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Field Permeability Testing in Missoula: Lefranc & Lugeon Solutions

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The Missoula Valley sits on an ancient glacial lakebed, where layers of silt, clay, and deep gravel channel the Clark Fork River’s groundwater. When a foundation hits clean gravel here, water flows fast—and that changes everything about your excavation plan. Contractors breaking ground near the aquifer in the Rattlesnake area or along the Bitterroot River quickly learn that surface guesses don’t work. A field permeability test removes that guesswork. Whether it’s a falling-head Lefranc method in fine alluvium or a Lugeon packer test in fractured bedrock near Mount Jumbo, we give you the in-situ hydraulic conductivity values that Missoula County plan reviewers expect. For projects requiring deeper stratigraphic control, we often pair this data with an SPT drilling program to verify soil layering across the site.

In Missoula’s glacio-fluvial deposits, a single Lugeon value can define the difference between a dry excavation and a flooded jobsite.

How we work

A common mistake in western Montana is treating all glacial till like impermeable barrier. Missoula’s geology is far more complex. We’ve seen projects where a single seam of openwork gravel beneath a dense lodgement till drained a dewatered excavation in under two hours. That’s a costly halt. The Lefranc test gives us a precise permeability coefficient at discrete depths in soil, while the Lugeon test applies steady pressure in rock to quantify joint connectivity and grout take. Our field teams run these tests using calibrated standpipes and downhole packers, following IBC Chapter 18 groundwater investigation requirements. We measure both transient and steady-state flow, delivering values in cm/sec that your geotechnical engineer can plug directly into seepage models or dewatering system designs without scaling errors from lab-to-field conversion.
Field Permeability Testing in Missoula: Lefranc & Lugeon Solutions
Technical reference image — Missoula

Local considerations

Missoula’s urban growth has pushed development onto the valley floor’s lower terraces, where the static water table often sits within ten feet of the surface. Older neighborhoods near the Clark Fork were built before modern drainage codes, and today’s infill projects face far stricter dewatering regulations. If you underestimate the mass permeability of a gravelly deposit here, you don’t just get a wet basement—you risk triggering settlement in adjacent structures as groundwater drawdown compresses the surrounding silt. A Lefranc test in the saturated zone gives your engineer the real k-value to design a wellpoint system that works, not one that barely keeps up. The City of Missoula Public Works requires groundwater control plans for any excavation deeper than the water table, and a field permeability test is the foundation of that submittal.

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Typical values

ParameterTypical value
Test MethodsLefranc (variable/failing head) in soil; Lugeon (packer test) in rock
Applicable FormationsGlacial till, lacustrine silt, alluvial gravel, fractured Belt Supergroup rock
Measured ParameterCoefficient of permeability (k) in cm/sec
Packer ConfigurationSingle or double pneumatic packer per NX/NQ borehole
Pressure StagesMulti-stage pressure steps per Houlsby criteria
Data OutputFlow vs. pressure plots, Lugeon values, transmissivity estimates
Reporting StandardASTM D6391 for Lugeon procedures; ASCE 7 groundwater provisions

Related services

01

Lefranc Test in Soil

We install a slotted standpipe in a borehole, seal the test section with bentonite, and measure head recovery. Ideal for the sandy silt and gravel lenses common in the Missoula Valley. Delivers a point-specific k-value that accounts for the natural soil fabric.

02

Lugeon Test in Rock

Using a wireline-deployed packer in NQ drillholes, we isolate fractured zones in the Belt Supergroup metasediments. We apply incremental pressure cycles to quantify rock mass permeability and identify the threshold for hydrojacking or grout take.

Regulatory framework

IBC 2021: Section 1803 (Geotechnical Investigations), ASCE 7-22: Groundwater Load Provisions, ASTM D6391: Lugeon Test, ASTM D2434: Permeability of Granular Soils (Lab Reference)

Questions and answers

How much does a field permeability test cost in Missoula?

A single Lefranc or Lugeon test in the Missoula area typically runs between US$610 and US$980 per test section. The final cost depends on borehole depth, number of pressure steps, and whether we need to coordinate with your driller or mobilize our own rig.

When does Missoula County require a Lugeon test instead of a Lefranc?

The county generally requires a Lugeon test when your excavation or foundation interacts with fractured bedrock—common on the slopes of Mount Sentinel or in the Rattlesnake foothills. If the geotechnical report identifies rock with visible jointing, a packer test quantifies the fracture flow that a Lefranc test cannot measure.

What’s the difference between a falling-head and constant-head Lefranc test?

We select the method based on soil type. In Missoula’s silty deposits, where permeability is low, a falling-head test is faster and equally accurate. In cleaner sands and gravels, a constant-head test maintains a steady water level so we can measure flow directly, avoiding the rapid drainage that skews falling-head readings.

Location and service area

We serve projects in Missoula and surrounding areas.

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