Page 262 - Dynamic Loading and Design of Structures
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Page 233

                 A compression wave from an explosion in air expands as a three-dimensional blast wave
               propagating at maximum velocities well above that of low amplitude sound waves. It reflects
               and refracts from solid surfaces and from atmospheric discontinuities.
                 Explosions also produce high temperatures, which are more locally concentrated than the
               pressure and decay rapidly, and also produce high velocity fragments from any confining
               structure, which may impact with a surface before the blast wave arrives. The synergistic
               effects of blast and fragment impact are not well understood.
                 If an explosion occurs in contact with a solid it produces stress of the same order of
               magnitude as the elastic modulus of the solid. The air pressure produced at close range has an
               initial peak, which is orders of magnitude larger than normal atmospheric pressure, but
               decreasing with distance travelled. Behind the peak the pressure is still above atmospheric but
               decreasing with time and falls below atmospheric. The potential of this underpressure to
               produce structural damage is not certain and in part depends on synchronization with the
               rebound of the structure.
                 An impact produces a localized application of pressure on the surface of the structure,
               which can only spread into the structure from the point of application. This is in contrast to
               explosions where the blast pressures rapidly engulf the entire surface of the structure. The
               important parameters of an impact, for diagnostic or forensic purposes, are the shape, velocity
               and mass of the impactor, and whether or not the impactor deformed.
                 When pressure is applied very rapidly to the surface of a structure then strain waves are
               generated which transfer the local dynamic surface deformations into overall structural
               deformations. An analysis of the transient stress state is necessary when the applied pressure
               changes more rapidly than the time taken for the strain waves to travel between the
               boundaries of the structure and establish a state of equilibrium between overall structural
               resistance and applied pressure effects. During this transition period the transient strain and
               stress conditions may produce local failures that are decoupled and of different shape from the
               failures that can occur due to overall structural deformation.
                 The strain waves propagate at characteristic velocities for the material and transfer
               momentum into the structure by dynamic displacements of the boundary surface. The rates of
               strain and stress that are produced locally in the material are orders of magnitude greater than
               those produced in the overall structural deformation, which are again orders of magnitude
               greater than under slowly applied loading. Most construction materials have enhanced
               properties at these high rates of strain.


                                            6.2 BLAST PHENOMENA



                                                6.2.1 Explosive sources
               A detonation wave travels through high explosives at 5,000–10,000 m/s. At a free air
               boundary the gaseous products expand at high velocity, pressure and temperature
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