Using H‐Convergence to Calculate the Numerical Errors for 1D Unsaturated Seepage in Transient Conditions

ABSTRACT Numerical modeling plays a pivotal role in understanding transient unsaturated flow, which is critical for applications such as groundwater recharge, stormwater management, and contaminant transport. This study investigates the effect of time step refinement on numerical solutions for a vertical infiltration 1D test in a vertical column. First, the element size, ES , was selected to have all calculations in the MCD, the mathematical convergence domain. Then, the numerical and mathematical convergences of the numerical solutions were studied versus the time step, Δ t . The study provided results for hydraulic head, unsaturated hydraulic conductivity, volumetric water content, and vertical water velocity versus elevation, elapsed time t , and Δ t . Asymptotic behavior was obtained for all unknowns when Δ t → 0. All results for all parameters gave linear relationships between the log of the numerical error and the log of Δ t , as predicted by mathematics. Thus, they proved that a good code converges mathematically when ES and Δ t are decreased. For this 1D problem, the MCD is reached for Δ t ≤ 1 s, which is a small MCD. For larger Δ t values (2 ≤ Δ t ≤ 100 s), the code converges numerically in the numerical convergence domain (NCD), where the solutions respect the user‐defined convergence criteria but deviate from the true mathematical convergence criterion, underscoring that a fine temporal discretization is critical. The study also demonstrates that small Δ t steps ensure physically consistent behavior, as reflected in smooth slope volumetric water content versus suction curves, whereas large Δ t steps produce oscillations and instability.

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Publication Details

Journal
International Journal for Numerical and Analytical Methods in Geomechanics
Published
2025-09-18
DOI
https://doi.org/10.1002/nag.70085
Citations
1
Primary Topic
Soil and Unsaturated Flow
Type
article
Field-Weighted Citation Impact
0.95
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article

Using H‐Convergence to Calculate the Numerical Errors for 1D Unsaturated Seepage in Transient Conditions

Robert P. Chapuis, Arij Krifa
1 citations
International Journal for Numerical and Analytical Methods in Geomechanics
Soil and Unsaturated Flow
0.95
article

Using H‐Convergence to Calculate the Numerical Errors for 1D Unsaturated Seepage in Transient Conditions

Robert P. Chapuis, Arij Krifa
article en
1 citations

Abstract

ABSTRACT Numerical modeling plays a pivotal role in understanding transient unsaturated flow, which is critical for applications such as groundwater recharge, stormwater management, and contaminant transport. This study investigates the effect of time step refinement on numerical solutions for a vertical infiltration 1D test in a vertical column. First, the element size, ES , was selected to have all calculations in the MCD, the mathematical convergence domain. Then, the numerical and mathematical convergences of the numerical solutions were studied versus the time step, Δ t . The study provided results for hydraulic head, unsaturated hydraulic conductivity, volumetric water content, and vertical water velocity versus elevation, elapsed time t , and Δ t . Asymptotic behavior was obtained for all unknowns when Δ t → 0. All results for all parameters gave linear relationships between the log of the numerical error and the log of Δ t , as predicted by mathematics. Thus, they proved that a good code converges mathematically when ES and Δ t are decreased. For this 1D problem, the MCD is reached for Δ t ≤ 1 s, which is a small MCD. For larger Δ t values (2 ≤ Δ t ≤ 100 s), the code converges numerically in the numerical convergence domain (NCD), where the solutions respect the user‐defined convergence criteria but deviate from the true mathematical convergence criterion, underscoring that a fine temporal discretization is critical. The study also demonstrates that small Δ t steps ensure physically consistent behavior, as reflected in smooth slope volumetric water content versus suction curves, whereas large Δ t steps produce oscillations and instability.

International Journal for Numerical and Analytical Methods in GeomechanicsVol. 49(18)
Polytechnique Montréal (CA)
Openalex Percentile: Top 21%
Soil and Unsaturated Flow
0.95
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