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A parent initially at rest emits an alpha particle and a recoiling heavy daughter. momentum conservation gives equal and opposite momenta, so their nonrelativistic kinetic energies satisfyHere $Q$ is the kinetic energy available to this branch; excitation of the daughter reduces it and may be followed by photon emission. For an illustrative $Q=5$ MeV, $m_{\alpha }=4\mathrm{u}$ and $M_d=236\mathrm{u}$, the energies are $4.917$ MeV in the alpha particle and $83.3$ keV in the daughter. The heavy daughter receives much less energy, but that does not imply much less atomic damage.

The fast alpha particle loses most of its energy through electronic stopping: ionization and electronic excitation along a relatively long path. It also undergoes nuclear collisions, particularly towards the end of its range, and can produce displacement damage. The slower, heavy, highly charged recoil couples strongly to surrounding nuclei and generates a compact displacement cascade. Successive knock-on atoms create vacancies, interstitial defects and clusters. Some Frenkel pairs recombine as the cascade relaxes; the initial collision count is therefore not the number of defects that remain.

A quantitative illustration comes from brannerite rather than an assumed universal ceramic. Simulations in the primary natural-mineral study used a $4.5$ MeV alpha particle and an $80$ keV daughter recoil. The corresponding ranges were about $13$ micrometres and $23$ nanometres. At the study's assumed $50$ eV threshold displacement energy, its tabulated results give roughly $560$–$571$ recoil atomic displacements and $91$–$100$ alpha particle atomic displacements per radioactive decay. The numbers depend strongly on the displacement threshold and material, but the shorter recoil path contains the dominant and much denser ballistic radiation damage.^[ref]

In a susceptible ceramic, cascade cores can accumulate into an amorphous fraction; defects and associated relaxation can also change volume, thermal conductivity and mechanical response. molecular dynamics simulations of zirconolite found a strongly disordered core surrounded by more isolated point defects, supporting this distinction between local cascade damage and an entirely transformed specimen.^[ref]

The alpha particle eventually becomes a helium atom after slowing and charge exchange. helium accumulation can have later microstructural effects distinct from the initial knock-on cascade. Material-dependent recombination and annealing limit surviving disorder; a change in diffraction or radiation-induced swelling is not automatically radiation-induced amorphization, and radiation-induced amorphization is not automatically dissolution or release of the contained radionuclide.

Consider a representative bulk volume $\mathcal{V}$ and let $f_a(t)$ be its amorphous fraction. With alpha-decay event rate density $R$, during $dt$ the expected number of independent alpha decay events is $R\mathcal{V}dt$. Each produces effective amorphization volume per decay $V_{\alpha }$, but only the fraction $1-f_a$ of a randomly placed damage region was previously crystalline. The expected new amorphous volume is thereforeDividing by $\mathcal{V}dt$ givesSeparate variables and integrate:Hence, with cumulative alpha-decay event density $D=Rt$,The product $Rt{V}_{\alpha }$ is dimensionless: events per cubic metre accumulated over time multiply cubic metres damaged per event. Here “dose” is an event density, not an absorbed energy per kilogram.

An independent probability interpretation reaches the same result. A particular point is covered by a number of random damage events with a Poisson distribution of mean $D{V}_{\alpha }$. Its probability of remaining crystalline is the zero-hit probability $e^{-D{V}_{\alpha }}$; the complementary fraction has been hit at least once. Overlapping events do not create a second copy of already amorphous material.

At small dose, $f_a\simeq D{V}_{\alpha }$; at larger dose, overlap bends the curve towards one. For example, $D{V}_{\alpha }=1$ gives $f_a=0.6321$, not full radiation-induced amorphization, and $f_a=0.99$ requires $D{V}_{\alpha }=\ln 100=4.6052$.

The derivation assumes a homogeneous, initially crystalline material; independent random event locations; one-event radiation-induced amorphization of a fixed effective volume; and no recovery of that volume. It is the direct-impact model, not a model requiring several prior hits to cross a damage threshold. If $R$ varies while $V_{\alpha }$ stays fixed, replace $Rt$ by ${\int }_0^{t}R(s)ds$. If annealing, material evolution or spatially correlated actinide distributions matter, this simple law need not hold. The subscript on $V_{\alpha }$ indexes an alpha decay event: it does not require the emitted alpha particle itself to produce the damaged volume.

Let $c(t)$ be the fraction still crystalline. Under the direct-impact amorphization model, damage events occur randomly and independently; an event striking already amorphous material does not create that much additional amorphous volume. Only the crystalline fraction can be newly converted, soThe product of the given event rate density and damage volume has units of inverse time:For $99\%$ radiation-induced amorphization, $c=0.01$, givingUsing $365.25$ days per year, the corresponding calendar date is approximately 3555 CE, measured from disposal preparation in 2050.

A linear estimate $f_a=Rvt$ misses repeated hits to already damaged regions and therefore predicts too rapid an approach to $99\%$. The exponential function model never reaches exactly $100\%$ in finite time. Its assumptions include constant dose rate, fixed effective damage volume, no annealing and no spatial correlation of damage. Actual alpha decay generates recoil damage as well as the alpha particle's track; the stated damage volume must be understood as the effective volume per radioactive decay for the chosen model.

Amorphous is not synonymous with dissolved or failed containment. Radiation damage can change swelling, connected porosity and leach behaviour, so testing must compare structural evolution with element release. Accelerated self-irradiation and parallel dissolution measurements are useful precisely because crystallinity alone is not the performance endpoint.^[ref]

Loss of long-range crystalline order through irradiation damage. radiation-induced amorphization does not itself demonstrate loss of chemical containment or a specified radionuclide release rate.

Volume increase caused by irradiation-induced defects and microstructure changes. Accumulating helium and defect clusters can contribute; radiation-induced swelling is not identical to radiation-induced amorphization.