2017
DOI: 10.1002/hyp.11240
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Time–space fractional governing equations of one‐dimensional unsteady open channel flow process: Numerical solution and exploration

Abstract: Although fractional integration and differentiation have found many applications in various fields of science, such as physics, finance, bioengineering, continuum mechanics, and hydrology, their engineering applications, especially in the field of fluid flow processes, are rather limited. In this study, a finite difference numerical approach is proposed to solve the time–space fractional governing equations of 1‐dimensional unsteady/non‐uniform open channel flow process. By numerical simulations, results of th… Show more

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Cited by 8 publications
(7 citation statements)
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“…Hence, they can modulate the memory of the unconfined aquifer flow, which, in turn, can modulate the memory of the watershed baseflow. Meanwhile, the Caputo derivative, as defined in its special form D β x i 0 f (x i ) in space in this study, was shown by Kavvas and Ercan (2016) and Ercan and Kavvas (2017) to be a nonlocal quantity where the effect of the boundary conditions on the groundwater flow within the flow domain can have long spatial memories with the decrease in the powers of the spatial fractional derivatives from unity. Similarly, it was shown by Kavvas et al (2017a) that the Caputo derivative in time, D α 0 f (t), as defined in this study, is nonlocal in time and can carry the effect of initial conditions on the groundwater flow for long time periods as the power in the time fractional derivative decreases from 1.…”
Section: Discussionmentioning
confidence: 66%
“…Hence, they can modulate the memory of the unconfined aquifer flow, which, in turn, can modulate the memory of the watershed baseflow. Meanwhile, the Caputo derivative, as defined in its special form D β x i 0 f (x i ) in space in this study, was shown by Kavvas and Ercan (2016) and Ercan and Kavvas (2017) to be a nonlocal quantity where the effect of the boundary conditions on the groundwater flow within the flow domain can have long spatial memories with the decrease in the powers of the spatial fractional derivatives from unity. Similarly, it was shown by Kavvas et al (2017a) that the Caputo derivative in time, D α 0 f (t), as defined in this study, is nonlocal in time and can carry the effect of initial conditions on the groundwater flow for long time periods as the power in the time fractional derivative decreases from 1.…”
Section: Discussionmentioning
confidence: 66%
“…The works by Guerrini and Swartzendruber () and El Abd and Milczarek () may further support the fractional units of hydraulic conductivity related variables with some confidence as they explained the anomalous behaviour observed in the experiments with the diffusivity coefficients of fractional time units and successfully modelled various experimental data on horizontal soil water flow by the formulated fractional diffusivity coefficients. The behaviour of the groundwater flow under fractional powers of the space and time derivatives obtained in this numerical study is consistent with the nature of the fractional derivatives that the spatial/temporal nonlocality would increase as the power of space/time derivative decrease from 1 (Ercan & Kavvas, ).…”
Section: Discussionmentioning
confidence: 99%
“…The resulting fractional governing equation can model the nonlocal phenomena of the groundwater flow field by taking the global correlations of time and space into consideration. The proposed time–space fractional governing equation of groundwater flow was derived based on the Caputo fractional derivative, which allows the implementation of the traditional physically interpretable initial and boundary conditions (Ercan & Kavvas, ; Podlubny, ). The proposed governing equation of transient groundwater flow in confined aquifers in fractional time and space reduces to a standard Cartesian groundwater flow governing equation in an integer‐order differential framework, when the fractional space and time orders become one.…”
Section: Introductionmentioning
confidence: 99%
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“…In order to solve Eq. ( 50 ) numerically, a first-order approximation of the Caputo’s fractional time derivative 45 and a second-order accurate Caputo’s fractional space derivative 56 schemes are coupled similar to the numerical solution of the fractional open channel flow problem as reported in Ercan and Kavvas 57 . When the fractional powers of space and time derivatives of Eq.…”
Section: Introductionmentioning
confidence: 99%