RADIOACTIVITY VS. HEIGHT IN NUCLEAR CLOUDS
0.9
633
T
0.6
|
0.7
_
0.6
—
0.5
+
0.4
4
0.3
=
0.2
4
Fig. 2—Ratio of air density (p)
to standard sea-levelair density
(pp = 1.293 x 107 g/cm) as a
function of altitude.
0.1
0
|
0
120 |
I
|
|
20
40
ALTITUDE, 10° FT
|
60
DT TTT TT
Tg,
a
4
100sew BASE OF MUSHROOM onmumeneree
_
<=
Oo
=
TT
—
&
e
4
—
e
|
a
“a
4a
80 -—
=
a
[
flee
O 60-—Lit
~
an
—
a&
°
7
a
-
&
—
Ww 40e-
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DOMINIC DATA
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jo
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—
L
“AIR BURST
SSURFACE BURST
—
107!
10!
7 on
gt
——_
10%
REDWING DATA _]
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1075
104
1033
107?
10°
PERCENT OF TOTAL ACTIVITY PER 1000-FT- THICK LAYER
Fig. 3—Variation with height of the percent of the total activity residing in a 1000-ft-thick horizontal layer of the cloud.