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Seismic source function for an underground nuclear explosion

Journal Article · · Bull. Seismol. Soc. Amer., v. 64, no. 1, pp. 131-148
The reduced displacement potential obtained from close-in observation of seismic displacement during an underground explosion usually takes the forM of a step function with or without a small overshoot. Theoretical prediction by shockwave calculation appears to agree with the close-in data. The step-function source has also been supported by the observations on Rayleigh waves at periods longer than 10 sec. Some inconsistency between the published data on residual potentials obtained from close-in data and those on seismic moments obtained from long-period Rayleigh waves were found. It appears that only about 1/3 of the residual potential is transmitted to the far-field at long periods. This discrepancy is, however, consistent with several observations made on teleseismic signals suggesting an impulse rather than a step as the primary form of the potential function. New observations of the two NTS events at distances 2.6 to 7.8 km using wide dynamic range, wide-band accelerometers, combined with data from the far-field, support a large overshoot 4 to 5 times the residual value. This result accounts for the efficiency of the M/sub s/-m/sub b/ discriminant between earthquakes and explosions with m/sub b/ around 4 and greater. The compaction of the source volume by spalling was suggested as a possible mechanism for the large overshoot. (auth)
Research Organization:
Massachusetts Inst. of Tech., Cambridge
Sponsoring Organization:
USDOE
NSA Number:
NSA-29-024160
OSTI ID:
4333101
Journal Information:
Bull. Seismol. Soc. Amer., v. 64, no. 1, pp. 131-148, Journal Name: Bull. Seismol. Soc. Amer., v. 64, no. 1, pp. 131-148; ISSN BSSAA
Country of Publication:
Country unknown/Code not available
Language:
English