The impact of aquifer stratification on saltwater intrusion characteristics. Comprehensive laboratory and numerical study. Issue 4 (29th April 2021)

• Record Type: Journal Article
• Authors: Etsias, Georgios; Hamill, Gerard A.; Águila, Jesús F.; Benner, Eric M.; McDonnell, Mark C.; Ahmed, Ashraf A.; Flynn, Raymond
• Is Part Of: Hydrological processes. Volume 35:Issue 4(2021)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2021-04-29
• Subjects: angle of intrusion -- aquifer heterogeneity -- aquifer stratification -- laboratory experiments -- saline intrusion -- SUTRA -- toe length -- width of the mixing zone; Hydrology -- Periodicals; Hydrology -- Research -- Periodicals; Hydrologic models -- Periodicals; Hydrological forecasting -- Periodicals; 631.432
• DOI: 10.1002/hyp.14120
• Languages: English
• ISSNs: 0885-6087

Abstract

Abstract: 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. Abstract : The length of saline intrusion in stratified aquifers is positively correlated to layer permeability contrast, total aquifer transmissivity and the number of strata. Permeability contrast between layers, their width, and relative position significantly impact the width of mixing zone and angle of intrusion. The presence of a low permeability upper layer results in the confinement of the saltwater wedge in the lower part of the aquifer until a critical head difference is applied to the system.