204

SHORT COMMUN.CALION
Tatl: |, Comparative uptake of different radwenuclides by vean plants. Duration of treatment in labelled
nutraad solution 2 15 ays
Uptake
Radionuclide

mri
NOR
atop);
alep,
Sr
Lis.d. (p= 0-05)

Concentration factor Transport
Roo
index

% uf added
Shoots

Roots

Shoots

0-09
9-61
0-29
0-06
8-77
2:06

76:35
36-98
90-64
68-01
2-80
20-05

0-91
84-60
2-69
0-58
83-14
5-83

4185
1787
4246
3324
142
1217

0-12
20-62
0-32
0-09
75-82
—_

Radionuclide content/g plant tissue

*Concentration factors --— -- —-—— - -~-

Radionuclide content/ml nutrient solution.

t Transport index = Shoot
conter content| A

Total plant content

times greater. Further, the amount of radium
translocated to shoots is comparable to that of
strontium.

likely to be influenced by various factors which

transfer of ***Ra to shoots suggests that among

Acknowoledgement—The autbors are grateful to Dr.

The present evidence of relatively rapid

the nuclides examined here ™*Ra is likely to

make the major contribution to radioactivity
in aerial tissues of plants grown under condi-

tions where root absorption is the principal
route ofentry ofthe nuclides. In situations where
plant organs are subject to considerable atmospheric washout of “Rn daughter products,
however, higher concentrations of ™*Ph and
°Po than "*Ra may be obtained.
It has been reported by Marneorp ef al.,(%
Ersensup ¢f af. and Mistry ot al.that the

contribution of radium isotopes to the alpha

activity found in the stem, leaves and fruits of

plants growing in the uranium and thorium

tich

high

background radiation areas far

exceeds that of thorium isotopes. The present

findings from nutrient culture experiments are
compatible with the above reports.

When plants are grown in soil containing

uranium series nuclides theie accumulation in

roots is considerably lower than that in roots of
plants grown in labelled nutrient solution as a
result of the great affinity of these nuclides for

exchangesites on the soil.@.**19 Furthermore,

comparative uptake of the nuctides from soil is

control their availability in the soil. In future we
plan to examine the uptake of these radionuclides by plans from contrasting soil types.
A. R. Gopat-Avznaar for his encouragement and
interest.

“

Biology Division
Bhabha Atomic Research Contre

T. J. D’Souza
K. B. Misray

Trombay, Bombay, India

REFERENCES
1. D'Souza T. J. and Mrsray K. B. (1966) Prelininary studies on the absorption and translocation of *#*Po and ***Pb by plants. Pree. All India
Symp. Radioactis. Maetrel. Ratieand. Bombay,
381-40.

2. Emansup M., Pernzow H., Dusw R. T., Rosen

F. X., Keozt G. and Curren T. L. (1963)
Naturally occurring radionuclides in foods and
waters from the Brazilian aress of high radio-

activity, pp. 854-854. fe J. A. S. Apass and

W. M. Lowner (Eds.), The netwal radiation
ervironment. University ofChicago Prem, Chicago.
3. Giuree K. B. and Murray K. B. (1970) The effect
of chelating agents on the absorption of radigen
by plants, Plant ead Sel 32 (in prea).

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