Example: Sledding
A little girl is riding her sled on a hill. If she starts a distance d up the hill, which makes an angle θ with the horizontal, how far will she travel along the flat snowy ground?
Facts
Child on incline of θ.
The total mass of the sled and child = m.
There’s a small bit of friction between the rails of the sled and the snow = (μ_k).
Slope length = L
Initial state: at rest, at height above horizontal
Final state: at rest on horizontal
Lacking
How far will she travel along the flat?
Approximations & Assumptions
Coefficient for kinetic friction for flat + incline is the same.
No wind resistance.
Representations
System: Sled + Kid + Earth
Surroundings: Snow
$$ \Delta E_{system} = W_{surroundings} $$$$ \Delta K + \Delta U_{g} = W_{friction} $$Solution
We could solve this using forces of kinematics; but, let’s apply the energy principle because we can avoid vector quantities in the calculation.
First we must decide the system and surroundings.
System: Sled+Kid+Earth Surroundings: Snow
Starting with the principle that change in energy in the system is equal to the work done by the surroundings.
$$ \Delta E_{system} = W_{surroundings} $$The change in energy can be in the form of change of kinetic and change in gravitational potential energy.
$$ \Delta K + \Delta U_{g} = W_{friction} $$No change
$$ \Delta K = 0 $$as its initial and final state of the sled is at rest.
$$ \Delta U_{g} = W_{friction} \rightarrow W_{friction}? $$Here, we pause because we have two different regions to consider.
![[ALT TEXT NEEDED: figure-01.jpg -- describe this figure for screen readers]](./media/rId15.jpg)
The frictional force is different in the two regions so we must consider the work they do separately.
$$ \Delta U_{g} = W_{1} + W_{2} $$Breaking work down into force by change in distance.
$$ \Delta U_{g} = {\overset{\rightarrow}{f}}_{1} \cdot \Delta{\overset{\rightarrow}{r}}_{1} + {\overset{\rightarrow}{f}}_{2} \cdot \Delta{\overset{\rightarrow}{r}}_{2} $$${\overset{\rightarrow}{r}}_{2}$ is what we are trying to solve for as this is the position change along flat part.
What’s $f_{1}$ and $f_{2}?$
![[ALT TEXT NEEDED: figure-02.jpg -- describe this figure for screen readers]](./media/rId18.jpg)
Need to find $f_{1}$ & $f_{2}$
To find $F_{1}$ we can say that the sum of the forces in the x direction are equal to $ma_{1}$ But we don’t need this because we know that $f_{1} = \mu_{k}N$.
$\sum F_{x} = f_{1} - mgsin\theta = ma_{1}$
The sum of the forces in the y direction we do need because this allows us to express N.
$$ \sum F_{y} = N - mgcos\theta = 0 $$$$ mgcos\theta = N $$If $f_{1} = \mu_{k}N$ then:
$$ f_{1} = \mu_{k}mgcos\theta $$To find $f_{2}$ we must do the same thing and add all the forces in the x and y directions. Again because not using kinematics we don’t need accelerations and instead want an equation that expresses $f_{2}$.
$$ \sum F_{x} = f_{2} = ma_{2} \rightarrow f_{2} = \mu_{k}N = \mu_{k}mg $$$$ \sum F_{y} = N - mg = 0 $$We substitute in for $f_{1}$, $f_{2}$ and d the distance down the slope into the previous equation for gravitational potential energy with minuses on the ${\overset{\rightarrow}{f}}'s$ as they are in opposition of the ${\overset{\rightarrow}{r}}'s$.
$$ \Delta U_{g} = {\overset{\rightarrow}{f}}_{1} \cdot \Delta{\overset{\rightarrow}{r}}_{1} + {\overset{\rightarrow}{f}}_{2} \cdot \Delta{\overset{\rightarrow}{r}}_{2} $$In the previous equation ${\overset{\rightarrow}{f}}_{1} \cdot \Delta{\overset{\rightarrow}{r}}_{1} \rightarrow W_{1} < 0$ and ${\overset{\rightarrow}{f}}_{2} \cdot \Delta{\overset{\rightarrow}{r}}_{2} \rightarrow W_{2} < 0$ because $\overset{\rightarrow}{f}$’s are opposite to $\Delta\overset{\rightarrow}{r}$’s
$$ \Delta U_{g} = - (\mu_{k}mgcos\theta)d - (\mu_{k}mg)x $$Substitute in the equation for gravitational potential energy for $\Delta U_{g}$
$$
- mg(y_{f} - y_{i}) = - \mu_{k}mgdcos\theta - \mu_{k}mgx $$
Rearrange to get the following expression.
$$ y_{f} - y_{i} = - \mu_{k}(dcos\theta + x) $$What is $y_{f} - y_{i}$ in terms of what we know? Eventually we want to express x in terms of variables we know.
![[ALT TEXT NEEDED: figure-03.jpg -- describe this figure for screen readers]](./media/rId22.jpg)
From the diagram of the incline we get:
$$ y_{f} - y_{i} = - dsin\theta $$Substitue $- dsin\theta$ for $y_{f} - y_{i}$ and then rearrange to express x in terms of known variables.
$$
- dsin\theta = - \mu_{k}(dcos\theta + x) $$
A check of the units reveals that:
\[x\]=m
\[d\]=m
Which makes sense as all the other quantities are unit less.
$E = \gamma mc^{2}$