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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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Numerical analysis of heat transport within fractured sedimentary rock: implications for temperature probes

TL;DR: In this article, thermal energy transport from ground surface into a fractured sedimentary rock aquifer is simulated numerically to gain insight into the response of temperature probes for identifying hydraulically active fractures in rock boreholes.
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Design of a Ground-Water Sampler for Collecting Volatile Organics and Dissolved Gases in Small-Diameter Wellsa

TL;DR: In this paper, a sampling device is described which collects ground-water samples containing volatile organic compounds and dissolved gases, and is designed to be lowered in a well to the desired depth, depressurized to slightly below the in situ pressure to allow entry of the sample and then repressurized prior to being returned to the surface.
Posted ContentDOI

Flowing wells: history and role as a root of groundwater hydrology

TL;DR: In this article, a review of the role of aquitards in the evolution of groundwater hydrology can be found, which can lead to a deeper understanding of the evolution and evolution of underground hydrology.
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Multiple lines of field evidence to inform fracture network connectivity at a shale site contaminated with dense non-aqueous phase liquids

TL;DR: In this paper, a conceptual model of the fracture networks in shale was evaluated at a site contaminated with chlorinated solvents and the results indicated a well-connected fracture network with many hydraulically active fractures not influenced by open hole cross-connection.
Journal Article

Internal characteristics of a bromide tracer zone during natural flow in the Borden aquifer, Ontario, Canada.

TL;DR: A planned natural gradient bromide tracer experiment, over a distance of 100 m, is in progress in a forest area at Canadian Forces Base Borden, Ontario, to provide information for the design of a monitoring network for a subsequent experiment involving a release of a three-component chlorinated solvent DNAPL into the unconfined sand aquifer as mentioned in this paper.