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2.1 Pressure at a Point 39<br />

z<br />

p s δx<br />

δs<br />

θ<br />

p y δx<br />

δz<br />

δ s<br />

δ z<br />

δ y<br />

θ<br />

δ x<br />

y<br />

x<br />

δx ________ δyδz<br />

γ<br />

2<br />

p z δx<br />

δy<br />

F I G U R E 2.1 Forces on an arbitrary wedge-shaped element of <strong>fluid</strong>.<br />

through the point. To answer this question, consider the free-body diagram, illustrated in Fig. 2.1,<br />

that was obtained by removing a small triangular wedge of <strong>fluid</strong> from some arbitrary location<br />

within a <strong>fluid</strong> mass. Since we are considering the situation in which there are no shearing stresses,<br />

the only external forces acting on the wedge are due to the pressure and the weight. For simplicity<br />

the forces in the x direction are not shown, and the z axis is taken as the vertical axis so the<br />

weight acts in the negative z direction. Although we are primarily interested in <strong>fluid</strong>s at rest, to<br />

make the analysis as general as possible, we will allow the <strong>fluid</strong> element to have accelerated motion.<br />

The assumption of zero shearing stresses will still be valid so long as the <strong>fluid</strong> element moves<br />

as a rigid body; that is, there is no relative motion between adjacent elements.<br />

The equations of motion 1Newton’s second law, F ma2 in the y and z directions are, respectively,<br />

a F dx dy dz<br />

y p y dx dz p s dx ds sin u r a<br />

2 y<br />

a F dx dy dz dx dy dz<br />

z p z dx dy p s dx ds cos u g r a<br />

2<br />

2 z<br />

where p s , p y , and p z are the average pressures on the faces, g and r are the <strong>fluid</strong> specific weight<br />

and density, respectively, and a y , a z the accelerations. Note that a pressure must be multiplied<br />

by an appropriate area to obtain the force generated by the pressure. It follows from the geometry<br />

that<br />

dy ds cos u dz ds sin u<br />

so that the equations of motion can be rewritten as<br />

The pressure at a<br />

p y p s ra dy<br />

y<br />

point in a <strong>fluid</strong> at<br />

2<br />

rest is independent<br />

p z p s 1ra z g2 dz<br />

of direction.<br />

2<br />

Since we are really interested in what is happening at a point, we take the limit as dx, dy, and dz<br />

approach zero 1while maintaining the angle u2, and it follows that<br />

p y p s p z p s<br />

or p s p y p z . The angle u was arbitrarily chosen so we can conclude that the pressure at a point<br />

in a <strong>fluid</strong> at rest, or in motion, is independent of direction as long as there are no shearing stresses<br />

p y p z<br />

present. This important result is known as Pascal’s law, named in honor of Blaise Pascal 11623–<br />

16622, a French mathematician who made important contributions in the field of hydrostatics. Thus,<br />

as shown by the photograph in the margin, at the junction of the side and bottom of the beaker, the<br />

p z<br />

pressure is the same on the side as it is on the bottom. In Chapter 6 it will be shown that for moving<br />

<strong>fluid</strong>s in which there is relative motion between particles 1so that shearing stresses develop2, the<br />

p y<br />

normal stress at a point, which corresponds to pressure in <strong>fluid</strong>s at rest, is not necessarily the same

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