Abstract:With ground-based, impulsive acoustic sources, the initial blast wave can be followed by additional noise that is difficult to interpret. As outlined by Embelton [J. Acoust. Soc. Am. 100 (1996)], a porous ground can lead to creeping, ground, and surface waves. In a recent test on a grass-covered field, the blast noise from exploding balloons had evidence of a secondary arrival that in some cases was larger than the blast wavefront. The balloons were filled with oxy-acetylene gas and placed on the ground or in … Show more
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