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Single-shot spatially resolved characterization of laser-induced shock waves in water

机译:水中激光激波的单次空间分辨特征

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We have developed an optical method for single-shot spatially resolved shock-wave peak-pressure measurements. A schlieren technique and streak photography were used to follow the propagation of the shock wave. The shock position r as a function of time was extracted from the streak images by digital image-processing techniques. The resulting r(t) curves were differentiated with respect to time to yield shock-wave velocities that were converted to shock pressures with the aid of the equation of the state of the medium. Features and limitations of the technique are demonstrated and discussed on the basis of measurements of shock-wave amplitudes generated by laser-induced breakdown in water. For this purpose, laser pulses of 6-ns duration and pulse energies of 1 and 10 mJ were focused into a cuvette containing water. Complete p(t) curves were obtained with a temporal resolution in the subnanosecond range. The total acquisition and processing time for a single event is similar to 2 min. The shock-peak. pressures at the source were found to be 8.4 +/- 1.5 and 11.8 +/- 1.6 GPa for pulse energies of 1 and 10 mJ, respectively. Within the first two source radii, the shock-wave pressure p(r) was found to decay on average in proportion to r(-1.3+/-0.2) for both pulse energies. Thereafter the pressure dropped in proportion to r(-2.2+/-0.1). In water the method can be used to measure shock-wave amplitudes exceeding 0.1 GPa. Because it is a single-shot technique, the method is especially suited for investigating events with large statistical variations. (C) 1998 Optical Society of America. [References: 28]
机译:我们已经开发了一种用于单次空间分辨激波峰值压力测量的光学方法。使用schlieren技术和条纹摄影来跟踪冲击波的传播。通过数字图像处理技术从条纹图像中提取作为时间的函数的冲击位置r。相对于时间微分所得的r(t)曲线,以产生冲击波速度,借助介质状态方程将其转换为冲击压力。在测量由激光引起的水中击穿产生的冲击波振幅的基础上,论证并讨论了该技术的特点和局限性。为此,将6 ns持续时间的激光脉冲以及1和10 mJ的脉冲能量聚焦到一个装有水的比色杯中。获得了完整的p(t)曲线,时间分辨率在亚纳秒范围内。单个事件的总采集和处理时间约为2分钟。令人震惊的高峰。发现对于1和10 mJ的脉冲能量,源处的压力分别为8.4 +/- 1.5 GPa和11.8 +/- 1.6 GPa。在前两个源半径内,发现两种脉冲能量的冲击波压力p(r)平均均与r(-1.3 +/- 0.2)成比例地衰减。此后,压力下降与r(-2.2 +/- 0.1)成比例。在水中,该方法可用于测量超过0.1 GPa的冲击波振幅。因为它是单发技术,所以该方法特别适合调查具有较大统计差异的事件。 (C)1998年美国眼镜学会。 [参考:28]

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