Kingdom (3). The soil levels of Zr°-

Nb*, which are less affected by the
1957 and earlier fallout than are levels
of the longer-lived nuclides, show a

maximum variation of 20 percent from

the New York City cumulative fallout
levels. In addition, the results of sys-

tematic ionization-chamber measurements of open-field dose rates performed by Vennart (3) in Belmont,

Surrey, England, closely parallel the
Zr“*-Nb™ dose rate curve of Fig. 3.

These observations imply (i) that
weathering and roughness of terrain
had little effect on doses from fallout

activities during the two-year period,

and (ii) that the most significant contribution to total-radiation dose rates
was made by radioactive zirconium,
or possibly by other fission products
of comparably short half-life.
Although the beta emitters in faliout are not sufficiently energetic to
cause significant external doses except
through direct deposition on body surfaces, internal doses do occur through
inhalation and ingestion of debris particles (5). In addition, the chemical
similarity of some of the radionuclides
to elements normally assimilated by the

body results in concentrated doses to
specific tissues. The over-all effect of

radiation on the population cannot be

known, therefore, until many complex
meteorological, physica), chemical, and
biological factors are thoroughly understood. It is clear, however, that any
valid assessment of the effect of radiation, past or future, must include consideration of fallout and more realistic
treatment of the short-lived fission products.
Refereaces and Notes
1, “Radiological

Health

Data

Reports,”

U.S.

Public Health Service Publs. Nos. PB I61371-1

throueh PB 161371-10 (1960-61).
2, “Strondum Program Quarterly Summary Reports,” U.S. Atomie Energy Comm. Publs.

Nos. HASL-42, HASL-51, HASL4S, HASL-

77, HASL-84, HASL-9$ (1958-61).
3. D. H. Peirson and L. Salmon, Nature 164,

1678

(1959);

J.

Vennart,

(bid.

188

722

W.F Libby, Proc. Vail. Acad. Sct. US. 48,
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G. A. Welford and W. R. Collins, Jr. Sct
ence 131, 1710 61960),

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ne Comm. Publ. No. HASL-42 (1958),
4
& A. Welford, W. R, Collins, Se, R. S.

Morse, D. C. Sutton, Talanra 5, 168 (1960);
WwW. R. Collins, Jr, U.S. Atomic Energy

Comm. Rept. No. HASL44 (1989); “Manual
of Standard Procedures,” U.S, Atomic En-

ergy Comm, Publ. No. NYO-4700 (1957).
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Rept. No. [DO-16408 (1957).
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and Radiochemistry (Wiley, New York, 195$).
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J, H. Harley, N. A. Halden, L. D. ¥. Ong,
U.S. Atomie Energy Comm. Rept. No. HASL93 (1960).
» D. Strominger, J. M. Hollanser, G. T. Seaborg, Ress. Modern Phys. 3@, 2 (1958).
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. The thermonuclear data are taken from an

unfinished report by John H. Harley and Naomi

(1960).
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. Report of the United Nations Scientific Comimuttee on the Effects of Atomic Radiation

ratory). We gratefully acknowledge their coOperation and assistance in this and other
phases of the study. We also acknowledge

Hazards to Man of Nuclear and Allied Radiations: A Second Report to the Medical
Research Council (Her Majesty's Stationery

Oratory), who did much of the sample
Preparation and analysis, and of Wayne M.

we

from similar latitudes in both the
United States (/, 4) and the United

(United

Nations,

New

Office, Londoa, 1960).

6. E.

A.

Martell,

Science

York,

129,

i958);

1197

The

11959);

and P. J. Drevinsky, ibid. 132. 1523

(1960).
7. L. B. Lockhart, Je, R. A. Baus, R. L. Patterson, Jr., A. W. Saunders, Jr., idtd. 130,

161 ¢1959); L. B. Lockhart, Jr, R. L. Patter-

son, Jr, A. W. Saunders, Jr., R. W. Black,
thid, 133, 184 (1960).

57

A.

Hailden

(Health

and

Safety

Labo-

the assistance of Gustave Farnham and Salvatore Garafalo (Health and Safety LabLowder,

who

reviewed

the

discussion

of

kamma-ray doses and dose rates.
. Climatological Data, Washington 9, Nos. 1-12
(1958); 10, Nos. t~12 (1959).
2. L. R. Solon, W. M. Lowder, A. V. Zila, H.
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