<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-04-14T05:18:44Z</responseDate><request verb="GetRecord" identifier="oai:www.recercat.cat:2117/25088" metadataPrefix="oai_dc">https://recercat.cat/oai/request</request><GetRecord><record><header><identifier>oai:recercat.cat:2117/25088</identifier><datestamp>2025-07-17T01:51:18Z</datestamp><setSpec>com_2072_1033</setSpec><setSpec>col_2072_452950</setSpec></header><metadata><oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
   <dc:title>Non-linear fractal percolation experiments in carstic and aggregation soils</dc:title>
   <dc:creator>Chierubini, Claudia</dc:creator>
   <dc:creator>Tarquis Alfonso, Ana Maria</dc:creator>
   <dc:creator>Redondo Apraiz, José Manuel</dc:creator>
   <dc:creator>Pastore, Nicola</dc:creator>
   <dc:contributor>Universitat Politècnica de Catalunya. Departament de Física Aplicada</dc:contributor>
   <dc:contributor>Universitat Politècnica de Catalunya. DF - Dinàmica No Lineal de Fluids</dc:contributor>
   <dc:subject>Àrees temàtiques de la UPC::Física</dc:subject>
   <dc:subject>Nonlinear oscillations</dc:subject>
   <dc:subject>Percolation&#xd;
Sediment Transport&#xd;
Karstic&#xd;
Fractal</dc:subject>
   <dc:subject>Oscil·lacions no lineals</dc:subject>
   <dc:description>The present study compares the performances and reliabilities of the classical Mobile – Immobile Model (MIM)&#xd;
and the Explicit Network Model (ENM) that takes expressly into account the network geometry for describing&#xd;
tracer transport behaviour in a fractured sample at bench scale. Though ENM shows better fitting results than&#xd;
MIM, the latter remains still valid as it proves to describe the observed curves quite well.&#xd;
The results show that the presence of nonlinear flow plays an important role in the behaviour of solute&#xd;
transport. Firstly the distribution of solute according to different pathways is not constant but it is related to the&#xd;
flow rate. Secondly nonlinear flow influences advection, in that it leads to a delay in solute transport respect to the&#xd;
linear flow assumption. Whereas nonlinear flow does not show to be related with dispersion. The experimental&#xd;
results show that in the study case the geometrical dispersion dominates the Taylor dispersion. However the&#xd;
interpretation with the ENM model shows a weak transitional regime from geometrical dispersion to Taylor&#xd;
dispersion for high flow rates.</dc:description>
   <dc:description>Postprint (published version)</dc:description>
   <dc:date>2014</dc:date>
   <dc:type>Conference report</dc:type>
   <dc:identifier>Chierubini, C. [et al.]. Non-linear fractal percolation experiments in carstic and aggregation soils. A: European Geosciences Union General Assembly. "Geophysical Research Abstracts". Vienna: 2014, p. 16436-16437.</dc:identifier>
   <dc:identifier>1607-7962</dc:identifier>
   <dc:identifier>https://hdl.handle.net/2117/25088</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:relation>http://www.geophysical-research-abstracts.net/</dc:relation>
   <dc:rights>http://creativecommons.org/licenses/by-nc-nd/3.0/es/</dc:rights>
   <dc:rights>Open Access</dc:rights>
   <dc:rights>Attribution-NonCommercial-NoDerivs 3.0 Spain</dc:rights>
   <dc:format>2 p.</dc:format>
   <dc:format>application/pdf</dc:format>
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