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ASTM D5195−21 specifies a nuclear method for determining the in-place wet density of soil and rock at depths below the surface. This standard, under the jurisdiction of ASTM Committee D18, calculates the wet density by comparing the detected rate of gamma radiation with previously established calibration data. The source and detector are placed at the desired depth in a bored hole, typically lined by an access tube to maintain consistent geometry throughout testing.
The test method covers the calculation of wet density by the attenuation of gamma radiation. The wet density, in mass per unit volume of the material under test, is derived directly from comparing the detected gamma count rate against calibration standards (Annex A1). Values are stated in either SI units or inch-pound units, which must be regarded separately as standard; values from the two systems shall not be combined (Section 1.3). All observed and calculated values must conform to the guide for significant digits and rounding established in Practice D6026 (Section 1.4).
| 🟦 Parameter | 📏 Specification / Requirement |
|---|---|
| Standard Designation | D5195 − 21 |
| Scope Coverage | Wet density of soil and rock in-place at depth |
| Measurement Principle | Attenuation of gamma radiation |
| Unit System Mandate | SI and inch-pound must be used independently |
| Digit Standardization | Practice D6026 for significant digits and rounding |
The use of nuclear sources requires strict adherence to safety protocols. Section 8 of the standard provides specific precautionary statements regarding the handling and operation of nuclear density gauges. Users must comply with all applicable regulatory limitations and establish appropriate safety, health, and environmental practices (Section 1.5).
Section 6 details potential interferences that can affect measurement accuracy, including variations in chemical composition and hydrogen content of the soil or rock. Comprehensive calibration procedures defined in Annex A1 are essential to mitigate these effects. Agencies performing this test should conform to the minimum requirements of Practice D3740 for quality assurance in geotechnical testing.
Calculation of wet density is strictly based on the comparison of detected gamma radiation with the established calibration relationship. The standard emphasizes that the procedures used for specifying how data are collected, recorded, and calculated represent the industry standard and a baseline for significant digits (Section 1.4.1).
When reporting results, the user can adjust significant digits based on material variation, purpose of the data, special purpose studies, or project objectives. This flexibility is explicit in the standard but does not diminish the requirement for procedurally sound collection. Specifically, reporting test results in units other than SI shall not be regarded as nonconformance with this standard (Section 1.3.1).
| 📐 Data Standard | 🎯 Requirement from D5195-21 |
|---|---|
| Calibration Source | Annex A1 (comparison to known density standards) |
| Calculation Basis | Detected gamma count rate vs calibration curve |
| Unit Compliance | SI or inch-pound can be used distinctly |
| Data Application | Significant digits adjusted for user objectives |
The standard directly calculates the wet density (mass per unit volume) of the soil or rock in-place by measuring the attenuation of gamma radiation between the source and detector placed in the access tube.
No. The standard explicitly requires that the two unit systems be regarded separately. Values from the two systems must not be combined. You must choose one system and use it consistently throughout the test and report.
All calibration data and the procedures for correlating gamma count rates to wet density are fully detailed in Annex A1 of ASTM D5195-21.
The gamma source and gamma detector are placed at the desired depth in a bored hole, which is typically lined by an access tube to maintain the integrity and geometry of the test cavity as outlined in Section 1.1.