MODELING PLOT SCALE DYE PENETRATION BY A DIFFUSION LIMITED AGGREGATION (DLA) MODEL

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dc.contributor.author Persson M.
dc.contributor.author Yasuda H.
dc.contributor.author Albergel J.
dc.contributor.author Berndtsson R.
dc.contributor.author Zante P.
dc.contributor.author Nasri S.
dc.contributor.author Ohrstrom P.
dc.date.accessioned 2021-03-11T07:47:43Z
dc.date.available 2021-03-11T07:47:43Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=771499
dc.identifier.citation Journal of Hydrology, 2001, 250, 1-4, 98-105
dc.identifier.issn 0022-1694
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/26609
dc.description.abstract Solute transport in the unsaturated zone often occurs in preferential flow paths. There are several reasons for this, e.g., water repellency, the occurrence of fissures and cracks, animal burrows, decomposed root threads etc. The resulting flow patterns often display a fractal resemblance which is difficult to predict using conventional transport models. A way to preserve the fractal property of observed data is to use the diffusion limited aggregation (DLA) model concept. In the present paper we use dye infiltration data to further develop the DLA model concept as applied to solute movement in soils. The DLA model is first calibrated against detailed field observations of dye infiltration. The model is shown to give a good description of observed mean and variance of dye penetration. After this, the calibrated model is verified against independent data from a nearby plot. The model is shown to reproduce observed dye patterns in a satisfactory way also at the verification plot.
dc.subject SOLUTE TRANSPORT
dc.subject DIFFUSION LIMITED AGGREGATION
dc.subject DYE IMAGE
dc.subject FRACTAL
dc.title MODELING PLOT SCALE DYE PENETRATION BY A DIFFUSION LIMITED AGGREGATION (DLA) MODEL
dc.type Статья


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