What Are Field Lines? Following the Flow of a Vector Field
What Are Field Lines, Anyway?
Imagine a windy day. You toss some leaves in the air and watch how they drift. If you were to trace each leaf's path, you’d end up with field lines — curves that follow the direction of the wind at every point.
In math, we study these ideas using vector fields. A vector field is a picture of arrows drawn all over the plane that tells you the direction and speed of something—like wind, water flow, or electric force—at each point.
A field line is a path that moves with the arrows. Wherever you are on the line, the direction you’re going matches the direction of the arrow at that spot.
How Do We Find Field Lines?
To find field lines, we use this rule:
The slope of the field line must match the direction of the vector field.
In math terms, this gives us a differential equation:
dy/dx = Fy / Fx
Here:
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Fx is the x-component (horizontal part) of the vector field.
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Fy is the y-component (vertical part).
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dy/dx is the slope of the field line at any point.
Let’s look at two examples to see how this works.
Example 1: The Field F = [y, x]
Suppose our vector field is F = [y, x].
That means:
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At any point (x, y), the arrow points y units to the right and x units upward.
To find the field lines, we set up the slope:
dy/dx = x / y
This tells us that the slope of the path depends on where we are in the field.
Let’s solve this equation:
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Multiply both sides by y:
y * dy = x * dx -
Integrate both sides:
∫y dy = ∫x dx
(This gives us the area under each side of the equation.) -
Solving gives:
(1/2) * y² = (1/2) * x² + C
(We can simplify this to:)
x² - y² = constant
These curves are called hyperbolas. So if you dropped a leaf in this field, it would follow a hyperbolic path!
Example 2: A Unit Vector Field
Now let’s look at a slightly different field:
F = [y, x] divided by the square root of (x² + y²)
This field still points in the same direction as before, but every arrow is exactly the same length. That’s why we call it a unit vector field — every vector has a length of 1.
We can do the same thing to find the field lines:
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Fx = y / √(x² + y²)
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Fy = x / √(x² + y²)
So:
dy/dx = (x / √(x² + y²)) / (y / √(x² + y²)) = x / y
That’s exactly the same equation as before!
Solving it gives us the same result:
x² - y² = constant
So even though the vector field has changed, the paths of the field lines are still the same.
Wait—If the Field Changed, Why Didn’t the Lines?
Great question! The key idea is that field lines depend on direction, not speed.
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In the first field (F = [y, x]), arrows get longer the farther you are from the origin. This means the wind “blows harder” as you move out.
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In the second field (unit vector field), all arrows have the same length. The wind has a steady speed no matter where you are.
But in both cases, the direction of each arrow is the same. That’s why the field lines — the paths you’d follow if you moved with the arrows — look the same.
What Does This Teach Us?
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Field lines show direction, not speed.
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Two different vector fields can have the same field lines if they point in the same directions.
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To find a field line, we solve an equation for the slope (dy/dx) that matches the direction of the field at every point
Try It Yourself!
Draw a bunch of arrows where each arrow at (x, y) points y units right and x units up. Then try to draw curves that always follow the arrows. You’ll get hyperbolas—just like we did with the math!
You can also play with these fields using tools like Desmos or GeoGebra to visualize the arrows and the paths. It’s a great way to see the math come alive.
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