The Florida peninsula presents a unique geotechnical profile for pavement engineers, and Orlando sits squarely on the sandy ridges of the Central Florida Highlands. Beneath the asphalt of I-4 and the sprawling subdivisions of Orange County lies a mix of Pleistocene-age sands, silty sands, and occasional clay lenses that can vary drastically within a single project site. The water table here often sits just three to six feet below the surface, which means subgrade strength measured at construction may not reflect conditions once the pavement has seen a few wet seasons. A laboratory CBR test, conducted in strict accordance with ASTM D1883, gives us the soaked bearing capacity values that are essential for designing flexible and rigid pavements that will survive Central Florida's intense summer rainfall without rutting or cracking. When we prepare samples at optimum moisture from a Proctor test and then soak them for 96 hours, we simulate the worst-case scenario the subgrade will face after years of service. This soaked CBR value becomes the cornerstone of the structural design, dictating everything from base course thickness to the need for lime or cement stabilization before placing the asphalt.
A soaked CBR value under 3% in Central Florida's sandy silts signals that subgrade stabilization is not optional — it is a prerequisite for any pavement that will carry truck traffic.
Method and coverage
In Orlando, we frequently see contractors surprised when a sandy fill that looks excellent in the field yields a soaked CBR below 5%. The culprit is almost always fines content that went unnoticed during visual classification. Our laboratory procedure begins with remolding the sample at the target density and moisture content determined by the
Proctor test, then submerging it in water with a surcharge load that simulates the weight of the pavement structure. Over four days of soaking, we record swell measurements and then penetrate the sample with a 1,954-square-inch piston at 0.05 inches per minute. The load readings at 0.1 and 0.2 inches of penetration are compared against the standard crushed stone reference to calculate the CBR percentage. For soils with significant gravel content, we often run a companion
grain size analysis to verify the material meets FDOT specifications for select fill or limerock base. What makes Orlando different from coastal Florida is the presence of sandy soils with just enough silt to create capillary action that keeps the subgrade saturated long after the rain stops. We see this most clearly in the Winter Park and Pine Hills areas, where the fine sand matrix holds water against gravity and can reduce effective CBR by 30 to 40 percent compared to the unsoaked value.
Top questions
How much does a laboratory CBR test cost in Orlando?
A standard laboratory CBR test on a single sample generally ranges from US$110 to US$180, depending on whether you need unsoaked only or the full 96-hour soaked procedure with swell measurements. The price varies based on the number of compaction points required to establish the moisture-density relationship and whether the sample needs to be remolded to a specified field density.
What is the difference between field CBR and laboratory CBR, and which one does FDOT require for design?
Field CBR tests are performed in situ using a portable loading device and are useful for rapid quality control during construction. Laboratory CBR tests, conducted under ASTM D1883, control moisture content, density, and soaking conditions precisely. FDOT pavement design procedures are calibrated to laboratory soaked CBR values because they represent the worst-case subgrade condition. For final structural design, the laboratory value is the one that matters.
How long does it take to get CBR test results?
A full soaked CBR test requires a minimum of five working days: one day for compaction and sample preparation, four days for the soaking period under surcharge, and a few hours for the penetration test and data reduction. We can provide preliminary unsoaked results in two days if the project schedule demands early direction on subgrade suitability.