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

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<strong>The</strong> <strong>Delft</strong> <strong>Sand</strong>, <strong>Clay</strong> & <strong>Rock</strong> <strong>Cutting</strong> <strong>Model</strong>.<br />

R<br />

h<br />

1 i<br />

1 , R2<br />

sin<br />

h<br />

<br />

2 b,m<br />

sin<br />

(9-21)<br />

Figure 9-15: <strong>The</strong> Curling Type or balling.<br />

Figure 9-16: <strong>The</strong> equilibrium of moments on the<br />

layer cut in hyperbaric rock.<br />

Substituting equations (9-10) and (9-11) into equation (9-20) gives:<br />

W2 sin( ) W1 sin( ) cos( )<br />

<br />

<br />

<br />

sin( )<br />

<br />

<br />

<br />

<br />

<br />

<br />

<br />

<br />

C cos( ) A cos<br />

1<br />

hi<br />

<br />

cos( )<br />

<br />

sin( ) sin<br />

<br />

<br />

<br />

<br />

<br />

<br />

W1<br />

<br />

<br />

<br />

<br />

W2 sin( ) W1 sin( ) <br />

<br />

cos( )<br />

sin( )<br />

<br />

<br />

<br />

<br />

<br />

<br />

<br />

C cos( )<br />

<br />

<br />

<br />

<br />

sin( )<br />

<br />

<br />

<br />

<br />

<br />

<br />

<br />

W2<br />

<br />

<br />

<br />

<br />

A cos<br />

h<br />

cos( )<br />

<br />

sin <br />

2 b,m<br />

(9-22)<br />

This can be written as a second degree function of the effective or mobilized blade height hb,m:<br />

2<br />

A x B x C<br />

0<br />

h<br />

b,m<br />

B B 4 A<br />

C<br />

x <br />

2<br />

A<br />

2<br />

(9-23)<br />

Page 306 of 454 TOC Copyright © Dr.ir. S.A. Miedema

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