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Appendices

1A More Complicated Physical Pendulum

We can make a more complicated physical pendulum by assuming the mass of the leg is linearly decreasing from the hip to the foot, i.e., the leg is more massive at the hip and less massive at the foot. See Figure 1

A physical pendulum composed of a rod with linearly-dependent mass density.

Figure 1:A physical pendulum composed of a rod with linearly-dependent mass density.

To do this we must calculate the center of mass and the moment of inertia. Fortunately, these have very similar methods of calculation. The center of mass is calculated as

Rcm=1Mimixi1M0LdmxR_{cm} = \frac{1}{M}\sum_i m_i x_i \rightarrow \frac{1}{M}\int_0^L dm\cdot x

Before we assume the leg has a linear mass density decreasing from hip to foot, let’s verify that the center of mass of the uniform cylinder is Rcm=L/2R_{cm}=L/2. The mass distribution looks like a constant density.

λ=dmdx=ML\lambda = \frac{dm}{dx} = \frac{M}{L}

where MM is the total mass of the leg, and LL is the total length of the leg. Rearranging for dmdm gives

dm=MLdxdm = \frac{M}{L} dx

The center of mass integral is written

Rcm=1M0LMLxdxRcm=1MMLx220LRcm=1LL22Rcm=L2\begin{align} R_{cm} &= \frac{1}{M}\int_0^L \frac{M}{L}x\cdot dx\nonumber\\ R_{cm} &= \frac{1}{M}\frac{M}{L}\frac{x^2}{2}\Bigg|_0^L\nonumber\\ R_{cm} &= \frac{1}{L}\frac{L^2}{2}\nonumber\\ R_{cm} &= \frac{L}{2}\nonumber \end{align}

Okay, the method seems to check out. For the improved model where the leg is a cylinder with linear mass distribution, we can write that linear density as

λ=dmdx=A(Lx)\lambda = \frac{dm}{dx} = A\left(L-x\right)

where AA is a constant similar to M/LM/L above but different (units are kg/m2) for the non-uniform mass distribution. Rearranging this equation

dm=A(Lx)dxdm = A\left(L-x\right)dx

Substituting this into Eqn. (1), we get

Rcm=1M0LA(Lx)xdxRcm=AM(Lx22x33)0LRcm=AML36\begin{align*} R_{cm} &= \frac{1}{M}\int_0^L A\left(L-x\right)x\cdot dx\nonumber\\ R_{cm} &= \frac{A}{M}\left(\frac{Lx^2}{2}-\frac{x^3}{3}\right)\Bigg|_0^L\nonumber\\ R_{cm} &= \frac{A}{M}\frac{L^3}{6} \end{align*}

The moment of inertia is calculated similarly as

I=imixi20Ldmx2I = \sum_i m_i x_i^2 \rightarrow \int_0^L dm\cdot x^2

Using our linear mass density again, we get

I=0LA(Lx)x2dxI=A(Lx33x44)0LI=AL412\begin{align*} I &= \int_0^L A\left(L-x\right)x^2 dx\nonumber\\ I &= A\left(\frac{Lx^3}{3}-\frac{x^4}{4}\right)\Bigg|_0^L\nonumber\\ I &= \frac{AL^4}{12} \end{align*}

Now, we can use the step time that was derived in chapter 1 on Locomotion.

τ=πIRMgτ=πAL412AL36MMgτ=πL2g\begin{align*} \tau &= \pi\sqrt{\frac{I}{RMg}}\nonumber\\ \tau &= \pi\sqrt{\frac{\frac{AL^4}{12}}{\frac{AL^3}{6M}Mg}}\nonumber\\ \tau &= \pi\sqrt{\frac{L}{2g}} \end{align*}

We see that this step time is smaller by 25% than the uniform cylinder because the fraction in the square root goes from 2/32/3 to 1/21/2.

2Fluid Friction and Viscosity

The inter-layer force proposed by Newton

Fvisc=ηAdvdrF_{visc} = \eta A \frac{dv}{dr}

describes the viscous (frictional) forces between two layers of fluid. If the layers are considered to be concentric cylinders sharing the central axis of the cylinder, we can write the area that two layers share as the surface area of a cylinder Acyl=2πrL A_{cyl} = 2\pi rL. Next, we consider the situation where this viscous force is exactly balanced by the pressure force pushing fluid down the cylinder.

Fpush=ΔPAcrosssection,F_{push} = \Delta P A_{cross-section},

where the area is now the cross-sectional (circular face) area where the fluid is being pushed into the vessel. The change is pressure comes from the fact that a pushing force is on one end of the vessel, and no force exists on the other end. This cross-sectional area is πr2\pi r^2. Starting with Newton’s Second Law

F=Fvisc+Fpush=0.\sum F = F_{visc}+F_{push} = 0.

In this equilibrium condition, velocity is constant, but as we’ll see the actual value of the velocity depends on the radius at which the fluid flows down the vessel. Substituting the area and moving the push force to the right hand side, we get

η2πrLdvdr=ΔPπr2.\eta \cdot 2\pi rL\frac{dv}{dr} = - \Delta P \pi r^2.

Let’s solve for vv by moving anything not involving vv to the right hand side.

dv=ΔP2ηLrdrdv = -\frac{\Delta P}{2\eta L} r dr

Next, we can get the velocity at a particular r by looking at a the integral contribution over small increments, drdr.

dv=ΔP2ηLrdr\int dv = - \frac{\Delta P}{2\eta L} \int r dr

This gives

v(r)=ΔP2ηLr22+C=ΔP4ηLr2+C\begin{align*} v(r) &= -\frac{\Delta P}{2\eta L} \frac{r^2}{2} + C \nonumber\\ &= -\frac{\Delta P}{4\eta L}r^2+C \end{align*}

We know the velocity cannot be zero at r=0r=0, the center of the vessel. The velocity at the outside edge where r=Rr=R, the velocity is zero, and the constant CC is

C=ΔP4ηLR2,C =\frac{\Delta P}{4\eta L} R^2,

where RR is the radius of the vessel. This gives the equation (7).

v(r)=ΔPR2r24ηLv(r) = \Delta P\frac{R^2-r^2}{4\eta L}

From this we see that the velocity is zero at the edge of the vessel and is maximum at the center. It follows a parabolic velocity profile.