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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 />

in the equations is the shear angle β. Assuming that the mechanism will choose a shear angle where the cutting<br />

energy is at a minimum, a shear angle β is found according to:<br />

<br />

(7-89)<br />

4 2<br />

If we substitute this solution in the cutting force equations we find:<br />

<br />

<br />

<br />

<br />

cos <br />

Fh 2 s c hi<br />

w<br />

1 sin<br />

sin<br />

F<br />

2 s c hi w<br />

1 sin<br />

(7-90)<br />

(7-91)<br />

<strong>The</strong> horizontal force will increase with an increasing blade angle, the vertical force also, but upwards directed. In<br />

the case of the Curling Type, the ac ratio r is not fully mobilized giving:<br />

<br />

<br />

sin <br />

rm<br />

2<br />

1 sin<br />

(7-92)<br />

<strong>The</strong> condition of having a normal force of zero on the blade can never fulfill the condition of having an equilibrium<br />

of moments on the layer cut, since the normal force on the blade is zero and is therefore rejected. Still this condition<br />

gives insight in the behavior of the equations of clay cutting and is therefore mentioned here.<br />

7.6.3. <strong>The</strong> Equilibrium of Moments.<br />

As mentioned in the previous paragraph, the equilibrium of moments on the layer cut has to be fulfilled. If we take<br />

the equilibrium of moments around the tip of the blade, there are only two forces participating in the equilibrium<br />

of moments, the normal force on the shear plane N1 and the normal force on the blade N2. <strong>The</strong>se forces have acting<br />

points R1 and R2 on the shear plane and on the blade. If the normal stresses are uniformly distributed, both acting<br />

points will be at the center (half way) the corresponding planes. <strong>The</strong> acting point of the normal force on the shear<br />

plane will be at half the length of the shear plane and the acting point of the normal force on the blade will be at<br />

half the (mobilized) length of the blade. Two factors are introduced to give the exact location of these acting points,<br />

λ1 on the shear plane and λ2 on the blade. When the moment N2·R2 on the blade is greater than the moment N1·R1<br />

on the blade curling will occur in such a way that both moments are equal. <strong>The</strong> contact length between the clay<br />

and the blade will be reduced to a mobilized contact length hb,m.<br />

<strong>The</strong> normal force on the shear plane is now equal to the force N1, because the internal friction angle is zero:<br />

Ccos( ) A<br />

N1<br />

<br />

sin( )<br />

(7-93)<br />

<strong>The</strong> normal force on the blade is now equal to the force N2, because the external friction angle is zero:<br />

N<br />

2<br />

C Acos( )<br />

<br />

sin( )<br />

(7-94)<br />

This gives for the equilibrium of moments:<br />

N1 R1 N2 R2<br />

(7-95)<br />

For both acting points we can write:<br />

R<br />

h<br />

1 i<br />

1 , R2<br />

sin<br />

h<br />

<br />

2 b,m<br />

sin<br />

(7-96)<br />

Page 224 of 454 TOC Copyright © Dr.ir. S.A. Miedema

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