I. Electrostatics.
Environmental Reflection of Charge
Let us take as an axiom the postulate on the adequacy of environmental reflection of a charge in relation to the dependence of a medium induced charge on the size of the initial charge and on nothing else. As it is possible to receive all the information about the charge q only if we go around it from all the sides and reflect it in a "mirror" closed around it, then
(1)
where D is a vector of the density of information "for us", i.e. the
charge induced in the unit of area of the surface S closed around the
charge; q is information about the initial charge "in itself"; is the
mentioned above relative dielectric medium permeability performing the
function of the factor of proportionality of the information "for us"
in the form of an integral (1) to the information "in itself" q.
If we differentiate (1) spaces inside the surface S in all its
volume, we shall receive a local form (1) as follows
(1a),
where is
the charge space density in each point inside S
The vector field with density D of the information "for us" is the electrostatic field, although instead of D the vector is very often used, which is called a shift vector. This allows to simplify (1) and (1à) as follows
(1b)
and
(1c)
If we accept as a second axiom that the force F,
affecting the trial charge q0, acting as a measuring instrument for the
electrostatic field, is proportional to D and q0, then
where is an absolute dielectric vacuum permeability; is electric field intensity and is dielectric medium permeability. If the charge q possesses spherical symmetry, and if we embrace it with the spherical surface S with the radius r, we shall receive from (1)
(3a)
It results from (3a) and (6) that, firstly, like charges repel one another and opposite charges attract one another and, secondly, that in the first case the energy of their interaction is positive and in the second case it is negative.
Expression (6) allows to define "classical" radius r0 of electron and positron, if we suppose that the whole internal energy mñ2 of these particles has a pure electric origin. Then where m0 and å are the mass and charge of electron (positron). Hence
(7)
Traditionally it has been considered that this proportion is not quite true because from the momentum of electron results, as it were, a little bit different proportion, which differs from (7) by half. But in Chapter II we shall deduce another proportion for the momentum compared to the traditional one, which gives a result for the electron radius that agrees with (7). If differentiate (6) in volume V, when dV = dS× dr, we shall have for the density w of the field energy either
(8à)
or w = (dqn /dS) (dU/dr) = D0 Å/2, (8b)
if instead of we consider 2 medium induced charges of opposite signs, so that du/dr = - E and 2dqn /dS = D0.
It results from (3) and (8b) that
although the intensity of the field of the sum of two charges q1 + q2 =
q equals the sum of the field intensities of each charge Å = Å1 + Å2,
the energy density of the field of the sum of two charges is W = W1 + W2
+ D1E2 /2 + + D2E1 /2, i.e. it is either bigger than the sum of the
energy densities of the field of each charge if they are like charges,
or it is smaller if they are opposite charges. This means that the
system of opposite charges is always stable and the system of like
charges is unstable.
From (1a) and (4) with acknowledgement of (2) results so-called Poisson
equation
(1d)
which will be necessary further on.
Now we shall also consider the field of a cylinder uniformly charged and infinite in length as we shall need this in the next Chapter.
As in this case we deal with cylindrical symmetry, it is enough to consider the field of an element dl of the cylinder length, at which falls the charge dq. Then embracing this element with optional cylindrical surface with radius r and length dl, we shall have according to (1) and (2)
hence
(9)
where is line density of the cylinder
charge. To sum up, we would like to state that the shift vector D
in its substance equals the induced charge dqn, falling at the unit dS
of the surface, normal field, i.e.
D = dqn /dS = dqn /(dl)2, (10) where dl is the length of
the ground side dS.