Long Term Effectiveness of Wellhead Protection Areas

A preventive instrument to ensure the protection of groundwater is the establishment of wellhead protect areas (WPA) for public supply wells. The shape of the WPA depends on the rate of pumping and aquifer characteristics, such as the transmissivity, porosity, hydraulic gradient, and aquifer thickne...

Full description

Bibliographic Details
Main Authors: Almeida, C. (Author), Carvalho, J.M (Author), Carvalho, M.D.R (Author), Paiva, M. (Author), Zeferino, J. (Author)
Format: Article
Language:English
Published: MDPI 2022
Subjects:
Online Access:View Fulltext in Publisher
LEADER 03217nam a2200541Ia 4500
001 10-3390-w14071063
008 220425s2022 CNT 000 0 und d
020 |a 20734441 (ISSN) 
245 1 0 |a Long Term Effectiveness of Wellhead Protection Areas 
260 0 |b MDPI  |c 2022 
856 |z View Fulltext in Publisher  |u https://doi.org/10.3390/w14071063 
520 3 |a A preventive instrument to ensure the protection of groundwater is the establishment of wellhead protect areas (WPA) for public supply wells. The shape of the WPA depends on the rate of pumping and aquifer characteristics, such as the transmissivity, porosity, hydraulic gradient, and aquifer thickness. If any parameter changes after the design of the WPA, it will no longer be effective in protecting the aquifer and its catchment. With population growth in urban areas, the pressure on groundwater abstraction increases. Changes in flow, drawdowns and hydraulic gradients often occur. The purpose of this work is to evaluate the effectiveness of the WPA after a long period of establishment, in public wells with continuous pumping, located in densely populated urban area of the municipality of Montijo (Portugal). Considering the aquifer scenario in 2020, new extended WPAs were calculated using the combined results of three analytical methods and numerical modelling. In 2009 the aquifer presented hydraulic gradients varying between 0.0005 and 0.002, giving rise to a protection area with essentially circular shape. Although there was no increase in extraction flow, in 2020 the hydraulic gradients vary from 0.0008 to 0.008, and the flow directions have changed because of the water level decline. The shape of the WPA in this case is essentially elliptical and longer upstream and it can pose difficulties in the protection of public water catchments, in an urban area with already defined and consolidated land use. The best protection of the public supply wells in disturbed aquifers is obtained through numerical modeling. © 2022 by the authors. Licensee MDPI, Basel, Switzerland. 
650 0 4 |a Analytical method 
650 0 4 |a analytical methods 
650 0 4 |a Aquifer characteristics 
650 0 4 |a Aquifer thickness 
650 0 4 |a Aquifers 
650 0 4 |a Catchments 
650 0 4 |a groundwater 
650 0 4 |a Groundwater resources 
650 0 4 |a Hydraulic gradients 
650 0 4 |a Hydrogeology 
650 0 4 |a Land use 
650 0 4 |a Numerical methods 
650 0 4 |a numerical modeling 
650 0 4 |a Numerical models 
650 0 4 |a Parameter changes 
650 0 4 |a population growth 
650 0 4 |a Population statistics 
650 0 4 |a Portugal 
650 0 4 |a protected area 
650 0 4 |a Protection of groundwater 
650 0 4 |a Public supply wells 
650 0 4 |a Runoff 
650 0 4 |a Transmissivity 
650 0 4 |a Urban areas 
650 0 4 |a Urban growth 
650 0 4 |a Water levels 
650 0 4 |a wellhead 
650 0 4 |a wellhead protection area 
650 0 4 |a Wellhead protection areas 
650 0 4 |a Wellheads 
700 1 |a Almeida, C.  |e author 
700 1 |a Carvalho, J.M.  |e author 
700 1 |a Carvalho, M.D.R.  |e author 
700 1 |a Paiva, M.  |e author 
700 1 |a Zeferino, J.  |e author 
773 |t Water (Switzerland)