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The coefficients of lateral earth pressure, K and depth relationship were proposed based on the analysis of measured maximum tensile force in the reinforcements.
However, theoretically, the form of the relationship between the amount of material in the water layer and water depth observed by Gao et al. may be produced by an a to water depth relationship that differs from the one used in the mechanistic model.
Numerical simulation results of the indentation of an elastic plastic half-space by a frictionless rigid paraboloïd of revolution show that the contact radius indentation depth relationship can be represented by a power law, which depends on the reduced Young's modulus of the contact, on the strain hardening exponent and on the yield stress of the indented material.
Figure 2b shows the depth relationship of tephra layers at the three sites.
All tuned points fall in an age versus depth relationship based on marker tephras and magnetostratigraphic events within uncertainties.
Fig. 2 A diagram showing age versus depth relationship at Site U1424 based on marker tephras and magnetostratigraphic events listed in Table 1.
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Seismicity data and calculated temperature versus depth relationships are in good agreement with the rheological model predictions.
b Depth relationships of correlative tephra layers between sites.
Temperature vs. depth relationships are established for seven gauged borewell locations.
Through this reconstruction, the mechanical compaction, pore pressures, effective stress, and porosity versus depth relationships are established.
Figure 1 shows one of the specific energy bite depth relationships derived from experimental data (Luo et al. 2004).
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