Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Bulletin of the Seismological Society of America Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Bulletin of the Seismological Society of America; January 1962; v. 52; no. 1; p. 67-75
© 1962 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by CARDER, D. S.
Right arrow Articles by MICKEY, W. V.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Ground effects from underground explosions

D. S. CARDER and W. V. MICKEY

U. S. DEPARTMENT OF COMMERCE COAST AND GEODETIC SURVEY, WASHINGTON 25, D. C.

Abstract

For equivalent TNT energy yields of 180 pounds to 19.2 kilotons at distances of 0.3 to 3200 kilofeet, a yield scaling law of W0.75 is indicated. Maximum earth particle displacements satisfy an exponential attenuation function of the form:


Formula 1

where A is maximum earth particle displacements in centimeters, C is a constant, W is yield in tons, D is distance from detector to source in feet, n is a wave propagation constant, k is a constant and f is the visually dominant frequency in cps of the measured pulse on the seismogram.

For distance of 0.3 to 9.8 kilofeet, C is 104.57, n is 2, and k is 1.75 x 10-6; from 9.8 to 525 kilofeet, C is 100.6, n is 1, and k is 1.83 x 10-6; from 525 to 3200 kilofeet C is 10-2.82, n is 0.5, and k is 7.6 x 10-7. The frequency exponent in the 525 to 3200 kilofeet range is negligible since the maximum displacements were observed to occur near one cps. Stations on desert alluvium recorded displacements 2 to 4 times greater than indicated by the above scaling functions.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
J. R. MURPHY and J. A. LAHOUD
Analysis of seismic peak amplitudes from underground nuclear explosions
Bulletin of the Seismological Society of America, December 1, 1969; 59(6): 2325 - 2341.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
W. K. CLOUD and D. S. CARDER
Ground effects from the Boxcar and Benham nuclear explosions
Bulletin of the Seismological Society of America, December 1, 1969; 59(6): 2371 - 2381.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
D. S. Carder and D. S. CARDER
Ground effects from the gnome and logan explosions
Bulletin of the Seismological Society of America, December 1, 1962; 52(5): 1047 - 1056.
[Abstract] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Seismological Society of America