为g(t)的复共轭;根据卷积运算的微分性质,高斯小波变换最终写为以下形式:
in
Figure FDA0003947768780000034
Figure FDA0003947768780000035
is the complex conjugate of g(t); according to the differential nature of the convolution operation, the Gaussian wavelet transform is finally written as the following form:
Figure FDA0003947768780000036
Figure FDA0003947768780000036
上式表明,选择高斯小波进行小波变换的表达式中显式地包含了含微分运算dn/dun与卷积运算f(u)*gs(u);由于高斯函数在实数域积分不为零性质,卷积运算解释为函数f在核函数gs(u)的加权平均平滑过程,不同阶数的高斯小波对应着对原始落石位移时域信号的不同阶数微分计算;通过小波变换,同时实现对含噪振动信号f的光滑及其在尺度s上的n阶微分。The above formula shows that the expression of choosing Gaussian wavelet for wavelet transform explicitly includes differential operation d n /du n and convolution operation f(u)*g s (u); is the zero property, the convolution operation is interpreted as the weighted average smoothing process of the function f in the kernel function g s (u), different orders of Gaussian wavelets correspond to different order differential calculations of the original rockfall displacement time domain signal; through wavelet transform , and at the same time realize the smoothing of the noisy vibration signal f and its nth order differential on the scale s.
6.根据权利要求1所述的非接触式落石防护动态响应信号自动识别及反馈方法,其特征在于:步骤(8)中,对于实际的时域振动信号,小波变换微分结果除了保证曲线形状与波峰波谷位置的准确性,还需要保证微分结果幅值的准确性;从步骤(7)发现,小波微分结果的幅值与小波尺度参数的sn相关,同时小波函数族的规范化处理也会影响微分运算的幅值结果;为了消除高斯小波变换过程对微分结果幅值的影响,引入幅值参数Amp,将落石位移时域信号的小波微分运算定义为:6. The non-contact rockfall protection dynamic response signal automatic identification and feedback method according to claim 1, characterized in that: in the step (8), for the actual time-domain vibration signal, the wavelet transform differential result is in addition to ensuring that the curve shape and The accuracy of the position of the peak and valley also needs to ensure the accuracy of the amplitude of the differential result; from step (7), it is found that the amplitude of the wavelet differential result is related to the s n of the wavelet scale parameter, and the normalization of the wavelet function family will also affect The amplitude result of the differential operation; in order to eliminate the influence of the Gaussian wavelet transform process on the differential result amplitude, the amplitude parameter A mp is introduced, and the wavelet differential operation of the rockfall displacement time domain signal is defined as:
Figure FDA0003947768780000041
Figure FDA0003947768780000041
数值微分过程将放大信号中噪声干扰的影响,逆向来看,数值积分过程对原始信号中的噪声干扰将起到抑制作用;因此通过对小波微分结果进行反向积分,对比与原始信号之间的重合程度,则用于衡量小波微分结果的准确性,积分结果与原始信号之间的重合程度越高,则认为微分后的结果越为准确可靠;由于小波变换前后两段时间序列具有相同的长度,采用欧氏距离评价落石位移时域信号与小波近似微分的积分结果之间的重合程度,欧式距离计算如下:The numerical differentiation process will amplify the influence of noise interference in the signal, and in reverse, the numerical integration process will inhibit the noise interference in the original signal; The degree of coincidence is used to measure the accuracy of the wavelet differential results. The higher the degree of coincidence between the integral result and the original signal, the more accurate and reliable the differential result is; since the two time series before and after the wavelet transform have the same length , the Euclidean distance is used to evaluate the coincidence degree between the time domain signal of the rockfall displacement and the integral result of the wavelet approximate differential. The Euclidean distance is calculated as follows:
Figure FDA0003947768780000042
Figure FDA0003947768780000042
其中j表示对原始时域信号小波微分结果的等距离抽样,m为采样信号离散点的个数,n为小波微分阶数;
Figure FDA0003947768780000043
为小波变换n阶微分结果
Figure FDA0003947768780000044
的数值积分,tk为求积节点,Ak为求积系数,亦称伴随节点tk的权;当n=0时,
Figure FDA0003947768780000045
为落石位移时域信号
Figure FDA0003947768780000046
与小波函数g0(t)的卷积平滑结果;
Where j represents the equidistant sampling of the wavelet differential results of the original time domain signal, m is the number of discrete points of the sampled signal, and n is the wavelet differential order;
Figure FDA0003947768780000043
is the nth order differential result of wavelet transform
Figure FDA0003947768780000044
, t k is the product node, A k is the product coefficient, also known as the weight of the accompanying node t k ; when n=0,
Figure FDA0003947768780000045
is the rockfall displacement time domain signal
Figure FDA0003947768780000046
Convolution smoothing result with wavelet function g 0 (t);
Figure FDA0003947768780000047
Figure FDA0003947768780000047
幅值参数Amp的值通过迭代求解得到,当n阶小波微分的一次积分与n-1阶小波微分之间的欧氏距离达到最小值EDmin,即曲线的重合程度最高时,幅值参数得到最优值;最后,通过落石位移时域信号与小波函数卷积运算反馈落石冲击位移信号;通过落石位移时域信号与一阶高斯小波卷积运算反馈落石冲击速度信号;通过落石位移时域信号与二阶高斯小波卷积运算反馈落石冲击加速度信号。The value of the amplitude parameter A mp is obtained by iterative solution. When the Euclidean distance between the first integral of the n-order wavelet differential and the n-1 order wavelet differential reaches the minimum value ED min , that is, when the coincidence degree of the curves is the highest, the amplitude parameter The optimal value is obtained; finally, the rockfall impact displacement signal is fed back through the rockfall displacement time domain signal and wavelet function convolution operation; the rockfall impact velocity signal is fed back through the rockfall displacement time domain signal and the first-order Gaussian wavelet convolution operation; the rockfall impact velocity signal is fed back through the rockfall displacement time domain The signal and the second-order Gaussian wavelet convolution operation feed back the rockfall impact acceleration signal.
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