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dc.contributor.authorGhosh, S.S.
dc.contributor.authorIyengar, A.N. Sekar
dc.date.accessioned2015-12-04T06:14:30Z
dc.date.accessioned2021-02-12T09:41:39Z-
dc.date.available2015-12-04T06:14:30Z
dc.date.available2021-02-12T09:41:39Z-
dc.date.issued2014
dc.identifier.citationPhys. Plasmas, v.21, 082104, 2014, doi: 10.1063/1.4891853en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/767-
dc.description.abstractIt is observed that the presence of a minority component of cooler electrons in a three component plasma plays a deterministic role in the evolution of solitary waves, double layers, or the newly discovered structures called supersolitons. The inclusion of the cooler component of electrons in a single electron plasma produces sharp increase in nonlinearity in spite of a decrease in the overall energy of the system. The effect maximizes at certain critical value of the number density of the cooler component (typically 15%–20%) giving rise to a hump in the amplitude variation profile. For larger amplitudes, the hump leads to a forbidden region in the ambient cooler electron concentration which dissociates the overall existence domain of solitary wave solutions in two distinct parameter regime. It is observed that an inclusion of the cooler component of electrons as low as < 1% affects the plasma system significantly resulting in compressive double layers. The solution is further affected by the cold to hot electron temperature ratio. In an adequately hotter bulk plasma (i.e., moderately low cold to hot electron temperature ratio), the parameter domain of compressive double layers is bounded by a sharp discontinuity in the corresponding amplitude variation profile which may lead to supersolitons.en_US
dc.language.isoenen_US
dc.subjectIon acoustic solitary wavesen_US
dc.subjectDouble layersen_US
dc.subjectForbidden regionsen_US
dc.subjectCooler electronsen_US
dc.titleEffect of cooler electrons on a compressive ion acoustic solitary wave in a warm ion plasma - Forbidden regions, double layers, and supersolitonsen_US
dc.typeArticleen_US
dc.identifier.accession091431
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