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sock Phenomena from Underwater °

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Seven projects investigated free-field blast and shock phenomena on
underwater shots Wahoo and Umbrella. Their primary objective was to ob-

tain the free-field input data needed for determination of safe delivery and

critical damage ranges for submarines, aircraft, and surface vessels operating in the vicinity of underwater nuclear detonations. In general, there
was a rather thorough amount of information available on free-field blast
and shock phenomena from HE tests. The only two nuclear underwater tests,

Crossroads Baker and Wigwam, however, had left many basic questions unanswered. The blast and shock projects therefore were generally aimed at
confirming and expanding Crossroads Baker and Wigwam results, providing
a tie-in between data from nuclear and HE tests, providing input data for
ships' damage projects, and generally increasing knowledge of underwater
explosion effects.
Deep Water Shot, Wahoo. Underwater Pressures - The Naval Ordnance
Laboratory and Naval Electronics Laboratory collaborated in measuring underwater pressures. Their main objectives were to confirm Wigwam results on
scaling for isovelocity conditions and to study the effects of refraction. Pressure data were obtained at five to,pine instrumented stations; peak pressures

ranged from

¥fere were four target ship stations; an ade-

quate number of pressure-time histories (at various depths to 1850 ft) were
obtained at the EC-2 (2346 ft) and the DD-593 (8887 ft). Only a few peak
pressures were recorded at the DD-474, while at the DD~-592 no data were
obtained. The data generally confirmed Wigwam results. Thermal gradients

showed considerable effect on the pressure field at the 8887-ft range and

also influenced peak pressures at depths less than 300 ft at the range of the
EC-2. The pressure-time data will be thoroughly analyzed, primarily by

NEL, for refraction effects, using the shot time underwater temperature field

provided by ONR-Hydrographic Office personnel. ONR-HO obtained its estimate of shot time underwater temperatures on the basis of bathythermograph
(ot) readings from the DD~-593 at H-—-15, H-—5, and H—1 min and pre-shot bt «
data taken from three points in the array starting on D-7 day.

Air Overpressure - The NOL installed three near-surface gages on

vessels in the array and self-recording gages on two balloons at heights of

500 and 1000 ft. Records were obtained from two gages from the balloon
station at 3413-ft range and two surface gages at 2346-ft range. Records

showed two distinct pulses; it is believed the first pulse resulted from under-

water shock transmitted across the water-air interface and the second from
bubbie effects.
2346-ft range.

Maximum pressure recorded was 0.21 psi at 30-ft elevation,
Peak pressures showed general agreement with predictions

based on HE results.

Surface Phenomena - The Scripps Institute of Oceanography measured
water waves and NOL studied all other surface phenomena, i.e., spray domes,

plumes, base surge, etc.

Photography from four aircraft and several surface

stations was the principal means of data collection. With the clear weather,
photographic coverage was excellent. Film analysis.in progress at this

writing is expected to provide thorough documentation of the phenomena of

interest. Surface phenomena bore a marked resemblance to Wigwam. Water
waves containing approximately 4% of the weapon energy were observed.

Hydrodynamic Yield - The Armour Research Foundation failed in its

attempt to measure the close-in propagation of the shock front.

The technique

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AFWL/HC

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