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Trajectory

From Wikipedia, the free encyclopedia
Path of a moving object
For other uses, seeTrajectory (disambiguation).
"Flightpath" redirects here. For other uses, seeFlightpath (disambiguation).
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Illustration showing the directional trajectory of a bullet fired at an uphill target

Atrajectory orflight path is the path that anobject withmass inmotion follows throughspace as a function of time. Inclassical mechanics, a trajectory is defined byHamiltonian mechanics viacanonical coordinates; hence, a complete trajectory is defined by position andmomentum, simultaneously.

The mass might be aprojectile or asatellite.[1] For example, it can be anorbit — the path of aplanet,asteroid, orcomet as it travels around acentral mass.

Incontrol theory, a trajectory is a time-ordered set ofstates of adynamical system (see e.g.Poincaré map). Indiscrete mathematics, a trajectory is a sequence(fk(x))kN{\displaystyle (f^{k}(x))_{k\in \mathbb {N} }} of values calculated by the iterated application of a mappingf{\displaystyle f} to an elementx{\displaystyle x} of its source.

Physics of trajectories

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A familiar example of a trajectory is the path of a projectile, such as a thrown ball or rock. In a significantly simplified model, the object moves only under the influence of a uniform gravitationalforce field. This can be a good approximation for a rock that is thrown for short distances, for example at the surface of theMoon. In this simple approximation, the trajectory takes the shape of aparabola. Generally when determining trajectories, it may be necessary to account for nonuniform gravitational forces and air resistance (drag andaerodynamics). This is the focus of the discipline ofballistics.

One of the remarkable achievements ofNewtonian mechanics was the derivation ofKepler's laws of planetary motion. In the gravitational field of a point mass or a spherically-symmetrical extended mass (such as theSun), the trajectory of a moving object is aconic section, usually anellipse or ahyperbola.[a] This agrees with the observed orbits ofplanets,comets, and artificial spacecraft to a reasonably good approximation, although if a comet passes close to the Sun, then it is also influenced by otherforces such as thesolar wind andradiation pressure, which modify the orbit and cause the comet to eject material into space.

Newton's theory later developed into the branch oftheoretical physics known asclassical mechanics. It employs the mathematics ofdifferential calculus (which was also initiated by Newton in his youth). Over the centuries, countless scientists have contributed to the development of these two disciplines. Classical mechanics became a most prominent demonstration of the power of rational thought, i.e.reason, in science as well as technology. It helps to understand and predict an enormous range ofphenomena; trajectories are but one example.

Consider a particle ofmassm{\displaystyle m}, moving in apotential fieldV{\displaystyle V}. Physically speaking, mass representsinertia, and the fieldV{\displaystyle V} represents external forces of a particular kind known as "conservative". GivenV{\displaystyle V} at every relevant position, there is a way to infer the associated force that would act at that position, say from gravity. Not all forces can be expressed in this way, however.

The motion of the particle is described by the second-orderdifferential equation

md2x(t)dt2=V(x(t)) with x=(x,y,z).{\displaystyle m{\frac {\mathrm {d} ^{2}{\vec {x}}(t)}{\mathrm {d} t^{2}}}=-\nabla V({\vec {x}}(t)){\text{ with }}{\vec {x}}=(x,y,z).}

On the right-hand side, the force is given in terms ofV{\displaystyle \nabla V}, thegradient of the potential, taken at positions along the trajectory. This is the mathematical form of Newton'ssecond law of motion: force equals mass times acceleration, for such situations.

Examples

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Uniform gravity, neither drag nor wind

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Trajectories of a mass thrown at an angle of 70°:
  withoutdrag
  withStokes drag
  withNewton drag

The ideal case of motion of a projectile in a uniform gravitational field in the absence of other forces (such as air drag) was first investigated byGalileo Galilei. To neglect the action of the atmosphere in shaping a trajectory would have been considered a futile hypothesis by practical-minded investigators all through theMiddle Ages inEurope. Nevertheless, by anticipating the existence of thevacuum, later to be demonstrated onEarth by his collaboratorEvangelista Torricelli[citation needed], Galileo was able to initiate the future science ofmechanics.[citation needed] In a near vacuum, as it turns out for instance on theMoon, his simplified parabolic trajectory proves essentially correct.

In the analysis that follows, we derive the equation of motion of a projectile as measured from aninertial frame at rest with respect to the ground. Associated with the frame is a right-hand coordinate system with its origin at the point of launch of the projectile. Thex{\displaystyle x}-axis is tangent to the ground, and they{\displaystyle y}axis is perpendicular to it ( parallel to the gravitational field lines ). Letg{\displaystyle g} be theacceleration of gravity. Relative to the flat terrain, let the initial horizontal speed bevh=vcos(θ){\displaystyle v_{h}=v\cos(\theta )} and the initial vertical speed bevv=vsin(θ){\displaystyle v_{v}=v\sin(\theta )}. It will also be shown that therange is2vhvv/g{\displaystyle 2v_{h}v_{v}/g}, and the maximum altitude isvv2/2g{\displaystyle v_{v}^{2}/2g}. The maximum range for a given initial speedv{\displaystyle v} is obtained whenvh=vv{\displaystyle v_{h}=v_{v}}, i.e. the initial angle is 45{\displaystyle ^{\circ }}. This range isv2/g{\displaystyle v^{2}/g}, and the maximum altitude at the maximum range isv2/(4g){\displaystyle v^{2}/(4g)}.

Derivation of the equation of motion

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Assume the motion of the projectile is being measured from afree fall frame which happens to be at (x,y) = (0,0) at t = 0. The equation of motion of the projectile in this frame (by theequivalence principle) would bey=xtan(θ){\displaystyle y=x\tan(\theta )}. The co-ordinates of this free-fall frame, with respect to our inertial frame would bey=gt2/2{\displaystyle y=-gt^{2}/2}. That is,y=g(x/vh)2/2{\displaystyle y=-g(x/v_{h})^{2}/2}.

Now translating back to the inertial frame the co-ordinates of the projectile becomesy=xtan(θ)g(x/vh)2/2{\displaystyle y=x\tan(\theta )-g(x/v_{h})^{2}/2} That is:

y=gsec2θ2v02x2+xtanθ,{\displaystyle y=-{g\sec ^{2}\theta \over 2v_{0}^{2}}x^{2}+x\tan \theta ,}

(wherev0 is the initial velocity,θ{\displaystyle \theta } is the angle of elevation, andg is the acceleration due to gravity).

Range and height

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Trajectories of projectiles launched at different elevation angles but the same speed of 10 m/s in a vacuum and uniform downward gravity field of 10 m/s2. Points are at 0.05 s intervals and length of their tails is linearly proportional to their speed.t = time from launch,T = time of flight,R = range andH = highest point of trajectory (indicated with arrows).

Therange,R, is the greatest distance the object travels along thex-axis in the I sector. Theinitial velocity,vi, is the speed at which said object is launched from the point of origin. Theinitial angle,θi, is the angle at which said object is released. Theg is the respective gravitational pull on the object within a null-medium.

R=vi2sin2θig{\displaystyle R={v_{i}^{2}\sin 2\theta _{i} \over g}}

Theheight,h, is the greatest parabolic height said object reaches within its trajectory

h=vi2sin2θi2g{\displaystyle h={v_{i}^{2}\sin ^{2}\theta _{i} \over 2g}}

Angle of elevation

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An example showing how to calculate bullet trajectory

In terms of angle of elevationθ{\displaystyle \theta } and initial speedv{\displaystyle v}:

vh=vcosθ,vv=vsinθ{\displaystyle v_{h}=v\cos \theta ,\quad v_{v}=v\sin \theta \;}

giving the range as

R=2v2cos(θ)sin(θ)/g=v2sin(2θ)/g.{\displaystyle R=2v^{2}\cos(\theta )\sin(\theta )/g=v^{2}\sin(2\theta )/g\,.}

This equation can be rearranged to find the angle for a required range

θ=12sin1(gRv2){\displaystyle \theta ={\frac {1}{2}}\sin ^{-1}\left({\frac {gR}{v^{2}}}\right)} (Equation II: angle of projectile launch)

Note that thesine function is such that there are two solutions forθ{\displaystyle \theta } for a given rangedh{\displaystyle d_{h}}. The angleθ{\displaystyle \theta } giving the maximum range can be found by considering the derivative orR{\displaystyle R} with respect toθ{\displaystyle \theta } and setting it to zero.

dRdθ=2v2gcos(2θ)=0{\displaystyle {\mathrm {d} R \over \mathrm {d} \theta }={2v^{2} \over g}\cos(2\theta )=0}

which has a nontrivial solution at2θ=π/2=90{\displaystyle 2\theta =\pi /2=90^{\circ }}, orθ=45{\displaystyle \theta =45^{\circ }}. The maximum range is thenRmax=v2/g{\displaystyle R_{\max }=v^{2}/g\,}. At this anglesin(π/2)=1{\displaystyle \sin(\pi /2)=1}, so the maximum height obtained isv24g{\displaystyle {v^{2} \over 4g}}.

To find the angle giving the maximum height for a given speed calculate the derivative of the maximum heightH=v2sin2(θ)/(2g){\displaystyle H=v^{2}\sin ^{2}(\theta )/(2g)} with respect toθ{\displaystyle \theta }, that isdHdθ=v22cos(θ)sin(θ)/(2g){\displaystyle {\mathrm {d} H \over \mathrm {d} \theta }=v^{2}2\cos(\theta )\sin(\theta )/(2g)}which is zero whenθ=π/2=90{\displaystyle \theta =\pi /2=90^{\circ }}. So the maximum heightHmax=v22g{\displaystyle H_{\mathrm {max} }={v^{2} \over 2g}} is obtained when the projectile is fired straight up.

Orbiting objects

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If instead of a uniform downwards gravitational force we consider two bodiesorbiting with the mutual gravitation between them, we obtainKepler's laws of planetary motion. The derivation of these was one of the major works ofIsaac Newton and provided much of the motivation for the development ofdifferential calculus.

Catching balls

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If a projectile, such as a baseball or cricket ball, travels in a parabolic path, with negligible air resistance, and if a player is positioned so as to catch it as it descends, he sees its angle of elevation increasing continuously throughout its flight. The tangent of the angle of elevation is proportional to the time since the ball was sent into the air, usually by being struck with a bat. Even when the ball is really descending, near the end of its flight, its angle of elevation seen by the player continues to increase. The player therefore sees it as if it were ascending vertically at constant speed. Finding the place from which the ball appears to rise steadily helps the player to position himself correctly to make the catch. If he is too close to the batsman who has hit the ball, it will appear to rise at an accelerating rate. If he is too far from the batsman, it will appear to slow rapidly, and then to descend.

For a proof of the above statement, seeTrajectory of a projectile § Catching balls.

Notes

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  1. ^It is theoretically possible for an orbit to be a radial straight line, a circle, or a parabola. These are limiting cases which have zero probability of occurring in reality.

See also

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References

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  1. ^Metha, Rohit. "11".The Principles of Physics. p. 378.

External links

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The WikibookHigh school physics has a page on the topic of:Projectile motion

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