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A History of Research and a Review of Recent Developments

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148<br />

Penetration <strong>and</strong> fragmentation<br />

The penetration length, L, which is the total length <strong>of</strong> the J-path, not the<br />

final vertical depth, p, was found from the tests to be linked to striking velocity<br />

through the parameter , where W p is the total projectile weight, not<br />

the weight <strong>of</strong> the explosive charge (W). The curves shown in Figure 7.2 are<br />

taken from ref. [7.13], <strong>and</strong> refer to four types <strong>of</strong> soil <strong>and</strong> projectiles having an<br />

‘average’ nose shape. Detailed information on other nose shapes are given in<br />

the reference.<br />

The vertical penetration <strong>of</strong> a range <strong>of</strong> general purpose bombs, with total<br />

weights in the range 100 to 2000 lb, in three different soils, is given in Figures<br />

7.3, 7.4 <strong>and</strong> 7.5. The curves were said by Stipe to agree with the scatter <strong>of</strong><br />

available data to within ±20%, <strong>and</strong> a rough interpolation between curves<br />

could be made for other soil types. Because the tests were mainly carried out<br />

with free-dropped aerial bombs, the striking velocity has been replaced by the<br />

altitude from which the bombs were dropped in level flight. In each experiment,<br />

delay fusing prevented explosion until full penetration had been achieved,<br />

<strong>and</strong> the results confirm the earlier statement that penetration into clay is about<br />

Figure 7.2 Length <strong>of</strong> the J-shaped penetration path (from Stipe, ref. 7.11; US Army<br />

TM5–855–1, 1965 <strong>and</strong> 1986).

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