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John A. Cherry

Researcher at University of Guelph

Publications -  237
Citations -  16717

John A. Cherry is an academic researcher from University of Guelph. The author has contributed to research in topics: Aquifer & Groundwater. The author has an hindex of 71, co-authored 234 publications receiving 15792 citations. Previous affiliations of John A. Cherry include University of Arizona & University of Illinois at Urbana–Champaign.

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Groundwater contamination: pump-and-treat remediation

TL;DR: In this paper, the authors explore reasons for the observed difficulty of groundswater cleanup and note some implications that become clear during this process, focusing mainly on organic contaminants, the most health-threatening chemicals detected in groundwater and because the greatest difficulties in groundwater remediation have been encountered at organic contamination sites.
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A natural gradient experiment on solute transport in a sand aquifer: 1. Approach and overview of plume movement

TL;DR: A large-scale field experiment on natural gradient transport of solutes in groundwater has been conducted at a site in Borden, Ontario as discussed by the authors, where over 19,900 samples have been collected over a 3-year period.
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Stable Isotopes of Oxygen and Nitrogen in Source Identification of Nitrate from Septic Systems

TL;DR: In this paper, stable isotopes, 15N and 18O, have been used as tracers to differentiate a contaminant nitrate plume emanating from a single domestic septic system, in a ground-water system characterized by high and similar nitrate content outside and inside of the contaminant plume.
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Migration of contaminants in groundwater at a landfill: A case study: 4. A natural-gradient dispersion test

TL;DR: A natural-gradient tracer test using a chloride solution with an initial injection volume of 0.7 m 3 was performed in the sandy aquifer at the Borden site as mentioned in this paper.
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A Field Exercise on Groundwater Flow Using Seepage Meters and Mini-piezometers

TL;DR: In this article, basic principles of physical hydrogeology and the nature of the hydrologic interactions between groundwater and surface water can be convincingly demonstrated in the field using two inexpensive and inexpensive tools.