§4. the Second Fundamental Form in the Last Section We Developed The
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Extended Rectifying Curves As New Kind of Modified Darboux Vectors
TWMS J. Pure Appl. Math., V.9, N.1, 2018, pp.18-31 EXTENDED RECTIFYING CURVES AS NEW KIND OF MODIFIED DARBOUX VECTORS Y. YAYLI1, I. GOK¨ 1, H.H. HACISALIHOGLU˘ 1 Abstract. Rectifying curves are defined as curves whose position vectors always lie in recti- fying plane. The centrode of a unit speed curve in E3 with nonzero constant curvature and non-constant torsion (or nonzero constant torsion and non-constant curvature) is a rectifying curve. In this paper, we give some relations between non-helical extended rectifying curves and their Darboux vector fields using any orthonormal frame along the curves. Furthermore, we give some special types of ruled surface. These surfaces are formed by choosing the base curve as one of the integral curves of Frenet vector fields and the director curve δ as the extended modified Darboux vector fields. Keywords: rectifying curve, centrodes, Darboux vector, conical geodesic curvature. AMS Subject Classification: 53A04, 53A05, 53C40, 53C42 1. Introduction From elementary differential geometry it is well known that at each point of a curve α, its planes spanned by fT;Ng, fT;Bg and fN; Bg are known as the osculating plane, the rectifying plane and the normal plane, respectively. A curve called twisted curve has non-zero curvature functions in the Euclidean 3-space. Rectifying curves are introduced by B. Y. Chen in [3] as space curves whose position vector always lies in its rectifying plane, spanned by the tangent and the binormal vector fields T and B of the curve. Accordingly, the position vector with respect to some chosen origin, of a rectifying curve α in E3, satisfies the equation α(s) = λ(s)T (s) + µ(s)B(s) for some functions λ(s) and µ(s): He proved that a twisted curve is congruent to a rectifying τ curve if and only if the ratio { is a non-constant linear function of arclength s: Subsequently Ilarslan and Nesovic generalized the rectifying curves in Euclidean 3-space to Euclidean 4-space [10]. -
Extension of the Darboux Frame Into Euclidean 4-Space and Its Invariants
Turkish Journal of Mathematics Turk J Math (2017) 41: 1628 { 1639 http://journals.tubitak.gov.tr/math/ ⃝c TUB¨ ITAK_ Research Article doi:10.3906/mat-1604-56 Extension of the Darboux frame into Euclidean 4-space and its invariants Mustafa DULD¨ UL¨ 1;∗, Bahar UYAR DULD¨ UL¨ 2, Nuri KURUOGLU˘ 3, Ertu˘grul OZDAMAR¨ 4 1Department of Mathematics, Faculty of Science and Arts, Yıldız Technical University, Istanbul,_ Turkey 2Department of Mathematics Education, Faculty of Education, Yıldız Technical University, Istanbul,_ Turkey 3Department of Civil Engineering, Faculty of Engineering and Architecture, Geli¸simUniversity, Istanbul,_ Turkey 4Department of Mathematics, Faculty of Science and Arts, Uluda˘gUniversity, Bursa, Turkey Received: 13.04.2016 • Accepted/Published Online: 14.02.2017 • Final Version: 23.11.2017 Abstract: In this paper, by considering a Frenet curve lying on an oriented hypersurface, we extend the Darboux frame field into Euclidean 4-space E4 . Depending on the linear independency of the curvature vector with the hypersurface's normal, we obtain two cases for this extension. For each case, we obtain some geometrical meanings of new invariants along the curve on the hypersurface. We also give the relationships between the Frenet frame curvatures and Darboux frame curvatures in E4 . Finally, we compute the expressions of the new invariants of a Frenet curve lying on an implicit hypersurface. Key words: Curves on hypersurface, Darboux frame field, curvatures 1. Introduction In differential geometry, frame fields constitute an important tool while studying curves and surfaces. The most familiar frame fields are the Frenet{Serret frame along a space curve, and the Darboux frame along a surface curve. -
Surface Integrals
VECTOR CALCULUS 16.7 Surface Integrals In this section, we will learn about: Integration of different types of surfaces. PARAMETRIC SURFACES Suppose a surface S has a vector equation r(u, v) = x(u, v) i + y(u, v) j + z(u, v) k (u, v) D PARAMETRIC SURFACES •We first assume that the parameter domain D is a rectangle and we divide it into subrectangles Rij with dimensions ∆u and ∆v. •Then, the surface S is divided into corresponding patches Sij. •We evaluate f at a point Pij* in each patch, multiply by the area ∆Sij of the patch, and form the Riemann sum mn * f() Pij S ij ij11 SURFACE INTEGRAL Equation 1 Then, we take the limit as the number of patches increases and define the surface integral of f over the surface S as: mn * f( x , y , z ) dS lim f ( Pij ) S ij mn, S ij11 . Analogues to: The definition of a line integral (Definition 2 in Section 16.2);The definition of a double integral (Definition 5 in Section 15.1) . To evaluate the surface integral in Equation 1, we approximate the patch area ∆Sij by the area of an approximating parallelogram in the tangent plane. SURFACE INTEGRALS In our discussion of surface area in Section 16.6, we made the approximation ∆Sij ≈ |ru x rv| ∆u ∆v where: x y z x y z ruv i j k r i j k u u u v v v are the tangent vectors at a corner of Sij. SURFACE INTEGRALS Formula 2 If the components are continuous and ru and rv are nonzero and nonparallel in the interior of D, it can be shown from Definition 1—even when D is not a rectangle—that: fxyzdS(,,) f ((,))|r uv r r | dA uv SD SURFACE INTEGRALS This should be compared with the formula for a line integral: b fxyzds(,,) f (())|'()|rr t tdt Ca Observe also that: 1dS |rr | dA A ( S ) uv SD SURFACE INTEGRALS Example 1 Compute the surface integral x2 dS , where S is the unit sphere S x2 + y2 + z2 = 1. -
On the Patterns of Principal Curvature Lines Around a Curve of Umbilic Points
Anais da Academia Brasileira de Ciências (2005) 77(1): 13–24 (Annals of the Brazilian Academy of Sciences) ISSN 0001-3765 www.scielo.br/aabc On the Patterns of Principal Curvature Lines around a Curve of Umbilic Points RONALDO GARCIA1 and JORGE SOTOMAYOR2 1Instituto de Matemática e Estatística, Universidade Federal de Goiás Caixa Postal 131 – 74001-970 Goiânia, GO, Brasil 2Instituto de Matemática e Estatística, Universidade de São Paulo Rua do Matão 1010, Cidade Universitária, 05508-090 São Paulo, SP, Brasil Manuscript received on June 15, 2004; accepted for publication on October 10, 2004; contributed by Jorge Sotomayor* ABSTRACT In this paper is studied the behavior of principal curvature lines near a curve of umbilic points of a smooth surface. Key words: Umbilic point, principal curvature lines, principal cycles. 1 INTRODUCTION The study of umbilic points on surfaces and the patterns of principal curvature lines around them has attracted the attention of generation of mathematicians among whom can be named Monge, Darboux and Carathéodory. One aspect – concerning isolated umbilics – of the contributions of these authors, departing from Darboux (Darboux 1896), has been elaborated and extended in several directions by Garcia, Sotomayor and Gutierrez, among others. See (Gutierrez and Sotomayor, 1982, 1991, 1998), (Garcia and Sotomayor, 1997, 2000) and (Garcia et al. 2000, 2004) where additional references can be found. In (Carathéodory 1935) Carathéodory mentioned the interest of non isolated umbilics in generic surfaces pertinent to Geometric Optics. In a remarkably concise study he established that any local analytic regular arc of curve in R3 is a curve of umbilic points of a piece of analytic surface. -
16.6 Parametric Surfaces and Their Areas
CHAPTER 16. VECTOR CALCULUS 239 16.6 Parametric Surfaces and Their Areas Comments. On the next page we summarize some ways of looking at graphs in Calc I, Calc II, and Calc III, and pose a question about what comes next. 2 3 2 Definition. Let r : R ! R and let D ⊆ R . A parametric surface S is the set of all points hx; y; zi such that hx; y; zi = r(u; v) for some hu; vi 2 D. In other words, it's the set of points you get using x = some function of u; v y = some function of u; v z = some function of u; v Example 1. (a) Describe the surface z = −x2 − y2 + 2 over the region D : −1 ≤ x ≤ 1; −1 ≤ y ≤ 1 as a parametric surface. Graph it in MATLAB. (b) Describe the surface z = −x2 − y2 + 2 over the region D : x2 + y2 ≤ 1 as a parametric surface. Graph it in MATLAB. Solution: (a) In this case we \cheat": we already have z as a function of x and y, so anything we do to get rid of x and y will work x = u y = v z = −u2 − v2 + 2 −1 ≤ u ≤ 1; −1 ≤ v ≤ 1 [u,v]=meshgrid(linspace(-1,1,35)); x=u; y=v; z=2-u.^2-v.^2; surf(x,y,z) CHAPTER 16. VECTOR CALCULUS 240 How graphs look in different contexts: Pre-Calc, and Calc I graphs: Calc II parametric graphs: y = f(x) x = f(t), y = g(t) • 1 number gets plugged in (usually x) • 1 number gets plugged in (usually t) • 1 number comes out (usually y) • 2 numbers come out (x and y) • Graph is essentially one dimensional (if you zoom in enough it looks like a line, plus you only need • graph is essentially one dimensional (but we one number, x, to specify any location on the don't picture t at all) graph) • We need to picture the graph in two dimensional • We need to picture the graph in a two dimen- world. -
Polynomial Curves and Surfaces
Polynomial Curves and Surfaces Chandrajit Bajaj and Andrew Gillette September 8, 2010 Contents 1 What is an Algebraic Curve or Surface? 2 1.1 Algebraic Curves . .3 1.2 Algebraic Surfaces . .3 2 Singularities and Extreme Points 4 2.1 Singularities and Genus . .4 2.2 Parameterizing with a Pencil of Lines . .6 2.3 Parameterizing with a Pencil of Curves . .7 2.4 Algebraic Space Curves . .8 2.5 Faithful Parameterizations . .9 3 Triangulation and Display 10 4 Polynomial and Power Basis 10 5 Power Series and Puiseux Expansions 11 5.1 Weierstrass Factorization . 11 5.2 Hensel Lifting . 11 6 Derivatives, Tangents, Curvatures 12 6.1 Curvature Computations . 12 6.1.1 Curvature Formulas . 12 6.1.2 Derivation . 13 7 Converting Between Implicit and Parametric Forms 20 7.1 Parameterization of Curves . 21 7.1.1 Parameterizing with lines . 24 7.1.2 Parameterizing with Higher Degree Curves . 26 7.1.3 Parameterization of conic, cubic plane curves . 30 7.2 Parameterization of Algebraic Space Curves . 30 7.3 Automatic Parametrization of Degree 2 Curves and Surfaces . 33 7.3.1 Conics . 34 7.3.2 Rational Fields . 36 7.4 Automatic Parametrization of Degree 3 Curves and Surfaces . 37 7.4.1 Cubics . 38 7.4.2 Cubicoids . 40 7.5 Parameterizations of Real Cubic Surfaces . 42 7.5.1 Real and Rational Points on Cubic Surfaces . 44 7.5.2 Algebraic Reduction . 45 1 7.5.3 Parameterizations without Real Skew Lines . 49 7.5.4 Classification and Straight Lines from Parametric Equations . 52 7.5.5 Parameterization of general algebraic plane curves by A-splines . -
Surface Normals and Tangent Planes
Surface Normals and Tangent Planes Normal and Tangent Planes to Level Surfaces Because the equation of a plane requires a point and a normal vector to the plane, …nding the equation of a tangent plane to a surface at a given point requires the calculation of a surface normal vector. In this section, we explore the concept of a normal vector to a surface and its use in …nding equations of tangent planes. To begin with, a level surface U (x; y; z) = k is said to be smooth if the gradient U = Ux;Uy;Uz is continuous and non-zero at any point on the surface. Equivalently,r h we ofteni write U = Uxex + Uyey + Uzez r where ex = 1; 0; 0 ; ey = 0; 1; 0 ; and ez = 0; 0; 1 : Supposeh now thati r (t) =h x (ti) ; y (t) ; z (t) hlies oni a smooth surface U (x; y; z) = k: Applying the derivative withh respect to t toi both sides of the equation of the level surface yields dU d = k dt dt Since k is a constant, the chain rule implies that U v = 0 r where v = x0 (t) ; y0 (t) ; z0 (t) . However, v is tangent to the surface because it is tangenth to a curve on thei surface, which implies that U is orthogonal to each tangent vector v at a given point on the surface. r That is, U (p; q; r) at a given point (p; q; r) is normal to the tangent plane to r 1 the surface U(x; y; z) = k at the point (p; q; r). -
On Jacobi Fields and Canonical Connection in Sub-Riemannian
On Jacobi fields and a canonical connection in sub-Riemannian geometry Davide Barilari♭ and Luca Rizzi♯ Abstract. In sub-Riemannian geometry the coefficients of the Jacobi equa- tion define curvature-like invariants. We show that these coefficients can be interpreted as the curvature of a canonical Ehresmann connection associated to the metric, first introduced in [15]. We show why this connection is naturally nonlinear, and we discuss some of its properties. Contents 1. Introduction 1 2. Jacobi equation revisited 3 3. The Riemannian case 4 4. The sub-Riemannian case 4 5. Ehresmanncurvatureandcurvatureoperator 9 Appendix A. Normal condition for the canonical frame 12 1. Introduction A key tool for comparison theorems in Riemannian geometry is the Jacobi equation, i.e. the differential equation satisfied by Jacobi fields. Assume γε is a one-parameter family of geodesics on a Riemannian manifold (M,g) satisfying k k i j (1)γ ¨ε +Γij (γε)γ ˙ εγ˙ε =0. ∂ The corresponding Jacobi field J = ∂ε ε=0 γε is a vector field defined along γ = γ0, and satisfies the equation ∂Γk (2) J¨k + 2Γk J˙iγ˙ j + ij J ℓγ˙ iγ˙ j =0. ij ∂xℓ The Riemannian curvature is hidden in the coefficients of this equation. To make arXiv:1506.01827v3 [math.DG] 28 Mar 2017 it appear explicitly, however, one has to write (2) in terms of a parallel transported n frame X1(t),...,Xn(t) along γ(t). Letting J(t) = i=1 Ji(t)Xi(t) one gets the following normal form: P (3) J¨i + Rij (t)Jj =0. -
A New Method for Finding the Shape Operator of a Hypersurface in Euclidean 4-Space
Filomat 32:17 (2018), 5827–5836 Published by Faculty of Sciences and Mathematics, https://doi.org/10.2298/FIL1817827U University of Nis,ˇ Serbia Available at: http://www.pmf.ni.ac.rs/filomat A New Method for Finding the Shape Operator of a Hypersurface in Euclidean 4-Space Bahar Uyar D ¨uld¨ula aYıldız Technical University, Education Faculty, Department of Mathematics and Science Education, Istanbul,˙ Turkey Abstract. In this paper, by taking a Frenet curve lying on a parametric or implicit hypersurface and using the extended Darboux frame field of this curve, we give a new method for calculating the shape operator’s matrix of the hypersurface depending on the extended Darboux frame curvatures. This new method enables us to obtain the Gaussian and mean curvatures of the hypersurface depending on the geodesic torsions of the curve and the normal curvatures of the hypersurface. 1. Introduction In differential geometry, the shape of a geometric object (curve, surface, etc.) has always been a point of interest. In Euclidean space, along a space curve we have only one direction to move. This direction is determined by the tangent vector of the curve. The curvature of the curve measures the rate of change of its tangent vector, and together with the torsion of the curve they give us some information to its shape. However, along a surface we have different directions to move. These directions constitute a plane at a point, called the tangent plane of the surface at that point. When we move along a given direction, the tangent plane and thereby the normal vector of this plane, that is, the unit normal vector of the surface will change its direction except for some special cases. -
Geodesic Methods for Shape and Surface Processing Gabriel Peyré, Laurent D
Geodesic Methods for Shape and Surface Processing Gabriel Peyré, Laurent D. Cohen To cite this version: Gabriel Peyré, Laurent D. Cohen. Geodesic Methods for Shape and Surface Processing. Tavares, João Manuel R.S.; Jorge, R.M. Natal. Advances in Computational Vision and Medical Image Process- ing: Methods and Applications, Springer Verlag, pp.29-56, 2009, Computational Methods in Applied Sciences, Vol. 13, 10.1007/978-1-4020-9086-8. hal-00365899 HAL Id: hal-00365899 https://hal.archives-ouvertes.fr/hal-00365899 Submitted on 4 Mar 2009 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Geodesic Methods for Shape and Surface Processing Gabriel Peyr´eand Laurent Cohen Ceremade, UMR CNRS 7534, Universit´eParis-Dauphine, 75775 Paris Cedex 16, France {peyre,cohen}@ceremade.dauphine.fr, WWW home page: http://www.ceremade.dauphine.fr/{∼peyre/,∼cohen/} Abstract. This paper reviews both the theory and practice of the nu- merical computation of geodesic distances on Riemannian manifolds. The notion of Riemannian manifold allows to define a local metric (a symmet- ric positive tensor field) that encodes the information about the prob- lem one wishes to solve. This takes into account a local isotropic cost (whether some point should be avoided or not) and a local anisotropy (which direction should be preferred). -
Math 314 Lecture #34 §16.7: Surface Integrals
Math 314 Lecture #34 §16.7: Surface Integrals Outcome A: Compute the surface integral of a function over a parametric surface. Let S be a smooth surface described parametrically by ~r(u, v), (u, v) ∈ D, and suppose the domain of f(x, y, z) includes S. The surface integral of f over S with respect to surface area is ZZ ZZ f(x, y, z) dS = f(~r(u, v))k~ru × ~rvk dA. S D When S is a piecewise smooth surface, i.e., a finite union of smooth surfaces S1,S2,...,Sk, that intersect only along their boundaries, the surface integral of f over S with respect to surface area is ZZ ZZ ZZ ZZ f dS = f dS + f dS + ··· + f dS, S S1 S2 Sk where the dS in each double integral is evaluated according the the parametric description of Si. Example. A parametric description of a surface S is ~r(u, v) = hu2, u sin v, u cos vi, 0 ≤ u ≤ 1, 0 ≤ v ≤ π/2. Here is a rendering of this surface. Here ~ru = h2u, sin v, cos vi and ~rv = h0, u cos v, −u sin vi, so that ~i ~j ~k 2 2 ~ru × ~rv = 2u sin v cos v = h−u, 2u sin v, 2u cos vi, 0 u cos v −u sin v and (with u ≥ 0), √ √ 2 4 2 k~ru × ~rvk = u + 4u = u 1 + 4u . The surface integral of f(x, y, z) = yz over S with respect to surface area is ZZ Z 1 Z π/2 √ yz dS = (u2 sin v cos v)(u 1 + 4u2) dvdu S 0 0 Z 1 √ sin2 v π/2 = u3 1 + 4u2 du 0 2 0 1 Z 1 √ = u3 1 + 4u2 du. -
(Paraboloid) Z = X 2 + Y2 + 1. (A) Param
PP 35 : Parametric surfaces, surface area and surface integrals 1. Consider the surface (paraboloid) z = x2 + y2 + 1. (a) Parametrize the surface by considering it as a graph. (b) Show that r(r; θ) = (r cos θ; r sin θ; r2 + 1); r ≥ 0; 0 ≤ θ ≤ 2π is a parametrization of the surface. (c) Parametrize the surface in the variables z and θ using the cylindrical coordinates. 2. For each of the following surfaces, describe the intersection of the surface and the plane z = k for some k > 0; and the intersection of the surface and the plane y = 0. Further write the surfaces in parametrized form r(z; θ) using the cylindrical co-ordinates. (a) 4z = x2 + 2y2 (paraboloid) (b) z = px2 + y2 (cone) 2 2 2 x2 y2 2 (c) x + y + z = 9; z ≥ 0 (Upper hemi-sphere) (d) − 9 − 16 + z = 1; z ≥ 0. 3. Let S denote the surface obtained by revolving the curve z = 3 + cos y; 0 ≤ y ≤ 2π about the y-axis. Find a parametrization of S. 4. Parametrize the part of the sphere x2 + y2 + z2 = 16; −2 ≤ z ≤ 2 using the spherical co-ordinates. 5. Consider the circle (y − 5)2 + z2 = 9; x = 0. Let S be the surface (torus) obtained by revolving this circle about the z-axis. Find a parametric representation of S with the parameters θ and φ where θ and φ are described as follows. If (x; y; z) is any point on the surface then θ is the angle between the x-axis and the line joining (0; 0; 0) and (x; y; 0) and φ is the angle between the line joining (x; y; z) and the center of the moving circle (which contains (x; y; z)) with the xy-plane.