Related Experiment Video
Updated: Dec 28, 2025

08:53
Automated 90Sr Separation and Preconcentration in a Lab-on-Valve System at Ppq Level
Published on: June 6, 2018
8.3K
A new primary emanation standard for Radon-222.
Florian Mertes1, Stefan Röttger1, Annette Röttger1
1Physikalisch-Technische Bundesanstalt, Bundesallee 100, 38116, Braunschweig, Germany.
Summary
New reference materials for radon-222 (Rn-222) were created using radium-226 (Ra-226) electrodeposition. These sources enable precise, stable radon atmosphere generation with low uncertainty for calibration purposes.
Area of Science:
- Nuclear physics and radiochemistry.
- Development of reference materials for radioactivity measurements.
Background:
- Accurate calibration of radon (Rn-222) monitoring equipment is crucial for radiation protection.
- Existing methods for generating stable radon atmospheres have limitations in precision and range.
Purpose of the Study:
- To develop new, stable emanation sources for radon-222 (Rn-222) using radium-226 (Ra-226).
- To establish a reliable method for generating reference atmospheres below 300 Bq⋅m⁻³ with low uncertainty.
Main Methods:
- Electrodeposition of Ra-226 onto stainless-steel discs.
- Alpha-particle spectrometry for Ra-226 activity determination.
- Gamma-ray spectrometry using HPGe detectors for Rn-222 emanation measurement.
- Utilizing the distorted equilibrium of the Ra-226 decay chain.
Main Results:
- New emanation sources for Rn-222 were successfully developed.
- Stable reference atmospheres below 300 Bq⋅m⁻³ were produced with uncertainties not exceeding 2% (k=1).
- Comparative measurements eliminated the need for emission probabilities and detection efficiency knowledge.
Conclusions:
- The developed emanation sources provide a reliable method for generating low-concentration Rn-222 reference atmospheres.
- This advancement supports accurate calibration of radiation monitoring instruments.
- The method offers high precision and stability for Rn-222 metrology.
Related Concept Videos
Types of Radioactivity
19.2K
The most common types of radioactivity are α decay, β decay, γ decay, neutron emission, and electron capture.
Alpha (α) decay is the emission of an α particle from the nucleus. For example, polonium-210 undergoes α decay:
Alpha (α) decay is the emission of an α particle from the nucleus. For example, polonium-210 undergoes α decay:
19.2K
Radioactivity and Nuclear Equations
26.7K
Nuclear chemistry is the study of reactions that involve changes in nuclear structure. The nucleus of an atom is composed of protons and, except for hydrogen, neutrons. The number of protons in the nucleus is called the atomic number (Z) of the element, and the sum of the number of protons and the number of neutrons is the mass number (A). Atoms with the same atomic number but different mass numbers are isotopes of the same element.
A nuclide of an element has a specific number of protons and...
A nuclide of an element has a specific number of protons and...
26.7K
Nuclear Stability
22.6K
Protons and neutrons, collectively called nucleons, are packed together tightly in a nucleus. With a radius of about 10−15 meters, a nucleus is quite small compared to the radius of the entire atom, which is about 10−10 meters. Nuclei are extremely dense compared to bulk matter, averaging 1.8 × 1014 grams per cubic centimeter. If the earth’s density were equal to the average nuclear density, the earth’s radius would be only about 200 meters.
To hold positively charged protons together...
To hold positively charged protons together...
22.6K
Radioactive Decay and Radiometric Dating
36.7K
Radioactivity is a spontaneous disintegration of an unstable nuclide and is a random process, as all the nuclei in the sample do not decay simultaneously. The number of disintegrations per unit time is called the activity (A), which is directly proportional to the number of nuclei in the sample. The decay constant (λ) is an average probability of decay per nucleus in unit time.
36.7K
Nuclear Transmutation
20.3K
Nuclear transmutation is the conversion of one nuclide into another. It can occur by the radioactive decay of a nucleus, or the reaction of a nucleus with another particle. The first manmade nucleus was produced in Ernest Rutherford’s laboratory in 1919 by a transmutation reaction, the bombardment of one type of nuclei with other nuclei or with neutrons. Rutherford bombarded nitrogen-14 atoms with high-speed α particles from a natural radioactive isotope of radium and observed...
20.3K
Biological Effects of Radiation
17.4K
All radioactive nuclides emit high-energy particles or electromagnetic waves. When this radiation encounters living cells, it can cause heating, break chemical bonds, or ionize molecules. The most serious biological damage results when these radioactive emissions fragment or ionize molecules. For example, α and β particles emitted from nuclear decay reactions possess much higher energies than ordinary chemical bond energies. When these particles strike and penetrate matter, they...
17.4K

