CHAPTER II, SECTION 1
As a result of the exploration borings and
laboratory tests, the following general criteria
were set up:

(a) Structures which were not critical from
a settlement standpoint were supported
on conventional spread footings.
(b) For structures where allowable settlerent was extremely critical, 12-inch
steel H-piles from 40 to 80 feet in
length were used.
Figur2 2-2 shows 12-inch H-piles, 80 feet long,

drive.i and capped. This foundation was used
for Station 20.

Detailed design criteria subsequently used
proved adequate; the final results showed there
was no appreciable settlement of any of the
struct res beyond critical limits.

WAV= ACTION STUDIES. A survey was
made of the Bikini Atoll early in Aprit 1953 to

determine wave conditions, wind conditions an-l
‘he relationship between wind and waves. The
study also included cloud cover and current observations.
Wave periods and heights were measured
with a wave staff. This wave staff was of the

type used by the U. S. Navy Hydrographic

Office. The displacement of water on the staff

from crest to trough was observed visually and
logged as each wave passed. Wave periods and

heights were recorded to the nearest half-foot.

Wind speeds were taken with a hand anemometer from the highest point on the bridge
of an LST. Wind direction was ascertained to
the nearest 16th point of the compass.
Currents in the lagoon were measured in
the passes by computing the drift of wood blocks
from an anchored vessel, and in the ocean b
fixing the position of a free-floating wavestaff

over a period of several months.

Cloud cover was estimated visually by percentages in 10% increments.

The results showed that the wind regime

was very stable, with the prevailing direction as

ENE with extreme observed directions of NE

and ESE. The wind speed was between . .ur and
20 knots with the greater percentage botween
nine and 19 knots. The mean cloud cover during
daylight hours was 3.10. *.ow cumulus was present nearly always with arm average base height

of 2,000 feet. It was found that the currents

in all
same
knots
at all

of the passes were approximately of the
velocity, the speed ranging between 0.5
anc 1.5 knots, without clange ir. direction
tides.

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