4.7 Article

Optimizing short time-step monitoring and management strategies using environmental tracers at flood-affected bank filtration sites

期刊

SCIENCE OF THE TOTAL ENVIRONMENT
卷 750, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.scitotenv.2020.141429

关键词

Pumping schemes; Quality precursors; Environmental tracer; Temperature; Stable isotopes; Electrical conductivity

资金

  1. Natural Sciences and Engineering Research Council of Canada (NSERC) [CRSNG-RDCPJ: 523095-17, CRSNG-RGPIN-2016-06780]
  2. Canada Graduate Scholarships-Master's (CGS M) program
  3. Geotop (Canada)

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Bank filtration is a common pre-treatment method for producing drinking water, but it can be vulnerable to contamination during flood events. Monitoring strategies for environmental tracers can help optimize water quality management decisions, especially in anticipating short timescale variability in water quality.
Bank filtration is a popular pre-treatment method to produce drinking water as it benefits from the natural capacity of the sediments to attenuate contaminants. Under flood conditions, bank filtration systems are known to be vulnerable to contamination, partly because flow patterns may evolve at short timescales and result in a rapid evolution of the origin and travel times of surface water in the aquifer. However, high frequency monitoring for water quality is not common practice yet, and water quality management decisions for the operation of bank filtration systems are typically based on weekly to monthly assays. The aim of this study is to illustrate how monitoring strategies of environmental tracers at flood-affected sites can be optimized and to demonstrate how tracer-based evidence can help to define adequate pumping strategies. Data acquisition spanned two intense flood events at a two-lake bank filtration site. Based on bacteriological indicators, the bank filtration system was shown to be resilient to the yearly recurring flood events but more vulnerable to contamination during the intense flood events. The origin of the bank filtrate gradually evolved from a mixture between the two lakes towards a contribution of floodwater and one lake only. Automatized measurements of temperature and electrical conductivity at observation wells allowed to detect changes in the groundwater flow patterns at a daily time-scale, while the regulatory monthly monitoring for indicator bacteria did not fully capture the potential short timescale variability of the water quality. The recovery to pre-flood conditions was shown to be accelerated for the wells operating at high rates (i.e., >= 1000 m(3)/day), partly because of floodwater storage in the vicinity of the less active wells. These results establish new perspectives to anticipate water quality changes through selected pumping schemes, which depend on and must be adapted to site-specific water quality issues. (C) 2020 Elsevier B.V. All rights reserved.

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