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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 />

Analyzing the equations for the influence of the weight (gravity) and the influence of the inertial forces shows a<br />

significant difference. <strong>The</strong> gravitational forces are proportional to the density of the soil ρs, the gravitational<br />

constant g, the thickness of the layer cut hi squared and the width of the blade w. <strong>The</strong> inertial forces are proportional<br />

to the density of the soil ρs, the cutting velocity vc squared, the thickness of the layer cut hi and the width of the<br />

blade w. This implies that the ratio between these two forces does not only depends on the geometry, but even<br />

stronger on the layer thickness hi and the cutting velocity vc. <strong>The</strong> thicker the layer cut, the higher the influence of<br />

gravity and the higher the cutting velocity, the higher the influence of inertia. One cannot say simply the higher<br />

the cutting velocity the higher the influence of inertia.<br />

2<br />

s i<br />

2<br />

s c i<br />

Gravitation : F g h w<br />

(5-18)<br />

Inertia : F v h w<br />

(5-19)<br />

<strong>The</strong> contribution of the inertial forces is determined by the following dimensionless parameter:<br />

2<br />

c<br />

v<br />

i<br />

(5-20)<br />

g h<br />

i<br />

In dredging a layer thickness of the magnitude of centimeters is common, while for a bulldozer a layer thickness<br />

of a magnitude of a meter is not strange. At the same cutting velocity, the relative influence of inertial forces will<br />

differ between dredging applications and the operation of bulldozers. If inertial forces dominate the cutting process,<br />

the cutting forces can be expressed as:<br />

2<br />

h s c i HI<br />

F v h w<br />

sin( ) cos( )<br />

With : HI<br />

sin( )<br />

sin( ) sin( )<br />

(5-21)<br />

2<br />

s c i VI<br />

F v h w<br />

sin( ) cos( )<br />

With : VI<br />

cos( )<br />

sin( ) sin( )<br />

(5-22)<br />

<strong>The</strong>se equations are derived from equations (5-6), (5-7), (5-9) and (5-10). <strong>The</strong> shear angle β can be derived<br />

analytically for the inertial forces, giving:<br />

2 <br />

(5-23)<br />

2 2<br />

Figure 5-13 shows the percentage of the contribution of the inertial forces to the horizontal cutting force for a layer<br />

thickness hi of 1.0 m at a cutting velocity of 0.5 m/sec, giving λi=0.025. Figure 5-14 shows the percentage of the<br />

contribution of the inertial forces to the horizontal cutting force for a layer thickness hi of 0.1 m at a cutting<br />

velocity of 15.7 m/sec, giving λi=250.<br />

Table 5-1 shows the inertial effect for the dimensionless inertial effect parameter λi ranging from 0.025 to 250.<br />

<strong>The</strong> percentage contribution of the inertial effect on the horizontal force is given as well as the shear angle, both<br />

horizontal and vertical cutting force coefficients based on equations (5-21) and (5-22) and both horizontal and<br />

vertical cutting force coefficients based on equations (5-13) and (5-14) for the case where the blade height hb<br />

equals the layer thickness hi. <strong>The</strong> table shows that the inertial effect can be neglected at very small values of the<br />

dimensionless inertial effect parameter λi, while at large values the gravitational effect can be neglected. <strong>The</strong> shear<br />

angle β decreases with an increasing dimensionless inertial effect parameter λi. Since the inertial forces are not<br />

influenced by the blade height hb, the cutting forces are not dependent on the blade height at high cutting velocities.<br />

At low cutting velocities there will be an effect of the blade height.<br />

Page 112 of 454 TOC Copyright © Dr.ir. S.A. Miedema

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