Acceleration and sound measurements during granular discharge from silos are used to show that silo music is a sound resonance produced by silo quake. The latter is produced by stick-slip friction between the wall and the granular material in tall narrow silos. For the discharge rates studied, the occurrence and frequency of flow pulsations are determined primarily by the surface properties of the granular material and the silo wall. The measurements show that the pulsating motion of the granular material drives the oscillatory motion of the silo and the occurrence of silo quake does not require a resonant interaction between the silo and the granular material.
IntroductionThe discharge of granular materials from silos is often characterized by vibrations or pulsations of the silo, termed 'silo quake', and a loud noise, termed 'silo music' [1][2][3][4][5][6][7][8]. Both of these are undesirable as silo quake may cause structural failure and silo music is a source of noise pollution. Unfortunately, the numerous conflicting studies published in the literature [1][2][3][4][5][6][7][8] do not give the silo designer a simple model to understand the physical processes that cause the pulsations, and to guide silo design or modification that would prevent the pulsations or at least minimize their effect. The purpose of this study is to investigate the cause of the noise and the pulsations, and the interaction between the motion of the granular material and the motion of the structure.Several studies of the discharge of granular material from silos have noted fluctuations in discharge rate and the production of noise and vibration [1][2][3][4][5][6][7][8]. The top of the granular material has been observed to move in discrete steps even though the discharge from the bottom of the silo was continuous [4,6]. For smooth-walled, tall, narrow silos, pulsations occurred during both mass and mixed flow. The pulsations were observed to stop at a critical height of granular material in the silo [1,3]. Methods suggested for preventing pulsations include roughening the walls in the transition zone between the bunker and the orifice [1][2][3] and placement of inserts along the silo walls [4].In an early study, Phillips [6] observed the motion of sand in a tube, which had a glass face, and was closed at the lower end by a flat bottom having a central orifice. When the orifice was opened, the sand in the upper part of the tube moved downward intermittently in jerks. Phillips noted, "when the flow begins, a curious rattling sound is heard which changes to a distinct musical note". He also did experiments in which the tube was first partly filled with mercury and then filled with sand. Once again, the free surface of the sand descended intermittently when the mercury was allowed to flow through the orifice. He observed that the length of the column of sand increased by about 2% during the 'stick' phase. Further, the motion of the granular material caused the wall of the tube to vibrate. Thus both silo music and silo quake occur...