Experimental and numerical investigation of saltwater intrusion dynamics on sloping sandy beach under static seaside boundary condition

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dc.contributor.author Dalai, Chitaranjan
dc.contributor.author Munusamy, Selva Balaji
dc.contributor.author Dhar, Anirban
dc.date.accessioned 2020-08-07T14:26:29Z
dc.date.available 2020-08-07T14:26:29Z
dc.date.issued 2020-10
dc.identifier.citation Dalai, Chitaranjan; Munusamy, Selva Balaji and Dhar, Anirban, "Experimental and numerical investigation of saltwater intrusion dynamics on sloping sandy beach under static seaside boundary condition", Flow Measurement and Instrumentation, DOI: 10.1016/j.flowmeasinst.2020.101794, vol. 75, Oct. 2020. en_US
dc.identifier.issn 0955-5986
dc.identifier.uri http://dx.doi.org/10.1016/j.flowmeasinst.2020.101794
dc.identifier.uri https://repository.iitgn.ac.in/handle/123456789/5594
dc.description.abstract Two-dimensional sandbox experiments were conducted to investigate the variable-density circulation and flow patterns in sloping beach configurations. The experiments provide new benchmark results for validating the sandbox models based on quantitative and qualitative measurements. Previous studies have considered density dependent flow in porous media, vertical beach face saltwater boundary, and multilayered hydrogeology ignoring a sloping beach face, which is a much more common phenomenon in real world. The present study considers sloping beach face under both homogeneous and low-permeability strata configurations. The geohydraulic processes encountered were quantified through pore-water pressure measurements and image analysis techniques. Moreover, validations were performed with numerical simulations (FEFLOW). A simple image analysis procedure is proposed with respect to two-dimensional laboratory scale benchmark experiments. Experimental results provided a detailed circulation flow path within and outside the saltwater wedge with sloping beach face. Fingering effect in porous media was also observed for both the experiments during initial time periods. Stability analysis shows the existence of a stationary convective flow pattern followed by gravitational instabilities under the quasi-steady state condition.
dc.description.statementofresponsibility by Chitaranjan Dalai, Selva Balaji Munusamy and Anirban Dhar
dc.language.iso en_US en_US
dc.publisher Elsevier en_US
dc.subject Saltwater intrusion en_US
dc.subject Circulation pattern en_US
dc.subject Pore water pressure en_US
dc.subject Sloping sandy beach en_US
dc.title Experimental and numerical investigation of saltwater intrusion dynamics on sloping sandy beach under static seaside boundary condition en_US
dc.type Article en_US
dc.relation.journal Flow Measurement and Instrumentation


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