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arXiv 1503.05640physics.flu-dyn
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背景定向纹影(BOS)技术在laser诱导的水下shock wave中的应用

Application of background-oriented schlieren (BOS) technique to a laser-induced underwater shock wave

Shota Yamamoto, Yoshiyuki Tagawa, Masaharu Kameda

摘要:

为了捕获激光水下冲击波,我们建立了一个基于背景定向纹影(BOS)技术的超高速成像系统。这种BOS技术能够提供二维密度梯度场的流体,并需要一个简单的设置。成像系统由超高速摄像机、激光频闪仪和图案化背景组成。该系统每隔0.2 $μ$ s拍摄一次图像。此外,由于受冲击扰动的水的密度变化非常小,所以该系统具有高空间分辨率$\sim$ 10 $μ$ m/像素。利用这个BOS系统,我们研究了冲击波的时间位置。实验结果表明,该高速成像系统能够成功地捕捉到以1500 m/s左右速度传播的水下冲击波的瞬时位置。局部密度梯度可以确定为高达$O$(10 $^3$ kg/m $^4$),这通过由水听器测量的压力时间历程估计的梯度来确认。

英文摘要:

We build an ultra-high-speed imaging system based on the background-oriented schlieren (BOS) technique in order to capture a laser-induced underwater shock wave. This BOS technique is able to provide two-dimensional density-gradient field of fluid and requires a simple setup. The imaging system consists of an ultra-high speed video camera, a laser stroboscope, and a patterned background. This system takes images every 0.2 $μ$s. Furthermore, since the density change of water disturbed by the shock is exceedingly small, the system has high spatial resolution $\sim$ 10 $μ$m/pixel. Using this BOS system, we examine temporal position of a shock wave. The position agrees well with that measured by conventional shadowgraph, which indicates that the high-speed imaging system can successfully capture the instantaneous position of the underwater shock wave that propagates with the speed of about 1500 m/s. The local density gradient can be determined up to $O$(10$^3$ kg/m$^4$), which is confirmed by the gradient estimated from the pressure time history measured by a hydrophone.

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