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Cranfield University

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Conclusions<br />

� The longitudinal soil movement below a track is tilted significantly backwards<br />

whereas the soil is tilted forward below a tyre in low slip applications. In both cases<br />

this movement is limited to the top 150 mm in weak soil conditions.<br />

� The influence of lugs on variation in soil displacement is limited to a depth of ap-<br />

proximately 150 mm.<br />

� Load per perimeter length appeared to describe measured increase in DBD more<br />

accurately than contact pressure alone. Soil density increase for individual treat-<br />

ments could be described by the reciprocal of three trems: area, perimeter, and an<br />

interaction term. The intercept was not significant which means that there is no off-<br />

set. Hence, it has been possible to define the sinkage from a tyre contact area per-<br />

spective.<br />

� Peak pressures replicating the pass of a tyre cause 1/3 more sinkage than the appli-<br />

cation of the constant average pressure.<br />

� The vertical “punching” soil failure found in the laboratory studies supports the<br />

findings of Seig (1985) and others and can be explained by both plate sinkage the-<br />

ory (Benoit and Gotteland, 2005) and passive earth pressure theory.<br />

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

177

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