u=⟨x1,y1,z1⟩v=⟨x2,y2,z2⟩u×v=⟨y1z2−z1y2,z1x2−x1z2,x1y2−y1x2⟩∣u×v∣=∣u∣∣v∣sinθ
The magnitude of the cross product is the area of a parallelogram formed by these two vectors.
Plane Equation
ax+by+cz=d p=w+su+tv
Parallel with:
ax+by+cz=0 p=su+tv
Move by ⟨2,3,4⟩ p=⟨2,3,4⟩+w+su+tv a(x−2)+b(y−3)+c(z−4)=d
Perpendicular:
n=⟨a,b,c⟩. n=u×v. n=∇f=fr×fθ.
Two planes are parallel when their normal vectors are parallel.
Movement in the direction of the gradient has a maximum slope equal to the magnitude of the gradient.
Movement perpendicular to the gradient has a slope of 0.
Critical Points
f(x,y), ∇f=0
Second Derivative Test
D(x0,y0)=fxxfyxfxyfyy=fxxfyy−fxy2D>0,fxx>0, relative minimum;
D>0,fxx<0, relative maximum;
D<0, saddle point;
D=0, don't know.
Fubini's Theorem: If f is continuous on a rectangular region R, then
∫∫Rf(x,y)dA=∫ab∫cdf(x,y)dydx=∫cd∫abf(x,y)dxdy
If f(x,y)=g(x)h(y), then
∫∫Rf(x,y)dA=(∫abg(x)dx)(∫cdh(y)dy)
Properties:
Any continuous function defined on a closed rectangle R is integrable.
If the set of discontinuities lies on a finite union of graphs of continuous functions, then f is integrable on R.
Mean Value Theorem for Double Integrals:
If f is continuous on a closed, bounded region R with area A, then there exists a point (x0,y0) in R such that
∫∫Rf(x,y)dA=f(x0,y0)⋅A(R)
Theorems
∫abd−cdx=∫ab∫cd1dydx, then ∫ab∫cdf(x,y)dydx.
Estimating: If g≤f≤h, then ∫∫RgdA≤∫∫RfdA≤∫∫RhdA
T is the unit tangent vector to C at the point r(t).
T=∣r(t)′∣r(t)′
Reparameterization
If C is parameterized by r(t),a≤t≤b and also by p(s),c≤s≤d, where r(t)=p(g(t)) for some differentiable function g(t) with g(a)=c and g(b)=d, then
∫Cf(x,y)ds=∫abf(r(t))∣r(t)′∣dt=∫cdf(p(s))∣p(s)′∣ds∫CF⋅dr=∫abF(r(t))⋅r(t)′dt=∫cdF(p(s))⋅p(s)′ds
Line Integrals of Gradient Fields
If F=∇f, then ∫CF⋅dr=f(r(b))−f(r(a))
Images
Let A be a matrix with det and let be the linear mapping of to given by (matrix multiplication). Then transforms parallelograms into parallelograms and vertices into vertices. Moreover, if is a parallelogram, must be a parallelogram.
A linear transformation matrix A is one-to-one and onto if and only if det(A)=0.
T maps [0,1]×[0,1] to the parallelogram spanned by the vectors ⟨a,c⟩ and ⟨b,d⟩. T(u,v)=⟨au+bv,cu+dv⟩. The area of the parallelogram is ∣det(A)∣=∣ad−bc∣.
Applications
Average Value
The average value of f over a region R is given by
favg=∫∫Rdxdy∫∫Rf(x,y)dxdy
Center of Mass
The total mass M of a lamina with density function δ(x,y) over a region R is given by
M=∫∫Rδ(x,y)dA
The center of mass (xˉ,yˉ) of a lamina with density function δ(x,y) over a region R is given by
xˉ=M∫∫Rxδ(x,y)dA,yˉ=M∫∫Ryδ(x,y)dA
Moment of Inertia
Moments of inertia about the coordinate axes with uniform density δ are given by
Ix=δ∫∫∫R(y2+z2)dV,Iy=δ∫∫∫R(x2+z2)dV,Iz=δ∫∫∫R(x2+y2)dV
Gravitational Force
The gravitational force exerted on a point mass m located at the point (x0,y0,z0) by a solid region R with density function δ(x,y,z) is given by
F=Gm∫∫∫Rr2δ(x,y,z)r^dV∣F∣=Gm∫∫∫Rrδ(x,y,z)dV
where G is the gravitational constant, r is the distance from the point mass to the point (x,y,z), and r^ is the unit vector pointing from (x,y,z) to (x0,y0,z0).
Isaac Newton's Breathtaking Proposition 71
A uniform spherical shell of mass M exerts a gravitational force on a point mass m located outside the shell as if all the shell's mass were concentrated at its center. If the point mass is located inside the shell, the net gravitational force exerted on it by the shell is zero.
Surface Integral
A parameterization of a surfaceS is a vector function r(u,v)=⟨x(u,v),y(u,v),z(u,v)⟩ defined on a region R in the uv-plane such that r is one-to-one and r(R)=S.
Tu=ru=∂u∂r and Tv=rv=∂v∂r are tangent vectors to the surface, and n=∣ru×rv∣ru×rv is the unit normal vector to the surface. The magnitude of the cross product ∣ru×rv∣ gives the area of the parallelogram spanned by the tangent vectors, which is used to compute the surface area element dS.
An equation of the tangent plane to the surface at a point r(u0,v0) is given by
n⋅(r−r(u0,v0))=0n1(x−x0)+n2(y−y0)+n3(z−z0)=0
The surface S is regular if Tu×Tv=0 for all (u,v) in R. This condition ensures that the surface does not have any singularities or self-intersections, allowing for a well-defined normal vector and surface area element.
Parametic equation of a surface:
ax+by+cz=dr(u,v)=w+su+tv
Parametic surface integral:
∬Sf(x,y,z)dS=∬Rf(r(u,v))∣ru×rv∣dudv
Vector field surface integral:
∬SF⋅dS=∬RF(r(u,v))⋅(ru×rv)dudv
dS=(ru×rv)dudv
How to find the parameterization of a surface defined by an implicit equation f(x,y,z)=0?
Find the normal vector n=∇f=⟨∂x∂f,∂y∂f,∂z∂f⟩.
Find two tangent vectors u and v such that n⋅u=0 and n⋅v=0.
Find a point w on the surface.
The parameterization is given by r(s,t)=w+su+tv.
Area of a surface defined by f(x,y,z)=0 is given by
A(S)=∬R∣∇f⋅k∣∣∇f∣dudv
where k is the unit vector in the z-direction. This formula arises from the fact that the area element dS can be expressed in terms of the gradient of f and the projection of the surface onto the xy-plane. The term ∣∇f∣ accounts for the rate of change of the surface, while ∣∇f⋅k∣ accounts for the angle between the surface and the xy-plane, ensuring that the area is correctly scaled based on the orientation of the surface.
A=∬R1+(∂x∂z)2+(∂y∂z)2dxdy
For rotation about the z-axis, the surface area is given by
A=∬R2πx2+y21+(∂x∂z)2+(∂y∂z)2dxdy
For rotation about the y-axis, the surface area is given by
A=∬R2πx1+(∂x∂y)2dx
Lemma 1. Let D be a y-simple region and let C be its boundary. Suppose P:D→R is of class C1. Then
∫C+Pdx=−∬D∂y∂Pdxdy
(The left-hand side denotes the line integral ∫C+Pdx+Qdy, where Q=0.)
Lemma 2. Let D be an x-simple region and let C be its boundary. Suppose Q:D→R is of class C1. Then
∫C+Qdy=∬D∂x∂Qdxdy
(The left-hand side denotes the line integral ∫C+Pdx+Qdy, where P=0.)
Theorems
Theorem 1:
Suppose D is a simple region and C is its boundary, and P:D→R and Q:D→R are of class C1. Then
∫C+Pdx+Qdy=∬D(∂x∂Q−∂y∂P)dxdy∫C−Pdx+Qdy=−∬D(∂x∂Q−∂y∂P)dxdy
Theorem 2:
Area via Green's Theorem. If C is a simple closed curve that bounds a region to which Green's theorem applies, then the area of the region D bounded by C=∂D is
A=21∮∂D(xdy−ydx)
Theorem 3: Vector Form of Green's Theorem. Let D⊂R2 be a region to which Green's theorem applies, let ∂D be its (positively oriented) boundary, and let F=Pi+Qj be a C1 vector field on D. Then
∮∂DF⋅ds=∬D(curlF)⋅kdA=∬D(∇×F)⋅kdA
Theorem 4: Divergence Theorem in the Plane. Let D⊂R2 be a region to which Green's theorem applies and let ∂D be its boundary. Let n denote the outward unit normal to ∂D. If c:[a,b]→R2, t↦c(t)=(x(t),y(t)) is a positively oriented parametrization of ∂D, then n is given by
n=[x′(t)]2+[y′(t)]2(y′(t),−x′(t))
(see Figure 18.9). Let F=Pi+Qj be a C1 vector field on D. Then
∮∂DF⋅nds=∬DdivFdA
Stokes' Theorem
div: div F=∇⋅F=∂x∂Fx+∂y∂Fy+∂z∂Fz.
curl: curl F=∇×F=⟨∂y∂Fz−∂z∂Fy,∂z∂Fx−∂x∂Fz,∂x∂Fy−∂y∂Fx⟩.
flux: ∬SF⋅dS=∬SF⋅ndS.
flux of curl: ∬S(∇×F)⋅dS.
n=∣ru×rv∣ru×rv is the unit normal vector to the surface.
Stokes' Theorem for Graph
∫∂SF⋅dr=∬S(∇×F)⋅dS=∬Scurl (F)⋅ndA
Stokes' Theorem for Parametrized Surface
∬S(∇×F)⋅dS=∫∂SF⋅dr
Conservative Vector Fields
If F=∇f, then ∫SF⋅dr=f(r(b))−f(r(a)).
Theorem 1: Conservative Fields. Let F be a C1 vector field defined on R3, except possibly for a finite number of points. The following conditions on F are all equivalent:
For any oriented simple closed curve C, ∫CF⋅ds=0.
For any two oriented simple curves C1 and C2 that have the same endpoints, ∫C1F⋅ds=∫C2F⋅ds.
F is the gradient of some function f; that is, F=∇f (and if F has one or more exceptional points where it fails to be defined, f is also undefined there).
∇×F=0.
A vector field satisfying one (and, hence, all) of the conditions 1–4 is called a conservative vector field.
Corollary 1: If F is a C1 vector field on R2 of the form Pi+Qj that satisfies ∂y∂P=∂x∂Q, then F=∇f for some f on R2.
Theorem 2: If F is a C1 vector field on all of R3 with ∇⋅F=0, then there exists a C1 vector field G with F=∇×G.
If F has a potential function f, then it satisfies the cross-partial property: ∂y∂Fx=∂x∂Fy.
Gauss' Theorem
Gauss' Divergence Theorem
Let W be a symmetric elementary region in space.
∭W(∇⋅F)dV=∬∂WF⋅dS∭W(div F)dV=∬∂W(F⋅n)dS
Gauss' Law
Let M be a symmetric elementary region in R3. If (0,0,0)∈/∂M, then