2019
DOI: 10.1002/hyp.13381
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A scale‐invariant property of the water retention curve in weakly heterogeneous vadose zones

Abstract: Abrupt changes of hydraulic properties in a vadose zone are modelled within a stochastic framework, which regards the saturated conductivity and parameters related to the distribution of soil pores as stationary, log‐normally distributed, random space functions. As a consequence, flow variables become random fields, and we aim at deriving an effective Richards equation. To obtain the latter, we adopt a perturbation expansion truncated at the first order (weakly heterogeneous media), which leads to the effectiv… Show more

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Cited by 4 publications
(3 citation statements)
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“…10 shows that there is a first range with evident simple-scaling behavior, which runs from values of / equal to 0.056 up to about 0.28, and then a second range with a different trend, showing an increase of K for the remaining part. This latter behavior is in accordance with what was found by Severino and De Bartolo (2019) in a recent study concerning the water retention curves.…”
Section: Resultssupporting
confidence: 93%
“…10 shows that there is a first range with evident simple-scaling behavior, which runs from values of / equal to 0.056 up to about 0.28, and then a second range with a different trend, showing an increase of K for the remaining part. This latter behavior is in accordance with what was found by Severino and De Bartolo (2019) in a recent study concerning the water retention curves.…”
Section: Resultssupporting
confidence: 93%
“…Our approach is based on a direct scaling since analyses do not fit any specific model of . This empirical approach is well-known in literature, see for example [ 52 ] and in other contexts as to estimate the rate of sea level rise at some selected tide gauges around the world [ 53 ], in porous media [ 54 , 55 ], and in the framework of fluid mechanics [ 56 , 57 ].…”
Section: Methodsmentioning
confidence: 99%
“…Our approach is based on a direct scaling since analyses do not fit any specific model of v(t). This empirical approach is well-known in literature, see for example [52] and in other contexts as to estimate the rate of sea level rise at some selected tide gauges around the world [53], in porous media [54,55], and in the framework of fluid mechanics [56,57].…”
Section: Direct Scaling Analysis On the Voltage Fluctuations: Taylor's Law Approachmentioning
confidence: 99%