Tiểu Luận On the classi cation of isoparametric hypersurfaces with four distinct principal curvatures in spher

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    On the classi cation of isoparametric hypersurfaces with four distinct principal curvatures in spheres
    By Stefan Immervoll
    Abstract
    In this paper we give a new proof for the classi cation result in [3]. We
    show that isoparametric hypersurfaces with four distinct principal curvatures
    in spheres are of Cli ord type provided that the multiplicities m1;m
    2
    of the
    principal curvatures satisfy m2  2m1 1. This inequality is satis ed for all
    but ve possible pairs (m1;m
    2
    ) with m1  m2
    . Our proof implies that for
    (m1;m
    2
    ) 6 = (1; 1) the Cli ord system may be chosen in such a way that the
    associated quadratic forms vanish on the higher-dimensional of the two focal
    manifolds. For the remaining ve possible pairs (m1;m
    2
    ) with m1  m2
    (see
    [13], [1], and [15]) this stronger form of our result is incorrect: for the three
    pairs (3; 4), (6; 9), and (7; 8) there are examples of Cli ord type such that
    the associated quadratic forms necessarily vanish on the lower-dimensional of
    the two focal manifolds, and for the two pairs (2; 2) and (4; 5) there exist
    homogeneous examples that are not of Cli ord type; cf. [5, 4.3, 4.4].
    1. Introduction
    In this paper we present a new proof for the following classi cation result
    in [3].
    Theorem 1.1. An isoparametric hypersurface with four distinct prin-cipal curvatures in a sphere is of Cli ord type provided that the multiplicities
    m1;m
    2
    of the principal curvatures satisfy the inequality m2  2m1 1.
    An isoparametric hypersurface M in a sphere is a (compact, connected)
    smooth hypersurface in the unit sphere of the Euclidean vector space
    V = R
    dim V
    such that the principal curvatures are the same at every point.
    By [12, Satz 1], the distinct principal curvatures have at most two di erent
    multiplicities m1
    , m2
    . In the following we assume that M has four distinct
    principal curvatures. Then the only possible pairs (m1;m
    2
    ) with m1 = m2
    are
    (1; 1) and (2; 2); see [13], [1]. For the possible pairs (m1;m
    2
    ) with m1 < m2
    we have (m1;m
    2
    ) = (4; 5) or 2
    (m1 1)
    divides m1 + m2
    + 1, where  : N ! N
    1012 STEFAN IMMERVOLL
    is given by
    (m) = fi j 1  i  m and i  0; 1; 2; 4 (mod 8)g ;
    see [15]. These results imply that the inequality m2  2m1 1 in Theorem 1.1
    is satis ed for all possible pairs (m1;m
    2
    ) with m1  m2
    except for the ve
    pairs (2; 2), (3; 4), (4; 5), (6; 9), and (7; 8).
    In [5], Ferus, Karcher, and Munzner introduced (and classi ed) a class of
    isoparametric hypersurfaces with four distinct principal curvatures in spheres
    de ned by means of real representations of Cli ord algebras or, equivalently,
    Cli ord systems. A Cli ord system consists of m + 1 symmetric matrices
    P0; : : : ; Pm with m  1 such that P
    2
    i
    = E and Pi Pj + Pj Pi
    = 0 for i; j =
    0; : : : ;m with i 6 = j , where E denotes the identity matrix. Isoparametric
    hypersurfaces of Cli ord type in the unit sphere S
    2l 1
    of the Euclidean vector
    space R
    2l
    have the property that there exists a Cli ord system P0; : : : ; Pm of
    symmetric (2l  2l)-matrices with l m 1 > 0 such that one of their two
    focal manifolds is given as
    fx 2 S
    2l 1
    j hPi
    x; xi = 0 for i = 0; : : : ;mg;
    where h  ;  i denotes the standard scalar product; see [5, Section 4, Satz (ii)].
    Families of isoparametric hypersurfaces in spheres are completely determined
    by one of their focal manifolds; see [12, Section 6], or [11, Proposition 3.2].
    Hence the above description of one of the focal manifolds by means of a Cli ord
    system characterizes precisely the isoparametric hypersurfaces of Cli ord type.
    For notions like focal manifolds or families of isoparametric hypersurfaces, see
    Section 2.
    The proof of Theorem 1.1 in Sections 3 and 4 shows that for an isopara-metric hypersurface (with four distinct principal curvatures in a sphere) with
    m2  2m1 1 and (m1;m
    2
    ) 6 = (1; 1) the Cli ord system may be chosen in such
    a way that the higher-dimensional of the two focal manifolds is described as
    above by the quadratic forms associated with the Cli ord system. This state-ment is in general incorrect for the isoparametric hypersurfaces of Cli ord type
    with (m1;m
    2
    ) = (3; 4), (6; 9), or (7; 8); see the remarks at the end of Section 4.
    Moreover, for the two pairs (2; 2) and (4; 5) there are homogeneous examples
    that are not of Cli ord type. Hence the inequality m2  2m1 1 is also a
    necessary condition for this stronger version of Theorem 1.1.
    Our proof of Theorem 1.1 makes use of the theory of isoparametric triple
    systems developed by Dorfmeister and Neher in [4] and later papers. We need,
    however, only the most elementary parts of this theory. Since our notion
    of isoparametric triple systems is slightly di erent from that in [4], we will
    present a short introduction to this theory in the next section. Based on
    the triple system structure derived from the isoparametric hypersurface M in
    the unit sphere of the Euclidean vector space V = R
    2l
    , we will introduce in
     
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