Vector Line Integrals
The second type of line integrals are vector line integrals. Vector line integrals allow us to integrate along a curve through a vector field. Consider a continuous vector field in [latex]{\mathbb{R}}^{3}[/latex]:
[latex]{\textbf{F}}(x,y,z) = P(x,y,z){\textbf{i}} + Q(x,y,z){\textbf{j}} + R(x,y,z){\textbf{k}}[/latex]
Suppose [latex]{\textbf{F}}[/latex] represents a force on a particle, and [latex]C[/latex] is a smooth curve in [latex]{\mathbb{R}}^{3}[/latex] contained in the domain of [latex]{\textbf{F}}[/latex]. How do we compute the work done by [latex]{\textbf{F}}[/latex] in moving a particle along [latex]C[/latex]?
To answer this question, first note that a particle can travel in two directions along a curve: forward or backward. The work done by the vector field depends on which direction the particle moves. We must specify a direction along curve [latex]C[/latex], called an orientation.
The specified direction is the positive direction along [latex]C[/latex], and the opposite direction is the negative direction. When [latex]C[/latex] has been given an orientation, we call it an oriented curve (Figure 1). The work done on the particle depends on the direction along the curve in which the particle is moving.
Defining the Vector Line Integral
Let [latex]{\textbf{r}}(t)[/latex] be a parameterization of [latex]C[/latex] for [latex]a \leq t \leq b[/latex] such that the curve is traversed exactly once and the particle moves in the positive direction along [latex]C[/latex]. We’ll build up the work calculation step by step.
Divide the parameter interval [latex][a,b][/latex] into [latex]n[/latex] subintervals [latex][t_{i-1}, t_i][/latex], [latex]0 \leq i \leq n[/latex], of equal width. Denote the endpoints [latex]{\textbf{r}}(t_0), {\textbf{r}}(t_1), \ldots, {\textbf{r}}(t_n)[/latex] by [latex]P_0, \ldots, P_n[/latex]. These points divide [latex]C[/latex] into [latex]n[/latex] pieces.
Let [latex]{\Delta}s_i[/latex] denote the length of the piece from [latex]P_{i-1}[/latex] to [latex]P_i[/latex]. For each [latex]i[/latex], choose a value [latex]{t}^{*}_{i}[/latex] in the subinterval [latex][{{t}_{{i} - {1}}}, {t}_{i}][/latex]. The endpoint of [latex]{\textbf{r}}{({t}^{*}_{i})}[/latex] is a point in the piece of [latex]C[/latex] between [latex]{P}_{{i} - {1}}[/latex] and [latex]{P}_{i}[/latex] (Figure 2).
If [latex]{\Delta}s_i[/latex] is small, then as the particle moves from [latex]P_{i-1}[/latex] to [latex]P_i[/latex] along [latex]C[/latex], it moves approximately in the direction of [latex]{\textbf{T}}(P_i)[/latex], the unit tangent vector at the endpoint of [latex]{\textbf{r}}{({t}^{*}_{i})}[/latex]. Let [latex]{P}^{*}_{i}[/latex] denote the endpoint of [latex]{\textbf{r}}{({t}^{*}_{i})}[/latex].
The work done by the force vector field in moving the particle from [latex]P_{i-1}[/latex] to [latex]P_i[/latex] is [latex]{\textbf{F}}{({P}^{*}_{i})} \cdot {({\Delta}{{s}_{i}}{\textbf{T}}{({P}^{*}_{i})})}[/latex]. Therefore, the total work done along [latex]C[/latex] is:
[latex]{\displaystyle\sum^{n}_{i = 1}} \ {\textbf{F}}{({P}^{*}_{i})} \cdot ({{\Delta}{s}_{i}}{\textbf{T}}{({P}^{*}_{i})}) = {\displaystyle\sum^{n}_{i = 1}} \ {\textbf{F}}{({P}^{*}_{i})} \cdot {\textbf{T}}{({P}^{*}_{i})}{{\Delta}{s}_{i}}[/latex].
Letting the arc length of the pieces of [latex]C[/latex] get arbitrarily small by taking a limit as [latex]n \to \infty[/latex] gives us the work done by the field in moving the particle along [latex]C[/latex]. The work done by [latex]{\textbf{F}}[/latex] in moving the particle in the positive direction along [latex]C[/latex] is:
[latex]W = \displaystyle\int_{C}{\textbf{F}} \cdot {\textbf{T}} ds[/latex]
This integral is called a vector line integral.
vector line integral
The vector line integral of vector field [latex]{\textbf{F}}[/latex] along oriented smooth curve [latex]C[/latex] is:
[latex]{\displaystyle\int_{C}}{\textbf{F}} \cdot {\textbf{T}}{ds} = {\displaystyle\lim_{{n}{\rightarrow}{\infty}}}{\displaystyle\sum^{n}_{i = 1}} \ {\textbf{F}}{({P}^{*}_{i})} \cdot {\textbf{T}}{({P}^{*}_{i})}{{\Delta}{s}_{i}}[/latex]
if that limit exists.
With scalar line integrals, neither the orientation nor the parameterization of the curve matters. As long as the curve is traversed exactly once, the value of the line integral is unchanged.
With vector line integrals, orientation is critical. If you hike up a mountain, the gravitational force of Earth does negative work on you. If you walk down the mountain by the exact same path, Earth’s gravitational force does positive work on you. Reversing the path changes the work value from negative to positive.
If [latex]C[/latex] is an oriented curve, then [latex]-C[/latex] represents the same curve but with opposite orientation.
Computing Vector Line Integrals with Parameterization
As with scalar line integrals, it’s easier to compute a vector line integral using the parameterization function [latex]{\textbf{r}}[/latex] and the variable [latex]t[/latex].
To translate the integral [latex]\displaystyle\int_{C}{\textbf{F}} \cdot {\textbf{T}} ds[/latex] in terms of [latex]t[/latex], recall that the unit tangent vector [latex]{\textbf{T}}[/latex] along [latex]C[/latex] is:
[latex]{\textbf{T}} = \frac{{\textbf{r}}'(t)}{\left | {\textbf{r}}'(t) \right |}[/latex]
(assuming [latex]\left | {\textbf{r}}'(t) \right | \neq 0[/latex])
Since [latex]ds = \left | {\textbf{r}}'(t) \right | dt[/latex], as we saw when discussing scalar line integrals, we have:
[latex]{\textbf{F}} \cdot {\textbf{T}} ds = {\textbf{F}}({\textbf{r}}(t)) \cdot \frac{{\textbf{r}}'(t)}{\left | {\textbf{r}}'(t) \right |}\left | {\textbf{r}}'(t) \right | dt = {\textbf{F}}({\textbf{r}}(t)) \cdot {\textbf{r}}'(t) dt[/latex]
This gives us a practical formula for computing vector line integrals.
computing vector line integrals
[latex]\displaystyle\int_{C}{\textbf{F}} \cdot {\textbf{T}} ds = \displaystyle\int^{b}_{a}{\textbf{F}}({\textbf{r}}(t)) \cdot {\textbf{r}}'(t) dt[/latex]
We often use the notation [latex]\displaystyle\int_{C}{\textbf{F}} \cdot d{\textbf{r}}[/latex] for the line integral [latex]\displaystyle\int_{C}{\textbf{F}} \cdot {\textbf{T}} ds[/latex].
[latex]\\[/latex]
If [latex]{\textbf{r}} = \langle x(t), y(t), z(t) \rangle[/latex], then [latex]d{\textbf{r}}[/latex] denotes the vector differential [latex]\langle x'(t), y'(t), z'(t) \rangle dt[/latex].
The previous examples illustrate an important property:
[latex]\displaystyle\int_{-C}{\textbf{F}} \cdot d{\textbf{r}} = -\displaystyle\int_{C}{\textbf{F}} \cdot d{\textbf{r}}[/latex]
Reversing the orientation of a curve changes the sign of a line integral. This makes physical sense when thinking about work—if you reverse direction, the work done changes sign.
Alternative Notation
Another standard notation for integral [latex]\displaystyle\int_{C}{\textbf{F}} \cdot d{\textbf{r}}[/latex] is [latex]\displaystyle\int_{C}P dx + Q dy + R dz[/latex]. In this notation, [latex]P[/latex], [latex]Q[/latex], and [latex]R[/latex] are functions, and we think of [latex]d{\textbf{r}}[/latex] as vector [latex]\langle dx, dy, dz \rangle[/latex].
To justify this convention, recall that [latex]d{\textbf{r}} = {\textbf{T}} ds = {\textbf{r}}'(t) dt = \left \langle \dfrac{dx}{dt}, \dfrac{dy}{dt}, \dfrac{dz}{dt} \right \rangle dt[/latex]. Therefore:
[latex]{\textbf{F}} \cdot d{\textbf{r}} = \langle P, Q, R \rangle \cdot \langle dx, dy, dz \rangle = P dx + Q dy + R dz[/latex]
If [latex]d{\textbf{r}} = \langle dx, dy, dz \rangle[/latex], then [latex]\dfrac{d{\textbf{r}}}{dt} = \left \langle \dfrac{dx}{dt}, \dfrac{dy}{dt}, \dfrac{dz}{dt} \right \rangle[/latex], which implies that [latex]d{\textbf{r}} = \left \langle \dfrac{dx}{dt}, \dfrac{dy}{dt}, \dfrac{dz}{dt} \right \rangle dt[/latex]. Therefore:
[latex]\begin{aligned} {\displaystyle\int_{C}}{\textbf{F}} \cdot {d}{\textbf{r}} & = {\displaystyle\int_{C}}{Pdx} + {Qdy} + {Rdz} \\ & = {\displaystyle\int}{\left ( {P}{({\textbf{r}}{(t)})}{\frac{dx}{dt}} + {Q}{({\textbf{r}}{(t)})}{\frac{dy}{dt}} + {R}{({\textbf{r}}{(t)})}{\frac{dz}{dt}} \right )}{dt}. \end{aligned}[/latex]
Piecewise Smooth Curves
We have learned how to integrate smooth oriented curves. Now suppose that [latex]C[/latex] is an oriented curve that is not smooth, but can be written as the union of finitely many smooth curves. In this case, we say that [latex]C[/latex] is a piecewise smooth curve.
To be precise, curve [latex]C[/latex] is piecewise smooth if [latex]C[/latex] can be written as a union of [latex]n[/latex] smooth curves [latex]C_{1}, C_{2}, \ldots, C_{n}[/latex] such that the endpoint of [latex]C_i[/latex] is the starting point of [latex]C_{i+1}[/latex] (Figure 4). When curves [latex]C_i[/latex] satisfy this condition, we write their union as [latex]C_{1} + C_{2} + \cdots + C_{n}[/latex].
The next theorem summarizes several key properties of vector line integrals.
theorem: properties of vector line integrals
Let [latex]{\textbf{F}}[/latex] and [latex]{\textbf{G}}[/latex] be continuous vector fields with domains that include the oriented smooth curve [latex]C[/latex]. Then:
- [latex]{\displaystyle\int_{C}}{({\textbf{F}} + {\textbf{G}})} \cdot {d}{\textbf{r}} = {\displaystyle\int_{C}}{\textbf{F}} \cdot {d}{\textbf{r}} + {\displaystyle\int_{C}}{\textbf{G}} \cdot {dr}[/latex]
- [latex]{\displaystyle\int_{C}}{k}{\textbf{F}} \cdot {d}{\textbf{r}} = {k}{\displaystyle\int_{C}}{\textbf{F}} \cdot {d}{\textbf{r}}[/latex], where [latex]k[/latex] is a constant
- [latex]{\displaystyle\int_{-C}}{\textbf{F}} \cdot {d}{\textbf{r}} = -{\displaystyle\int_{C}}{\textbf{F}} \cdot {d}{\textbf{r}}[/latex]
- Suppose instead that [latex]C[/latex] is a piecewise smooth curve in the domains of F and G, where [latex]{C} = {C_1} + {C_2} + ... + {C_n}[/latex] and [latex]{C_1}, {C_2}, ..., {C_n}[/latex]are smooth curves such that the endpoint of [latex]C_i[/latex] is the starting point of [latex]{C}_{{i} + {1}}[/latex]. Then:
[latex]{\displaystyle\int_{C}}{\textbf{F}} \cdot {d}{\textbf{s}} = {\displaystyle\int_{C_1}}{\textbf{F}} \cdot {d}{\textbf{s}} + {\displaystyle\int_{C_2}}{\textbf{F}} \cdot {d}{\textbf{s}} + ... + {\displaystyle\int_{C_n}}{\textbf{F}} \cdot {d}{\textbf{s}}[/latex]
Understanding the Properties
Notice the similarities between these properties and the properties of single-variable integrals.
Properties 1 and 2 say that line integrals are linear, which is true of single-variable integrals as well. Property 3 says that reversing the orientation of a curve changes the sign of the integral. If we think of the integral as computing the work done on a particle traveling along [latex]C[/latex], then this makes sense—if the particle moves backward rather than forward, the value of the work done has the opposite sign. This is analogous to the equation [latex]{\displaystyle\int^{b}_{a}}{f}{(x)}{dx} = {-}{\displaystyle\int^{a}_{b}}{f}{(x)}{dx}[/latex].
Finally, if [latex][a_1, a_2][/latex], [latex][a_2, a_3][/latex], [latex]\ldots[/latex], [latex][a_{n-1}, a_n][/latex] are intervals, then:
[latex]{\displaystyle\int^{a_n}_{a_1}}{f}{(x)}{dx} = {\displaystyle\int^{a_2}_{a_1}}{f}{(x)}{dx} + {\displaystyle\int^{a_3}_{a_1}}{f}{(x)}{dx} + ... + {\displaystyle\int^{a_n}_{a_{n-1}}}{f}{(x)}{dx},[/latex]
This is analogous to property 4.