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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 />

16.8.2. Calc.: <strong>Cutting</strong> Forces & Mechanisms.<br />

Consider a rock with a compressive strength of 100 MPa and a tensile strength of -10 MPa. <strong>The</strong> angle of<br />

internal friction is 20 degrees, the angle of external friction is 13.33 degrees. A blade angle of 60 degrees is<br />

used and a blade height of 0.1 m and blade width w=1 m. <strong>The</strong> layer thickness is 0.1 m.<br />

<strong>The</strong> shear angle is:<br />

<br />

= 43.33 degrees<br />

2 2<br />

<strong>The</strong> cohesion or shear strength is:<br />

<br />

<br />

UCS 1<br />

sin <br />

c =35 MPa<br />

2 <br />

cos <br />

<br />

<strong>The</strong> normal stress on the shear plane is:<br />

ccos( ) N1<br />

cos( ) 21.52 M Pa<br />

sin( )<br />

<strong>The</strong> shear stress on the shear plane is:<br />

S1<br />

N1<br />

<br />

c tan =42.84 MPa<br />

<strong>The</strong> normal stress in the center of the Mohr circle is:<br />

C N1 S1<br />

<br />

tan 37.1 MPa<br />

<strong>The</strong> radius of this Mohr circle is now:<br />

S1<br />

R <br />

cos <br />

<br />

<br />

45.59 MPa<br />

<strong>The</strong> minimum principle stress of this Mohr circle is:<br />

R 8.48 MPa<br />

min C<br />

Since -8.48 MPa>-10 MPa there is no tensile failure but shear failure.<br />

<strong>The</strong> horizontal force is now:<br />

2ch i wcos( )sin( )<br />

Fh HF chi w 1.912 35 0.11 6.691 MN<br />

1<br />

cos( )<br />

<strong>The</strong> vertical force is now:<br />

2ch i wcos( )cos( )<br />

F<br />

VF<br />

chi<br />

w 0.572 35 0.11 2.0 MN<br />

1<br />

cos( )<br />

Page 422 of 454 TOC Copyright © Dr.ir. S.A. Miedema

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