Albert Donald G, Swearingen Michelle E, Perron Frank E, Carbee David L
U.S. Army Engineer Research and Development Center, Cold Regions Research and Engineering Laboratory, 72 Lyme Road, Hanover, New Hampshire 03755, USA.
U.S. Army Engineer Research and Development Center, Construction Engineering Research Laboratory, 2902 Newmark Drive, Champaign, Illinois 61822, USA.
J Acoust Soc Am. 2015 Aug;138(2):735-47. doi: 10.1121/1.4923365.
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.
在美国东北部,针对一条30米路径的声脉冲传播进行了测量,测量地点包括开阔地以及七种不同的林分,这些林分由落叶树种、常绿树种或混合树种组成。在森林中记录的波形通常显示出在高度多孔的地面上传播时脉冲伸长的特征,高频散射波到达叠加在基本波形形状上。为确定地面特性而进行的波形分析得出,夏季通过声学确定的层厚度为4 - 8厘米,与直接测量的枯枝落叶层厚度相差在2厘米以内。在冬季,声学厚度与特定地点的积雪深度相关。夏季森林地点的有效流阻率值为50 - 88 kN s m(-4),而在冬季发现了典型的较低雪流阻率值。混响时间(T60)通常约为2秒,但有两个林分(种植在方形网格上的落叶林和修剪过的云杉林)的混响时间较低,约为1.2秒。一个地面非常粗糙的地点夏季流阻率值非常低,混响时间也最长,约为3秒。这些测量结果可为森林内声传播的理论预测提供有用参数。