When an object absorbs radiation it possesses more energy. That increased energy may have different results, depending on the particular nature of the specific object. The object may become warmer, or it may move faster, or it may expand, or it may exert increased pressure on the walls of its container, or some of the electrons in the atoms of which it's comprised may step up to higher orbitals.
One process will be photolysis
the breakdown of a molecule.
eg ozone being broken down when radiation hits it and and oxygen radical forms
O3 + hv --> O2 + O.
As radiation passes through a material it can be absorbed. When radiation from radioactive substances collides with neutral atoms or molecules these may become ionised.
It is stored as heat.
some of the radiation is absorbed in the atmosphere
What kind of radiation? Remember, Beta radiation is particles (electrons)and Alpha radiation is Helium nuclei.Some radiation will transfer energy to particles ... which may speed them up,it may heat them,it may cause fluorescence.
"Absorbed"
The radiation that are absorbed are not all useful. Only the harmful ones are.
Gases absorb radiation and some is absorbed in the atmosphere :)
they are absorbed, depositing their energy in whatever absorbed them.
The thermal energy increases.
some of the radiation is absorbed in the atmosphere
Most of the solar radiation is absorbed when it reaches the surface of the earth. Some of the solar radiation is also absorbed in the atmosphere.
This absorbed energy is then re-radiated as heat
Absorbed dose is the amount of radiation energy absorbed per kilogram of irradiated material.
It is absorbed.
The three changes of state during which energy is absorbed is: conduction, convection, & radiation.
It decreases.
What kind of radiation? Remember, Beta radiation is particles (electrons)and Alpha radiation is Helium nuclei.Some radiation will transfer energy to particles ... which may speed them up,it may heat them,it may cause fluorescence.
All three.Incoming solar radiation: 100%Reflected or scattered by the atmosphere: 6% : Absorbed by the atmosphere: 16%Continuing incoming solar radiation: 78%Reflected by clouds: 20% : Absorbed by clouds: 3%Continuing incoming solar radiation: 55%Reflected by the earth's surface: 4% : Absorbed by the earth's surface (lands and oceans): 51%
"Absorbed"