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These test methods detail the determination of the total or wet density of soil and soil-aggregate in place using nuclear gauges at shallow depths. The standard covers two primary configurations: the Backscatter Method, where the source and detectors remain on the surface, and the Direct Transmission Method, where the source or a detector is placed at a known depth of up to 300 mm (12 in.) below the surface.
The density of the material in mass per unit volume is determined by comparing the detected rate of gamma radiation against previously established calibration data. The Backscatter method is ideal for immediate surface density evaluation, while the Direct Transmission method provides a measurement integrating the density of a deeper soil layer. These methods are under the jurisdiction of ASTM Subcommittee D18.08 on Special and Construction Control Tests.
| 🟦 Feature | 📏 Direct Transmission | 📐 Backscatter |
|---|---|---|
| 🎯 Max Depth | 300 mm (12 in.) | Surface |
| ⚡ Principle | Attenuation of Gamma Radiation | |
| 📌 Configuration | Source/Detector in Hole | Both on Surface |
These test methods serve as rapid, nondestructive techniques ideal for quality control and acceptance testing during construction. The nondestructive nature permits repetitive measurements at a single test location without disturbing the soil, allowing for rigorous statistical evaluation of compaction efforts. The user must compare detected radiation rates with previously established calibration data specific to the soil type and gauge being used.
ASTM D2922-05 designates SI units as the standard. For the inch-pound system, it explicitly uses the gravitational system where the pound (lbf) is a unit of force. The standard clarifies that recording density in lbm/ft³ from mass scales should not be deemed nonconformance with these test methods. D2922 is often used in conjunction with methods for moisture content (D 3017) and compaction characteristics (D 698, D 1557). For soils containing large particles, Practice D 4718 provides necessary corrections for unit weight and water content.
| 📄 Standard | 💡 Application |
|---|---|
| D 698 / D 1557 | Laboratory Compaction Characteristics |
| D 3017 | In-Place Water Content (Nuclear, Shallow Depth) |
| D 4718 | Oversize Particle Corrections |
| D 2216 | Laboratory Determination of Water Content |
The source or detector can be placed at a known depth up to 300 mm (12 in.) from the surface.
The gauge measures the attenuation of gamma radiation through the material. The detected gamma count rate is compared to calibration data to determine the wet or total density.
SI units are the standard. For inch-pound units, the gravitational system (lbf) is used, but reporting density in lbm/ft³ from mass scales is not considered nonconformance.
They allow for repetitive measurements at a single test location without significant excavation or disturbance of the soil structure, making them ideal for construction quality control and acceptance testing.