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

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 />

Figure 8-27: <strong>The</strong> Flow Type cutting mechanism in ductile rock cutting.<br />

<strong>The</strong> specific energy Esp is defined as the amount of energy used/required to excavate 1 m 3 of soil/rock. This can<br />

be determined by dividing the cutting power Pc by the production Q and results in the cutting force Fh in the<br />

direction of the cutting velocity vc, divided by the cross section cut hi·w:<br />

E<br />

sp<br />

Pc Fh<br />

vc Fh<br />

<br />

Q h w v h w<br />

i c i<br />

(8-97)<br />

<strong>The</strong> model for rock cutting under atmospheric conditions is based on the Flow Type of cutting mechanism.<br />

Although in general rock will encounter a more brittle failure mechanism and the Flow Type considered represents<br />

the ductile failure mechanism, the Flow Type mechanism forms the basis for all cutting processes. <strong>The</strong> definitions<br />

of the Flow Type mechanism are shown in Figure 8-27.<br />

Figure 8-28 illustrates the forces on the layer of rock cut. <strong>The</strong> forces shown are valid in general. <strong>The</strong> forces acting<br />

on this layer are:<br />

1. A normal force acting on the shear surface N1 resulting from the grain stresses.<br />

2. A shear force S1 as a result of internal friction N1·tan(.<br />

3. A shear force C as a result of the shear strength (cohesion) c or c. This force can be calculated by multiplying<br />

the cohesive shear strength c with the area of the shear plane.<br />

4. A force normal to the blade N2 resulting from the grain stresses.<br />

5. A shear force S2 as a result of the soil/steel friction N2·tan( or external friction.<br />

<strong>The</strong> normal force N1 and the shear force S1 can be combined to a resulting grain force K1.<br />

<strong>The</strong> forces acting on a straight blade when cutting rock, can be distinguished as:<br />

6. A force normal to the blade N2 resulting from the grain stresses.<br />

7. A shear force S2 as a result of the soil/steel friction N2·tan(or external friction.<br />

<strong>The</strong>se forces are shown in Figure 8-29. If the forces N2 and S2 are combined to a resulting force K2 the resulting<br />

force K2 is the unknown force on the blade. By taking the horizontal and vertical equilibrium of forces an<br />

expression for the force K2 on the blade can be derived.<br />

<strong>The</strong> horizontal equilibrium of forces:<br />

F h K 1 sin( ) C cos( ) K 2 sin( ) 0<br />

(8-98)<br />

<strong>The</strong> vertical equilibrium of forces:<br />

F v K 1 cos( ) C sin( ) K 2 cos( ) 0<br />

(8-99)<br />

Page 274 of 454 TOC Copyright © Dr.ir. S.A. Miedema

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