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dc.contributor.authorAtangana, A.
dc.contributor.authorUnlu, Canan
dc.date.accessioned2021-03-06T07:57:38Z
dc.date.available2021-03-06T07:57:38Z
dc.date.issued2016
dc.identifier.citationAtangana A., Unlu C., "New groundwater flow equation with its exact solution", SCIENTIA IRANICA, cilt.23, ss.1837-1843, 2016
dc.identifier.issn1026-3098
dc.identifier.otherav_deafb35a-5952-46a3-bb7b-1fcc45229ce0
dc.identifier.othervv_1032021
dc.identifier.urihttp://hdl.handle.net/20.500.12627/146707
dc.identifier.urihttps://doi.org/10.24200/sci.2016.3930
dc.description.abstractA new model of groundwater flowing within a confined aquifer was proposed using the concept of local derivative with fractional order. The derivative, used in this model, obeys all the properties of a local derivative, and has a fractional order. The new groundwater flow equation was solved analytically via three different analytical methods. The first method was the well-known method of separation of variables. The problem with this method is the introduction of the eigenvalue that does not have physical meaning. The second method was achieved using novel integral equation called Atangana-transform, and this method yields an exact solution. An alternative method based on the modified Boltzmann transformation also yields the exact solution. Some numerical simulations were done to express the efficiency of the model. (C) 2016 Sharif University of Technology. All rights reserved.
dc.language.isoeng
dc.subjectMühendislik, Bilişim ve Teknoloji (ENG)
dc.subjectMühendislik ve Teknoloji
dc.subjectMÜHENDİSLİK, MULTİDİSİPLİNER
dc.subjectMühendislik
dc.subjectHarita Mühendisliği-Geomatik
dc.titleNew groundwater flow equation with its exact solution
dc.typeMakale
dc.relation.journalSCIENTIA IRANICA
dc.contributor.departmentUniversity of the Free State , ,
dc.identifier.volume23
dc.identifier.issue4
dc.identifier.startpage1837
dc.identifier.endpage1843
dc.contributor.firstauthorID234056


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