2022
DOI: 10.1038/s41598-022-11437-9
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The difference between semi-continuum model and Richards’ equation for unsaturated porous media flow

Abstract: Semi-continuum modelling of unsaturated porous media flow is based on representing the porous medium as a grid of non-infinitesimal blocks that retain the character of a porous medium. This approach is similar to the hybrid/multiscale modelling. Semi-continuum model is able to physically correctly describe diffusion-like flow, finger-like flow, and the transition between them. This article presents the limit of the semi-continuum model as the block size goes to zero. In the limiting process, the retention curv… Show more

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Cited by 7 publications
(11 citation statements)
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“…Let us recall the 2D semi-continuum model that was introduced by Kmec et al (2021). Here, we use the same model with an appropriate scaling of the retention curve with the block size (Vodák et al, 2022). The porous medium is represented as a rectangular grid of N × M square blocks of uniform size ∆x × ∆x.…”
Section: Semi-continuum Modelmentioning
confidence: 99%
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“…Let us recall the 2D semi-continuum model that was introduced by Kmec et al (2021). Here, we use the same model with an appropriate scaling of the retention curve with the block size (Vodák et al, 2022). The porous medium is represented as a rectangular grid of N × M square blocks of uniform size ∆x × ∆x.…”
Section: Semi-continuum Modelmentioning
confidence: 99%
“…A crucial idea behind the semi-continuum model is the appropriate scaling of the main branches of the retention curve which was first introduced by Vodák et al (2022). The scaling of the retention curve is based on the fact that the shape of the retention curve depends on the size (especially the height) of the sample on which the measurement is made (Larson and Morrow, 1981;Hunt et al, 2013;Silva et al, 2018).…”
Section: Scaling Of the Retention Curvementioning
confidence: 99%
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