15 research outputs found

    Complements of hypersurfaces, variation maps and minimal models of arrangements

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    We prove the minimality of the CW-complex structure for complements of hyperplane arrangements in Cn\mathbb C^n by using the theory of Lefschetz pencils and results on the variation maps within a pencil of hyperplanes. This also provides a method to compute the Betti numbers of complements of arrangements via global polar invariants

    Toward effective detection of the bifurcation locus of real polynomial maps

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    Singular open book structures from real mappings

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    We prove extensions of Milnor's theorem for germs with nonisolated singularity and use them to find new classes of genuine real analytic mappings ψ\psi with positive dimensional singular locus \Sing \psi \subset \psi^{-1}(0), for which the Milnor fibration exists and yields an open book structure with singular binding.Comment: more remark

    Tame Functions with strongly isolated singularities at infinity: a tame version of a Parusinski's Theorem

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    Let f be a definable function, enough differentiable. Under the condition of having strongly isolated singularities at infinity at a regular value c we give a sufficient condition expressed in terms of the total absolute curvature function to ensure the local triviality of the function f over a neighbourhood of c and doing so providing the tame version of Parusinski's Theorem on complex polynomials with isolated singularities at infinity.Comment: 20 page

    On the Zeta-function of a polynomial at infinity

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    We use the notion of Milnor fibres of the germ of a meromorphic function and the method of partial resolutions for a study of topology of a polynomial map at infinity (mainly for calculation of the zeta-function of a monodromy). It gives effective methods of computation of the zeta-function for a number of cases and a criterium for a value to be atypical at infinity

    Factors Related with CH<sub>4</sub> and N<sub>2</sub>O Emissions from a Paddy Field: Clues for Management implications - Fig 5

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    <p>Temporal variation of soil temperature (A), soil salinity (B), pH (C), Eh (D), and Fe<sup>3+</sup> (E) and available N (F) concentrations in the paddy field. Error bars indicate the standard error of the mean of triplicate measurements.</p

    CONNECTIVITY VIA NONGENERIC PENCILS

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