2017
DOI: 10.2495/wrm170221
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Integrating Numerical Models in River Basin Management Plans: The Freewat Project

Abstract: The EU Water Framework Directive (WFD) requires the achievement of good status in the water environment through the implementation of River Basin Management Plans (RBMP). The long-term impact of these plans and their contribution to the achievement of good status is however generally difficult to predict and quantify, thus presenting an important constraint in this planning process. Numerical models are a tool which can enable water managers to predict the effective impact of measures on a water-body scale, an… Show more

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Cited by 3 publications
(3 citation statements)
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“…[2010]; b: Cassar [2010]; c: Cooke et al. [2018]; d: Bakalowicz and Mangion [2003]; e: Sapiano, Schembri, Debattista, and Theuma [2017] and Sapiano, Schembri, and Debattista [2017]; f: ERA [2015]) and combined with measured data obtained from core samples (porosity, hydraulic conductivity, density, and resistivity) and P‐wave velocities measured within borehole BH3 using a three‐component geophone and hydrophone streamer with an offset of 10.6 m. UCL‐T and LCL‐X are incomplete due to insufficient saturation during laboratory measurements, indicating low permeability. Computed porosities derived from the ratio of saturated water volume to sample volume coincide well with literature values, whereas measured hydraulic conductivities are several orders of magnitude smaller.…”
Section: Methods and Resultsmentioning
confidence: 99%
“…[2010]; b: Cassar [2010]; c: Cooke et al. [2018]; d: Bakalowicz and Mangion [2003]; e: Sapiano, Schembri, Debattista, and Theuma [2017] and Sapiano, Schembri, and Debattista [2017]; f: ERA [2015]) and combined with measured data obtained from core samples (porosity, hydraulic conductivity, density, and resistivity) and P‐wave velocities measured within borehole BH3 using a three‐component geophone and hydrophone streamer with an offset of 10.6 m. UCL‐T and LCL‐X are incomplete due to insufficient saturation during laboratory measurements, indicating low permeability. Computed porosities derived from the ratio of saturated water volume to sample volume coincide well with literature values, whereas measured hydraulic conductivities are several orders of magnitude smaller.…”
Section: Methods and Resultsmentioning
confidence: 99%
“…The MSLA system takes the shape of a freshwater lens floating above saltwater. The occurrence of groundwater abstractions threatens the hydrodynamic balance at the saltwater/freshwater interface, triggering intrusion of saltwater [44]. According to Malta's 2nd Water Catchment Management Plan (WCMP) [45], the Gozo MSLA system is in poor quantitative status and a deep assessment of its evolution in response to climate change and overexploitation is necessary, in order to identify management strategies to fulfil WCMP requirements.…”
Section: Island Of Gozo Maltamentioning
confidence: 99%
“…Hydraulic conductivity, porosity and specific storage of the geological formations outcropping across the Maltese Islands (average values)[33,34,[36][37][38][39][40][41][42][43].…”
mentioning
confidence: 99%