quadric surfaces, partial derivatives. sections 12.6 and ...nirobles/files241/lecture07.pdfpartial...
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Math 241: Multivariable calculus, Lecture 7Quadric Surfaces, Partial derivatives.
Sections 12.6 and 14.2, 14.3
go.illinois.edu/math241fa17
Wednesday, September 13th, 2017
go.illinois.edu/math241fa17.
Quadric Surfaces.
Definition
A Quadric Surface is the collection of points (x , y , z) that satisfy asecond degree equation:
Ax2 + By2 + Cz2 + Dxy + Eyz + Fxz + Gx + Hy + Iz + J = 0
Looks complicated!
However we can shift and rotate our surfaceand then it becomes simpler: it can always be written as
Ax2 + By2 + Cz2 + J = 0, or as Ax2 + By2 + Iz = 0
(Different A,B,C , I , J!). The type of surface you get depends onthe signs of A,B,C , . . . .
go.illinois.edu/math241fa17.
Quadric Surfaces.
Definition
A Quadric Surface is the collection of points (x , y , z) that satisfy asecond degree equation:
Ax2 + By2 + Cz2 + Dxy + Eyz + Fxz + Gx + Hy + Iz + J = 0
Looks complicated!
However we can shift and rotate our surfaceand then it becomes simpler: it can always be written as
Ax2 + By2 + Cz2 + J = 0, or as Ax2 + By2 + Iz = 0
(Different A,B,C , I , J!). The type of surface you get depends onthe signs of A,B,C , . . . .
go.illinois.edu/math241fa17.
Quadric Surfaces.
Definition
A Quadric Surface is the collection of points (x , y , z) that satisfy asecond degree equation:
Ax2 + By2 + Cz2 + Dxy + Eyz + Fxz + Gx + Hy + Iz + J = 0
Looks complicated! However we can shift and rotate our surfaceand then it becomes simpler:
it can always be written as
Ax2 + By2 + Cz2 + J = 0, or as Ax2 + By2 + Iz = 0
(Different A,B,C , I , J!). The type of surface you get depends onthe signs of A,B,C , . . . .
go.illinois.edu/math241fa17.
Quadric Surfaces.
Definition
A Quadric Surface is the collection of points (x , y , z) that satisfy asecond degree equation:
Ax2 + By2 + Cz2 + Dxy + Eyz + Fxz + Gx + Hy + Iz + J = 0
Looks complicated! However we can shift and rotate our surfaceand then it becomes simpler: it can always be written as
Ax2 + By2 + Cz2 + J = 0, or as Ax2 + By2 + Iz = 0
(Different A,B,C , I , J!).
The type of surface you get depends onthe signs of A,B,C , . . . .
go.illinois.edu/math241fa17.
Quadric Surfaces.
Definition
A Quadric Surface is the collection of points (x , y , z) that satisfy asecond degree equation:
Ax2 + By2 + Cz2 + Dxy + Eyz + Fxz + Gx + Hy + Iz + J = 0
Looks complicated! However we can shift and rotate our surfaceand then it becomes simpler: it can always be written as
Ax2 + By2 + Cz2 + J = 0, or as Ax2 + By2 + Iz = 0
(Different A,B,C , I , J!). The type of surface you get depends onthe signs of A,B,C , . . . .
go.illinois.edu/math241fa17.
Coordinate Transform
Example 0.1
Consider the equation
x2 + y2 + z2 − 2x = 3
Simplify equation by shifting coordinates
Note that we can complete the square:x2 − 2x = x2 − 2x + 1− 1 = (x − 1)2 − 1. Using this in theequation we see that it is equivalent to
(x − 1)2 + y2 + z2 − 1 = 3, or (x − 1)2 + y2 + z2 = 4
so we have a sphere with radius 2. After shifting the x-axis byx 7→ x + 1 we get a standard equation
x2 + y2 + z2 = 4.
go.illinois.edu/math241fa17.
Coordinate Transform
Example 0.1
Consider the equation
x2 + y2 + z2 − 2x = 3
Simplify equation by shifting coordinates
Note that we can complete the square:x2 − 2x = x2 − 2x + 1− 1 = (x − 1)2 − 1. Using this in theequation we see that it is equivalent to
(x − 1)2 + y2 + z2 − 1 = 3, or (x − 1)2 + y2 + z2 = 4
so we have a sphere with radius 2. After shifting the x-axis byx 7→ x + 1 we get a standard equation
x2 + y2 + z2 = 4.
go.illinois.edu/math241fa17.
Coordinate Transform
Example 0.1
Consider the equation
x2 + y2 + z2 − 2x = 3
Simplify equation by shifting coordinates
Note that we can complete the square:x2 − 2x = x2 − 2x + 1− 1 = (x − 1)2 − 1.
Using this in theequation we see that it is equivalent to
(x − 1)2 + y2 + z2 − 1 = 3, or (x − 1)2 + y2 + z2 = 4
so we have a sphere with radius 2. After shifting the x-axis byx 7→ x + 1 we get a standard equation
x2 + y2 + z2 = 4.
go.illinois.edu/math241fa17.
Coordinate Transform
Example 0.1
Consider the equation
x2 + y2 + z2 − 2x = 3
Simplify equation by shifting coordinates
Note that we can complete the square:x2 − 2x = x2 − 2x + 1− 1 = (x − 1)2 − 1. Using this in theequation we see that it is equivalent to
(x − 1)2 + y2 + z2 − 1 = 3,
or (x − 1)2 + y2 + z2 = 4
so we have a sphere with radius 2. After shifting the x-axis byx 7→ x + 1 we get a standard equation
x2 + y2 + z2 = 4.
go.illinois.edu/math241fa17.
Coordinate Transform
Example 0.1
Consider the equation
x2 + y2 + z2 − 2x = 3
Simplify equation by shifting coordinates
Note that we can complete the square:x2 − 2x = x2 − 2x + 1− 1 = (x − 1)2 − 1. Using this in theequation we see that it is equivalent to
(x − 1)2 + y2 + z2 − 1 = 3, or (x − 1)2 + y2 + z2 = 4
so we have a sphere with radius 2. After shifting the x-axis byx 7→ x + 1 we get a standard equation
x2 + y2 + z2 = 4.
go.illinois.edu/math241fa17.
Coordinate Transform
Example 0.1
Consider the equation
x2 + y2 + z2 − 2x = 3
Simplify equation by shifting coordinates
Note that we can complete the square:x2 − 2x = x2 − 2x + 1− 1 = (x − 1)2 − 1. Using this in theequation we see that it is equivalent to
(x − 1)2 + y2 + z2 − 1 = 3, or (x − 1)2 + y2 + z2 = 4
so we have a sphere with radius 2. After shifting the x-axis byx 7→ x + 1 we get a standard equation
x2 + y2 + z2 = 4.
go.illinois.edu/math241fa17.
Coordinate Transform
Example 0.1
Consider the equation
x2 + y2 + z2 − 2x = 3
Simplify equation by shifting coordinates
Note that we can complete the square:x2 − 2x = x2 − 2x + 1− 1 = (x − 1)2 − 1. Using this in theequation we see that it is equivalent to
(x − 1)2 + y2 + z2 − 1 = 3, or (x − 1)2 + y2 + z2 = 4
so we have a sphere with radius 2. After shifting the x-axis byx 7→ x + 1 we get a standard equation
x2 + y2 + z2 = 4.
go.illinois.edu/math241fa17.
Coordinate Transform
Example 0.1
Consider the equation
x2 + y2 + z2 − 2x = 3
Simplify equation by shifting coordinates
Note that we can complete the square:x2 − 2x = x2 − 2x + 1− 1 = (x − 1)2 − 1. Using this in theequation we see that it is equivalent to
(x − 1)2 + y2 + z2 − 1 = 3, or (x − 1)2 + y2 + z2 = 4
so we have a sphere with radius 2. After shifting the x-axis byx 7→ x + 1 we get a standard equation
x2 + y2 + z2 = 4.
go.illinois.edu/math241fa17.
Example 0.2
Sketch the graph of x2
9 + y2 + z2
9 = 1.
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Example 0.2
Sketch the graph of x2
9 + y2 + z2
9 = 1.
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go.illinois.edu/math241fa17.
Example 0.2
Sketch the graph of x2
9 + y2 + z2
9 = 1.
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go.illinois.edu/math241fa17.
Example 0.3
Sketch the graph of x2 − y2 + z2 = 1.
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Example 0.3
Sketch the graph of x2 − y2 + z2 = 1.
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Example 0.3
Sketch the graph of x2 − y2 + z2 = 1.
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go.illinois.edu/math241fa17.
Example 0.4
Sketch the graph of x2 + y2 − z = 0.
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Example 0.4
Sketch the graph of x2 + y2 − z = 0.
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go.illinois.edu/math241fa17.
Example 0.4
Sketch the graph of x2 + y2 − z = 0.
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go.illinois.edu/math241fa17.
partial derivatives
• fx(a, b) = ∂f (x ,y)∂x |(x ,y)=(a,b) = limh→0
f (a+h,b)−f (a,b)h . Same for
fy (a, b).
• Easy to calculate: the partial fx is just the ordinary derivativeof f (x , y), where y is considered a constant.
• In the same way we can define second partialsfxx , fyy , fxy = fyx , for nice functions.
• In the same way we can define partials of functions of 3 ormore variables.
go.illinois.edu/math241fa17.
partial derivatives
• fx(a, b) = ∂f (x ,y)∂x |(x ,y)=(a,b) = limh→0
f (a+h,b)−f (a,b)h . Same for
fy (a, b).
• Easy to calculate: the partial fx is just the ordinary derivativeof f (x , y), where y is considered a constant.
• In the same way we can define second partialsfxx , fyy , fxy = fyx , for nice functions.
• In the same way we can define partials of functions of 3 ormore variables.
go.illinois.edu/math241fa17.
partial derivatives
• fx(a, b) = ∂f (x ,y)∂x |(x ,y)=(a,b) = limh→0
f (a+h,b)−f (a,b)h . Same for
fy (a, b).
• Easy to calculate: the partial fx is just the ordinary derivativeof f (x , y), where y is considered a constant.
• In the same way we can define second partialsfxx , fyy , fxy = fyx , for nice functions.
• In the same way we can define partials of functions of 3 ormore variables.
go.illinois.edu/math241fa17.
partial derivatives
• fx(a, b) = ∂f (x ,y)∂x |(x ,y)=(a,b) = limh→0
f (a+h,b)−f (a,b)h . Same for
fy (a, b).
• Easy to calculate: the partial fx is just the ordinary derivativeof f (x , y), where y is considered a constant.
• In the same way we can define second partialsfxx , fyy , fxy = fyx , for nice functions.
• In the same way we can define partials of functions of 3 ormore variables.
go.illinois.edu/math241fa17.
partial derivatives
• fx(a, b) = ∂f (x ,y)∂x |(x ,y)=(a,b) = limh→0
f (a+h,b)−f (a,b)h . Same for
fy (a, b).
• Easy to calculate: the partial fx is just the ordinary derivativeof f (x , y), where y is considered a constant.
• In the same way we can define second partialsfxx , fyy , fxy = fyx , for nice functions.
• In the same way we can define partials of functions of 3 ormore variables.
go.illinois.edu/math241fa17.
Math 241: Problem of the day
Level curves for a function f : R2 → R are shown.
• What is f (2, 0)?• What is fx(2, 0)?• What is fx(2, ε), ε > 0?• Decide whether fxy (2, 0) is positive, negative or zero.
f=−2
21
f=4
f=3
f=2
f=1
f=0
f=−1
go.illinois.edu/math241fa17.
Math 241: Problem of the day
Level curves for a function f : R2 → R are shown.• What is f (2, 0)?
• What is fx(2, 0)?• What is fx(2, ε), ε > 0?• Decide whether fxy (2, 0) is positive, negative or zero.
f=−2
21
f=4
f=3
f=2
f=1
f=0
f=−1
go.illinois.edu/math241fa17.
Math 241: Problem of the day
Level curves for a function f : R2 → R are shown.• What is f (2, 0)?• What is fx(2, 0)?
• What is fx(2, ε), ε > 0?• Decide whether fxy (2, 0) is positive, negative or zero.
f=−2
21
f=4
f=3
f=2
f=1
f=0
f=−1
go.illinois.edu/math241fa17.
Math 241: Problem of the day
Level curves for a function f : R2 → R are shown.• What is f (2, 0)?• What is fx(2, 0)?• What is fx(2, ε), ε > 0?
• Decide whether fxy (2, 0) is positive, negative or zero.
f=−2
21
f=4
f=3
f=2
f=1
f=0
f=−1
go.illinois.edu/math241fa17.
Math 241: Problem of the day
Level curves for a function f : R2 → R are shown.• What is f (2, 0)?• What is fx(2, 0)?• What is fx(2, ε), ε > 0?• Decide whether fxy (2, 0) is positive, negative or zero.
f=−2
21
f=4
f=3
f=2
f=1
f=0
f=−1
go.illinois.edu/math241fa17.
Partial derivatives: applications.
Recall that an ODE (ordinary differential equation) is an equationinvolving a function of one variable and its derivatives: e.g. y ′ = yis exponential growth/decay equation.
A PDE (partial differential equation) is an equation involving afunction of several variables and its derivatives:e.g. ut = uxx + uyy + uzz is the heat equation.
go.illinois.edu/math241fa17.
Partial derivatives: applications.
Recall that an ODE (ordinary differential equation) is an equationinvolving a function of one variable and its derivatives
: e.g. y ′ = yis exponential growth/decay equation.
A PDE (partial differential equation) is an equation involving afunction of several variables and its derivatives:e.g. ut = uxx + uyy + uzz is the heat equation.
go.illinois.edu/math241fa17.
Partial derivatives: applications.
Recall that an ODE (ordinary differential equation) is an equationinvolving a function of one variable and its derivatives: e.g. y ′ = yis exponential growth/decay equation.
A PDE (partial differential equation) is an equation involving afunction of several variables and its derivatives:e.g. ut = uxx + uyy + uzz is the heat equation.
go.illinois.edu/math241fa17.
Partial derivatives: applications.
Recall that an ODE (ordinary differential equation) is an equationinvolving a function of one variable and its derivatives: e.g. y ′ = yis exponential growth/decay equation.
A PDE (partial differential equation) is an equation involving afunction of several variables and its derivatives
:e.g. ut = uxx + uyy + uzz is the heat equation.
go.illinois.edu/math241fa17.
Partial derivatives: applications.
Recall that an ODE (ordinary differential equation) is an equationinvolving a function of one variable and its derivatives: e.g. y ′ = yis exponential growth/decay equation.
A PDE (partial differential equation) is an equation involving afunction of several variables and its derivatives:e.g. ut = uxx + uyy + uzz is the heat equation.
go.illinois.edu/math241fa17.
Tangent planes and differentiability.
Tangent plane to graph z = f (x , y) at (a, b) is graph of the linearapproximation:
L(a,b)(x , y) = f (a, b) + fx(a, b)(x − a) + fy (a, b)(y − b).
Compare with g : R→ R, where linear approximation at a is
La(x) = g(a) + g ′(a)(x − a).
Tangent plane: z = L(a,b)(x , y).
When is this really tangent?
go.illinois.edu/math241fa17.
Tangent planes and differentiability.
Tangent plane to graph z = f (x , y) at (a, b) is graph of the linearapproximation:
L(a,b)(x , y) = f (a, b) + fx(a, b)(x − a) + fy (a, b)(y − b).
Compare with g : R→ R, where linear approximation at a is
La(x) = g(a) + g ′(a)(x − a).
Tangent plane: z = L(a,b)(x , y).
When is this really tangent?
go.illinois.edu/math241fa17.
Tangent planes and differentiability.
Tangent plane to graph z = f (x , y) at (a, b) is graph of the linearapproximation:
L(a,b)(x , y) = f (a, b) + fx(a, b)(x − a) + fy (a, b)(y − b).
Compare with g : R→ R, where linear approximation at a is
La(x) = g(a) + g ′(a)(x − a).
Tangent plane: z = L(a,b)(x , y).
When is this really tangent?
go.illinois.edu/math241fa17.
Tangent planes and differentiability.
Tangent plane to graph z = f (x , y) at (a, b) is graph of the linearapproximation:
L(a,b)(x , y) = f (a, b) + fx(a, b)(x − a) + fy (a, b)(y − b).
Compare with g : R→ R, where linear approximation at a is
La(x) = g(a) + g ′(a)(x − a).
Tangent plane: z = L(a,b)(x , y).
When is this really tangent?
go.illinois.edu/math241fa17.
Tangent planes and differentiability.
Tangent plane to graph z = f (x , y) at (a, b) is graph of the linearapproximation:
L(a,b)(x , y) = f (a, b) + fx(a, b)(x − a) + fy (a, b)(y − b).
Compare with g : R→ R, where linear approximation at a is
La(x) = g(a) + g ′(a)(x − a).
Tangent plane: z = L(a,b)(x , y).
When is this really tangent?
go.illinois.edu/math241fa17.
Tangent planes and differentiability.
Tangent plane to graph z = f (x , y) at (a, b) is graph of the linearapproximation:
L(a,b)(x , y) = f (a, b) + fx(a, b)(x − a) + fy (a, b)(y − b).
Compare with g : R→ R, where linear approximation at a is
La(x) = g(a) + g ′(a)(x − a).
Tangent plane: z = L(a,b)(x , y).
When is this really tangent?
go.illinois.edu/math241fa17.
Differentiability
We say that f (x , y) is differentiable at (a, b) if fx(a, b) and fy (a, b)exist and
0 = lim(h,k)→(0,0)
f (a + h, b + k)− L(a,b)(a + h, b + k)√h2 + k2
= lim(h,k)→(0,0)
f (a + h, b + k)− f (a, b)− fx(a, b)h − fy (a, b)k√h2 + k2
fx(a, b) and fy (a, b) can exist without f being differentiable at(a, b).
Example:
f (x , y) =
{ xyx2+y2 for (x , y) 6= (0, 0)
0 for (x , y) = (0, 0)
go.illinois.edu/math241fa17.
Differentiability
We say that f (x , y) is differentiable at (a, b) if fx(a, b) and fy (a, b)exist and
0 = lim(h,k)→(0,0)
f (a + h, b + k)− L(a,b)(a + h, b + k)√h2 + k2
= lim(h,k)→(0,0)
f (a + h, b + k)− f (a, b)− fx(a, b)h − fy (a, b)k√h2 + k2
fx(a, b) and fy (a, b) can exist without f being differentiable at(a, b).
Example:
f (x , y) =
{ xyx2+y2 for (x , y) 6= (0, 0)
0 for (x , y) = (0, 0)
go.illinois.edu/math241fa17.
Differentiability
We say that f (x , y) is differentiable at (a, b) if fx(a, b) and fy (a, b)exist and
0 = lim(h,k)→(0,0)
f (a + h, b + k)− L(a,b)(a + h, b + k)√h2 + k2
= lim(h,k)→(0,0)
f (a + h, b + k)− f (a, b)− fx(a, b)h − fy (a, b)k√h2 + k2
fx(a, b) and fy (a, b) can exist without f being differentiable at(a, b).
Example:
f (x , y) =
{ xyx2+y2 for (x , y) 6= (0, 0)
0 for (x , y) = (0, 0)
go.illinois.edu/math241fa17.
Differentiability
We say that f (x , y) is differentiable at (a, b) if fx(a, b) and fy (a, b)exist and
0 = lim(h,k)→(0,0)
f (a + h, b + k)− L(a,b)(a + h, b + k)√h2 + k2
= lim(h,k)→(0,0)
f (a + h, b + k)− f (a, b)− fx(a, b)h − fy (a, b)k√h2 + k2
fx(a, b) and fy (a, b) can exist without f being differentiable at(a, b).
Example:
f (x , y) =
{ xyx2+y2 for (x , y) 6= (0, 0)
0 for (x , y) = (0, 0)
go.illinois.edu/math241fa17.
Differentiability
We say that f (x , y) is differentiable at (a, b) if fx(a, b) and fy (a, b)exist and
0 = lim(h,k)→(0,0)
f (a + h, b + k)− L(a,b)(a + h, b + k)√h2 + k2
= lim(h,k)→(0,0)
f (a + h, b + k)− f (a, b)− fx(a, b)h − fy (a, b)k√h2 + k2
fx(a, b) and fy (a, b) can exist without f being differentiable at(a, b).
Example:
f (x , y) =
{ xyx2+y2 for (x , y) 6= (0, 0)
0 for (x , y) = (0, 0)
go.illinois.edu/math241fa17.
Differentiability
We say that f (x , y) is differentiable at (a, b) if fx(a, b) and fy (a, b)exist and
0 = lim(h,k)→(0,0)
f (a + h, b + k)− L(a,b)(a + h, b + k)√h2 + k2
= lim(h,k)→(0,0)
f (a + h, b + k)− f (a, b)− fx(a, b)h − fy (a, b)k√h2 + k2
fx(a, b) and fy (a, b) can exist without f being differentiable at(a, b).
Example:
f (x , y) =
{ xyx2+y2 for (x , y) 6= (0, 0)
0 for (x , y) = (0, 0)
go.illinois.edu/math241fa17.
Two theorems on differentiability
Theorem. If f is differentiable at (a, b) then f is continuous at(a, b).
Theorem. If fx and fy exist and are continuous near (a, b) then fis differentiable at (a, b).
This means there is some δ > 0 so that fx and fy exist and arecontinuous on a disk of radius δ > 0 about (a, b):
(x − a)2 + (y − b)2 < δ.
Clairaut’s Theorem. If f is defined near (a, b) and fxy and fyx arecontinuous near (a, b), then fxy (a, b) = fyx(a, b).
go.illinois.edu/math241fa17.
Two theorems on differentiability
Theorem. If f is differentiable at (a, b) then f is continuous at(a, b).
Theorem. If fx and fy exist and are continuous near (a, b) then fis differentiable at (a, b).
This means there is some δ > 0 so that fx and fy exist and arecontinuous on a disk of radius δ > 0 about (a, b):
(x − a)2 + (y − b)2 < δ.
Clairaut’s Theorem. If f is defined near (a, b) and fxy and fyx arecontinuous near (a, b), then fxy (a, b) = fyx(a, b).
go.illinois.edu/math241fa17.
Two theorems on differentiability
Theorem. If f is differentiable at (a, b) then f is continuous at(a, b).
Theorem. If fx and fy exist and are continuous near (a, b) then fis differentiable at (a, b).
This means there is some δ > 0 so that fx and fy exist and arecontinuous on a disk of radius δ > 0 about (a, b):
(x − a)2 + (y − b)2 < δ.
Clairaut’s Theorem. If f is defined near (a, b) and fxy and fyx arecontinuous near (a, b), then fxy (a, b) = fyx(a, b).
go.illinois.edu/math241fa17.
Two theorems on differentiability
Theorem. If f is differentiable at (a, b) then f is continuous at(a, b).
Theorem. If fx and fy exist and are continuous near (a, b) then fis differentiable at (a, b).
This means there is some δ > 0 so that fx and fy exist and arecontinuous on a disk of radius δ > 0 about (a, b):
(x − a)2 + (y − b)2 < δ.
Clairaut’s Theorem. If f is defined near (a, b) and fxy and fyx arecontinuous near (a, b), then fxy (a, b) = fyx(a, b).
go.illinois.edu/math241fa17.
Two theorems on differentiability
Theorem. If f is differentiable at (a, b) then f is continuous at(a, b).
Theorem. If fx and fy exist and are continuous near (a, b) then fis differentiable at (a, b).
This means there is some δ > 0 so that fx and fy exist and arecontinuous on a disk of radius δ > 0 about (a, b):
(x − a)2 + (y − b)2 < δ.
Clairaut’s Theorem. If f is defined near (a, b) and fxy and fyx arecontinuous near (a, b), then fxy (a, b) = fyx(a, b).
go.illinois.edu/math241fa17.