Please use this identifier to cite or link to this item: http://hdl.handle.net/2289/3975
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dc.contributor.authorSridhar, S.-
dc.contributor.authorSingh, Nishant K.-
dc.date.accessioned2011-04-08T05:42:00Z-
dc.date.available2011-04-08T05:42:00Z-
dc.date.issued2010-12-
dc.identifier.citationJournal of Fluid Mechanics, 2010, Vol. 664, p265en
dc.identifier.issn0022-1120 (Online)-
dc.identifier.issn1469-7645-
dc.identifier.urihttp://hdl.handle.net/2289/3975-
dc.descriptionRestricted Access. An open-access version is available at arXiv.org (one of the alternative locations)en
dc.description.abstractWe study large-scale kinematic dynamo action due to turbulence in the presence of a linear shear flow in the low-conductivity limit. Our treatment is non-perturbative in the shear strength and makes systematic use of both the shearing coordinate transformation and the Galilean invariance of the linear shear flow. The velocity fluctuations are assumed to have low magnetic Reynolds number (Re-m), but could have arbitrary fluid Reynolds number. The equation for the magnetic fluctuations is expanded perturbatively in the small quantity, Re-m. Our principal results are as follows: (i) the magnetic fluctuations are determined to the lowest order in Rem by explicit calculation of the resistive Green's function for the linear shear flow; (ii) the mean electromotive force is then calculated and an integro-differential equation is derived for the time evolution of the mean magnetic field. In this equation, velocity fluctuations contribute to two different kinds of terms, the 'C' and 'D' terms, respectively, in which first and second spatial derivatives of the mean magnetic field, respectively, appear inside the space-time integrals; (iii) the contribution of the D term is such that its contribution to the time evolution of the cross-shear components of the mean field does not depend on any other components except itself. Therefore, to the lowest order in Re-m, but to all orders in the shear strength, the D term cannot give rise to a shear-current-assisted dynamo effect; (iv) casting the integro-differential equation in Fourier space, we show that the normal modes of the theory are a set of shearing waves, labelled by their sheared wavevectors; (v) the integral kernels are expressed in terms of the velocity-spectrum tensor, which is the fundamental dynamical quantity that needs to be specified to complete the integro-differential equation description of the time evolution of the mean magnetic field; (vi) the C term couples different components of the mean magnetic field, so they can, in principle, give rise to a shear-current-type effect. We discuss the application to a slowly varying magnetic field, where it can be shown that forced non-helical velocity dynamics at low fluid Reynolds number does not result in a shear-current-assisted dynamo effect.en
dc.language.isoenen
dc.publisherCambridge University Pressen
dc.relation.urihttp://adsabs.harvard.edu/abs/2010JFM...664..265Sen
dc.relation.urihttp://arxiv.org/abs/0910.2141en
dc.relation.urihttp://dx.doi.org/10.1017/S0022112010003745en
dc.rights2010 Cambridge University Pressen
dc.subjectDynamo theoryen
dc.subjectMHD and electrohydrodynamicsen
dc.titleThe shear dynamo problem for small magnetic Reynolds numbersen
dc.typeArticleen
Appears in Collections:Research Papers (A&A)

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