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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 />

M.2 Pore Pressures in 200 μm <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-10: α=30º, hi=33 mm, hb=100 mm.<br />

<strong>The</strong> dimensionless water pore pressures on the blade. Experiments in 200 m sand, with α=30°, β=30º, φ=38º,<br />

δ=30º, ni=38.53%, nmax=43.88%, ki=0.000165 m/s, kmax=0.000320 m/s, hi=33 mm, hb=100 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-11: α=30º, hi=50 mm, hb=100 mm.<br />

<strong>The</strong> dimensionless water pore pressures on the blade. Experiments in 200 m sand, with α=30°, β=29º, φ=38º,<br />

δ=30º, ni=38.53%, nmax=43.88%, ki=0.000165 m/s, kmax=0.000320 m/s, hi=50 mm, hb=100 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-63 of 228

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