3
ee:
antes
a meget one
A
opyene tape teee
e
Ofbtn
this, Lf
wa
uahke
tho choatenl
coterninations
as
to what portiens are radio strontimm, but of this total activity,
we have 25 Dell in four milos; S7 at Co and G4 at 142,
«
-
a
indicates
ae
-
that the vedlo
ate
te
.
9
cA
4
~~.
FY
.
as,
“4
a
4
This ezada
mr,
stautiwa dueronses at distances,
ante
ey
ote Sgn
-
as
miles out is as far as wo would work,
nyo™~
ft is
Dt Ay
«
-“
rc
1:20
A
2 part of our pro-
Gxeam, and wo intend to So out os far as 699 milcs,
if MNeCCscary,
following thas last sorias, to sse just how far out this reletionshiv will hold.
Cortainiy 1% dindicsntes in terzs of tho
avellability of the komb residuc that wa cannet jucce this in
terms of meter readings 21012 oF gust enviroenncntal contomins-
tion,
We aro dealint with seno fracticn cf the total fall-out
that is not distributed in this manner but is distributed rathor
uniformly over a rather lavse area.
This sumsests the smaller
particic sises which will tend to bo carried Zurthor and tond
Preliminary data scon
bi
to diffuse a little further,
=
an
ae
to
SUSTSst
that this relationship holds,
It is not cnough to go out in an aveoa aud say this
is how much activity is there.
It has to be interpreted as to
what it- moans or why it is there,
Somstinos way it is thore is
scemotimes easier than what it moans.
At UCLA, wa have more or less brezen our
work down
into the phenomenolcesy of what are the factors of different
fall-out distributions Waich are the thinss Dr, Lerson has just
Ciscussed, and then what is the biclozical significance of it.
Ve have to have the two bits of data in order to got a prover