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Artificially radioactive products in the atmosphere

Abstract

The by-product activity arising from atom bomb test was investigated in Heidelberg by a filtration method during March 1953. The measurement of the activity on the filter was accomplished by a cylindrical ..beta..-counter. The decay was proportional to t/sup -/(1 + x), where x is of the order of magnitude of 0.1, and thus approaches t/sup -1/. The time of explosion can be determined by extrapolation of the reciprocal activity as a function of time.
Authors:
Publication Date:
Jan 01, 1956
Product Type:
Journal Article
Reference Number:
EDB-81-011957
Resource Relation:
Journal Name: Z. Angew. Phys.; (Germany, Federal Republic of); Journal Volume: 8
Subject:
54 ENVIRONMENTAL SCIENCES; 45 MILITARY TECHNOLOGY, WEAPONRY, AND NATIONAL DEFENSE; FALLOUT; BETA DETECTION; NUCLEAR EXPLOSIONS; AIR; DECAY; FEDERAL REPUBLIC OF GERMANY; FILTRATION; SAMPLING; CHARGED PARTICLE DETECTION; DETECTION; EUROPE; EXPLOSIONS; FLUIDS; GASES; RADIATION DETECTION; SEPARATION PROCESSES; WESTERN EUROPE; 500300* - Environment, Atmospheric- Radioactive Materials Monitoring & Transport- (-1989); 450200 - Military Technology, Weaponry, & National Defense- Nuclear Explosions & Explosives
OSTI ID:
6797071
Country of Origin:
Germany
Language:
English
Other Identifying Numbers:
Journal ID: CODEN: ZAPHA
Submitting Site:
TIC
Size:
Pages: 361-364
Announcement Date:
Jan 01, 1981

Citation Formats

Schumann, G. Artificially radioactive products in the atmosphere. Germany: N. p., 1956. Web.
Schumann, G. Artificially radioactive products in the atmosphere. Germany.
Schumann, G. 1956. "Artificially radioactive products in the atmosphere." Germany.
@misc{etde_6797071,
title = {Artificially radioactive products in the atmosphere}
author = {Schumann, G}
abstractNote = {The by-product activity arising from atom bomb test was investigated in Heidelberg by a filtration method during March 1953. The measurement of the activity on the filter was accomplished by a cylindrical ..beta..-counter. The decay was proportional to t/sup -/(1 + x), where x is of the order of magnitude of 0.1, and thus approaches t/sup -1/. The time of explosion can be determined by extrapolation of the reciprocal activity as a function of time.}
journal = []
volume = {8}
journal type = {AC}
place = {Germany}
year = {1956}
month = {Jan}
}