## Equation

**Photon Energy**

Photons are transverse waves of energy as a result of particle vibration. The equation to calculate photon energy uses the energy wave equation and the longitudinal energy difference between two points measured as a distance (r) from the atom’s nucleus. The difference in longitudinal wave energy creates a new transverse wave (photon). An explanation is provided in the section below.

## Classical Constant Form |
## Wave Constant FormTransverse Energy Equation |

Using classical constants * | Using energy wave constants |

**Variables:**

*δ: amplitude factor variable for constructive wave interference. A single proton and electron is one. Calculations can be found in the Amplitude Factors table.**r: distance variable for starting position (r*_{0}) and ending position (r) of electron in an atom (in meters). Calculations can be found in the Orbital Distances table.

* Electron energy (E_{e}) can be further derived but are used for readability.

**Photon Frequency **

Photons can also be expressed in terms of frequency or wavelength. Beyond hydrogen, many photon experiments present results as energy so the Transverse Energy Equation is used in the calculations on this site for elements beginning with helium. *Same variables as the Transverse Energy Equation.*

## Classical Constant FormPhoton Frequency Equation |
## Wave Constant FormPhoton Frequency Equation |

Using classical constants | Using energy wave constants |

**Photon Wavelength **

Photon wavelengths can also be represented in classical and wave formats. *Same variables as the Transverse Energy Equation.*

## Classical Constant FormPhoton Wavelength Equation |
## Wave Constant FormPhoton Wavelength Equation |

Using classical constants | Using energy wave constants |

## Explanation of Equation

The derivation of the Transverse Energy Equation in wave format begins with the fundamental equation for calculating energy in a volume:

**Energy Wave Equation**

A photon is generated by the vibration of a particle. It is a traveling wave originating from the particle, which is constantly reflecting longitudinal waves. Now, it also has a transverse component during its vibration before the particle comes to rest. Thus, it has a longitudinal component (l) and transverse component (t) that will become its electric and magnetic components. The vibration creates two photons traveling in opposite directions. In the creation of a photon in an atom, one of the photons will be absorbed by the nucleus and cause recoil as explained here.

The transverse component has a frequency that depends on the speed of the vibration of the particle, which may happen during orbital transitions in an atom until a particle like the electron settles into an orbital. The faster the vibration, the higher the frequency of the transverse component.

**Detailed Assumptions**

The photon frequency, wavelength and energy equations are built and derived from these assumptions. The orbital distance calculations are found in the tables for orbital distances, with further detail in the *Atomic Orbitals* paper. An explanation of how photons are created and absorbed, including incident and scattered angles are presented in the *Photons* paper.

The following assumptions were made when understanding particle interaction, including atomic orbitals:

- Particle vibration creates a transverse wave. A particle may vibrate upon annihilation, when transitioning between orbitals in an atom, or when an entire atom vibrates due to kinetic energy.
- Longitudinal amplitude difference creates particle motion as particles seek to minimize amplitude.
- The difference in longitudinal energy is transferred to transverse energy in two photons that travel in opposite directions, perpendicular to particle vibration.
- Particles and their antimatter counterparts attract because of destructive waves between the particles; like particles (e.g. electron-electron) repel due to constructive waves, seeking to minimize amplitude.
- Electrons in an atomic orbital are both attracted and repelled by the nucleus. A positron is assumed to be at its core to attract the orbital electron; opposing forces in the nucleus repel the orbital electron as explained in the Atoms section.

**Conservation of Energy – Longitudinal Waves to Transverse Waves**

The transverse wave energy for the photon is a result of a difference in longitudinal wave energy as two opposite phase particles destructively interfere, which is the case with a proton and electron. The energy difference in longitudinal wave form in classical terms is:

The values E_{e} and r_{e} are the energy of the electron and classical electron radius, respectively. Q is the particle group count that is also used in force equations. These values can be replaced by their wave constants form.

There are two photons created, thus each photon (E_{t}) is half of the longitudinal energy above. For two particle groups (Q) at distance (r), the equation works. But in an atom, this is limited to hydrogen or ionized atoms that have only one electron. For all other atoms, there are multiple electrons at varying distances. As a result, a variable called the amplitude factor (δ), replaces Q_{1} and Q_{2 }as the method to calculate constructive wave interference on an electron from multiple particles at varying distances. The calculations of amplitude factor is explained here. Substituting for this variable, and taking half of the longitudinal energy for one photon, leads to the Transverse Energy Equation.

**Calculations and Examples**

A summary of calculations and some examples using the equations are provided here. The remainder of the calculations and examples are detailed in the *Particle Energy and Interaction *paper. A summary of photon interactions in atoms is detailed in the *Photons *paper.