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Low frequency acoustic pulse propagation in temperate forests

机译:低频声脉冲在温带森林中的传播

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摘要

Measurements of acoustic pulse propagation for a 30-m path were conducted in an open field and in seven different forest stands in the northeastern United States consisting of deciduous, evergreen, or mixed tree species. The waveforms recorded in forest generally show the pulse elongation characteristic of propagation over a highly porous ground surface, with high frequency scattered arrivals superimposed on the basic waveform shape. Waveform analysis conducted to determine ground properties resulted in acoustically determined layer thicknesses of 4-8 cm in summer, within 2 cm of the directly measured thickness of the litter layers. In winter the acoustic thicknesses correlated with the site-specific snow cover depths. Effective flow resistivity values of 50-88 kN s m(-4) were derived for the forest sites in summer, while lower values typical for snow were found in winter. Reverberation times (T60) were typically around 2 s, but two stands (deciduous and pruned spruce planted on a square grid) had lower values of about 1.2 s. One site with a very rough ground surface had very low summer flow resistivity value and also had the longest reverberation time of about 3 s. These measurements can provide parameters useful for theoretical predictions of acoustic propagation within forests.
机译:在美国东北部的阔叶林,常绿树种或混交树种的七个不同林分中,在空旷的地方进行了30米路径声脉冲传播的测量。森林中记录的波形通常显示在高度多孔的地面上传播的脉冲伸长特性,高频散射波到达叠加在基本波形上。为了确定地面特性而进行的波形分析导致,在夏季,声学确定的层厚为4-8厘米,在直接测量的垫料层厚度的2厘米以内。冬季,声学厚度与特定地点的积雪深度相关。夏季森林站点的有效流阻值为50-88 kN s m(-4),而冬季则典型的是较低的雪。混响时间(T60)通常约为2 s,但两个支架(落叶和修剪的云杉种植在方格上)的较低值约为1.2 s。一个地面非常粗糙的位置的夏季流动电阻率值非常低,混响时间最长,约为3 s。这些测量可以提供对森林内声传播的理论预测有用的参数。

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