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DIFFERENTIAL GEOMETRY: A First Course in Curves and Surfaces

DIFFERENTIAL GEOMETRY: A First Course in Curves and Surfaces

DIFFERENTIAL GEOMETRY: A First Course in Curves and Surfaces

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§3. Surface Theory with Differential Forms 97so from the fact that {e 1 , e 2 , e 3 } is a basis for R 3 we <strong>in</strong>fer thatSimilarly, we obta<strong>in</strong>dω 1 = ω 2 ∧ ω 21 = −ω 2 ∧ ω 12 = ω 12 ∧ ω 2 <strong>and</strong> dω 2 = ω 1 ∧ ω 12 .( 3∑ )0 = d(de i )=d ω ik e k ==k=13∑dω ij e j −j=13∑k=1(dω ik e k − ω ik ∧3∑ ( 3∑ω ik ∧ ω kj)e j =j=1∑so dω ij − 3 ω ik ∧ ω kj =0for all i, j.k=1k=1We also have the follow<strong>in</strong>g additional consequence of the proof:3∑ )ω kj e jj=13∑j=1(dω ij −Proposition 3.2. The shape operator is symmetric, i.e., h 12 = h 21 .□3∑ω ik ∧ ω kj)e j ,Proof. From the e 3 component of the equation d(dx) =0 <strong>in</strong> the proof of Theorem 3.1 we have0=ω 1 ∧ ω 13 + ω 2 ∧ ω 23 = ω 1 ∧ (h 11 ω 1 + h 12 ω 2 )+ω 2 ∧ (h 21 ω 1 + h 22 ω 2 )=(h 12 − h 21 )ω 1 ∧ ω 2 ,k=1so h 12 − h 21 =0.□Recall that V is a pr<strong>in</strong>cipal direction if de 3 (V) isascalar multiple of V. So e 1 <strong>and</strong> e 2 arepr<strong>in</strong>cipal directions if <strong>and</strong> only if h 12 =0<strong>and</strong> we have ω 13 = k 1 ω 1 <strong>and</strong> ω 23 = k 2 ω 2 , where k 1 <strong>and</strong>k 2 are, as usual, the pr<strong>in</strong>cipal curvatures.It is important to underst<strong>and</strong> how our battery of forms changes if we change our mov<strong>in</strong>g frameby rotat<strong>in</strong>g e 1 , e 2 through some angle θ (which may be a function).Lemma 3.3. Suppose e 1 = cos θe 1 + s<strong>in</strong> θe 2 <strong>and</strong> e 2 = − s<strong>in</strong> θe 1 + cos θe 2 for some function θ.Then we haveω 1 = cos θω 1 + s<strong>in</strong> θω 2ω 2 = − s<strong>in</strong> θω 1 + cos θω 2ω 12 = ω 12 + dθω 13 = cos θω 13 + s<strong>in</strong> θω 23ω 23 = − s<strong>in</strong> θω 13 + cos θω 23Note, <strong>in</strong> particular, that ω 1 ∧ ω 2 = ω 1 ∧ ω 2 <strong>and</strong> ω 13 ∧ ω 23 = ω 13 ∧ ω 23 .Proof. We leave this to the reader <strong>in</strong> Exercise 1.□It is often convenient when we study curves <strong>in</strong> surfaces (as we did <strong>in</strong> Sections 3 <strong>and</strong> 4 of Chapter2) to use the Darboux frame, a mov<strong>in</strong>g frame for the surface adapted so that e 1 is tangent to thecurve. (See Exercise 3.) For example, α is a geodesic if <strong>and</strong> only if <strong>in</strong> terms of the Darboux framewe have ω 12 =0as a 1-form on α.Let’s now exam<strong>in</strong>e the structure equations more carefully.

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