Douady S, Manning A, Hersen P, Elbelrhiti H, Protière S, Daerr A, Kabbachi B
Matière et Systèmes Complexes, CNRS & Université Paris 7, CC7057, Jussieu, 75005 Paris, France.
Phys Rev Lett. 2006 Jul 7;97(1):018002. doi: 10.1103/PhysRevLett.97.018002.
Since Marco Polo it has been known that some sand dunes have the peculiar ability to emit a loud sound with a well-defined frequency, sometimes for several minutes. The origin of this sustained sound has remained mysterious, partly because of its rarity in nature. It has been recognized that the sound is not due to the air flow around the dunes but to the motion of an avalanche, and not to an acoustic excitation of the grains but to their relative motion. By comparing singing dunes around the world and two controlled experiments, in the laboratory and the field, we prove that the frequency of the sound is the frequency of the relative motion of the sand grains. Sound is produced because moving grains synchronize their motions. The laboratory experiment shows that the dune is not needed for sound emission. A velocity threshold for sound emission is found in both experiments, and an interpretation is proposed.
