490 CHAPTER 18. DIFFERENTIAL FORMS

Then

dω = Pydy∧dx+Pzdz∧dx+Qxdx∧dy+Qzdz∧dy+Rxdx∧dz+Rydy∧dz

Now let r : [0,1]2→ R3,r (s,u) = (x(s,u) ,y(s,u) ,z(s,u)). Then letting the various func-tions be defined at r (s,u) ,∫

rdω =

∫[0,1]2

(Py det

(ys yuxs xu

)+Pz det

(zs zuxs xu

)+Qx det

(xs xuys yu

)

+Qz det(

zs zuys yu

)+Rx det

(xs xuzs zu

)+Ry det

(ys yuzs zu

))dsdu

This equals ∫[0,1]2

(Ry−Qz)(yszu− yuzs)+(Pz−Rx)(xuzs− xszu)

+(Qx−Py)(xsyu− xuys)dsdu

By the definition of surface area on S≡ r([0,1]2

), see Definition 14.2.1 the area increment

on the surface r([0,1]2

)is√|yszu− yuzs|2 + |xuzs− xszu|2 + |xsyu− xuys|2dsdu

= det(Dr (u,s)∗Dr (s,u)

)1/2 dsdu

also the vector (Ry−Qz)i+(Pz−Rx) j+ (Qx−Py)k is the curl of the vector field F ≡Pi+Qj+Rj. Thus in more familiar calculus notation, the above integral is of the form∫

S≡r([0,1]2)∇×F ·pdS where p is a vector which is in the direction of

(yszu− yuzs)i+(xuzs− xszu)j+(xsyu− xuys)k.

It happens that this vector p is perpendicular to the surface S at every point where rs×ru ̸=0,which is seen to occur in the above formula. Recall that this follows from noting that, as(hopefully) discussed in beginning calculus,you have rs ·rs×ru = ru ·rs×ru = 0 and thisis sufficient to claim, based on geometric reasoning that it is perpendicular to the surface.Thus

∫r dω is one side of the usual Stoke’s theorem from calculus. You could generalize

to chains of rectangles as well.Next consider what happens with

∫∂r ω . This is just like it was with Green’s theorem

but with more terms. To save on space, P(x(1,u) ,y(1,u) ,z(1,u)) is denoted as P(1,u)with similar considerations for Q and R. Then this results in∫ 1

0

(P(1,u)

∂x(1,u)∂u

+Q(1,u)∂y(1,u)

∂u+R(1,u)

dz(1,u)du

)du

−∫ 1

0

(P(0,u)

∂x(0,u)∂u

+Q(0,u)∂y(0,u)

∂u+R(1,u)

dz(1,u)du

)du

+∫ 1

0P(s,0)

∂x(s,0)∂ s

+Q(s,0)∂y(s,0)

∂ s+R(s,0)

dz(s,0)ds

ds

−∫ 1

0P(s,1)

∂x(s,1)∂ s

+Q(s,1)∂y(s,1)

∂ s+R(s,1)

dz(s,1)ds

ds

490 CHAPTER 18. DIFFERENTIAL FORMSThend@ = P,dy \dx + P,dz/\ dx + Q,dx \ dy + Q,dz\ dy + Rydx \dz+ Rydy \ dzNow let r : [0,1]? > R°,r(s,u) = (x(s,u) ,y(s,u),z(s,u)). Then letting the various func-tions be defined at r(s,u),do= | P. det Ys Yu P. det Zs fu det Xs Xy[ an (2 «( ay PEN xe ay + Orde Ys Yu+-0.cet( Ss Su ) + Rraet( “su ) + Raet( Ys Yu )) asaYs Yu Zs fu Zs SuThis equalsI, iP (Ry _ Q:) (YsZu —Yuts) + (P; _ Ry) (Xuzs —Xsu)+ (Qx _ Py) (XsYu —Xyys) dsduBy the definition of surface areaonS=r ((0. 1) , See Definition 14.2.1 the area incrementon the surface r ((0. 1) isbse — yues|" + [XuZs ~ xsZul” + XsVu — xyys|-dsdu= det (Dr (u,s)* Dr (s,u)) ? dsdualso the vector (Ry — Q,)i+ (P,—Rx) J+ (Qx—P,)k is the curl of the vector field F =Pi+Qj-+Rj. Thus in more familiar calculus notation, the above integral is of the formf s=r((0,1]2) V x F’- pdS where p is a vector which is in the direction of(¥sZu —yuzs) t+ (XuZs —XsZu) J + (XsYu —XuYs) k.It happens that this vector p is perpendicular to the surface S at every point where r, x r, 40,which is seen to occur in the above formula. Recall that this follows from noting that, as(hopefully) discussed in beginning calculus,you have ry: rs X Ty = Ty- Ts X Ty =O and thisis sufficient to claim, based on geometric reasoning that it is perpendicular to the surface.Thus f,,dq@ is one side of the usual Stoke’s theorem from calculus. You could generalizeto chains of rectangles as well.Next consider what happens with f5,,@. This is just like it was with Green’s theorembut with more terms. To save on space, P(x(1,u),y(1,u),z(1,u)) is denoted as P(1,u)with similar considerations for Q and R. Then this results in1 Xx Uu Uu Uu[ (P10) (tu) PE eR SE ) du1 dx (0,u) dy (0,u) dz(1,u)-| (70,0) A 5000.0) POs RL) SE") duou+ [ "P(s,0) 245.0) ay 0) +R(s,0) 2(s,1) dy (s, 1) dz(s,1)dI Ox-| P(s,1) — +O(s,1) 5 + R(5,1)dz(s,0) |.+Q(s,0)dsS