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In-Situ Permeability Testing with Lefranc & Lugeon Methods in Orlando

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A contractor excavating for a stormwater retention pond near Lake Nona hit saturated sand at just six feet depth. The water inflow slowed production to a crawl, and the dewatering plan on paper no longer matched reality. That scenario plays out across Orlando more often than developers expect, given the high water table that sits just below our sandy surface soils. A field permeability test — specifically the Lefranc or Lugeon method — delivers the in-situ hydraulic conductivity values you need to size pumps, design cutoff walls, or calculate infiltration rates before the first bucket hits the ground. Whether you’re working on a municipal drainage project in Winter Park or a commercial foundation in the tourist corridor, knowing how water actually moves through the formation, rather than relying on lab estimates from disturbed samples, changes the entire approach. We pair these tests with test pits when visual soil profiling helps target the right test intervals, and lean on grain-size data to confirm the permeability range we measure in the field.

Lab permeability from reconstituted samples tells you what the soil could do. A Lefranc or Lugeon test tells you what the formation actually does, in place, under real groundwater conditions.

Method and coverage

ASTM D6391 governs the downhole permeability test procedures we run, but the value of a Lefranc or Lugeon test in Orlando goes beyond checking a specification box. The city sits on a mix of Pleistocene sands, silty lenses, and in many areas, the upper Floridan aquifer within reach of construction depths — a hydrogeologic setting where packer tests (Lugeon) in boreholes reveal fracture flow and variable permeability zones that steady-state Lefranc tests in granular soils might miss. We execute falling-head, rising-head, and constant-head configurations depending on the formation response, and we use inflatable packers for rock intervals to isolate specific fracture zones. For projects near the Wekiva Basin or any area with protected wetlands, demonstrating accurate infiltration rates with field data — not textbook assumptions — keeps permitting moving. That same precision matters when engineers design dewatering systems for deep excavations along I-4 Ultimate corridor, where a misjudged permeability coefficient can mean the difference between a dry excavation and a flooded pit. Our in-situ permeability protocols integrate directly with the geotechnical baseline report, giving the design team a defensible number for numerical groundwater models.
In-Situ Permeability Testing with Lefranc & Lugeon Methods in Orlando
Technical reference image — Orlando

Regional considerations

The soil profile changes drastically between downtown Orlando’s sandy ridges and the lower-elevation areas near Boggy Creek, where organic silts and higher groundwater dominate. A project on the east side might encounter clean SP sands with permeability above 1x10^-3 cm/sec — fast draining but requiring aggressive dewatering. Move toward the Conway chain of lakes and you can hit interbedded silts where permeability drops two orders of magnitude, yet perched water creates localized instability that surprises crews. Skipping field permeability tests in either setting turns the dewatering design into guesswork. Undersized pumps flood the excavation and trigger sediment transport fines, potentially creating voids under adjacent pavement or utilities. Oversized systems waste fuel and rack up unnecessary rental costs. For infiltration-based stormwater designs now required by Orange County and City of Orlando code, overestimating permeability from grain-size correlations alone risks basin failure during the heavy summer rain season — exactly when the system must perform.

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Process video

Technical parameters

ParameterTypical value
Test methodLefranc (granular soils), Lugeon (rock/fractured)
ASTM standardASTM D6391-11 (reapproved 2020)
Test configurationsFalling head, rising head, constant head
Borehole diameter range4 to 8 inches typical for Lefranc
Packer type (Lugeon)Single or double inflatable packer
Typical test interval5 to 10 feet, formation-dependent
Reporting unitscm/sec or ft/day, as specified
Water source requirementClean water, truck-mounted tank or hydrant

Complementary services

01

Lefranc Variable-Head Test

Borehole permeability testing in granular soils above the water table. We run falling-head or rising-head protocols, measuring the rate of water level change to calculate hydraulic conductivity. Ideal for stormwater infiltration design and dewatering planning in Orlando's sandy formations.

02

Lugeon Packer Test

Pressurized water injection into discrete intervals of fractured limestone or weathered rock using single or double inflatable packers. Quantifies fracture permeability in Lugeon units and identifies zones of high water inflow critical for deep foundation design in karst-prone areas.

03

Dewatering Feasibility Assessment

Combines field permeability data with borehole logs and groundwater monitoring to estimate dewatering flow rates, radius of influence, and pumping duration. Delivers the numbers your contractor needs to size wellpoint or deep-well systems before mobilization.

Standards that apply

ASTM D6391-11 (2020): Standard Test Method for Field Measurement of Hydraulic Conductivity Using Borehole Infiltration, ASTM D2487-17: Standard Practice for Classification of Soils for Engineering Purposes (Unified Soil Classification System), Orange County Stormwater Management Manual (infiltration testing requirements)

Top questions

How much does a field permeability test cost in Orlando?

A single Lefranc or Lugeon test in the Orlando area typically runs between US$590 and US$1,070 per test interval, depending on depth, access conditions, and whether the borehole is already available or needs to be drilled. Multiple test intervals in the same borehole reduce the per-test cost. We provide a firm quote after reviewing the boring layout and target depths.

When is a Lugeon test required instead of a Lefranc test?

Use a Lugeon test when the formation is rock or heavily fractured material — common in Orlando where limestone of the Ocala Group sits at moderate depth. The Lugeon method uses a packer to isolate a specific section of the borehole and injects water under pressure, measuring fracture flow in Lugeon units. A Lefranc test is the right choice for granular soils above rock, where water flows through pore spaces rather than fractures.

How long does an in-situ permeability test take on site?

A single Lefranc test interval in sandy soil can stabilize within 30 to 60 minutes. Lugeon tests in fractured rock take longer — typically 90 minutes to 2 hours per interval — because we run multiple pressure steps to evaluate flow regime changes. The total field time depends on how many intervals you need tested and the drilling setup.

Can you run permeability tests in existing monitoring wells?

Yes, with some limitations. A rising-head or falling-head test can be performed in an existing well if the well screen and filter pack are appropriate for the formation being tested. The method is often called a slug test. Results are valid for the screened interval only, so if you need depth-specific data, a new borehole with open-hole or packer-isolated testing may be more useful.

Location and service area

We serve projects across Orlando and its metropolitan area.

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