2017
DOI: 10.1016/j.jhydrol.2017.06.042
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A 3-D numerical model of the influence of meanders on groundwater discharge to a gaining stream in an unconfined sandy aquifer

Abstract: A 3-D numerical model of the influence of meanders on groundwater discharge to a gaining stream in an unconfined sandy aquifer. Journal of Hydrology, 552, 168-181. https://doi. Abstract 24Groundwater discharge to streams depends on stream morphology and groundwater flow direction, 25 but are not always well understood. Here a 3-D groundwater flow model is employed to investigate 26 the impact of meandering stream geometries on groundwater discharge to streams in an unconfined 27 and homogenous sandy aquifer at… Show more

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Cited by 22 publications
(24 citation statements)
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References 56 publications
(37 reference statements)
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“…These trends in the hydraulic head are consistent over time and the temporal changes in groundwater head monitored in screens located in the shallow unconfined aquifer at wells 1448 and 1495 are similar to changes in stream water level (Balbarini et al ). Thus, groundwater flow conditions can be described by assuming a steady‐state simulation.…”
Section: Resultssupporting
confidence: 64%
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“…These trends in the hydraulic head are consistent over time and the temporal changes in groundwater head monitored in screens located in the shallow unconfined aquifer at wells 1448 and 1495 are similar to changes in stream water level (Balbarini et al ). Thus, groundwater flow conditions can be described by assuming a steady‐state simulation.…”
Section: Resultssupporting
confidence: 64%
“…The groundwater equipotential lines (m asl) and labels are marked with darker blue lines and numbers, respectively. The hydropotential map was developed by Balbarini et al () based on hydraulic head measurements from March 25 to 27, 2012. Wells used to develop the groundwater flow model and to collect contaminant concentration samples are indicated by black dots.…”
Section: Study Sitementioning
confidence: 99%
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“…Most of the highest contaminant concentrations are located in the upper meltwater sand. The focus of this study is on the upper aquifer, which is in close hydraulic contact with the stream (Balbarini et al, ). The control plane (S–S′) employed to estimate the contaminant mass discharge at the Grindsted stream is located perpendicular to the groundwater flow and parallel to the stream meander (Figure c).…”
Section: Field Sitesmentioning
confidence: 99%
“…A sketch of the contaminant plume of total chlorinated ethenes is illustrated (using measurements from groundwater samplings from the water table to 3 m below). The approximate flow direction of the plume (shown as blue arrows) is derived from isopotential curves and groundwater flow modeling carried out at the site (Balbarini et al ; Rønde et al ). The dashed lines at the bottom map indicate the location of the cross sections described in the Methods section and Figure .…”
Section: Study Sitementioning
confidence: 99%