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DC Field | Value | Language |
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dc.contributor.author | Etsias, G | - |
dc.contributor.author | Hamill, GA | - |
dc.contributor.author | Águila, JF | - |
dc.contributor.author | Benner, EM | - |
dc.contributor.author | McDonnell, MC | - |
dc.contributor.author | Ahmed, AA | - |
dc.contributor.author | Flynn, R | - |
dc.date.accessioned | 2023-09-16T19:18:28Z | - |
dc.date.available | 2023-09-16T19:18:28Z | - |
dc.date.issued | 2021-03-12 | - |
dc.identifier | ORCID iDs: Georgios Etsias https://orcid.org/0000-0002-6750-3994; Ashraf A. Ahmed https://orcid.org/0000-0003-4287-8295 | - |
dc.identifier | e14120 | - |
dc.identifier.citation | Etsias, G. et al. (2021) 'The impact of aquifer stratification on saltwater intrusion characteristics. Comprehensive laboratory and numerical study', Hydrological Processes, 35 (4), e14120, pp. 1 - 21. doi: 10.1002/hyp.14120. | en_US |
dc.identifier.issn | 0885-6087 | - |
dc.identifier.uri | https://bura.brunel.ac.uk/handle/2438/27207 | - |
dc.description | Data availability statement: The data that support the findings of this study are available from the corresponding author upon reasonable request. | en_US |
dc.description | Supporting Information is available online at https://onlinelibrary.wiley.com/doi/10.1002/hyp.14120#support-information-section . | - |
dc.description.abstract | Copyright © 2021 The Authors. Laboratory experiments and numerical simulations were utilized in this study to assess the impact of aquifer stratification on saltwater intrusion. Three homogeneous and six layered aquifers were investigated. Image processing algorithms facilitated the precise calculation of saltwater wedge toe length, width of the mixing zone, and angle of intrusion. It was concluded that the length of intrusion in stratified aquifers is predominantly a function of permeability contrast, total aquifer transmissivity and the number of heterogeneous layers, being positively correlated to all three. When a lower permeability layer overlays or underlays more permeable zones its mixing zone widens, while it becomes thinner for the higher permeability strata. The change in the width of the mixing zone (WMZ) is positively correlated to permeability contrast, while it applies to all strata irrespectively of their relative vertical position in the aquifer. Variations in the applied hydraulic head causes the transient widening of WMZ. These peak WMZ values are larger during saltwater retreat and are negatively correlated to the layer's permeability and distance from the aquifer's bottom. Moreover, steeper angles of intrusion are observed in cases where low permeability layers overlay more permeable strata, and milder ones in the inverse aquifer setups. The presence of a low permeability upper layer results in the confinement of the saltwater wedge in the lower part of the stratified aquifer. This occurs until a critical hydraulic head difference is applied to the system. This hydraulic gradient value was found to be a function of layer width and permeability contrast alike. | en_US |
dc.description.sponsorship | Engineering and Physical Sciences Research Council Standard Research. Grant Number: EP/R019258/1. | en_US |
dc.format.extent | 1 - 21 | - |
dc.format.medium | Print-Electronic | - |
dc.language | English | - |
dc.language.iso | en_US | en_US |
dc.publisher | Wiley | en_US |
dc.rights | Copyright © 2021 The Authors. Hydrological Processes published by John Wiley & Sons Ltd. This is an open access article under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits use, distribution and reproduction in any medium, provided the original work is properly cited. | - |
dc.rights.uri | https://creativecommons.org/licenses/by/4.0/ | - |
dc.subject | angle of intrusion | en_US |
dc.subject | aquifer heterogeneity | en_US |
dc.subject | aquifer stratification | en_US |
dc.subject | laboratory experiments | en_US |
dc.subject | saline intrusion | en_US |
dc.subject | SUTRA | en_US |
dc.subject | toe length | en_US |
dc.subject | width of the mixing zone | en_US |
dc.title | The impact of aquifer stratification on saltwater intrusion characteristics. Comprehensive laboratory and numerical study | en_US |
dc.type | Article | en_US |
dc.identifier.doi | https://doi.org/10.1002/hyp.14120 | - |
dc.relation.isPartOf | Hydrological Processes | - |
pubs.issue | 4 | - |
pubs.publication-status | Published | - |
pubs.volume | 35 | - |
dc.identifier.eissn | 1099-1085 | - |
dc.rights.holder | The Authors | - |
Appears in Collections: | Dept of Civil and Environmental Engineering Research Papers |
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FullText.pdf | Copyright © 2021 The Authors. Hydrological Processes published by John Wiley & Sons Ltd. This is an open access article under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits use, distribution and reproduction in any medium, provided the original work is properly cited. | 8.55 MB | Adobe PDF | View/Open |
This item is licensed under a Creative Commons License