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298 - Fracture network and groundwater flux characterization<br />

using a suite of high resolution methods in a sedimentary<br />

bedrock aquifer<br />

Lucas A.F.S. Ribeiro, Jessica R. Meyer, & Beth L. Parker<br />

G360 Centre for Applied Groundwater Research, School of Engineering, University of<br />

Guelph, Guelph, Ontario, Canada<br />

In fractured rocks, contaminant distribution and flux are strongly influenced by the characteristics<br />

and connectivity of fracture networks. This study focuses on characterizing the<br />

fracture network and hydraulics along a 2-D transect down-gradient of a DNAPL source<br />

zone in sedimentary rock. Five boreholes were continuously cored along the transect to<br />

depths between 55 and 63 mbgs. The lithology, sedimentary structures, and fractures observed<br />

in core were described in detail and were complemented by a comprehensive suite of<br />

borehole geophysics collected in the open boreholes. Active line source (ALS) temperature<br />

logging was collected in FLUTe lined holes to identify hydraulically active fractures under<br />

ambient conditions and hydraulic conductivity data were collected from FLUTe transmissivity<br />

profiling and straddle packer testing. Additionally, transient hydraulic heads were<br />

collected using transducer arrays installed behind FLUTe liners. The data collected from<br />

the core and open and lined boreholes were used to design Westbay MLSs to provide high<br />

resolution head profiles. 3-D fracture network characterization is achieved by combining<br />

the 5 transect borehole datasets with 11 boreholes containing similar datasets. Fracture<br />

scan-line surveys were also done in analogous formations in outcrops to provide regional<br />

structural trends and to inform fracture lengths, especially for vertical joint sets that inform<br />

the mechanical unit boundaries. The application of numerous high resolution borehole<br />

methods and the combined use of surface and borehole fracture datasets contribute to the<br />

definition of the site specific fracture network. The fracture network information is then<br />

integrated with the hydraulic data to provide robust estimates of groundwater flux across<br />

the 2-D transect enhancing the understanding of the present contaminant distribution and<br />

providing key information for discrete fracture network numerical models for groundwater<br />

flow and contaminant transport.<br />

POSTER SESSION:<br />

Groundwater Issues from Mining &<br />

Aggregates<br />

Thursday October 29, 16:40<br />

Room: Regent<br />

169 - Numerical Groundwater Modeling of the Lithium Brine<br />

Extraction at the Salar de Atacama<br />

152 IAH-CNC 2015 WATERLOO CONFERENCE

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