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Where C is the speed of light and qe is the fundamental unit of electrical charge. Substituting the appropriate values:

I used the units
that are correct for this new theory. Even so, the value of the constant of
proportionality is very recognizable. Its magnitude is the same as that of
Boltzmann's constant. The units are not the same. However, this circumstance
only represents that there is a major conflict between the units of this theory
and those of current modern physics. I offer the possibility that:
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Where k represents Boltzmann's constant. I did not include my usual subscripts because I want to show it in a form consistent with the well-known energy as a function of frequency equation given before it. I will shortly show an application for this new relationship.
There can also be shown a relationship between photon momentum and frequency. I will solve for the proportionality constant of this relationship. Force is defined as:
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Then, using the
equation derived in the last section, I can write:
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Where k is Boltzmann's constant. Solving
for momentum:
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The proportionality
constant is:
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Introducing a symbol for this constant:
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The
relationship can then be written for photons as:
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It is of
theoretical importance that Boltzmann's constant appears to be a part of the
frequency relationships discussed above. This occurs because:
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This
relationship now allows me to mix formulas that contain either of these
constants. For example, I can investigate the possible theoretical meaning of
equating:
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And:
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Combining these
equations yields:
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Rearranging
terms:
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Or:
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The right side of
this equation offers an interesting interpretation that is consistent with
results offered earlier in this theory. The value of the incremental xc is the local
measurement of the radius of the hydrogen atom. I have previously shown the
remote measurement is 2/3
the local measurement. This result then offers an explanation for the value of 3/2 in the known expression for the
kinetic energy of an ideal gas molecule. That expression is:
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The fraction 3/2 is an inverse representation of the
remote measurement of the radius of the hydrogen atom. Solving for T:

This formula shows that temperature is a remote measurement. The units of temperature are those of velocity. It appears that temperature is the rate of propagation of kinetic energy between gas atoms. Substituting the value of length of the photon:
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Yielding the
relationship:
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Which says, what is already commonly established: That temperature is directly related to frequency.
These equations
were derived using photon qualities. Therefore, they demonstrate the
quantization of force, energy, momentum and temperature. They are applicable to
helping define quantum mechanics type properties of the universe.
THERMODYNAMIC ENTROPY
Thermodynamic
entropy is defined as a mathematical function. It does not have a physical
explanation in the classical terms from which it was derived. In this theory, temperature,
entropy, Boltzmann’s constant and Planck’s constant will be given clear,
physical meanings.
My use of the
term, thermodynamic properties, refers to those for which we may make
macroscopic measurements. Pressure and temperature are representative of this
definition. There is one further general requirement. The measurement of such
properties must be done under conditions of equilibrium. Temperature is
commonly defined as a property that demonstrates when two or more systems are
in thermal equilibrium.
If two systems have the same temperature, they are in thermal equilibrium. If they are placed in contact, separated only by a wall that readily transfers heat, then, from the macroscopic perspective no heat will be exchanged. Heat is energy in transit, and there is no resultant energy transferred.
Equilibrium can be approximated even for systems undergoing change, so long as the changes are quasi-static. When external forces act on a system, or when the system exerts a force that acts on its surroundings, then all such forces must act quasi-statically. This means forces must vary so slightly that any thermodynamic imbalance is infinitesimally small. In other words, the system is always infinitesimally near a state of true equilibrium. If a property such as temperature changes, it must occur so very slowly that there is no more than an infinitesimal temperature variation between any two points within the system.
In the work that follows, all parts of a system are in states of equilibrium with one another. Different systems are not necessarily in equilibrium with one another. However, all changes that occur between systems or parts of systems occur sufficiently slowly that each part of all systems, and each system as a whole, from the macroscopic perspective, remain infinitesimally close to equilibrium.
Entropy is
defined as a mathematical function demonstrating an ideal relationship between
the transfer of heat and constant temperature. The entropy function is:
![]()
Where DS is a change in entropy, DQ is the transfer of heat either into or out of a system, and T is the temperature of the system in degrees Kelvin. This equation is based upon an ideal model of an engine called a Carnot engine. The engine operates in a Carnot cycle.
a. There are two near infinite sources of heat. One is at temperature Thigh, the other at temperature Tlow. The Carnot engine operates cyclically between these two temperatures. The engine will absorb heat from source Thigh and reject heat to source Tlow. For this example the working substance is a simple gas. Before the cycle begins, the engine is in contact and thermal equilibrium with heat source Tlow. This is the point from which the cycle will start:
b. The engine is separated from source Tlow and the first part of the cycle begins. The gas is adiabatically, i.e. no conduction of heat either into or out of the gas, compressed until its temperature rises to the level of Thigh.
c. The engine is placed in contact with source Thigh and the second part of the cycle begins. The gas volume expands while remaining at temperature Thigh.
d. The engine is removed from contact with Thigh. The heated gas continues to expand adiabatically, i.e. no heat flows in or out, until its temperature falls to that of source Tlow.
e. The engine is put in contact with source Tlow and, the gas is compressed while remaining at temperature Tlow until the engine has returned to its initial state of temperature and volume.
It is known for
a Carnot cycle that:
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The values of Thigh
and Tlow may both vary, but the relationship remains true. This
relationship is the basis of the definition of thermodynamic entropy. The entropy
definition is:
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The entropy of
the gas will increase when expanding while in contact with Thigh
and will decrease when compressing while in contact with Tlow.
Therefore, the increase in entropy is given by:
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And the
decrease in entropy is given by:
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For a Carnot
cycle, their sum is:
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There is no net
change in entropy for the Carnot engine. For a series of Carnot engines joined side
by side, they would have an increase in entropy given by:
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For the latter
part of the cycle, the decrease in entropy would equal:
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The convention
is that heat entering the engine is positive and heat leaving is negative. For
both series of variations of heat, it does not matter how their individual
temperatures vary. The change in entropy, whether increasing or decreasing, is
always equal to its final value minus its initial value. In other words, the
sums of changes in entropy, either increasing or decreasing, will be the same
regardless of how the temperature varies.
If the
series of engines each have infinitesimally small transfers of heat, then
the equations become differential. The equation for the increase in entropy
becomes:
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The corresponding decrease in entropy would have an analogous change in form. In the differential form, the equations for the series of Carnot engines accurately represent a continuous path on a generalized work diagram so long as the engine represented is quasi-static, i.e. no dissipative effects, and reversible, i.e. returns to initial conditions at the end of each cycle. The differential forms of these equations may be solved by means of calculus for the changes in entropy of this ideal type of engine.
The classical
definition of entropy, expressed in terms of macroscopic properties, shows how
entropy is calculated, but does not make clear what entropy is. It is a
mathematical function and not an explained physics property. Heat is energy in
transit. I am using the mks
system of units, so the units of entropy are joules per degree Kelvin.
It is temperature that masks the identity of entropy. Temperature is an indefinable property in theoretical physics. It is accepted as a fundamentally unique property along with distance, time, mass, and electric charge. If the physical action that is temperature was identified, then, entropy would be explainable.
What is
entropy? It is something whose nature should be easily seen, because, its
derivation is part of the operation of the simple, fundamental Carnot engine.
The answer can be found in the operation of the Carnot engine. The Carnot
engine is the most efficient engine, theoretically speaking. Its efficiency is
independent of the nature of the working medium, in this case a simple gas. The
efficiency depends only upon the values of the high and low temperatures in
degrees Kelvin. Degrees Kelvin must be used because the Kelvin temperature
scale is derived based upon the Carnot cycle.
The engine’s equation
of efficiency and the definition of the Kelvin temperature scale are the basis
for the derivation of the equation:
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Something very important happens during this derivation that establishes a definite rate of operation of the Carnot cycle. The engine is defined as operating quasi-statically. The general requirement for this to be true is that the engine should operate so slowly that the temperature of the working medium should always measure the same at any point within the medium. This is a condition that must be met for a system to be described as operating infinitesimally close to equilibrium.
There are a
number of rates of operation that will satisfy this condition; however, there
is one specific rate above which the equilibrium will be lost. Any slower rate
will work fine. The question is: What is this rate of operation that separates
equilibrium from disequilibrium? It is important to know this because this is
the rate that becomes fixed into the derivation of the Carnot engine. This
occurs because the engine is defined such that the ratio of its heat absorbed
to its heat rejected equals the ratio of the temperatures of the high and low
heat sources:
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This special
rate of operation could be identified if the physical meaning of temperature
was made clear. In this new theory, temperature is indicative of the rate of
exchange of energy between molecules. It is not quantitatively the same as the
rate, because, temperature is assigned unique units of measurement that are not
time, distance, or a combination of these two. Temperature is assigned the
units of degrees and its scale is arbitrarily fitted to the freezing and
boiling points of water.
The temperature
difference between these points on the Kelvin scale is set at 100 degrees. For
this reason, the quantitative measurement of temperature is not the same as the
quantitative measurement of exchange of energy between molecules. However, this
discrepancy can be moderated with the introduction of a constant of
proportionality:
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Multiplying by dt:
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This equation
indicates that the differential of entropy is:
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Both dS and dt are variables. It is necessary to determine a value for the
constant kT. This value may be contained in the ideal gas law:
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Where k is Boltzmann’s constant. If I let n=1, then the equation gives the kinetic energy of a single molecule. In this case E becomes DE an incremental value of energy. Substituting:
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This suggests
that for an ideal gas molecule:
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In other words, the entropy of a single ideal gas molecule is a constant. The condition under which this is true is when the gas molecules act like billiard balls and their pressure is very close to zero. Near zero pressure for any practical temperature requires that the gas molecules be low in number and widely dispersed.
I interpret
this to mean, under these conditions, that the thermodynamic measurement of
temperature and kinetic energy approach single molecule status. Normally,
thermodynamic properties do not apply to small numbers of molecules. However,
sometimes it is instructive to establish a link between individual molecules
and thermodynamic properties, as is done in the development of the kinetic
theory of gases. The case at hand is an inherent part of the kinetic theory of
gases.
The ideal gas
law written for a single gas molecule gives reason to consider that for a
single molecule:
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Substituting
for Boltzmann’s constant:
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I have defined
Entropy as:
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Therefore, I
write:
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If I could
establish a value for Dt, then I could calculate kT. Since this calculation is assumed to apply to a single gas
molecule and is a constant value, I assume that in this special case, Dt is a fundamental increment of time. In this theory, there
is one fundamental increment of time. It is:
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Substituting
this value and solving for kT:

Substituting
the units for each quantity as determined by this new theory and dropping the
single molecule indicator:
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The value kT is a unit free
constant of proportionality. It also follows that Boltzmann’s constant is
defined as:
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For the ideal
gas equation, the entropy of each molecule is a constant:
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However, thermodynamic
entropy is defined as an aggregate macroscopic function. I have a value for the
constant kT,
but the increment of time in the macroscopic function is not a constant. There
are a great number of molecules involved and their interactions overlap and add
together. It is a variable. I expand the meaning of entropy into its more
general form and substitute kT into the general thermodynamic definition of entropy:
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The Dt in this equation is not the same as the Dtc in the equation for a single
molecule. In the macroscopic version, it is the time required for a quantity of
energy, in the form of heat, to be transferred at the rate represented by the
temperature in degrees Kelvin. Substituting this equation for entropy into the
general energy equation:
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Recognizing
that the increment of energy represents an increment of heat entering or
leaving the engine, and solving for DS:
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Solving for Dt:
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This function
of Dt is what would have become defined
as the function of entropy if temperature had been defined directly as the rate
of transfer of energy between molecules. The arbitrary definition of
temperature made it necessary for the definition of entropy to include the
proportionality constant kT.
Writing an equation to show this:

In particular:

For a Carnot
engine:
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Therefore:

And the increments of time must be equivalent. This is why the increase in entropy is exactly the opposite of the decrease in entropy for the Carnot engine. The increments of time are identical. The increment of heat entering the engine carries the positive sign, and the increment of energy leaving the engine carries the negative sign.
Now, I consider
an engine that operates infinitesimally close to equilibrium conditions, but
has heat loss that does not result in work. The heat that is successfully
converted into work can be represented by a series of Carnot engines. For this
series, the change in entropy per cycle is zero. The lost heat can be treated
as if it just passes through the engine. The engine becomes a pathway for the
lost heat to travel from the high heat source to the low heat source.
The entropy of the engine is not changed by this loss of heat. The entropies that are affected are those of the high heat source and the low heat source. The entropies are measures of time required for the lost heat to be released by the high heat source and later absorbed by the low heat source. The net change in entropy is:
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The quantity of heat transferred is the same in both cases. The rates at which that heat will be transferred are different. The low temperature represents a slower rate of exchange of heat than for the high temperature. This means it takes longer for the low temperature source to absorb the quantity of lost heat than it does for the high temperature source to emit the heat.
This time difference is the change that occurs and it is what is represented by the measure of change of entropy. The high heat source loses entropy because it requires extra time for the lost heat to leave the source. The low heat source gains entropy because it requires extra time to absorb the heat that is simply passing through the engine without being converted into work.
Heat that
leaves a source is negative heat. Heat that enters a source is positive heat.
There is a decrease in molecular activity for the heat source that gives up the
heat. There is a corresponding increase in molecular activity for the heat
source that receives the heat. There is no net change of energy. What is lost
here is gained there.
In my definition of entropy, I established meaning for Boltzmann’s constant. In this theory, giving meaning to Boltzmann’s constant necessarily means establishing meaning for Planck’s constant. Establishing meaning for fundamental constants contributes to achieving a unified theory.
In this theory,
Boltzmann’s constant has acquired the definition of:
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I have
previously shown a relationship between Planck’s constant h and Boltzmann’s constant k:
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Substituting for
k and rearranging terms:
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I moved the fraction into the parenthesis with photon length because, as has been shown earlier in the theory, this term demonstrates the definition to include a remote measurement. In other words, we determine the value of Planck’s constant by making remote macroscopic measurements of the energy of photons.
This
interpretation of Planck’s constant allows for a modification to the definition
of entropy. Using the equation:
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Since:
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Substituting:
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Since:
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Substituting:
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Rearranging:
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Planck’s
constant is a part of the above equation so long as it applies to an ideal gas.
However, for the entropy definition Dtc was replaced with the variable Dt in order that the equation may apply to more general cases.
Making the same change in this analogous derivation:
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Defining an
analogy to entropy for frequency:
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Substituting:
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So, Planck’s constant is the constant ∆Sp for an ideal gas, while the form above is the variable form for general cases. Now I wish to give a detailed general definition for Planck's constant.
The potential energy
of the hydrogen electron in its first energy level is:
![]()
Where:
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Substituting
for the speed of light:

The denominator
on the right side is the period of the frequency. Therefore:
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Also, the
potential energy for a circular orbit can be expressed as:
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Therefore:
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Solving for
Planck’s constant:
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This result defines Planck’s constant in terms of properties of the hydrogen atom.
I have preliminarily defined temperature as:
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I have also derived:
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Solving for kT :

Since:
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Then:

I have established a relationship
between Planck’s constant and Boltzmann’s constant in the form of:
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Substituting for Planck’s constant:

Substituting for kT :
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Or, in terms of
momentum:
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Where:
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I have defined:
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Substituting
for kB :
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Also:
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And, from an
earlier result:
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Yielding:
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The first set
of parenthesis contains the potential energy of the hydrogen electron in its
first energy level. The second set is the period of time required for the
electron to complete one radian. The third set is the angular velocity of the
electron in units of radians per second.
This theory’s definition of Planck’s constant first changes frequency into radians per second. Then, it converts radians per second, for the subject frequency, into a measure of the number of radians traveled during the period of time required for the hydrogen electron to travel one radian. Finally, the result of the first two steps is multiplied by the potential energy of the hydrogen electron in its first energy level. In other words, Planck’s constant uses fundamental properties of the hydrogen atom as the standard by which to convert frequencies into quantities of energy.
THE NATURE OF MASS
This theory has identified the property of mass as being the inverse of a fundamental measure of change of velocity of light. This nature of mass can be expressed as the property of acceleration of photons. The direction of this acceleration is different for different particles. It is the size of the associated acceleration and its direction that gives magnitude and polarity to mass.
Mass and the Radius of the Hydrogen
Atom ![]()
Since the speed
of light varies widely between the proton and electron of the hydrogen atom,
then the length of a photon passing between them should change accordingly. In
this case I cannot treat the whole photon length as a differential value. In
this case, the differential of photon length is a much smaller value. It is
useful to imagine a very small length of photon traveling from the proton to
the electron. I will call this very small section of photon length a
sub-photon.
The
accelerating proton stores energy in this sub-photon. As the sub-photon moves
away from the proton center, the speed of light increases dramatically and the
sub-photon length increases dramatically. I have shown earlier that force is
conserved in the photon and, for this example, in the sub-photon length. The
force stored in the sub-photon is given by:
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Since force is
measured at a point then this formula applies equally well to each part of the
sub-photon.