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Is the surface parameterization r ( u , v ) = u 2 v , v + 1 , sin u , 0 u 2 , 0 v 3 smooth?

Yes

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Surface area of a parametric surface

Our goal is to define a surface integral, and as a first step we have examined how to parameterize a surface. The second step is to define the surface area of a parametric surface. The notation needed to develop this definition is used throughout the rest of this chapter.

Let S be a surface with parameterization r ( u , v ) = x ( u , v ) , y ( u , v ) , z ( u , v ) over some parameter domain D . We assume here and throughout that the surface parameterization r ( u , v ) = x ( u , v ) , y ( u , v ) , z ( u , v ) is continuously differentiable—meaning, each component function has continuous partial derivatives. Assume for the sake of simplicity that D is a rectangle (although the following material can be extended to handle nonrectangular parameter domains). Divide rectangle D into subrectangles D i j with horizontal width Δ u and vertical length Δ v . Suppose that i ranges from 1 to m and j ranges from 1 to n so that D is subdivided into mn rectangles. This division of D into subrectangles gives a corresponding division of surface S into pieces S i j . Choose point P i j in each piece S i j . Point P i j corresponds to point ( u i , v j ) in the parameter domain.

Note that we can form a grid with lines that are parallel to the u -axis and the v -axis in the uv -plane. These grid lines correspond to a set of grid curves    on surface S that is parameterized by r ( u , v ) . Without loss of generality, we assume that P i j is located at the corner of two grid curves, as in [link] . If we think of r as a mapping from the uv -plane to 3 , the grid curves are the image of the grid lines under r . To be precise, consider the grid lines that go through point ( u i , v j ) . One line is given by x = u i , y = v ; the other is given by x = u , y = v j . In the first grid line, the horizontal component is held constant, yielding a vertical line through ( u i , v j ) . In the second grid line, the vertical component is held constant, yielding a horizontal line through ( u i , v j ) . The corresponding grid curves are r ( u i , v ) and r ( u , v j ) , and these curves intersect at point P i j .

Two diagrams, showing that grid lines on a parameter domain correspond to grid curves on a surface. The first shows a two-dimensional rectangle in the u,v plane. The horizontal rectangle is in quadrant 1 and broken into 9x5 rectangles in a grid format. One rectangle Dij has side lengths delta u and delta v. The coordinates of the lower left corner are (u_i *, v_j *). In three dimensions, the surface curves above the x,y plane. The D_ij portion has become S_ij on the surface with lower left corner P_ij.
Grid lines on a parameter domain correspond to grid curves on a surface.

Now consider the vectors that are tangent to these grid curves. For grid curve r ( u i , v ) , the tangent vector at P i j is

t v ( P i j ) = r v ( u i , v j ) = x v ( u i , v j ) , y v ( u i , v j ) , z v ( u i , v j ) .

For grid curve r ( u , v j ) , the tangent vector at P i j is

t u ( P i j ) = r u ( u i , v j ) = x u ( u i , v j ) , y u ( u i , v j ) , z u ( u i , v j ) .

If vector N = t u ( P i j ) × t v ( P i j ) exists and is not zero, then the tangent plane at P i j exists ( [link] ). If piece S i j is small enough, then the tangent plane at point P i j is a good approximation of piece S i j .

Two diagrams. The one on the left is two dimensional and in the first quadrant of the u,v coordinate plane. A point u_0 is marked on the horizontal u axis, and a point v_0 is marked on the vertical v axis. The point (u_0, v_0) is shown in the plane. The diagram on the right shows the grid curve version. Now, the u_0 is marked as r(u_0, v) and the v_0 is marked as r(u, v_0). The (u_0, v_0) point is labeled P. Coming out of P are three arrows: one is a vertical N arrow, and the other two are t_u and t_v for the tangent plane.
If the cross product of vectors t u and t v exists, then there is a tangent plane.

The tangent plane at P i j contains vectors t u ( P i j ) and t v ( P i j ) , and therefore the parallelogram spanned by t u ( P i j ) and t v ( P i j ) is in the tangent plane. Since the original rectangle in the uv -plane corresponding to S i j has width Δ u and length Δ v , the parallelogram that we use to approximate S i j is the parallelogram spanned by Δ u t u ( P i j ) and Δ v t v ( P i j ) . In other words, we scale the tangent vectors by the constants Δ u and Δ v to match the scale of the original division of rectangles in the parameter domain. Therefore, the area of the parallelogram used to approximate the area of S i j is

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Source:  OpenStax, Calculus volume 3. OpenStax CNX. Feb 05, 2016 Download for free at http://legacy.cnx.org/content/col11966/1.2
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