39
. Beagles.
Physies

igh June
n of Bas:

diological
ugh June

Atherton,
d Radon
(7 (1958),
‘trometry,
HO.

H. Com-

and Bats
al Labo-

Report,

‘etention
> (1958).
abolism:

iple but

Theoret.

ie Variahe Dog,

unlikely. However, metabolites do travel along the ray
tracheids, tritiated water enters heartwood, and in
coitwoods fission products are found in wood formed
prior to the existence of bomb fallout.‘®
This paper reports on the use of *1°Pb tracer to estimate the rates of radial translocation of lead in trees.
Also measured was 7!°Po, which gives an indication of
the transport of this nuclide. These nuclides occur in
nature and are derived from the °8U chain which de-

exvs to “°6Ra and then through a chain of short-lived
daughters to 2°Pb, which has a 21.4-year half-life.
This nuclide then decays to 5-day 7!°Bi and finally to
TABLE 14.

which,

nd acmeasent of

ted by

y and
2s and
ncient
ced at
lina
s type

1s
28

Bar
1-2

0
1.5

48
as
GS
7

5-6
7-8
9-11
12-14

xs
Ys

15-16
17-18

lls
12S

38

indiod is

0.83 + 0.10
2.09 + 0.29

5.5
7.5
10.0
13.0

0.261
0.221
0.184
0,207

0.202
0.176
0.239
0.2388

0.77
0.80
1.29
1.15

19-20

15.5
17.5

19.5

0.192 + 0.017
0.221 + 0.017

0.268 + 0.020

0.170 + 0.026

063 + 0.11

2)-23
24-25

22.0
24.5

0.2690 + 0.018
0.266 + 0.022

0.238 + 0.025
0.254 + 0.040

0.88 + 0.11
0.95 + 0.17

3.5

0.214 + 0.019

26.5
28.5
33.0
36.0

38-39

0.271
0.250
0.208
0.240

38.5

+
+
+
+

+
+
+
+

0.024
0.017
0.017
0.017

0.021
0.020
0.017
0.019

0.148 + 0.018

0.192 + 0.026

+
+
+
+

0.042
0.023
0.025
0.032

0.280 + 0.027
0.269 + 0.026

0.196
0.227
0.221
0.081

+
+
+
+

+
+
+
+

1.46 + 0.19
122 + 0.15

0.027
0.043
0.03
0.03

0.72
0.91
1.06
0.34

0.266 + 0.048

+
+
+
+

0.12
0.19
0.20
0.16

1.86 + 0.38

0.178 + 0.019
0.202 + 0.019

0.157 + 0.042
0.164 + 0.043

0.88 + 0.26
0.81 + 0.22

20S
JES
2S

44-45
46-47
48-49

44.5
46.5
48.5

0.142 + 0.017
0.179 + 0.019
0.058 + 0.011

0.167 + 0.018

0.216 + 0.042
0.110 + 0.042
0.076 + 0.026

0.146 + 0.041

1.562 + 0.34
0.62 + 0,24
1.31 + 0.51

0.87 + 0,26

JEN
25S

§2-53
54-55

52.5
54.5

0.138 + 0.018
0.124 + 0.017

0.103 + 0.014

0.194 + 0.044
0.146 + 0.041

0.126 + 0.035

1.41 + 0.37
1.18 + 0.37

58-59
60-61

38.5
60.5
02.5
65.0

0.119
0.0902
0.080
0.085

0.146
0.104
0.125
0.086

1.22 + 0.38

71.5
75.0
78.5

0.077 + 0.031

0.88 + 0.38

0.069 + 0.010
0.055 + 0.009
0.051 + 0.008

0.064 + 0.026
0.071 + 0.028
0.089 + 0.021

0.92 + 0.39
1.29 + 0.47
0.76 + 0.42

0.045 + 0.007
0.061 + 0.007

0.042 + 0.012
0.048 + 0.012

0.93 + 0.30
0.79 + 0.22

0.046 + 0.021
0.082 + 0.017

0.92 + 0.44
| 1.08 + 0.23

50-51

PAS
278
28S
30
SS

318

KNE

ENE
ENE

338

3008
oF

38 Center

50.5

56-57
|

56.5

62-03
62-07

64-05
70-73

- 73-17
77-80

78

79
80

84-86

88-92
90-95

100

;

64.5

85.0

90.0
92.5

100.0

0.016
0.013
0.012
0.010

0.087 + 0.018

|

78.0

79.0
80.0

+
+
+
+

'
~

~
|

;

0.053 + 0.007
0.085 + 0.007

0.050 + 0.008
0.086 + 0.010

0.057 £ 0.008

+
+
+
+

1.22 + 0.38

0.041
0.083
0.031
0.017

1.14 + 0.40
1.56 + 0.44
1.01 + 0.23

0.0386 + 0.012

0.69 + 0.24

0.086 + 0.021

0.073 + 0.0L}

Mean

0.265 + 0.016

0.082 + 0.009

0.17
0.12
0.18
0.18

40.5
42.5

23S

RapCa

0.90 + 0.15

40-41
42-43

3308
S48

iving

Ratiosponmen

Iss
19 8

ments

yf the
on of

»°Pb, 7°Po ann #6Ra 2ONCENTRATIONS IN Hiexory

0.192 + 0.021
0.329 + 0.029

26-27
28-29
32-34
35-37

17s

328

roots

excretion, and that the input rates are constant, the

“40Ph, concentration would decrease with its 21.4-year
radioactive half-life as one goes from the younger to
the older wood (outer rings toward the center).

0.233 + 0.014
0.157 + 0.017

3-4

138
4s
los
lis

iounts

r the
rable

222Rn, may be easily translocated, the “!°Pb moves

through the biosphere independently of its predecessors. Although the origins of the stable and radioactive
lead in the tree may differ, one would expect that after
entry their metabolic behaviors would be similar, if
not identical. Thus, if we assume no circulation, no

Sinplenunber] Ageing, ateanase, umn nciig ary mpo,pctiedty

IOS

n par; could:

138-day 7°Po. Because of their different chemistries

and because the radioactive rare gas intermediate,

2.15 + 0.63

| 1.28 £ 0.32

!

—

1.11 + 0.34 (S.D.)

:

.

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