BJR
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS

British Journal of Radiology (1956) 29, 317-325
© 1956 British Institute of Radiology
doi: 10.1259/0007-1285-29-342-317

This Article
Right arrow Full Text (PDF)
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in PubMed
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 Chamberlain, A. C.
Right arrow Articles by Dyson, E. D.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Chamberlain, A. C.
Right arrow Articles by Dyson, E. D.

The Dose to the Trachea and Bronchi from the Decay Products of Radon and Thoron

A. C. Chamberlain, M.A. and E. D. Dyson, M.A., M.B., B.Ch., Graduate I.E.E.

Atomic Energy Research Establishment, Harwell, Didcot, Berks

This excerpt was created in the absence of an abstract.

When air containing radon or thoron is breathed some of the decay products* are deposited on the surface of the respiratory system, and the radiation from this active deposit then gives a dose to the epithelium. The {alpha} radiation is probably of greatest importance because of its relative biological efficiency and also because the {alpha} dose is so greatly localised. For this reason an estimate of the dose requires a knowledge of the distribution of the active deposit in different parts of the respiratory system, with particular reference to the bronchi where the majority of lung cancers are first seen.

Mitchell (1945) considered the dose to the bronchial epithelium on the assumptions that the concentration of radon in the bronchus is the same as in the outside air, and that all the active deposit formed in the bronchus is deposited on the walls and remains there until it decays. On these assumptions Mitchell's calculations gave the dose to the bronchial epithelium from a radon concentration of 10–9 c/1. in air as 0·8 mrep/h.

More recently it has become clear that the active deposit formed in the outside air and breathed in along with the radon or thoron contributes more to the total dose than does the active deposit formed within the lung.

Cohn, Skow and Gong (1953) exposed rats to the air in an air-tight but not dust-free room in which radon in equilibrium with radium had been allowed to stand for a period of 30 days.

Accepted for publication August 1, 1955.




This article has been cited by other articles:


Home page
ScienceHome page
G. Frey, G. FREY, P. K. HOPKE, and J. J. STUKEL
Effects of Trace Gases and Water Vapor on the Diffusion Coefficient of Polonium-218
Science, January 30, 1981; 211(4481): 480 - 481.
[Abstract] [PDF]


Home page
ScienceHome page
E. P. Radford Jr. and V. R. Hunt
Polonium-210: A Volatile Radioelement in Cigarettes
Science, January 17, 1964; 143(3603): 247 - 249.
[Abstract] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
BJR DMFR IMAGING  ALL BIR JOURNALS 
Copyright © 1956 by the British Institute of Radiology.