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The Delft Sand, Clay & Rock Cutting Model, 2019a

The Delft Sand, Clay & Rock Cutting Model, 2019a

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Experiments in Water Saturated <strong>Sand</strong>.<br />

0.30<br />

No Cavitation<br />

Dimensionless Pore Pressure<br />

0.27<br />

0.24<br />

0.21<br />

0.18<br />

0.15<br />

0.12<br />

0.09<br />

0.06<br />

0.03<br />

0.00<br />

<strong>The</strong>ory Measurement - Wear Measurement - No Wear<br />

Figure M-14: α=45º, hi=70 mm, hb=141 mm.<br />

<strong>The</strong> dimensionless water pore pressures on the blade. Experiments in 200 m sand, with α=45°, β=24º, φ=38º,<br />

δ=30º, ni=38.53%, nmax=43.88%, ki=0.000165 m/s, kmax=0.000320 m/s, hi=70 mm, hb=141 mm, w=0.2 m, z=0.6<br />

m and a non-cavitating cutting process.<br />

0.30<br />

No Cavitation<br />

Dimensionless Pore Pressure<br />

0.27<br />

0.24<br />

0.21<br />

0.18<br />

0.15<br />

0.12<br />

0.09<br />

0.06<br />

0.03<br />

0.00<br />

<strong>The</strong>ory Measurement - Wear Measurement - No Wear<br />

Figure M-15: α=45º, hi=141 mm, hb=141 mm.<br />

<strong>The</strong> dimensionless water pore pressures on the blade. Experiments in 200 m sand, with α=45°, β=25º, φ=38º,<br />

δ=30º, ni=38.53%, nmax=43.88%, ki=0.000165 m/s, kmax=0.000320 m/s, hi=141 mm, hb=141 mm, w=0.2 m, z=0.6<br />

m and a non-cavitating cutting process.<br />

Copyright © Dr.ir. S.A. Miedema TOC Page M-65 of 228

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