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

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

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Which <strong>Cutting</strong> Mechanism for Which Kind of Soil?<br />

<strong>The</strong> horizontal and vertical forces on the blade, chisel or pick point are:<br />

F h W2<br />

sin( ) K2<br />

sin(<br />

) Acos( )<br />

(4-22)<br />

F W cos( ) K cos(<br />

) Asin( )<br />

(4-23)<br />

v 2<br />

2<br />

<strong>The</strong> equilibrium of moments around the blade tip is:<br />

N<br />

W <br />

R G R N<br />

W <br />

1 1 1 3 2 2 2<br />

R<br />

(4-24)<br />

Analyzing these equations results in the following conclusions:<br />

Since the argument in the cosine of the cohesive term in the force K1 is always greater than 90 degrees, the<br />

cosine is negative and the term as a whole is positive. This results in positive forces on the blade, chisel or<br />

pick point and also positive normal forces. <strong>The</strong> minimum normal stress however equals the normal stress on<br />

the shear plane, minus about the radius of the Mohr circle. <strong>The</strong> result may be a negative minimum normal<br />

stress. If this negative minimum normal stress is smaller than the negative tensile strength, brittle tensile failure<br />

will occur. Otherwise brittle shear failure will occur. In both cases the forces calculated are peak forces. <strong>The</strong><br />

average forces are somewhere between 50% and 100% of the peak forces.<br />

On the blade the normal stresses are always high enough to avoid the occurrence of the Curling Type. In fact<br />

the forces on the blade do not depend on the length of the blade. <strong>The</strong> cohesive force on the shear plane however<br />

depends on the (mobilized) cohesion or shear strength, so the Tear Type, here named the Chip Type may<br />

occur.<br />

When the argument of the sine in the denominator gets close to 180 degrees, the forces become very large. If<br />

the argument is greater than 180 degrees, the forces would become negative. Since both conditions will not<br />

happen in nature, nature will find another cutting mechanism, the wedge mechanism.<br />

4.5. <strong>Cutting</strong> <strong>Rock</strong> Hyperbaric.<br />

In the case of hyperbaric rock cutting, the pore pressures cannot be neglected anymore. Gravity and inertial forces<br />

can still be neglected. Usually rock has no adhesion. When the hydrostatic pressure is larger than or approaching<br />

the UCS value of the rock, the rock tends to fail in a semi-ductile manner, named cataclastic failure. It is almost<br />

like the hydrostatic pressure can be added to the tensile strength of the rock.<br />

<strong>Rock</strong> cutting under hyperbaric conditions (deep sea mining) is dominated by the internal shear strength, the pore<br />

vacuum pressure forces and by the internal and external friction angles. <strong>The</strong> main cutting mechanism is the<br />

Crushed Type, cataclastic semi-ductile cutting. This is covered in Chapter 9: <strong>Rock</strong> <strong>Cutting</strong>: Hyperbaric<br />

Conditions.<br />

Figure 4-8: <strong>The</strong> Crushed Type in hyperbaric rock cutting.<br />

Copyright © Dr.ir. S.A. Miedema TOC Page 101 of 454

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