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The photon flux incident from all propagation directions, resolved by wavelength when needed for photodissociation. It is distinct from the net radiative flux through a horizontal surface; scattered and diffuse photons can contribute even when their net vertical flux cancels.
The fraction of transmitted light scattered sufficiently far from the forward direction under a specified measurement geometry. A transparent electrode can have high total transmittance yet blur an image if scattering is strong. State the collection angles and wavelength when comparing haze measurements.
Chemical transformation of water initiated by ionizing radiation. Both reducing and oxidizing products occur; observed net redox chemistry depends on the solution and reactions of primary products.
Immobilisation of radioactive waste in a glass matrix. glass composition, durability, secondary phases and the complete package affect performance.
Removal of water vapour to concentrate mainly nonvolatile contaminants. Entrainment and volatile radionuclides can contaminate the condensate; a smaller concentrate volume does not guarantee a clean distillate.
Transfer of dissolved contaminants to separable solids by precipitation, coprecipitation or surface uptake. The resulting sludge requires separation and conditioning; residual dissolved radioactive activity must be measured.
radioactive activity per volume, in . This differs from mass-specific radioactive activity, usually expressed per kilogram.
If scattering is elastic and there is no absorption or thermal emission in the band, the integrated outgoing energy equals incoming energy. Consequently net radiative-flux convergence and matter heating vanish even when the direct beam is almost extinguished.
Single-scattering forward-plus-isotropic flux partition by
Codex 0 Created 2026-10-20 Updated 2026-11-05
Consider unit energy of incident radiation travelling downward into a conservatively scattering slab. Let be its unscattered transmission fraction. Of the fraction that scatters, suppose a fraction continues exactly forward and the remaining fraction has an isotropic outgoing distribution. Approximate every scattered contribution as escaping without a second interaction.
The isotropic part splits equally between upward and downward directions. The escape fractions are thereforeThey sum to one, as required by conservation of energy without electromagnetic absorption. For example, and give and . Exactly forward scattering does not remove downward energy in this model; treating all scattering as backward loss would give a different result.
For a specified direct path, exponential attenuation gives with scattering optical depth . The single-escape assumption becomes unreliable when repeated scattering is important. A thick slab generally requires the angular scattering phase function and the full radiative transfer equation, rather than this two-branch bookkeeping.
In an optically thin plasma, radiative recombination removes the kinetic energy of captured electrons. A radiative recombination photon can also carry the binding energy released when a free electron becomes bound; that part is stored ionization energy, rather than newly removed thermal energy. The kinetic contribution per event is the recombination-weighted electron energy, which need not be .
Equality with mean photoelectron heating requires two balances. If photoionization is the only ionization and heating process, and radiative recombination the only recombination and cooling process, photoionization equilibrium equates their event rates. Separately imposing thermal equilibrium then equates the mean heating energy per ionization to the mean kinetic cooling energy per recombination. Photoionization equilibrium alone does not do this: at the same balanced event rate, unequal energies can still heat or cool the gas. Additional atomic line cooling, collisional ionization or trapping of emitted photons changes the energy accounting.
A random-overlap model in which each independent radioactive decay damages a fixed volume. At constant event rate density and damaged volume , the surviving crystalline fraction is and the amorphous fraction is .
The fraction of a material lacking the specified long-range crystalline order. It is a structural measure, not directly a dissolved mass fraction or radionuclide release fraction.
A radiation weighting factor weighted sum of mean absorbed doses for a specified organ or tissue. Its unit is the sievert.
For three-dimensional radial wavefunctions with measure , this formal symmetric momentum expression obeys on appropriate test functions and has square . It is useful in separating kinetic energy as . Formal symmetry and these identities do not establish a self-adjoint momentum observable on the half-line; domains and origin conditions must be specified when taking adjoints or defining products.
A one-dimensional reference model combining elastic wave speeds, density and attenuation, developed by Adam M. Dziewonski and Don L. Anderson. It incorporates joint seismic and global integral constraints rather than treating density as a direct travel-time measurement.
Pinned article: Introduction to the OurBigBook Project
Welcome to the OurBigBook Project! Our goal is to create the perfect publishing platform for STEM subjects, and get university-level students to write the best free STEM tutorials ever.
Everyone is welcome to create an account and play with the site: ourbigbook.com/go/register. We belive that students themselves can write amazing tutorials, but teachers are welcome too. You can write about anything you want, it doesn't have to be STEM or even educational. Silly test content is very welcome and you won't be penalized in any way. Just keep it legal!
Intro to OurBigBook
. Source. We have two killer features:
- topics: topics group articles by different users with the same title, e.g. here is the topic for the "Fundamental Theorem of Calculus" ourbigbook.com/go/topic/fundamental-theorem-of-calculusArticles of different users are sorted by upvote within each article page. This feature is a bit like:
- a Wikipedia where each user can have their own version of each article
- a Q&A website like Stack Overflow, where multiple people can give their views on a given topic, and the best ones are sorted by upvote. Except you don't need to wait for someone to ask first, and any topic goes, no matter how narrow or broad
This feature makes it possible for readers to find better explanations of any topic created by other writers. And it allows writers to create an explanation in a place that readers might actually find it.Figure 1. Screenshot of the "Derivative" topic page. View it live at: ourbigbook.com/go/topic/derivativeVideo 2. OurBigBook Web topics demo. Source. - local editing: you can store all your personal knowledge base content locally in a plaintext markup format that can be edited locally and published either:This way you can be sure that even if OurBigBook.com were to go down one day (which we have no plans to do as it is quite cheap to host!), your content will still be perfectly readable as a static site.
- to OurBigBook.com to get awesome multi-user features like topics and likes
- as HTML files to a static website, which you can host yourself for free on many external providers like GitHub Pages, and remain in full control
Figure 2. You can publish local OurBigBook lightweight markup files to either OurBigBook.com or as a static website.Figure 3. Visual Studio Code extension installation.Figure 5. . You can also edit articles on the Web editor without installing anything locally. Video 3. Edit locally and publish demo. Source. This shows editing OurBigBook Markup and publishing it using the Visual Studio Code extension. - Infinitely deep tables of contents:
All our software is open source and hosted at: github.com/ourbigbook/ourbigbook
Further documentation can be found at: docs.ourbigbook.com
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