2.
~
es
system was
os
«
San
.
:
48
ny
ake
te
.
ene
to run hydecueariie seaticns covery
3,
wat
~
1c miles
«
a
ot
"7
Saye
a9
we
wend
¢.
Stay
.
ode
2.
oe
anorontinacoly
VWiosa
we
Grpooprd
12
Eanson
bottles
to a maninia
3
ote pn
depth of“ COO meters,
c
~
.
_
feur
bottles.
fen
*
*
%
a
te"
Im 2.
bowvoon,
wo
used a shatlbow
tostfa wath
”
so
-“~
Syery
hour
on At
the ahalka]
& suedace samvle of wator.,
= ..
.
hour, in
betwaon,
wo took
Those camples
(?)
snip by @ rather sinpie caleium coaay,
-
J’.
-
ae
4
o
rates
wore measured aboavd
Tals wes not advances
aN
ty
ol
radio teshnignue, Ent wo could verform this as wa wont along.
om,
wre
mets
a eye
ap Tey
4
4
4a
watt
Cuyv routs
waco
prodicatcd
semawnat
by cur
gindings 3in connscticon
wy dee
.
*
with the cort
stroans,
and
so on,
Lh
°
ma gen
ae
aay
Anpycnimately,
wa
continrved
on Comm HUwajglein for about Tour doseocs and came
ast tno Magrdancs dowa to Uindanou, 3
up by truck
tha fairly
senthorn ond of
¢
Hindanou, and over te lisy Guinea uy along tho Philinnpine Coast
into Olsinawa, and frou Cisinawa davo the China Sea out just belov
Kyusu and back into Japan.
On the return trip from Tokyo to San Francisco, we could
not follow this sams prozram, but we id take surface sanpics
every four hours on the return journey.
Rather remarkably, wa
found the levels of activity about in tho ranze which wo expected,
I would say that an avevrace activity might be in tho
neighborhoscd, susatiny of the surface now, of 40 to &) disintegra.
tions per minute
por liter of water.
It is of interast to note
that this comosres with G09 disintovrations per minute duc to
potassiva--2 moan the normal potassium in sea water--so the
dneroase in level is not vory remarkable, but it is definite.
You seo, you have your north equatorial curront coming in,