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Reducibility of nilpotent commuting varieties
Let be the set of nilpotent by matrices over an algebraically
closed field . For each , let be the variety consisting
of all pairwise commuting -tuples of nilpotent matrices. It is well-kown
that is irreducible for every . We study in this note the
reducibility of for various values of and . In particular it
will be shown that the reducibility of , the variety of
commuting -tuples of by matrices, implies that of under
certain condition. Then we prove that is reducible for all . The ingredients of this result are also useful for getting a new lower
bound of the dimensions of and . Finally, we
investigate values of for which the variety of nilpotent
commuting triples is reducible.Comment: 8 page
On the origin of the unusual behavior in the stretching of single-stranded DNA
Force extension curves (FECs), which quantify the response of a variety of
biomolecules subject to mechanical force (), are often quantitatively fit
using worm-like chain (WLC) or freely-jointed chain (FJC) models. These models
predict that the chain extension, , normalized by the contour length
increases linearly at small and at high forces scale as where = 0.5 for WLC and unity for FJC. In contrast,
experiments on ssDNA show that over a range of and ionic concentration,
scales as , which cannot be explained using WLC or FJC models.
Using theory and simulations we show that this unusual behavior in FEC in ssDNA
is due to sequence-independent polyelectrolyte effects. We show that the arises because in the absence of force the tangent correlation function,
quantifying chain persistence, decays algebraically on length scales on the
order of the Debye length. Our theory, which is most appropriate for monovalent
salts, quantitatively fits the experimental data and further predicts that such
a regime is not discernible in double stranded DNA.Comment: Accepted for publication in JC
Trace element contents of selected antarctic meteorites, 1
Data are reported for volatile/mobile Ag, As, Au, Bi, Cd, Co, Cs, Cu, Ga, In, Rb, Sb, Se, Te, T1 and Zn in exterior and/or interior samples of four Antarctic meteorites: 77005 (unique achondrite); 77257 (unreilite); 77278 (L3); 77299 (H3). Exterior samples reflect contamination and/or leaching by weathering but trace element (ppm-ppt) contents in interior samples seem reasonable for representatives of these rare meteoritic types. The 77005 achondrite seems related to shergottites; other samples extend compositional ranges previously known for their types. With suitable precautions, Antarctic meteorite finds yield trace element data as reliable as those obtained from previously known falls
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