Overview
ISO 10573:1995 specifies an in situ, non‑destructive method for determining soil water content in the unsaturated zone using a neutron depth probe. The standard describes the measurement principle, required apparatus, installation of access tubes, field calibration, counting procedures and reporting of volumetric water content profiles. It is intended for investigations of water storage, water balance and water distribution in soils where repeated measurements at fixed locations are needed.
Key topics and technical requirements
- Principle: A neutron source (commonly 241Am–Be) emits fast neutrons that are thermalized mainly by collisions with hydrogen nuclei. The detector count rate of thermal neutrons is proportional to hydrogen concentration and therefore related to soil water content.
- Measuring volume: The measuring volume is approximately spherical; radius depends on soil bulk density and moisture (typical sphere of influence ~0.1–0.2 m in wet soils to ~0.8 m in very dry soils).
- Apparatus:
- Neutron depth probe (source + thermal neutron detector + readout).
- Thin‑walled access tubing (aluminum/alloy preferred for neutron transparency) and installation equipment.
- Field sampling and drying equipment for gravimetric reference measurements.
- Calibration:
- Field (in situ) calibration is required for accurate absolute water content because soil composition, bulk density and gradients affect counts.
- Calibration curves are derived by regression of count rate (independent variable) versus volumetric water content (dependent variable) for each soil layer and range of hydrological conditions.
- Reference counts in invariant media (e.g., water barrel) are recommended to monitor instrument drift.
- Measurement procedures: Two counting modes-fixed counting time or fixed number of counts-are described. Multiple short counts can be used to assess precision.
- Safety and regulation: The method involves radioactive sources; operators must comply with national and international radiation regulations and use trained personnel. IAEA and ICRP guidelines are referenced.
- Limitations: Relatively rapid measurements but poorer depth resolution than some other methods; counts influenced by hydrogen in non‑water materials and neutron absorption by certain elements.
Открыть превью (PDF)Soil quality — Determination of water content in the unsaturated zone — Neutron depth probe method
