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out in heterogeneous and anisotropic littoral silts and sands. A field site was instrumented<br />

with five direct-push wells arranged in a diamond pattern using about 10-m spacing. Direct-push<br />

wells were installed with long screens placed in direct contact with natural sediments,<br />

thus allowing flexibility in the design of high-resolution hydraulic tests using packers.<br />

In these wells, horizontal K (Kh) was estimated at a 15-cm spacing using an electromagnetic<br />

flowmeter and multilevel slug tests, while Kh, K anisotropy (Kv/Kh) and specific storage (Ss)<br />

were characterized at 60-cm vertical intervals using vertical interference slug tests within a<br />

well and tomographic slug tests across wells. Furthermore, sediment samples were collected<br />

near the wells to assess Kh and Kv using grain size analyses and laboratory permeameter tests,<br />

respectively. The hydraulic property fields obtained from the different measurement methods<br />

were then quantitatively evaluated by predicting transient head responses from independent<br />

hydraulic tests using a forward numerical model. Results show that independent hydraulic<br />

tests are fairly well reproduced with vertical interference slug tests. So, even though this approach<br />

requires more complex numerical inverse analysis than conventional hydraulic tests<br />

with analytical solutions, it proves to be relatively time efficient considering that Kh, Kv/Kh<br />

and Ss can be estimated together. Tomographic slug tests are also shown to better represent<br />

transient hydraulic responses between wells, but the additional instrumentation costs and<br />

data burden involved compared to vertical interference slug tests should be carefully considered<br />

for practical field studies. Finally, this study shows that the strong Kv/Kh anisotropy<br />

at the scale of test measurements can make K characterization challenging. The study also<br />

highlights the need for hydraulic methods that can reliably estimate Kv/Kh, since groundwater<br />

flow is strongly influenced by K anisotropy.<br />

262 - Advanced techniques for site characterization: Real-Time<br />

High-Resolution Site Characterization of the Subsurface Using<br />

and MIP, LIF and HPT<br />

Patrick O’Neill<br />

Vertex Environmental Inc, Cambridge, Ontario, Canada<br />

In-situ site characterization can be a key component of site delineation and remediation.<br />

In-situ site characterization allows for large amounts of detailed data to be collected quickly<br />

and cost-effectively compared to traditional techniques. These data, combined with traditional<br />

Phase II Environmental Site Assessment (ESA) methods, greatly enhance the understanding<br />

of the presence, concentration and distribution of contaminants in the subsurface,<br />

which can lead to more efficient and focused monitoring and remediation programs.<br />

Three high-resolution characterization technologies have recently been introduced to<br />

Canada. These include, the Membrane Interface Probe (MIP) for dissolved phase contamination,<br />

the Laser-Induced Fluorescence (LIF) probe for free-phase petroleum hydrocarbon<br />

(PHC) contamination, and the Hydraulic Profiling Tool (HPT) for measuring<br />

the subsurface permeability and ultimately estimating the hydraulic conductivity of the<br />

subsurface. All three probes are advanced to depth by direct push methods (Geoprobe).<br />

The MIP is a heated probe that is used to volatilize dissolved and sorbed contaminants.<br />

The contaminants diffuse through a semi-permeable membrane on the probe and are sub-<br />

100 IAH-CNC 2015 WATERLOO CONFERENCE

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