15.6
A line integral measures how a vector field contributes along a curve from one point to another.
The Fundamental Theorem for Line Integrals applies when the vector field comes from a potential function.
In other words, the vector field F is the gradient of a potential function g of two or three variables.
The theorem states that, for such a field, the line integral along a smooth curve depends only on the values of the potential function at the endpoints.
So, if two different smooth curves, C_1 and C_2, connect the same two points, the line integral is the same on both curves.
As a result, the line integral becomes path-independent, simplifying complex calculations.
In physics, this theorem applies to conservative force fields such as gravity. When an object moves through such a field, the work done by gravity equals the line integral of the gravitational force along its path. Because gravitational force equals the negative gradient of a potential energy function, the work depends only on the initial and final positions.
For example, whether a ball falls straight down or follows a curved path, the work done is the same.
A line integral describes the accumulated contribution of a vector field along a curve connecting two points. It is used to evaluate how the direction and magnitude of a vector field interact with the direction of motion along a path. In certain cases, this calculation can be greatly simplified by identifying whether the vector field is associated with a potential function.
Let F be a vector field in two or three dimensions. If there exists a scalar function g such that
\begin{equation*}\mathbf{F} = \nabla g\end{equation*}
Then F is called a gradient field, and g is called a potential function. The gradient vector points in the direction of the greatest increase of the potential function and gives the rate of that increase.
Fundamental Theorem for Line Integrals
For a smooth curve C beginning at point A and ending at point B, the Fundamental Theorem for Line Integrals states that
\begin{equation*}\int_C \mathbf{F} \cdot d\mathbf{r} = g(B) - g(A)\end{equation*}
This means that the line integral of a gradient field can be evaluated using only the values of the potential function at the endpoints of the curve.
Path Independence
An important consequence of the theorem is path independence. If two smooth curves, C1 and C2, connect the same points A and B, then
\begin{equation*}\int_{C_1} \mathbf{F} \cdot d\mathbf{r} =\int_{C_2} \mathbf{F} \cdot d\mathbf{r}\end{equation*}
So, the integral does not depend on the shape, length, or direction changes of the path, but only on the starting and ending locations.
A line integral measures how a vector field contributes along a curve from one point to another.
The Fundamental Theorem for Line Integrals applies when the vector field comes from a potential function.
In other words, the vector field F is the gradient of a potential function g of two or three variables.
The theorem states that, for such a field, the line integral along a smooth curve depends only on the values of the potential function at the endpoints.
So, if two different smooth curves, C_1 and C_2, connect the same two points, the line integral is the same on both curves.
As a result, the line integral becomes path-independent, simplifying complex calculations.
In physics, this theorem applies to conservative force fields such as gravity. When an object moves through such a field, the work done by gravity equals the line integral of the gravitational force along its path. Because gravitational force equals the negative gradient of a potential energy function, the work depends only on the initial and final positions.
For example, whether a ball falls straight down or follows a curved path, the work done is the same.
From Chapter 15:
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