Punctual Hilbert scheme and certified approximate singularities

Angelos Mantzaflaris, B. Mourrain, Á. Szántó
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引用次数: 4

Abstract

In this paper we provide a new method to certify that a nearby polynomial system has a singular isolated root and we compute its multiplicity structure. More precisely, given a polynomial system f = (f1, ..., fN) ∈ C[x1, ..., xn]N, we present a Newton iteration on an extended deflated system that locally converges, under regularity conditions, to a small deformation of f such that this deformed system has an exact singular root. The iteration simultaneously converges to the coordinates of the singular root and the coefficients of the so-called inverse system that describes the multiplicity structure at the root. We use α-theory test to certify the quadratic convergence, and to give bounds on the size of the deformation and on the approximation error. The approach relies on an analysis of the punctual Hilbert scheme, for which we provide a new description. We show in particular that some of its strata can be rationally parametrized and exploit these parametrizations in the certification. We show in numerical experimentation how the approximate inverse system can be computed as a starting point of the Newton iterations and the fast numerical convergence to the singular root with its multiplicity structure, certified by our criteria.
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准时希尔伯特格式与证明近似奇点
本文给出了一种证明邻近多项式系统存在奇异孤立根的新方法,并计算了其多重结构。更准确地说,给定一个多项式系统f = (f1,…, fN)∈C[x1,…], xn]N,在正则条件下,我们给出了一个扩展压缩系统的牛顿迭代,该系统局部收敛于f的一个小变形,使得该变形系统具有一个精确奇异根。迭代同时收敛到奇异根的坐标和描述根处多重结构的所谓逆系统的系数。用α-理论检验证明了该方法的二次收敛性,并给出了变形大小和近似误差的界。该方法依赖于对准时希尔伯特方案的分析,为此我们提供了一种新的描述。我们特别指出,它的一些地层可以合理地参数化,并在证明中利用这些参数化。我们通过数值实验证明了近似逆系统可以作为牛顿迭代的起点,并通过我们的准则证明了它的多重结构快速收敛到奇异根。
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