{"title":"利用反向传播神经网络识别井间探地雷达轨迹上的首破时间","authors":"D. Rucker, T. Ferré, M. Poulton","doi":"10.1117/12.462226","DOIUrl":null,"url":null,"abstract":"Manually picking the first anival of energy in a series of cross borehole GPR ray traces can be time consuming and subjective, especially when large data sets need to be processed. One possible remedy is the application of a back propagating neural network. Neural network applications have been used previously in seismic studies to pick the arrival of the P and S waves (Dai and MacBeth, 1997; McCormack et al. 1993; Murat et al. 1992). One particular method, which applied a moving window over the trace, is used here with slight modification. Noisy time-amplitude records were first normalized to range from —1 and 1 . These data were then filtered such that values between —1 and a negative threshold were set to —1 , values between 1 and a positive threshold were set to 1 and all other values were set to zero. The filtered wave was fed through a neural network that searched for a pattern related to a first arrival. Several filtering parameters were tested, including the size of the moving window, the values of the positive and negative thresholds, and neural network parameters pertaining to training and testing. With minimal training, the neural network performed very well compared to hand picking of arrival times on large data sets.","PeriodicalId":256772,"journal":{"name":"International Conference on Ground Penetrating Radar","volume":"388 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2002-04-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Back propagation neural network for identifying first-break times on cross-borehole ground-penetrating radar traces\",\"authors\":\"D. Rucker, T. Ferré, M. Poulton\",\"doi\":\"10.1117/12.462226\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Manually picking the first anival of energy in a series of cross borehole GPR ray traces can be time consuming and subjective, especially when large data sets need to be processed. One possible remedy is the application of a back propagating neural network. Neural network applications have been used previously in seismic studies to pick the arrival of the P and S waves (Dai and MacBeth, 1997; McCormack et al. 1993; Murat et al. 1992). One particular method, which applied a moving window over the trace, is used here with slight modification. Noisy time-amplitude records were first normalized to range from —1 and 1 . These data were then filtered such that values between —1 and a negative threshold were set to —1 , values between 1 and a positive threshold were set to 1 and all other values were set to zero. The filtered wave was fed through a neural network that searched for a pattern related to a first arrival. Several filtering parameters were tested, including the size of the moving window, the values of the positive and negative thresholds, and neural network parameters pertaining to training and testing. With minimal training, the neural network performed very well compared to hand picking of arrival times on large data sets.\",\"PeriodicalId\":256772,\"journal\":{\"name\":\"International Conference on Ground Penetrating Radar\",\"volume\":\"388 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2002-04-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"International Conference on Ground Penetrating Radar\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1117/12.462226\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"International Conference on Ground Penetrating Radar","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1117/12.462226","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
在一系列井间探地雷达射线轨迹中,人工选择第一个能量值既耗时又主观,尤其是在需要处理大型数据集的情况下。一种可能的补救方法是应用反向传播神经网络。以前在地震研究中已经使用神经网络应用来选择P波和S波的到达(Dai和MacBeth, 1997;McCormack et al. 1993;Murat et al. 1992)。这里使用了一种特殊的方法,即在跟踪上应用移动窗口,并进行了轻微修改。噪声时间振幅记录首先归一化为-1和1的范围。然后对这些数据进行过滤,使-1和负阈值之间的值设置为-1,1和正阈值之间的值设置为1,所有其他值设置为零。过滤后的波被输入一个神经网络,该网络搜索与第一次到达有关的模式。测试了几个滤波参数,包括移动窗口的大小、正阈值和负阈值以及与训练和测试相关的神经网络参数。与在大型数据集上手动挑选到达时间相比,只需最少的训练,神经网络的表现就非常好。
Back propagation neural network for identifying first-break times on cross-borehole ground-penetrating radar traces
Manually picking the first anival of energy in a series of cross borehole GPR ray traces can be time consuming and subjective, especially when large data sets need to be processed. One possible remedy is the application of a back propagating neural network. Neural network applications have been used previously in seismic studies to pick the arrival of the P and S waves (Dai and MacBeth, 1997; McCormack et al. 1993; Murat et al. 1992). One particular method, which applied a moving window over the trace, is used here with slight modification. Noisy time-amplitude records were first normalized to range from —1 and 1 . These data were then filtered such that values between —1 and a negative threshold were set to —1 , values between 1 and a positive threshold were set to 1 and all other values were set to zero. The filtered wave was fed through a neural network that searched for a pattern related to a first arrival. Several filtering parameters were tested, including the size of the moving window, the values of the positive and negative thresholds, and neural network parameters pertaining to training and testing. With minimal training, the neural network performed very well compared to hand picking of arrival times on large data sets.