PNNL

Abstract

So called “aerodynamic debris” has often been observed from explosion debris collected on the fringe of surface nuclear tests, and is assumed to result from ejection of melted and re-condensing ground materials drawn up into the rising explosion fireball. The material forms small glassy particulates measuring ~1mm, ranging in shape from near perfectly spherical glassy beads to more elongated forms and occasionally agglomerates of two or more particles displaying some degree of fusion. Producing material with a similar range of characteristics in the laboratory may be quite challenging, as the temperatures required can exceed 1500°C while keeping the particulates suspended in constant motion. In this paper we describe an apparatus that can heat lofted sediment particulates up to 1mm very rapidly above their melting points, allowing extended interactions times from seconds to minutes. Examples of the different material forms produced will be compared to real aerodynamic debris recovered from nuclear explosions described in the literature.