| نویسندگان | Abolfazl Akbarpour,Ahmad Jafarzadeh,Mohsen Pourreza-Bilondi,Abbas Khashei Siuki,Mehdi Azizi |
| نشریه | Acta Geophysica |
| شماره صفحات | 1-18 |
| ضریب تاثیر (IF) | 0.91 |
| نوع مقاله | Full Paper |
| تاریخ انتشار | 2022 |
| نوع نشریه | چاپی |
| کشور محل چاپ | هلند |
| نمایه نشریه | JCR،Scopus |
چکیده مقاله
Abstract
This study intends to investigate the impacts of scheme type, time step, and error threshold on the stability of numerical
simulation in the groundwater modeling. Hence, a two-dimensional finite element (FE) was implemented to simulate groundwater
flow in a synthetic test case and a real-world study (Birjand aquifer). To verify the proposed model in both cases, the
obtained results were compared with analytical solutions and observed values. The stability of numerical results was analyzed
through different schemes and time-step sizes. Besides, the effect of the error threshold was examined by considering different
threshold values. The results confirmed that the FE model has a good capacity to simulate groundwater fluctuations
even for the real problem with more complexities. Examination of implicit outputs indicated that groundwater simulations
based on this scheme have good accuracy, stability, and proper convergence in all time intervals. However, in the explicit
and Crank–Nicolson schemes the time interval should be less than or equal to 0.001 and 0.1 day, respectively. Also, results
reveal that for making stability in all schemes the value of the error threshold should not be more than 0.0001 m. Moreover, it
derived that the boundary conditions of the aquifer influence the stability of numerical outputs. Finally, it was comprehended
that as time interval and error threshold increases, the oscillation rate propagated.
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