GEOTECHNICAL ENGINEERING
Austin, USA
contact@geotechnical-engineering1.org
HomeIn-Situ TestingField permeability test (Lefranc/Lugeon)

Field Permeability Testing (Lefranc & Lugeon) in Austin

The difference between building near Lake Austin and developing on the clay-rich uplands east of I-35 isn't just the view. It's the water. In Westlake Hills, fractured limestone of the Edwards Formation can drain a pond in hours if you don't quantify the mass permeability correctly. Over in the Blackland Prairie zones, tight expansive clays hold water and create hydrostatic pressure against basement walls. Both scenarios demand the same thing before you move a single yard of dirt: reliable field permeability data. Our team runs Lefranc tests in soil boreholes and Lugeon tests in rock to give you the in-situ hydraulic conductivity numbers that desk studies can't predict. When we combine these with test pits for visual soil profiling, you get a complete picture of how water moves through your site.

A single packer test in fractured limestone can save a developer from a multimillion-dollar water inflow problem during excavation.

Methodology and scope

Central Texas weather doesn't do subtle. A dry month can crack the ground open, then a single storm drops six inches of rain and suddenly your retention basin is an accidental swimming pool. Field permeability testing bridges the gap between lab estimates and what the ground actually does under fluctuating moisture. The Lefranc method gives us a point measurement in soil, either by constant head or falling head, and it's ideal for infiltration galleries and stormwater management design per City of Austin drainage criteria. When we hit the Glen Rose limestone, we switch to the Lugeon test: packer-isolated stages under controlled pressure. This tells us if the rock mass needs grouting before you excavate or if your anchor bond zone will hold. We run the numbers against ASTM D6391 and local experience with the Edwards Aquifer rules.
Field Permeability Testing (Lefranc & Lugeon) in Austin

Local considerations

The most common mistake we see in Austin is contractors assuming a soil boring log is enough to design an infiltration system. It isn't. A visual classification of 'silty clay' tells you nothing about field hydraulic conductivity, and that number can vary by two orders of magnitude depending on macropores, root holes, or fissures in the weathered rock. We've inspected detention basins that failed because the designer used a textbook permeability value from the lab while the actual in-situ rate was 10 times lower. The basin overflowed into the adjacent property, and the legal headache lasted two years. A two-hour Lefranc test during the geotechnical investigation would have caught the discrepancy. If your project falls within the Edwards Aquifer contributing zone, additional in-situ permeability documentation is not optional; it's a regulatory requirement for TCEQ compliance.

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Regulatory framework

Field permeability testing in Austin (Lefranc & Lugeon) conforms to ASTM D6391-11, ASTM D2487-17e1, ASTM D1586-18, the City of Austin Environmental Criteria Manual, and the TCEQ Edwards Aquifer Protection Program.

Other technical services

01

Lefranc Permeability in Soil

Constant and falling head tests in soil boreholes for infiltration rate design, stormwater compliance, and retention pond sizing. We test at multiple depths to capture vertical variability in the soil profile.

02

Lugeon Testing in Rock Mass

Single and double packer tests in NQ/HQ core holes to evaluate rock mass permeability. Essential for grouting design, deep excavation planning, and slope stability analysis in the Edwards Limestone.

03

Permeability for Environmental Compliance

Testing programs designed to meet TCEQ requirements for the Edwards Aquifer contributing and recharge zones. We coordinate with your environmental consultant to deliver defensible data for permit applications.

Typical parameters

ParameterTypical value
Test methodASTM D6391 (Lefranc/Lugeon)
Soil test typeConstant head or falling head
Rock test zonesPacker-isolated, single or double
Typical test depth10 to 150 ft below grade
Reporting outputHydraulic conductivity k (cm/s)
Lugeon value interpretation1 to 100+ Lugeons
Aquifer protection complianceTCEQ Edwards Aquifer rules

Frequently asked questions

What does a Lefranc or Lugeon test cost in Austin?
How long does a field permeability test take on site?

A single Lefranc test in soil usually takes 45 to 90 minutes once the drill rig reaches the target depth. A multi-stage Lugeon test in rock can take two to four hours depending on the number of pressure stages and the packer setup time. We can typically complete a standard program of four to six tests in one field day.

Do I need a Lugeon test or is a Lefranc test enough?

It depends on the geology at your test depth. If you are testing in soil, residual clay, or completely weathered rock, a Lefranc test is appropriate. If you are testing in competent limestone where fractures control the flow, you need a Lugeon test with a packer system. Many Austin sites require both, starting with Lefranc in the upper soil zone and switching to Lugeon once we hit bedrock.

Can you test below the water table?

Yes, we routinely perform Lefranc and Lugeon tests below the water table. For these tests we use a falling head method in soil or constant pressure injection in rock. The data is corrected for hydrostatic pressure and we report the in-situ saturated hydraulic conductivity. This is common for deep excavations and basement waterproofing design in Austin.

Location and service area

We serve projects across Austin and surrounding areas.

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