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Material Type: Quiz; Class: MULTIVAR CALCULUS; Subject: Mathematics; University: University of California - Berkeley; Term: Summer 2006;
Typology: Quizzes
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(a) How do you find the slope of a tangent line to a polar curve? If a polar curve has equation r = f (θ), then the tangent to the point (r(θ 0 ), θ 0 ) is
f ′(θ 0 ) sin θ 0 + f (θ 0 ) cos θ 0 f ′(θ)f ′(θ 0 ) cos θ 0 − f (θ 0 ) sin θ
(b) How do you find the area of a region bounded by a polar curve? The area bounded by the lines θ = α, θ = β and the arc of the curve r = f (θ) between α and β is
∫ (^) β α
1 2 [f^ (θ)]
(^2) dθ.
(c) How do you find the length of a polar curve? The length of the arc of the curve r = f (θ) between θ = α and θ = β is
∫ (^) β α
[f (θ)]^2 + [f ′(θ)]^2 dθ.
Completing the square gives us
1 2
x^2 + 1(y − 1)^2 = 1
which is an ellipse with vertices at (±
2 , 1) and foci at (± 1 , 1).
x 1 = a + b sin(t) x 2 = cos(t) y 1 = c + d cos(t) y 2 = sin(t)
where a, b, c, d are all constants. By drawing pictures, show that the two paths may have 0, 1, 2, 3, 4 or infinitely many points of intersection. For each picture, give values of a, b, c, d which produces something like what you’ve drawn.
For 0, we can just take some circle which gets nowhere near the second shape, say (a, b, c, d) = (10, 1 , 0 , 1). To get 1, we need something which just touches the unit circle, like (2, 1 , 0 , 1). To get 2, we need something which passes through the circle, like (1, 1 , 0 , 1). To get 3, it needs to pass through the circle on one side and just touch it on the other, like (− 1 , 2 , 0 , 1). To get 4, it needs to pass through boths sides, like (0, 2 , 0 , 12 ). To get infinitely many, it has to be the same shape, ie. we need (0, 1 , 0 , 1).
x = r cos θ y = r sin θ z = z
(b) Do the same for spherical coordinates.
x = ρ sin φ cos θ y = ρ sin φ sin θ z = ρ cos φ
To find the equation of a plane we need two things: a point on it (check) and a vector normal to it. We don’t have the latter yet, so let’s find one by first finding two vectors in the plane. Name the points given A, B, C. Then AC¯ = 〈− 2 , 2 , 1 〉 and BC¯ = 〈− 5 , 1 , 0 〉 are in it. Their cross-product will be a vector normal to it. This is: ∣∣ ∣∣ ∣∣
i j k − 2 2 1 − 5 1 0
Hence, an equation of the plane is:
〈− 1 , − 5 , 8 〉 · (r − 〈 3 , 0 , 0 〉) = 0.
qa × b + pb︸ ︷︷ ︸ × a =a×b
pqb︸ ︷︷ ︸ × b = =(p − q)a × b
x = t^2 + t, y = sin(t), z = et
at the point (0, 0 , 1). To find equations for a line we need a point on it (check), and a vector along it. To find the latter, we must differentiate the vector function 〈t^2 + t, sin(t), et〉 and evaluate that at t = 0 (as this is the only value of t which gives us the point (0, 0 , 1)).
d dt
〈t^2 + t, sin(t), et〉 = 〈 2 t + 1, cos(t), et〉
∴
d dt 〈t^2 + t, sin(t), et〉 t=0 = 〈 1 , 1 , 1 〉
So, the vector equation of the line is r(s) = 〈 0 , 0 , 1 〉 + s〈 1 , 1 , 1 〉. Translating this into a parametric equation gives us
x = s, y = s, z = 1 + s.
u = x 1 + x 1 x 2 + x 1 x 2 x 3 +... + x 1 x 2 · · · xn.
This function is linear in xk for any k = 1,... , n. All the terms before the first appearance of xk drop out, and the xk disappears from all the other terms, leaving us with:
∂xk
(x 1 + x 1 x 2 + x 1 x 2 x 3 +... + x 1 x 2 · · · xn) = x 1 x 2 · · · xk + x 1 x 2 · · · xkxk+1 +... + x 1 x 2 · · · xn xk = x 1 x 2 · · · xk− 1 (xk+1 + xk+1xk+2 +... + xk+1xk+2 · · · xn).
If a function, f , is continuous on a closed bounded subset, D, of R^2 then f attains an absolute maximum value f (x 1 , y 1 ) and an absolute minimum value f (x 2 , y 2 ) for some points (x 1 , y 1 ) and (x 2 , y 2 ) in D. (b) Are the following subsets of R^2 closed? Bounded? If you claim one is bounded, give a bound; if you claim one isn’t closed, give a boundary point which isn’t contained in the set. i. S^1 := {(x, y) : x^2 + y^2 = 1}. Bounded by 1, closed. ii. {(x, y) : 0 ≤ y < 1 }. Not bounded; not closed, (0, 1) is a boundary point which isn’t in the set. iii. {(0, 0), (1, 3), (− 4 , 0)}. Bounded by 4; closed.
fx(x, y) = 3x^2 y + 24x fy(x, y) = x^3 − 8 fxx(x, y) = 6xy + 24 fyy(x, y) = 0 fxy = 6x.
At critical points, we have fy(x, y) = 0, so x = 2. Hence, y = (−(3)(2)24)(2) 2 = −4. Plugging in the appropriate values, we get that D = − 144 < 0, so this is a saddle point.
L^2 − x^2 − y^2
subject to x, y ≥ 0, x^2 + y^2 ≤ L^2 , ie. we’re maximising over a quarter-circle. We also note that if x, y or z = 0, then the volume is zero, so we don’t have to bother checking along the curves. So, we just have the 2D optimization to do. Instead of working with V which has an annoying square root in, instead we’ll maximize
W = V 2 = x^2 y^2 (L^2 − x^2 − y^2 ).
This has the following first derivatives:
Wx = 2xy^2 (L^2 − x^2 − y^2 ) − 2 x^3 y^2 = 2xy^2 L^2 − 2 xy^4 − 4 x^3 y^2 Wy = 2yx^2 L^2 − 2 yx^4 − 4 y^3 x^2
(The formula for W is symetric in x and y so there’s no need to do any calculations for Wy). We set these equal to 0 and cancel xs, ys (as we can assume x and y aren’t 0 as that would give us a volume of 0) and a 2, getting.
L^2 − 2 x^2 − y^2 = 0 L^2 − 2 y^2 − x^2 = 0.
Solving these equations simultaneously gives x = y =
L/3 (we may reject the negative square root, as we’re requiring x, y, z ≥ 0). Hence, the largest possible volume is (L/3)^3 /^2.
−(1 − y)(1 − z) = λ (I) −(1 − x)(1 − z) = λ (II) −(1 − x)(1 − y) = λ (III) x + y + z = 2 (IV ).
Using (II) and (III), we can get
(1 − x)(1 − z) = (1 − x)(1 − y).
So long as x 6 = 1, we can cancel the (1 − x). But, if x = 1 then the area is 0, by Heron’s formula, so we can ignore this case and conclude that, for the maximum,
y = z
Substituting this into (I) gives
−(1 − y)^2 = λ
and substituting this into (III) gives
(1 − x)(1 − y) = (1 − y)^2
By the same argument as above for x, y can’t be 1 at the maximum area, so we can cancel (1 − y)s and simplify to get
x = y Job done. (We’ve already got y = z, so we have x = y = z, so the triangle is equilateral. Note: we never used (IV), which shouldn’t actually be too suprising).
(a) The mass. ∫ ∫
D
ρ(x, y) dA
(b) The center of mass.
(¯x, ¯y) =
D ρ(x, y)^ dA
D
xρ(x, y) dA,
D
yρ(x, y) dA
(c) Which of the above integrals could come out negative? The mass couldn’t; the coordinates of the center of mass could.
0
√y
x^3 + 1 dx dy.
Drawing a picture, we see that x-values between 0 and 1 are used and, given a value of x, y ranges between 0 and x^2. Hence, the integral we want to do is
0
∫ (^) x 2
0
x^3 + 1 dy dx =
0
x^2
x^3 + 1 dx u = x^3 + 1
du 3 x^2 dx
=
1
u du
=
u^3 /^2 ]^21
=
The marginal p.d.f for Aloysius’ line is
fA(x) :=
1 6 x^ ∈^ [1,^ 7] 0 x /∈ [1, 7].
The marginal p.d.f. for Betty’s line is
fB (y) :=
4 e −y/ (^4) y ≥ 0 0 y < 0.
The surface area is
D
1 + z x^2 + z^2 y dA. (b) Under what circumstances could the above expression come out negative? Zero? It can never be negative. It could only be zero if D wasn’t really a region of the plane, but a curve or a point.
E xz dV^ where^ E^ is the solid tetrahedron with vertices (0,^0 ,^ 0),^ (0,^1 ,^ 0),^ (1,^1 ,^ 0),^ (0,^1 ,^ 1). Three of the faces are parallel to axes; the one that isn’t is the one with vertices (0, 0 , 0), (1, 1 , 0), (0, 0 , 1). This face is a plane containing the point (0, 0 , 0) and the vectors 〈 1 , 1 , 0 〉 and 〈 0 , 1 , 1 〉. Hence, one of its normal vectors is 〈 1 , − 1 , 1 〉, so it has equation x − y + z = 0. The region of the xy-plane that the region sits on is the half of the square with corners (0, 0) and (1, 1) above the line x = y. We set up our integral with z on the inside, to take advantage of the way we’ve packaged up the information so far. The integral is:
0
x
∫ (^) y−x
0
xz dz dy dx =
0
x
x(y − x)^2 dy dx
0
x(1 − x)^3 dx u = 1 − x
0
u^3 − u^4 du
=
0
y
∫ (^) y 0 f^ (x, y, z)^ dz dx dy^ as an integral with differentials in the order dy dx dz. Drawing a picture, we see that this region is a tetrahedron with vertices at (0, 0 , 0), (1, 0 , 0), (1, 1 , 0), (1, 1 , 1). So, z ranges from 0 to 1. Given a value of z, x runs from z to 1. Given a value of x and z which actually cuts through the tetrahedron, y runs from z to x. Hence the integral is ∫ (^1)
0
z
∫ (^) x
z
f (x, y, z) dy dx dz.
E (x
(^3) + xy (^2) ) dV where E is the solid in the first octant that lies beneath the paraboloid z = 1 − x^2 − y^2. As we’re in the first octant, θ ranges from 0 to π/2. r ranges from 0 to 1 (independently of θ). Given a value of r, z ranges from 0 to 1 − r^2. Hence the integral we want is
∫ (^) π/ 2
0
0
∫ (^1) −r 2
0
(r^3 cos^3 θ + r^3 cos θ sin^2 θ)r dz dr dθ =
∫ (^) π/ 2
0
0
∫ (^1) −r 2
0
r^4 cos θ(cos^2 θ + sin^2 θ) dz dr dθ
∫ (^) π/ 2
0
0
(r^4 − r^6 ) cos θ dr dθ
r^5 −
r^7 ]^10 [sin θ]π/ 0 2
=
R e
x^2 +4y^2 dA where R is the ellipse x (^2) + 4y (^2) ≤ 1.
We make the change x = u, 2 y = v, hoping to be able to use polar later. Solving for x and y gives x = u, y = v/2, giving us a Jacobian of 12. x^2 + 4y^2 ≤ 1 is equivalent to u^2 + v^2 ≤ 1 – let this region of the (uv)-plane by R′. Then the integral is equal to
∫ ∫
R′
eu (^2) +v 2
2
dA(u,v).
We observe that this is much easier to evaluate in polar coordinates, so we switch to them getting
∫ (^2) π
0
0
rer
2 dr dθ =
π 2
0
et^ dt t = r^2
π 2
(e − 1).
C
P dx + Q dy =
D
∂x
∂y
dA.
C F^ ·^ dr^ where^ C^ is the upper semi-circle from (0,^ −1) to (2π,^ 1). We know that
fx = ey^ − y sin x fy = xey^ + cos x + 2y.
Integrating these gives,
f = xey^ + y cos x + g(y) f = xey^ + y cos x + y^2 + h(x)
Comparing these, we see a choice that works for f is f (x, y) = xey^ + y cos x + y^2. Hence,
C
F · dr = f (2π, 1) − f (0, −1)
= 2πe + 2
C 1 F·dR^ is positive and^
C 2 F·dr^ is negative. However, these two paths have the same endpoints, so, if F were conservative, they’d be equal by the Fundamental Theorem for Line Integrals. Hence, F is not conservative.
D
F(x(u, v), y(u, v), z(u, v)) · (ru × rv) dA.
If F is the velocity field of a fluid and the surface is a permeable membrane, then the integral is the net rate at which fluid is flowing from the front to the back of it.
ru = 〈 1 , 0 , v〉 rv = 〈 0 , 1 , u〉 ∴ ru × rv = 〈−v, −u, − 1 〉 ∴ |ru × rv| =
1 + u^2 + v^2
So, the integral we want is ∫ ∫
D
1 + u^2 + v^2 dA
which is easiest evaluated in polar coordinates:
∫ (^2) π
0
0
r
1 + r^2 dr dθ = π
1
t dtt = 1 + r^2
dt = 2r dr
=
2 π 3 t^3 /^2 ]^21
=
2 π 3
Recall from homework that any field of the form 〈f (x), g(y), h(z)〉 is irrotational and from class that any field of the form 〈f (y, z), g(x, z), h(x, y)〉 is incompressible. Luckily, F can be broken down like that:
F = 〈x^2 , sin(y), z〉 + 〈yz, cos(x + z), xe−y〉.