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The ASTM D3972-09 standard (reapproved 2015) specifies a radiochemical method for the determination of alpha-particle-emitting isotopes of uranium in water. The method employs chemical separation techniques followed by alpha pulse-height analysis, ensuring accurate isotopic quantification for environmental and process monitoring applications.
This test method covers the analysis of both soluble uranium and uranium present in suspended matter. It is designed for water samples including uranium processing effluents and substitute ocean water. The standard requires the addition of a 232U tracer to monitor chemical yield. Compliance with SI units is mandatory, and users must follow the safety warnings provided in Section 9. Referenced documents include practices for water sampling (D1066, D3370), alpha spectrometry (D3084, C1163), and quality control (D5847, D7282). For definitions of terms used, refer to Terminologies C859 and D1129.
The analytical process involves several critical steps to isolate and measure uranium isotopes:
Sample Preparation: The water sample is acidified, and 232U tracer is added. If the sample contains carbonate or bicarbonate ions, it must be boiled under acidic conditions to convert them to CO₂ and expel the gas.
Coprecipitation: Uranium is coprecipitated with ferrous hydroxide. The precipitate is collected and dissolved in concentrated hydrochloric acid. If the precipitate does not dissolve, a mixture of concentrated nitric and hydrofluoric acids is used.
Anion Exchange: The dissolved uranium is loaded onto an anion-exchange resin in 8 M HCl. Uranium is retained while other radionuclides are washed through. Elution is performed with 0.1 M HCl.
Electrodeposition and Counting: The purified uranium is electrodeposited onto a stainless steel disk. The disk is then analyzed by alpha pulse-height spectrometry to determine the activity of each uranium isotope.
| 🟦 Step | 📏 Reagent/Condition | 🎯 Purpose |
|---|---|---|
| Tracer Addition | 232U | Yield Monitor |
| Carbonate Removal | Boiling, Acidification | Prevent Complexation |
| Coprecipitation | Ferrous Hydroxide | Uranium Scavenging |
| Dissolution | Conc. HCl or HNO₃/HF | Precipitate Dissolution |
| Anion Exchange | 8 M HCl / 0.1 M HCl | Uranium Purification |
| Electrodeposition | Stainless Steel Disk | Alpha Spectrometry Mount |
The standard emphasizes strict quality control practices as outlined in D5847 and D7282. Alpha spectrometry must be performed in accordance with Practice D3084. The use of the 232U tracer is essential for determining the chemical recovery of uranium. Method precision and bias should be evaluated using Practice D2777.
| 📐 Practice | ⚡ Application |
|---|---|
| D2777 | Precision and Bias |
| D3084 | Alpha-Particle Spectrometry |
| D5847 | Quality Control Specifications |
| D7282 | Instrument Setup and QC |
| C1163 | Mounting Actinides for Alpha Spectrometry |
The 232U tracer acts as an isotopic yield monitor. It allows the analyst to correct for uranium losses during the chemical separation and electrodeposition steps, ensuring accurate quantification of the sample’s uranium isotopes.
Seawater contains carbonate and bicarbonate ions that can complex uranium, preventing its coprecipitation with ferrous hydroxide. Boiling under acidic conditions converts these ions to CO₂, which is driven off, allowing quantitative recovery of uranium.
The electrodeposited disk is analyzed using alpha pulse-height spectrometry (also known as alpha-particle spectrometry). This technique separates and measures the alpha-particle energies emitted by different uranium isotopes, such as 238U, 234U, and 235U.
This method is applicable to uranium processing effluents and substitute ocean water. It has been validated for soluble uranium and uranium in suspended matter. Users are responsible for verifying the method’s validity for untested water matrices.