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Cranfield University

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Abstract<br />

Ancillary experiments showed that the dense layer at the surface from the tracks originates<br />

from a backward soil movement limited to the uppermost 150 mm. The lug influence of<br />

both tyres and tracks was insignificant from 200 mm depth downwards. From heuristical<br />

data analysis the load per perimeter length was identified as an important variable. Peaked<br />

pressure history caused about 1/3 more sinkage than constant contact pressures.<br />

Ph.D. Thesis Dirk Ansorge (2007)<br />

II

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