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Acoustic background noise from sailplane-mounted microphones

机译:来自帆纸式麦克风的声学背景噪声

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One of many options for monitoring acoustic events at altitude is a sailplane-mounted sensor. In an attempt to determine the limiting background noise for acoustic measurements from a sailplane, in-flight measurements were made with microphones installed in a Schempp-Hirth Standard Cirrus and a Blanik L23. Recordings were made in steady gliding flight in a stable atmosphere at speeds ranging from 45 to 80 knots. The background noise from a sailplanemounted microphone shows three distinct regions. The first region, above 100 Hz, is sensorinfluenced flow noise and the pressure spectral density is well characterized by a nondimensional relation. The second region, from several hertz to 100 Hz, is probably the result of sampling pre-existing pressure fluctuations in the atmosphere. For these measurements made in a convectively stable atmosphere, the pressure spectral density was between 0.005 and 0.01 Pa per root hertz (48 to 54 dB with respect to 20 μPa per root hertz). The third region, below 1 Hz, is dominated by pressure fluctuations that correlate strongly with altitude variations - either natural oscillations of the glider or pilot control inputs.
机译:监控高度声学事件的许多选项之一是横向安装的传感器。在尝试确定来自横幅的声学测量的限制背景噪声,使用安装在Schempp-Hard标准Cirrus和Blanik L23中的麦克风进行飞行测量。在稳定的气氛中,在稳定的气氛中,在稳定的气氛下,速度的速度在45到80节中。 SailplaneMounted麦克风的背景噪声显示了三个不同的区域。第一区域,高于100Hz,是传感器源性流动噪声,并且压力谱密度很好地表征了不矛盾的关系。从几个赫兹到100Hz的第二个区域可能是在大气中采样预先存在的压力波动的结果。对于在具有对流稳定的气氛中进行的这些测量,压力谱密度为0.005至0.01PA赫兹(48至54dB,相对于每根赫兹20μPA)。第三区,低于1Hz,由高度变化强烈地相关的压力波动来支配 - 滑翔机或导频控制输入的自然振荡。

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