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

机译:背景技术(BOs)技术在工程中的应用   激光诱导水下冲击波

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摘要

We build an ultra-high-speed imaging system based on the background-orientedschlieren (BOS) technique in order to capture a laser-induced underwater shockwave. This BOS technique is able to provide two-dimensional density-gradientfield of fluid and requires a simple setup. The imaging system consists of anultra-high speed video camera, a laser stroboscope, and a patterned background.This system takes images every 0.2 $\mu$s. Furthermore, since the densitychange of water disturbed by the shock is exceedingly small, the system hashigh spatial resolution $\sim$ 10 $\mu$m/pixel. Using this BOS system, weexamine temporal position of a shock wave. The position agrees well with thatmeasured by conventional shadowgraph, which indicates that the high-speedimaging system can successfully capture the instantaneous position of theunderwater shock wave that propagates with the speed of about 1500 m/s. Thelocal density gradient can be determined up to $O$(10$^3$ kg/m$^4$), which isconfirmed by the gradient estimated from the pressure time history measured bya hydrophone.
机译:我们建立了一个基于背景定向刻痕(BOS)技术的超高速成像系统,以捕获激光引起的水下冲击波。这种BOS技术能够提供二维的流体密度梯度场,并且需要简单的设置。成像系统由超高速摄像机,激光频闪仪和带图案的背景组成,该系统每0.2 s \ mu $ s拍摄一次图像。此外,由于受到冲击干扰的水的密度变化非常小,所以该系统具有高的空间分辨率$ \ sim $ 10 $ \ mu $ m /像素。使用此BOS系统,我们可以检查冲击波的时间位置。该位置与常规阴影图测量的位置非常吻合,这表明高速成像系统可以成功捕获以大约1500 m / s的速度传播的水下冲击波的瞬时位置。可以确定高达$ O $(10 $ ^ 3 $ kg / m $ ^ 4 $)的局部密度梯度,这可以通过水听器测得的压力时间历史估算出的梯度来确定。

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