1 Integration of vectors

If a vector depends upon time t , it is often necessary to integrate it with respect to time. Recall that i ̲ , j ̲ and k ̲ are constant vectors and must be treated thus in any integration. Hence the integral,

I ̲ = ∫ ( f ( t ) i ̲ + g ( t ) j ̲ + h ( t ) k ̲ ) d t

is evaluated as three scalar integrals i.e. I ̲ = ∫ f ( t ) d t i ̲ + ∫ g ( t ) d t j ̲ + ∫ h ( t ) d t k ̲

Example 1

If r ̲ = 3 t i ̲ + t 2 j ̲ + ( 1 + 2 t ) k ̲ , evaluate ∫ 0 1 r ̲ d t .

Solution

∫ 0 1 r ̲ d t = ∫ 0 1 3 t d t i ̲ + ∫ 0 1 t 2 d t j ̲ + ∫ 0 1 ( 1 + 2 t ) d t k ̲

= 3 t 2 2 0 1 i ̲ + t 3 3 0 1 j ̲ + t + t 2 0 1 k ̲ = 3 2 i ̲ + 1 3 j ̲ + 2 k ̲

1.1 Trajectories

To simplify the modelling of the path of a body projected from a fixed point we usually ignore any air resistance and effects due to the wind. Once this initial model is understood other variables and effects can be introduced into the model.

A particle is projected from a point O with velocity u ̲ and an angle θ above the horizontal as shown in Figure 1.

Figure 1

A graph shows a curved line, with coordinate axes labeled \(x\) and \(y\), and vectors indicating angles \(\theta\) and \(\text{u}\) originating from the origin.

Long description

The only force acting on the particle in flight is gravity acting downwards, so if m is the mass of the projectile and taking axes as shown, the force due to gravity is − m g j ̲ . Now using Newton’s second law (rate of change of momentum is equal to the applied force) we have

d ( m v ̲ ) d t = − m g j ̲

Cancelling the common factor m and integrating we have

v ̲ ( t ) = − g t j ̲ + c ̲ where c ̲ is a constant vector .

However, velocity is the rate of change of position: v ̲ ( t ) = d r ̲ d t so

d r ̲ d t = − g t j ̲ + c ̲

Integrating once more:

r ̲ ( t ) = − 1 2 g t 2 j ̲ + c ̲ t + d ̲ where d ̲ is another constant vector.

The values of these constant vectors may be determined by using the initial conditions in this problem: when t = 0 then r ̲ = 0 ̲ and v ̲ = u ̲ . Imposing these initial conditions gives

d ̲ = 0 ̲ and c ̲ = u cos θ i ̲ + u sin θ j ̲ where u is the magnitude of u ̲ . This gives

r ̲ ( t ) = u t cos θ i ̲ + ( u t sin θ − 1 2 g t 2 ) j ̲ .

The interested reader might try to show why the path of the particle is a parabola.

Exercises
  1. Given r ̲ = 3 sin t i ̲ − cos t j ̲ + ( 2 − t ) k ̲ , evaluate ∫ 0 π r ̲ d t .
  2. Given v ̲ = i ̲ − 3 j ̲ + k ̲ , evaluate:
    1. ∫ 0 1 v ̲ d t ,
    2. ∫ 0 2 v ̲ d t
  3. The vector, a ̲ , is defined by a ̲ = t 2 i ̲ + e − t j ̲ + t k ̲ . Evaluate
    1. ∫ 0 1 a ̲ d t ,
    2. ∫ 2 3 a ̲ d t ,
    3. ∫ 1 4 a ̲ d t
  4. Let a ̲ and b ̲ be two three-dimensional vectors. Is the following result true?

    ∫ t 1 t 2 a ̲ d t × ∫ t 1 t 2 b ̲ d t = ∫ t 1 t 2 a ̲ × b ̲ d t

    where × denotes the vector product.

  1. 6 i ̲ + 1.348 k ̲
    1. i ̲ − 3 j ̲ + k ̲
    2. 2 i ̲ − 6 j ̲ + 2 k ̲
    1. 0.333 i ̲ + 0.632 j ̲ + 0.5 k ̲
    2. 6.333 i ̲ + 0.0855 j ̲ + 2.5 k ̲
    3. 21 i ̲ + 0.3496 j ̲ + 7.5 k ̲
  2. No.