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The analytical solution of the transient radial diffusion equation with a nonuniform loss term
Author(s) -
Loridan Vivien,
Ripoll JeanFrançois,
Vuyst Florian
Publication year - 2017
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
eISSN - 2169-9402
pISSN - 2169-9380
DOI - 10.1002/2017ja023868
Subject(s) - eigenfunction , eigenvalues and eigenvectors , piecewise , diffusion equation , mathematical analysis , term (time) , constant (computer programming) , diffusion , physics , mathematics , computer science , quantum mechanics , economy , economics , programming language , service (business)
Abstract Many works have been done during the past 40 years to perform the analytical solution of the radial diffusion equation that models the transport and loss of electrons in the magnetosphere, considering a diffusion coefficient proportional to a power law in L shell and a constant loss term. In this paper, we propose an original analytical method to address this challenge with a nonuniform loss term. The strategy is to match any L ‐dependent electron losses with a piecewise constant function on M subintervals, i.e., dealing with a constant lifetime on each subinterval. Applying an eigenfunction expansion method, the eigenvalue problem becomes presently a Sturm‐Liouville problem with M interfaces. Assuming the continuity of both the distribution function and its first spatial derivatives, we are able to deal with a well‐posed problem and to find the full analytical solution. We further show an excellent agreement between both the analytical solutions and the solutions obtained directly from numerical simulations for different loss terms of various shapes and with a diffusion coefficient D L L ∼ L 6 . We also give two expressions for the required number of eigenmodes N to get an accurate snapshot of the analytical solution, highlighting that N is proportional to 1 /t 0, where t 0 is a time of interest, and that N increases with the diffusion power. Finally, the equilibrium time, defined as the time to nearly reach the steady solution, is estimated by a closed‐form expression and discussed. Applications to Earth and also Jupiter and Saturn are discussed.