Related Experiment Video
Updated: May 15, 2026

10:42
Preparing an Isotopically Pure 229Th Ion Beam for Studies of 229mTh
Published on: May 3, 2019
Chemical evolution via beta decay: a case study in strontium-90
N A Marks1, D J Carter, M Sassi
1Nanochemistry Research Institute, Curtin University, Perth, WA 6845, Australia. N.Marks@curtin.edu.au
Summary
Beta decay in solids can alter material chemistry over time, not just through direct defect creation. This research framework impacts nuclear waste storage and materials design.
Area of Science:
- Solid-state physics and chemistry
- Nuclear materials science
- Radioactive decay
Background:
- Understanding the effects of radioactive decay in solid materials is crucial for applications like nuclear waste storage.
- Beta decay involves the transformation of a nucleus, releasing energy and particles that can interact with the surrounding solid matrix.
- Previous models often focused on direct defect creation, potentially overlooking other significant effects.
Purpose of the Study:
- To develop a framework for analyzing the physical and chemical consequences of beta decay within solid materials.
- To quantify the roles of momentum-induced recoil, defect creation, and chemical evolution.
- To investigate the implications for material stability and design.
Main Methods:
- Utilized strontium-90 ((90)Sr) as a representative beta-decaying isotope.
- Employed density functional theory (DFT) for chemical evolution analysis.
- Incorporated Bader analysis, phonon calculations, and cohesive energy calculations.
- Compared recoil energies with threshold displacement energies for defect formation.
Main Results:
- Recoil energies from beta decay are often insufficient to create defects like Frenkel pairs.
- Chemical evolution over time emerges as a significant consequence of beta decay.
- Demonstrated counter-intuitive chemical behavior in strontium titanate (SrTiO(3)) and strontium hydride (SrH(2)) due to beta decay.
- Electronic excitation effects were noted as material-dependent and difficult to quantify.
Conclusions:
- Beta decay's impact on solids extends beyond direct defect creation, with chemical evolution being a key factor.
- The findings necessitate a re-evaluation of models for radioactive material behavior.
- This research provides critical insights for the safe storage of nuclear waste and the design of novel materials exposed to radiation.
Related Concept Videos
Nuclear Stability
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 in the...
To hold positively charged protons together in the...
Types of Radioactivity
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:
Nuclear Transmutation
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 protons being...
Radioactivity and Nuclear Equations
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...
Isotopes and Radioisotopes
In the early 1900s, English chemist Frederick Soddy realized that an element could have atoms with different masses that were chemically indistinguishable. These different types are called isotopes — atoms of the same element that differ in mass. Isotopes differ in mass because they have different numbers of neutrons but are chemically identical because they have the same number of protons. Soddy was awarded the Nobel Prize in Chemistry in 1921 for this discovery.
An isotope containing more...
An isotope containing more...
Radioactive Decay and Radiometric Dating
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.

