Bank filtration is often utilized at groundwater intake plants located in sand and gravel-dominated glaciofluvial formations bordered by a lake or a river. Bank filtration is favourable, since it can increase the amount of water that can be sustainably abstracted from an aquifer, and it may balance changes in the groundwater level. On the other hand, bank filtration may lower groundwater quality if the quality of infiltrating surface water is not sufficient. To provide up-to-date information for risk management and preparedness plans that are applicable to groundwater intake plants utilising bank filtration, several tools and methods were tested. A feasible test site was selected for piloting to better understand the processes that take place during bank filtration. Several traditional research methods were used to map the geological structure of the test aquifer. In addition, methods to assess seasonal changes in groundwater recharge patterns and groundwater quantity, as well as surface water and groundwater quality, were tested and piloted. The studies enabled the identification of infiltration zones from the lake to the aquifer, as well as the main groundwater flow paths within the aquifer. The conducted studies also provided practical experience on how to best monitor any future changes in natural surface water–groundwater interaction, as well as in induced bank filtration, expected due to climate change or increasing water demand.
Read full abstract- All Solutions
Editage
One platform for all researcher needs
Paperpal
AI-powered academic writing assistant
R Discovery
Your #1 AI companion for literature search
Mind the Graph
AI tool for graphics, illustrations, and artwork
Unlock unlimited use of all AI tools with the Editage Plus membership.
Explore Editage Plus - Support
Overview
5251 Articles
Published in last 50 years
Articles published on Surface Water Quality
Authors
Select Authors
Journals
Select Journals
Duration
Select Duration
5118 Search results
Sort by Recency