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and biologists of various kinds but we never did get to see the physi-

cians,

This is very interesting.

But, out of that conference we saw some Japanese data, from
their Shunkotsu Maru expedition, which I think was right in the middle of the test, wasn't it, Lauren?
DONALDSON:
EISENBUD:
expedition?

Yes.

Do you remember the date of the Shunkotsu Maru

DONALDSON: They left May 24th.
EISENBUD: They sailed into the equatorial current just west of
Bikini and took profile measurements which indicated that about
200,000 curics a day were drifting out of the lagoon into the equatorial

current.

This is while the other tests were going on.

This informa-

tion was given to me ina little packet, It wasn't discussed very much,
I read it on the way back and I got interested init. Asa result of
that and the fact that it was a simple extrapolation to show that this
would go into the Kuroshiro Current in the Philippines and then heaa
north to the Japanese coast, it seemed prudent to get out and get
some measurements, This was done through an operation control

which was carried on jointly between the Coast Guard and Dr. Donaldson's laboratory and ours, and that took place, I believe, in March,
about a year after the 1954 event,

DONALDSON:

This expedition left on February 25, 1955.

EISENBUD: And got some very good data on the distribution of
radioactivity in the Western Pacific as a result of that test.
FREMONT-SMITH:

Was it appreciable?

EISENBUD: Yes. The radioactivity was detected everywhere that
the expedition went. It started essentially from the Marshall Islands
and proceeded west to Guam and then north in the Kuroshiro Current
to Japan, where they put in and exchanged data with the Japanese.
Then, as‘ recall, Lauren you correct me—I'm just reconstructing
this—they came back in the Alaska Current and went down the West
Coast of the United States and completed a cruise of some three and
a half or four months during which time they actually followed the

current all the way around.

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