Random fractional kinematic wave equations of overland flow: The HPM solutions and applications

• A time–space random fractional kinematic wave equation (rfKWE) is presented. • Numerical solutions developed using the homotopy perturbation method (HPM). • Data from laboratory experiments used for estimating the model parameters. • New procedures presented for calculating the steady-state infiltration rate etc. • Inter-relationships between model’s random parameters investigated. This paper presents new findings from analyses of a random fractional kinematic wave equation (rfKWE) for overland flow. The rfKWE is featured with orders of temporal and spatial fractional derivatives and with the roughness parameter, the effective rainfall intensity and infiltration rate as random variables. The new solutions are derived with the aid of a numerical method named the homotopy perturbation method (HPM) and approximate solutions are presented for different situations. The solutions are evaluated with data from overland flow flumes with simulated rainfall in the laboratory. The results suggest that on an infiltrating surface the temporal nonlocality of overland flow represented by the temporal order of fractional derivatives diminishes over time while the spatial nonlocality manifested by the spatial order of fractional derivatives continue if there is overland flow. It shows that the widely used unit discharge-height relationship is a special case of the solution of the rfKWE. Procedures are demonstrated for determining the fractional roughness coefficient, n f , the order of spatial fractional derivatives, ρ , and the steady-state infiltration rate during the overland flow, A s . The analyses of the data show that the mean spatial order of fractional derivatives is ρ = 1.25 , the mean flow pattern parameter m = 1.50 , and the mean fractional roughness coefficient is n f = 0.002 which is smaller than the conventional roughness coefficient, n = 0.108 . With these average values of the parameters and their standard deviations, simulations were performed to demonstrate the use of the methods, which is also a comparison of the classic KWE and rfKWE models.

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Publication Details

Journal
Journal of Hydrology
Published
2024-10-28
DOI
https://doi.org/10.1016/j.jhydrol.2024.132234
Citations
2
Primary Topic
Fractional Differential Equations Solutions
Type
article
Field-Weighted Citation Impact
0.79

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article

Random fractional kinematic wave equations of overland flow: The HPM solutions and applications

Ninghu Su, Fengbao Zhang
2 citations
Journal of Hydrology
Fractional Differential Equations Solutions
0.79
article

Random fractional kinematic wave equations of overland flow: The HPM solutions and applications

Ninghu Su, Fengbao Zhang
article en
2 citations

Abstract

• A time–space random fractional kinematic wave equation (rfKWE) is presented. • Numerical solutions developed using the homotopy perturbation method (HPM). • Data from laboratory experiments used for estimating the model parameters. • New procedures presented for calculating the steady-state infiltration rate etc. • Inter-relationships between model’s random parameters investigated. This paper presents new findings from analyses of a random fractional kinematic wave equation (rfKWE) for overland flow. The rfKWE is featured with orders of temporal and spatial fractional derivatives and with the roughness parameter, the effective rainfall intensity and infiltration rate as random variables. The new solutions are derived with the aid of a numerical method named the homotopy perturbation method (HPM) and approximate solutions are presented for different situations. The solutions are evaluated with data from overland flow flumes with simulated rainfall in the laboratory. The results suggest that on an infiltrating surface the temporal nonlocality of overland flow represented by the temporal order of fractional derivatives diminishes over time while the spatial nonlocality manifested by the spatial order of fractional derivatives continue if there is overland flow. It shows that the widely used unit discharge-height relationship is a special case of the solution of the rfKWE. Procedures are demonstrated for determining the fractional roughness coefficient, n f , the order of spatial fractional derivatives, ρ , and the steady-state infiltration rate during the overland flow, A s . The analyses of the data show that the mean spatial order of fractional derivatives is ρ = 1.25 , the mean flow pattern parameter m = 1.50 , and the mean fractional roughness coefficient is n f = 0.002 which is smaller than the conventional roughness coefficient, n = 0.108 . With these average values of the parameters and their standard deviations, simulations were performed to demonstrate the use of the methods, which is also a comparison of the classic KWE and rfKWE models.

Journal of HydrologyVol. 645
Institute of Soil and Water Conservation (CN), James Cook University (AU), Northwest A&F University (CN)
Ministry of Education of the People's Republic of China, Northwest A and F University, Science Foundation of Ministry of Education of China
Openalex Percentile: Top 29%
Fractional Differential Equations Solutions
0.79
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