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A History of Research and a Review of Recent Developments

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100<br />

Structural loading from local explosions<br />

gauge installation procedures in rock <strong>and</strong> soil has been discussed by Florence,<br />

Keough <strong>and</strong> Mak [5.7]. In particular they investigated theoretically the effect<br />

<strong>of</strong> bonded <strong>and</strong> unbonded interfaces between the gauge <strong>and</strong> the surrounding<br />

soil. They assumed that a bonded interface would transmit compression <strong>and</strong><br />

shear, <strong>and</strong> an unbonded interface compressive loads only. Their calculations<br />

show that lack <strong>of</strong> interface bonding produces a non-uniform stress distribution<br />

at the gauge which produces inaccuracies at low stresses. At higher stresses<br />

plastic flow in the soil increases, <strong>and</strong> causes the stress distribution to be more<br />

uniform. This improves accuracy.<br />

5.3 CONCENTRATED EXTERNAL LOADS ON UNDERWATER<br />

STRUCTURES<br />

Much <strong>of</strong> the load-measuring research in this field has been conducted by naval<br />

research teams interested in the response <strong>of</strong> ship <strong>and</strong> submarine structures to<br />

local explosions from mines <strong>and</strong> torpedoes. Minesweepers <strong>and</strong> similar vessels<br />

are likely to suffer shock loading from the explosion <strong>of</strong> underwater charges at<br />

what are called ‘intermediate st<strong>and</strong>-<strong>of</strong>fs’, which can induce flexural motion<br />

or ‘whipping’ <strong>of</strong> the hull as well as local rupture <strong>and</strong> damage. We have already<br />

examined the characteristics <strong>of</strong> bubble pulsations <strong>and</strong> shock waves at long<br />

distance, but now we must evaluate the intermediate st<strong>and</strong>-<strong>of</strong>f effects. Hicks<br />

[5.8], in discussing explosion-induced hull whipping, suggests that British naval<br />

scientists are interested in peak instantaneous pressures in the 100 to 400 bar<br />

range, with durations between 300 <strong>and</strong> 600 microseconds. He concludes that<br />

with the acoustic velocity <strong>of</strong> sound in water at 1500m/s, the shock wave occupies<br />

a thin shell <strong>of</strong> water that might be about 1 metre in thickness.<br />

Hicks investigated how far the formulae for loading from distant explosions<br />

can be applied to close explosions. In the latter case there would seem to be<br />

a loss <strong>of</strong> accuracy for explosions near the bow <strong>and</strong> stern, where divergent<br />

flow around the end <strong>of</strong> the vessel might introduce non-uniformity into the<br />

analysis. Hicks, however, concluded that the accuracy <strong>of</strong> the distant-flow<br />

approximations for close point sources was extraordinarily good, <strong>and</strong> he<br />

assumed that the distant-flow analysis was adequate for normal st<strong>and</strong>-<strong>of</strong>fs.<br />

For very close st<strong>and</strong>-<strong>of</strong>fs the pressure bubble is likely to completely engulf<br />

the hull <strong>and</strong> this distorts the analysis too much for the distant-flow equations<br />

to be applicable.<br />

Loading from intermediate st<strong>and</strong>-<strong>of</strong>fs has also been investigated recently<br />

by Haxton <strong>and</strong> Haywood [5.9], who took as their model an underwater cylinder<br />

subjected to a pressure pulse originating from a point distant about one radius<br />

from the wall <strong>of</strong> the cylinder. It was assumed that the peak instantaneous<br />

pressure from the explosion varied inversely with distance, <strong>and</strong> that the radial<br />

component <strong>of</strong> the incident particle velocity could be neglected in the shadow<br />

<strong>of</strong> the cylinder. Referring to Figure 5.7, the peak instantaneous pressure depends<br />

on the radius Rt <strong>and</strong> the angle θt, <strong>and</strong> the point <strong>of</strong> grazing incidence, beyond

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