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Excerpt
hiddentrue

Analyzing a continuous momentum flux (water from a hose).

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Photo from Wikimedia Commons
Original by Doclector

When you spray water from a garden hose you feel a backward force as you hold the nozzle. Similarly, anything you spray the water at feels a force in the direction away from the spray. What is the origin of this force, and what determines its magnitude?

Composition Setup

Solution

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idsysa
System:
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Element of water stream as a acting on an article, also treated as a .

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idinta
Interactions:
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We will ignore the vertical direction, so that the only interaction is the force due to the changes in momentum of the water and the item hit..

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idmoda
Model:
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.

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Approach:

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Diagrammatic Representation

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Imagine a stream of water as a cylinder of uniform cross-sectional area A and density ρ. We consider an elemental unit of this that is Δx long. It travels, as does the rest of the stream, horizontally at velocity v (We will ignore the downward force of gravity here).

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idmatha
Mathematical Representation

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Consider the element of length Δx and area A and density ρ. Its mass m must therefore be

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{excerpt:hidden=true}Analyzing a continuous momentum flux (water from a hose).{excerpt}

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|!Hose Spraying Water.jpg!|
|Photo from Wikimedia Commons
Original by Doclector|


When you spray water from a garden hose you feel a backward force as you hold the nozzle. Similarly, anything you spray the water at feels a force in the direction away from the spray. What is the origin of this force, and what determines its magnitude?

{composition-setup}{composition-setup}

  

h4. Solution

{toggle-cloak:id=sysa} *System:*  {cloak:id=sysa}Element of water stream as a [point particle] acting on an article, also treated as a [point particle]. {cloak}

{toggle-cloak:id=inta} *Interactions:* {cloak:id=inta}We will *ignore the vertical direction*, so that the only interaction is the force due to the changes in momentum of the water and the item hit..

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{toggle-cloak:id=moda} *Model:*  {cloak:id=moda}[Momentum and External Force].{cloak}

{toggle-cloak:id=appa} *Approach:*  

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{toggle-cloak:id=diaga} {color:red} *Diagrammatic Representation* {color}

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|!Momentum Transport 01.PNG!|
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Imagine a stream of water as a cylinder of uniform cross-sectional area *A* and density {*}ρ{*}. We consider an elemental unit of this that is {*}Δx{*} long. It travels, as does the rest of the stream, horizontally at velocity *v* (We will ignore the downward force of gravity here).


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{toggle-cloak:id=matha} {color:red} *Mathematical Representation* {color}

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Consider the element of length {*}Δx{*} and area *A* and density {*}ρ{*}. Its mass must therefore be
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{latex}\begin{large}\[ m = \rho A \Delta x \] \end{large}{latex}
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{latex}


Since it travels with velocity v, its momentum is thus

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\begin{large} \[ m^{\rm car}v^{\rm car}_{x,i} \vec{p} = \left(m^{\rm car} + m^{\rm rain}\right)v_{x,frho A \Delta x \vec{v} \] \end{large}


Let's assume that this element of the stream strikes an object (a wall, say), and breaks up, dissipating in all directions. the stream element loses all of its momentum in the process. The change in momentum of the stream element is thus

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\begin{large} \[ \Delta \vec{p} = \rho A \Delta x \vec{v} \] \end{large}


If this happens in a time Δt, then the change in momentum with time (which is just the Average Force) is

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\begin{large} \[ \vec{F_{avg}} = \frac{\Delta \vec{p}}{\Delta t} = \rho A \vec{v} \frac{\Delta x}{\Delta t} \] \end{large}


But Δx/Δt = v , so the magnitude of the Average Force is thus

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{latex}

{note}It might be confusing that we can treat the rain, which falls individually as drops, as if it were one solid object.  The reason we can get away with this is the assumption that all the rain drops fall with exactly the same x-momentum, and that they end up at rest with respect to the car.  Because all the drops experience the same momentum change we can simply group them together and consider the momentum of the "rain block".{note}

All that remains is to determine the mass of the rain.  We can do this by noting that the density of water is 1000 kg/m{color:black}^3^{color} and that the water has filled the car to 2.0 cm deep, indicating a collected mass of:

{latex}\begin{large}\[ m^{\rm rain} = \rho^{\rm water}V^{\rm rain} = (\mbox{1000 kg/m}^{3})(\mbox{10 m}\times\mbox{3 m}\times\mbox{0.02 m}) = \mbox{600 kg} \]\end{large}{latex}

where ρ^water^ is the density of water and _V_^rain^ is the volume of the accumulated rain.

We can now solve to find:

{latex}\begin{large} \[ vF_{x,favg} = \frac{m^{\rm car}v^{\rm car}_{x,i}}{m^{\rm car} + m^{\rm rain}} = \mbox{1.6 m/s}\rho A v^{2} \]\end{large}{latex}

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