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The Disintegration of {sup 103}Rh{sup m}

Abstract

A technique for determination of the disintegration rate of {sup 103}Rh{sup m} in thick foils is described. In addition values for the following parameters were determined: - total internal conversion coefficient {alpha} = 1531 {+-} 30; - K shell internal conversion coefficient {alpha}{sub K} = 127 {+-} 6; - conversion ratio R= K/L+M+..... = 0.0914 {+-} 0.0043. (author)
Authors:
Czock, K. H.; Haselberger, N.; Reichel, F. [1] 
  1. International Atomic Energy Agency, Vienna (Austria)
Publication Date:
Sep 15, 1974
Product Type:
Technical Report
Report Number:
INDC(IAE)-004/G; IAEA-RL-26
Resource Relation:
Other Information: 2 figs., 2 tabs., 29 refs.
Subject:
73 NUCLEAR PHYSICS AND RADIATION PHYSICS; CONVERSION RATIO; FOILS; INTERNAL CONVERSION; K SHELL; RHODIUM 103
OSTI ID:
22163484
Research Organizations:
International Atomic Energy Agency, International Nuclear Data Committee, Vienna (Austria)
Country of Origin:
IAEA
Language:
English
Other Identifying Numbers:
TRN: XA13R1198117918
Availability:
Available from INIS in electronic form. Also available on-line: https://www-nds.iaea.org/publications/indc/indc-iae-004G.pdf
Submitting Site:
INIS
Size:
13 page(s)
Announcement Date:
Nov 29, 2013

Citation Formats

Czock, K. H., Haselberger, N., and Reichel, F. The Disintegration of {sup 103}Rh{sup m}. IAEA: N. p., 1974. Web.
Czock, K. H., Haselberger, N., & Reichel, F. The Disintegration of {sup 103}Rh{sup m}. IAEA.
Czock, K. H., Haselberger, N., and Reichel, F. 1974. "The Disintegration of {sup 103}Rh{sup m}." IAEA.
@misc{etde_22163484,
title = {The Disintegration of {sup 103}Rh{sup m}}
author = {Czock, K. H., Haselberger, N., and Reichel, F.}
abstractNote = {A technique for determination of the disintegration rate of {sup 103}Rh{sup m} in thick foils is described. In addition values for the following parameters were determined: - total internal conversion coefficient {alpha} = 1531 {+-} 30; - K shell internal conversion coefficient {alpha}{sub K} = 127 {+-} 6; - conversion ratio R= K/L+M+..... = 0.0914 {+-} 0.0043. (author)}
place = {IAEA}
year = {1974}
month = {Sep}
}