Title: Parametric, Vector and Polar Function
1Parametric, Vector and Polar Function
210.1 Parametric Functions (1)Derivative
- If f(t) and g(t) are functions of t, then the
curve given by the parametric equations x f(t)
, y g(t) can be treated as the graph of a
function of the parameter t.
310.1 Parametric Functions (2)Derivative
When a body travels in x-y plane, the parametric
equations can be used to model the bodys
motion and path.
410.1 Parametric Functions (3)Derivative
510.1 Parametric Functions (4, Example
1)Derivative
610.1 Parametric Functions (5) Derivatives d2y/dx2
710.1 Parametric Functions (6, Example 2)
Derivatives d2y/dx2
- Example 2 Find d2y/dx2 as a function t, if x t
- t2, - y t - t3
810.1 Parametric Functions (7) Length of a Smooth
Curve
x
910.1 Parametric Functions (8, Example 3) Length
of a Smooth Curve
- Example 3 Find the length of the astroid, if x
cos3 t - y sin3 t
1010.1 Parametric Functions (9, Example 4)Cycloids
1110.1 Parametric Functions (10)Cycloids
(Exploration 1-1)
1210.1 Parametric Functions (11)Cycloids
(Exploration 1-2)
1310.1 Parametric Functions (12, Example 5)Cycloids
1410.1 Parametric Functions (13)Surface Area
1510.1 Parametric Functions (14)Surface Area
1610.1 Parametric Functions (15)Surface Area
1710.1 Parametric Functions (16, Example 6)Surface
Area
1810.1 Parametric Functions (17)Surface Area
(Exercises 29)
1910.2 Vectors in the Plane (1) Component Form
- Scalar a real number to describe the quantity
of the physical terminology, such as mass,
length, density. - Vector not only a real number but also
direction to describe the quantity of the
physical terminology, such as position, velocity,
force.
2010.2 Vectors in the Plane (2) Component Form
2110.2 Vectors in the Plane (3, Example 1)
Component Form
2210.2 Vectors in the Plane (4) Component Form
- Vector form
- unit vector form v a i b j
- component form v lta, bgt
The value vx abd vy are the component of v. The
magnitude (length) of v is
2310.2 Vectors in the Plane (5, Example 2)
Component Form
2410.2 Vectors in the Plane (6) Component Form
2510.2 Vectors in the Plane (7, Example 3)
Component Form
2610.2 Vectors in the Plane (8) Component Form
2710.2 Vectors in the Plane (9) Vector Operations
2810.2 Vectors in the Plane (10, Example 4) Vector
Operations
2910.2 Vectors in the Plane (11) Vector Operations
3010.2 Vectors in the Plane (12, Theorem 1) Angle
Between Vectors
3110.2 Vectors in the Plane (13) Angle Between
Vectors
3210.2 Vectors in the Plane (14, Example 5) Angle
Between Vectors
3310.2 Vectors in the Plane (15, Example 6)
Applications
3410.2 Vectors in the Plane (16, Example 6)
Applications
3510.3 Vector-valued Functions (1) Standard Unit
Vectors
- Any vector v a i b j can be considered as a
linear - combination of two standard unit vectors
- i ?1, 0 ? and j ?0, 1 ?
- This is so called unit vector form of a vector
- v ?a, b ? ?a, 0 ? ?0, b ?
- a?1, 0 ? b?0, 1 ? a i b j
a horizontal (x) component b vertical (y)
component
3610.3 Vectors in the Plane (2, Example 1) Standard
Unit Vectors
3710.3 Vector-valued Functions (3) Planar Curves
- The component of a vector is a function (not a
real number), namely - r(t) f(t) i g(t) j
3810.3 Vector-valued Functions (4) Planar Curves
(Example 2)
3910.3 Vector-valued Functions (5) Planar Curves
- Exercise 10.3 (20) A curve function as follows
- r(t) sin t i t j, t gt 0
4010.3 Vector-valued Functions (6) Limits and
Continuity
4110.3 Vector-valued Functions (7) Limits and
Continuity (Example 3)
4210.3 Vector-valued Functions (8) Limits and
Continuity
4310.3 Vector-valued Functions (9) Limits and
Continuity (Example 4)
4410.3 Vector-valued Functions (10) Limits and
Continuity
4510.3 Vector-valued Functions (11) Derivatives
and Motion
- Suppose that r(t) f(t) i g(t) j is the
position of a particle moving along a curve in
the plane and that f(t) and g(t) are
differentiable functions of t. Then the
difference between the particles positions at
time tDt and the time t is
4610.3 Vector-valued Functions (12) Derivatives
and Motion
- As Dt approaches zero, three things seem to
happen simultaneously. - Q approaches P along the curve.
- The secant line PQ seems to approach a limiting
position tangent to the curve at P. - The quotient Dr(t)/Dt approaches the limit
4710.3 Vector-valued Functions (13) Derivatives
and Motion
4810.3 Vector-valued Functions (14) Derivatives
and Motion
- If dr/dt is continuous and never 0 for both
component, the curve traced by r is smooth, there
are no sharp corners or cusps. - The vector dr/dt when different from 0, is also a
vector tangent to the curve. The tangent line to
the curve at a point P (f(a), g(a)) is defined
be the line through P parallel to dr/dt at t a.
4910.3 Vector-valued Functions (15) Derivatives
and Motion
5010.3 Vector-valued Functions (16) Derivatives
and Motion (Example 5-a,b)
5110.3 Vector-valued Functions (17) Derivatives
and Motion (Example 5-c)
5210.3 Vector-valued Functions (18) Derivatives
and Motion (Example 6-a)
5310.3 Vector-valued Functions (19) Derivatives
and Motion (Example 6-b )
5410.3 Vector-valued Functions (20)
Differentiation Rules
5510.3 Vector-valued Functions (21)
Differentiation Rules
5610.3 Vector-valued Functions (22) Integrals
5710.3 Vector-valued Functions (23) Integrals
(Example 7)
5810.3 Vector-valued Functions (24) Integrals
5910.3 Vector-valued Functions (25) Integrals
(Example 8)
6010.3 Vector-valued Functions (26) Integrals
(Example 9-a)
6110.3 Vector-valued Functions (26) Integrals
(Example 9-a)
6210.3 Vector-valued Functions (26) Integrals
(Example 9-b)
6310.4 Modeling Projection Motion (1)Ideal
Projection Motion
- A particle moving in a vertical plane
- Only gravity force acts on the particle
6410.4 Modeling Projection Motion (2)Ideal
Projection Motion
- Assumption
- The projectile is launched from the original at
time t 0, with an initial velocity vo which
make an angle with the horizontal.
6510.4 Modeling Projection Motion (3)Ideal
Projection Motion
- Equation of motion
- Newtons second law of motion the force acting
on the projectile is equal to the projectiles
mass times its acceleration
- Question
- Can we know the motion status e.g. position,
velocity, acceleration etc.
6610.4 Modeling Projection Motion (4)Ideal
Projection Motion
This is ideal projectile motion with vector
equation. a launch angle, vo initial speed.
6710.4 Modeling Projection Motion (5)Ideal
Projection Motion
The vector equation also can be expressed as
parameter equations
6810.4 Modeling Projection Motion (5)Ideal
Projection Motion (Example 1)
6910.4 Modeling Projection Motion (7) Height,
Flight time, and Range
What is so called Flight time ?
7010.4 Modeling Projection Motion (8) Height,
Flight time, and Range
7110.4 Modeling Projection Motion (9) Height,
Flight time, and Range
72Modeling Projection Motion (10, Example2)
7310.4 Modeling Projection Motion (11) Ideal
Trajectories Are Parabolic
7410.4 Modeling Projection Motion (12) Ideal
Trajectories Are Parabolic (Example 3)
7510.4 Modeling Projection Motion (13) Ideal
Trajectories Are Parabolic (Example 3-a)
?
ymax 74 ft
y
vo
a
6 ft
90 ft
x
7610.4 Modeling Projection Motion (14) Ideal
Trajectories Are Parabolic (Example 3-b)
7710.4 Modeling Projection Motion (15) Ideal
Trajectories Are Parabolic (Example 3-c)
7810.4 Modeling Projection Motion (16) Ideal
Trajectories Are Parabolic (Example 3-d)
7910.4 Modeling Projection Motion (17) Projectile
Motion with Wind Gusts (Example 4-a)
8010.4 Modeling Projection Motion (18) Projectile
Motion with Wind Gusts (Example 4-a)
8110.4 Modeling Projection Motion (19) Projectile
Motion with Wind Gusts (Example 4-b)
8210.4 Modeling Projection Motion (20) Projectile
Motion with Wind Gusts (Example 4-c)
8310.4 Modeling Projection Motion (21) Projectile
Motion with Wind Gusts (Exploration 1-1)
8410.4 Modeling Projection Motion (22) Projectile
Motion with Wind Gusts (Exploration 1-2)
y
vo152
8.8
a
3 ft
x
400 ft
8510.4 Modeling Projection Motion (23) Projectile
Motion with Wind Gusts (Exploration 1-3)
y
vo152
15 ft
3 ft
x
400 ft
8610.4 Modeling Projection Motion (24)Projectile
Motion with Air Resistance
- Drag Force
- Drag force is one of the most popular external
force acting to the projectile. - Drag force acts in a direction opposite to the
velocity of the projectile. - Low velocity, the drag force is proportional to
the speed which is called linear. - High speed, the drag force is proportional to
different powers of the speed over different
velocity ranges.
8710.4 Modeling Projection Motion (25)Projectile
Motion with Air Resistance
8810.4 Modeling Projection Motion (26)Projectile
Motion with Air Resistance
8910.4 Modeling Projection Motion (26)Projectile
Motion with Air Resistance
9010.4 Modeling Projection Motion (27)Projectile
Motion with Air Resistance
9110.4 Modeling Projection Motion (28)Projectile
Motion with Air Resistance
9210.4 Modeling Projection Motion (29)Projectile
Motion with Air Resistance (Exploration 2-1)
9310.4 Modeling Projection Motion (30)Projectile
Motion with Air Resistance (Exploration 2-1)
9410.4 Modeling Projection Motion (31)Projectile
Motion with Air Resistance (Exploration 2-2)
9510.4 Modeling Projection Motion (32)Projectile
Motion with Air Resistance (Exploration 2-3)
9610.5 Polar Coordinates and Polar Graphs (1)
Polar Coordinates
9710.5 Polar Coordinates and Polar Graphs (2)
Polar Coordinates (Example 1)
9810.5 Polar Coordinates and Polar Graphs (3)
Polar Graphing
9910.5 Polar Coordinates and Polar Graphs (4)
Polar Graphing (Example 2)
10010.5 Polar Coordinates and Polar Graphs (5)
Polar Graphing (Example 3)
10110.5 Polar Coordinates and Polar Graphs (6)
Polar Graphing
10210.5 Polar Coordinates and Polar Graphs (7)
Polar Graphing (Exploration 1)
10310.5 Polar Coordinates and Polar Graphs (8)
Relating Polar and Cartesian Coordinates
10410.5 Polar Coordinates and Polar Graphs (9)
Relating Polar and Cartesian Coordinates (Example
4)
10510.5 Polar Coordinates and Polar Graphs (10)
Relating Polar and Cartesian Coordinates (Example
5)
What is the graph for r 0
10610.5 Polar Coordinates and Polar Graphs (11)
Relating Polar and Cartesian Coordinates (Example
6)
10710.5 Polar Coordinates and Polar Graphs (12)
Relating Polar and Cartesian Coordinates (Exp. 2)
10810.6 Calculus of Polar Curve (1)Slope
- A function y f(x), one may find its derivative
by dy/dx - Any Cartesian function is equivalent to polar
system. - How to find the slope in term of polar coordinate
?
dy/dx
y
Function y f(x)
Function r f (q)
x
10910.6 Calculus of Polar Curve (2)Slope
- Since in polar coordinate r f(q)
- One expresses x r cosq f(q)cos(q)
11010.6 Calculus of Polar Curve (3)Slope
horizontal tangent
y
vertical tangent
x
11110.6 Calculus of Polar Curve (4)Slope (Example
1-a)
11210.6 Calculus of Polar Curve (5)Slope (Example
1-b)
11310.6 Calculus of Polar Curve (6)Slope (Example 1)
11410.6 Calculus of Polar Curve (7)Slope (Example 2)
11510.6 Calculus of Polar Curve (8)Slope (Example 2)
11610.6 Calculus of Polar Curve (9)Area in the Plane
- The region OTS is bounded by the rays q a and
q b and curve r f(q).
O
11710.6 Calculus of Polar Curve (10)Area in the
Plane
O
x
11810.6 Calculus of Polar Curve (11)Area in the
Plane (Example 3)
11910.6 Calculus of Polar Curve (12)Area in the
Plane (Example 4)
12010.6 Calculus of Polar Curve (13)Area in the
Plane
12110.6 Calculus of Polar Curve (14)Area in the
Plane (Example 5)
12210.6 Calculus of Polar Curve (15) Length of a
Curve
12310.6 Calculus of Polar Curve (16) Length of a
Curve (Example 6)
12410.6 Calculus of Polar Curve (17)Area of a
Surface of Revolution
12510.6 Calculus of Polar Curve (18)Area of a
Surface of Revolution
12610.6 Calculus of Polar Curve (19)Area of a
Surface of Revolution (Example 7)