1.1 Lines and Planes
1.2 Polar Coordinates and
velocity and acceleration,
[not in 2004 Winter - covered in ENGR 1405]
1.3 Area, Arc Length and
Curvature
1.4 Classification of Conic
Sections (simplest cases only)
1.5 Classification of Quadric
Surfaces (simplest cases only)
1.6 The Equation and Area of a
Surface of Revolution
1.7 Hyperbolic functions and their
comparison to trigonometric functions
1.8 Integration by Parts
1.9 Leibnitz Differentiation of
an Integral
A plane is a two dimensional object.
The orientation of a plane in 3 is determined by any non-zero normal
vector n.
Knowledge of the position vector a to any
point
then fixes its position.
The general point
r•n = a•n |
---|
(which is the vector equation of the plane).
If the Cartesian components of n are (A, B, C), then the Cartesian equation of the plane is
Ax + By + Cz + D = 0 |
(where D = –a•n =
–(Axo + Byo
+ Czo) ).
Given three non-collinear points A, B, C
in a plane, more vector equations for the plane are:
where R is the general point
(x, y, z);
and the two-parameter vector form
r = a + s u
+ t v ,
where s and t are
any real numbers,
a is any one of
and u and v are any two of
.
A line is a one dimensional object.
The orientation of a line is determined by any non-zero
tangent (or direction) vector v.
Knowledge of the position vector a to
any point
The general point (x, y, z) with position vector r is also on the line if and only
if
r = a + t v , |
the vector parametric form, where t is any real number.
The symmetric Cartesian equation of the line is
(except when one or more of v1,
v2, v3 are zero),
where v1, v2,
v3 are the Cartesian components of
the tangent vector v.
The angle
between any two lines is also the angle between their direction
vectors v1, v2:
(not in 2004 Winter – covered in ENGR 1405)
If (r, )
is a pair of polar coordinates for a point not at the pole, then
so are
(r,
+ 2n
)
and
(–r,
+ (2n + 1)
).
(0, )
is at the pole for any value of
.
Conversion between polar and Cartesian:
If x < 0 and
y > 0 (2nd quadrant), then |
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A point is on a curve r = f
()
if and only if at least one member of the set
{ (r,
+ 2n
)
and
(–r,
+ (2n + 1)
) }
satisfies the equation r = f
().
The slope at any point on a curve, whose equation r = f
()
is expressed in the polar parametric form
)
cos
,
f (
)
sin
),
then the line
=
o
is a tangent to the curve at the pole.
To sketch a polar curve, divide the range of values of
into intervals
at whose endpoints one or more of the following is true:
r = 0
r becomes undefined
or
dr/d
= 0 (or becomes undefined)
Then follow the behaviour of r as
increases inside each interval.
The arc length along the curve r = f
()
from
=
to
=
is
[Be careful to take the positive square root throughout the range of integration.]
The area swept out by the radius vector is
(not in 2004 Winter – covered in ENGR 1405)
Let the unit vectors at a point in
2
in the radial and transverse directions be
respectively, so that the displacement vector of the point is
.
Also use the “over-dot” notation for differentiation
with respect to the parameter t:
.
If t represents time, then the velocity is
.
The radial component of velocity is
.
The transverse component of velocity is
.
The radial component of acceleration is
.
The transverse component of acceleration is
.
For future reference in other courses (but not required in
ENGR 2422),
in spherical polar coordinates (r,
,
) in
3:
The area A of a region in
2
bounded by the lines
If the position on the curve is expressed parametrically as
where x(ta) = a   and x(tb) = b.
When the position of a point on a curve in
3
is given as a vector function of one scalar parameter, r(t),
then the tangent vector is
The distance travelled along the curve is the arc length s .
so that the element of arc length is
If t is time, then v = ds / dt is the speed.
The length L along a curve from a point where the parameter value is t0 to a point where the parameter value is t1 is
The principal normal vector N is the rate of change of the unit tangent vector with respect to the distance travelled along the curve:
The magnitude of the principal normal vector is the curvature:
In terms of the displacement vector r(t) and denoting differentiation with respect to the parameter t by the overdot notation, another formula for the curvature is
The radius of curvature is the reciprocal of the curvature:
At any point on a curve, an orthonormal basis for
3
can be constructed, using the unit tangent, principal unit normal and
unit binormal vectors, with
.
The eccentricity e is a parameter related to
the slope of the plane relative to the cone.
e | Type | Standard equation | Location, other details |
e = 0 | circle | x2 + y2 = r2 | centre O, radius r |
0 < e < 1 | ellipse | ![]() |
centre O, vertices (±a, 0) semi-major axis a, semi-minor axis b = a ![]() foci at (±ae, 0) |
e = 1 | parabola | y2 = 4ax | vertex at O, focus at (a, 0) |
e > 1 | hyperbola | ![]() |
centre O, vertices (±a, 0), asymptotes y = ± bx / a, foci at (±ae, 0) |
e =
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rectangular hyperbola |
xy = k | centre O, axes are asymptotes |
Degenerate conic sections (the plane passes through the apex of the cone) |
|||
0 < e < 1 | point | ![]() |
at O |
e > 1 | line pair | ![]() |
through O, y = ± bx / a |
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Ellipsoid | (Axis lengths a , b , c ) |
---|---|---|
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Hyperboloid of One Sheet | (Ellipse axis lengths a , b; aligned along the z axis) |
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Hyperboloid of Two Sheets | (Ellipse axis lengths b , c; aligned along the x axis) |
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Elliptic Paraboloid | (Ellipse axis lengths a , b; aligned along the z axis) |
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Hyperbolic Paraboloid | (Hyperbola axis length a; aligned along the z axis) |
Degenerate cases:
|
|
If the curve y = f (x) is rotated once
about the line 3
generated by this revolution is
(y – c)2 + z2 = (f (x) – c)2 |
The curved surface area (excluding the circular cross-sections at
both ends) of this surface of revolution, between
Trigonometric identities | Hyperbolic function identities |
---|---|
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ex = cosh x + sinh x |
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tan x = sin x / cos x | tanh x = sinh x / cosh x |
sec x = 1 / cos x | sech x = 1 / cosh x |
csc x = 1 / sin x | csch x = 1 / sinh x |
cot x = 1 / tan x | coth x = 1 / tanh x |
cos (–x) = + cos x | cosh (–x) = + cosh x |
sin (–x) = – sin x | sinh (–x) = – sinh x |
tan (–x) = – tan x | tanh (–x) = – tanh x |
cos2x + sin2x = 1 | cosh2x – sinh2x = 1 |
sec2x = 1 + tan2x | sech2x = 1 – tanh2x |
csc2x = 1 + cot2x | csch2x = coth2x – 1 |
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cos (A+B) = cos A cos B – sin A sin B | cosh (A+B) = cosh A cosh B + sinh A sinh B |
cos 2x = cos2x –
sin2x = 2 cos2x – 1 = 1 – 2 sin2x |
cosh 2x = cosh2x +
sinh2x = 2 cosh2x – 1 = 1 + 2 sinh2x |
sin (A+B) = sin A cos B + cos A sin B | sinh (A+B) = sinh A cosh B + cosh A sinh B |
sin 2x = 2 sin x cos x | sinh 2x = 2 sinh x cosh x |
Also:
See the examples done in class and on problem sets.
Some forms that can be obtained from integration by parts:
Special cases: