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SEISMIC DECOUPLING FOR EXPLOSIONS IN SPHERICAL CAVITIES. For Report for Period December 1959-March 1960

Technical Report ·
OSTI ID:4080284

A series of paired explosions in a salt mine near Winnfield, La., was conducted to test a theory by A.L. Latter concerning seismic decoupling by underground cavities. The theory predicted a decoupling of 132. Free-field and surface measurements from an explosion in either a 6-ftor a 15-ft-radius spherical cavity were compared with similar measurements from a completely tamped explosion of equal size. Shot sizes were from 20 lb up to a ton. Surface measurements were made out to 100 kin and covered the frequency range from 0.05 to 100 cps. The experiment confirmed that decoupling does occur. For explosions that produce an average cavity pressure up to one-fifth and possibly more of the lithostatic overburden pressure, seismic waves were decoupled by more than l00, i.e., two orders of magnitude. Even for explosions producing an average cavity pressure of six times the lithostatic overburden pressure, the seismic waves were decoupled by 20 - more than a full order of magnitude. Minimum decoupling factors as a function of frequency are presented. (auth)

Research Organization:
California. Univ., Livermore. Lawrence Radiation Lab.
NSA Number:
NSA-15-005858
OSTI ID:
4080284
Report Number(s):
UCRL-6068
Country of Publication:
United States
Language:
English

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