用地震声缺陷镜评价桩的连续性

E. Degaev, Boris S. Kraev, Dmitry G. Bobylev
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引用次数: 1

摘要

介绍。作者介绍了用地震声缺陷镜进行的桩连续性研究的结果。测试在罗斯托夫地区和莫斯科进行。给出了测试桩的反射图,以及随后对设计桩身长度和连续性的解释和确认。材料和方法。研究结果采用Spektr 4.3,其工作原理基于弹性波传播理论。该装置用于记录在预设脉冲参数下桩对外界冲击的响应。信号通过一个加速度计传感器记录下来,并连接到一台装有数字化和解读输入信息软件的专用计算机上。数据处理结果以计算机图形图像(反射图)的形式呈现,显示桩的长度、连续性、损伤(如果有的话)及其位置。结果。确定了土壤均匀性与信号纯度之间的关系。在密度不同的两种土的界面处,声波被反射并部分通过,形成假缺陷的特征峰。为了消除虚假缺陷,有必要对层状土壤进行研究。结论。结果证实了土壤均匀性对信号纯度的影响。土壤结构的非均质性越高,反射图显示的假峰数量越多。正确解释桩基连续性试验结果的前提是对地质剖面进行研究,并对每一桩的超声传播速度进行初步的仪器识别。
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Using seismoacoustic defectoscopy to assess the continuity of piles
Introduction. The authors present the results of pile continuity studies conducted using seismoacoustic defectoscopy. Tests were conducted in the Rostov region and Moscow. Reflectograms of tested piles, as well as the subsequent interpretation and confirmation of the design length and continuity of the pile shaft are provided. Materials and methods. The research results were obtained using Spektr 4.3, whose operating principle is based on the theory of elastic wave propagation. This device is used for the recording of the pile response to external impacts with the preset pulse parameters. The signal is recorded by means of an accelerometer sensor, connected to a special computer with the software for the digitization and interpretation of incoming information. Data processing results are presented in the form of computer graphic images (reflectograms), which show the pile length, continuity, damages (if any) and their location. Results. The dependence between soil homogeneity and signal purity has been identified. At the interface between two types of soils that are different in density, the sound wave was reflected and partially passed further, creating characteristic peaks of false defects. To eliminate false defects, studies of layered soils are necessary. Conclusions. The results confirm the effect of the soil homogeneity on signal purity. The higher the heterogeneity of the soil structure, the bigger the number of false peaks that the reflectogram demonstrates. A prerequisite for the correct interpretation of the results of pile continuity testing is the study of the geological section and preliminary instrumental identification of the ultrasound propagation velocity for each individual pile.
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