The problem of a charged particle moving through a localized electric field is a classic in physics, beautifully bridging the concepts of electrostatics and kinematics. It is essentially the electrostatic equivalent of a ball thrown horizontally off a cliff!
Analyzing the Setup
Imagine a charged particle, with mass m and charge q, cruising along the x-axis with a constant velocity v0
Everything is peaceful until it crosses the origin. Suddenly, it enters a region of width d where a uniform electric field E=−Ej^ is pointing straight down.
Just like gravity pulls a projectile downwards, this electric field exerts a constant downward force on our particle. Because there is no force in the horizontal direction, the horizontal velocity vx remains perfectly constant at v0.
The Parabolic Journey
Inside the electric field (
0<x≤d), the particle experiences a vertical acceleration:
ay=m−qE
Since the horizontal velocity is constant, the time it takes to cross this region is simply the distance divided by the speed:
t=v0d
By the time the particle reaches the exit boundary at
x=d, it has acquired a vertical velocity. Using the first equation of motion (
v=u+at), we find:
vy=ayt=(m−qE)(v0d)=mv0−qEd
We also need to know exactly
where it exits. Using the second equation of motion (
s=ut+21at2), the vertical displacement is:
y1=21ayt2=21(m−qE)(v0d)2=2mv02−qEd2
Breaking Free
The Straight Line
Once the particle crosses x=d, the electric field vanishes. With no forces acting on it, Newton's First Law dictates that the particle must continue in a straight line at a constant velocity.
The slope
m′ of this straight line is simply the ratio of its velocity components:
m′=vxvy=v0mv0−qEd=mv02−qEd
Now, we have a point
(d,y1) and a slope
m′. We can use the point-slope form of a straight line equation:
y−y1=m′(x−x1)
Substituting our values:
y−(2mv02−qEd2)=mv02−qEd(x−d)
Final Calculation
Let's expand and simplify this equation.
y+2mv02qEd2=mv02−qEdx+mv02qEd2
Moving the constant term to the right side:
y=mv02−qEdx+mv02qEd2−2mv02qEd2
Notice how
1−21=21. The
d2 terms combine beautifully:
y=mv02−qEdx+2mv02qEd2
Finally, factoring out the common terms, we arrive at our elegant final equation:
y=mv02qEd(2d−x)
A Brilliant Geometric Insight: If you look closely at the final equation, what happens when y=0? You get x=d/2. This means if you extend the straight-line path backwards, it intersects the x-axis at exactly half the horizontal distance. This is a universal geometric property of all such parabolic trajectories!