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Untitled - Sciencemadness Dot Org

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SHOCK INITIATION PROPERTIES<br />

each shot, the shock wave trajectory measured back from the transition to high-<br />

order detonation and superimposing the plots using the transition as a fiducial.<br />

Detonation velocities are obtained from x-t data measured in the high-order region.<br />

Technique 5. In Technique 5, the driving plate free-surface velocity always is<br />

measured with electrical pin contactors. Buildup data from all experiments on a<br />

given density of explosive are pooled on the assumption of a single curve buildup<br />

and are fitted by the least squares method to the empirical function,<br />

D = A1T(l-*3) [1 - exp (-A2TA3)] + (A/, - A1A2)T ,<br />

where D is the distance to detonation, T is the time to detonation at any point on<br />

the buildup curve, A, is the detonation velocity, and A,, A,, and A, are arbitrary<br />

constants. The shock velocities are evaluated from the derivative of the above func-<br />

tion,<br />

u so = A1(l - A3)T-*3 b - exp (-AZTA3)] + A1A2A3 exp (-A2TA3) + Ai - A1A2 ,<br />

using the coefficients fitted to the pooled data and the time to detonation, T = t*,<br />

observed in the individual experiments. This shock velocity value is then used with<br />

the driving plate free-surface velocity determined as before.<br />

Technique 6. In Technique 6, a flash gap consisting of grooved Lucite blocks is<br />

used to measure the driving plate free-surface velocity. Also, shock velocities are<br />

determined by reading the average slopes from the streak records. Samples thus<br />

analyzed had two phase-velocity regions, the normal high-order detonation and an<br />

intermediate velocity region. The two abrupt changes in phase velocity are read<br />

from the streak records to give the distance to the intermediate region and the dis-<br />

tance to detonation. All other analysis is done using Technique 5.<br />

Technique 7. In Technique 7, the x-t data are digitized into 70 discrete points. A<br />

linear fit is made to three adjacent x-t points, and the slope is taken as the velocity<br />

at the midpoint of the line. Then one x-t end point is dropped, a new one is added on<br />

the other end, a new linear fit is made, and the velocity is found. This running linear<br />

least squares process is repeated until all 70 x-t points have been used. The u-x data<br />

are then extrapolated to zero thickness (x = 0) to find the initial shock velocity, U,,.<br />

All other analysis is done as in Technique 1.<br />

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