Inertia and principal directions. About the centre of mass, the inertia tensor is
It relates angular momentum and angular velocity by and gives rotational kinetic energy . The principal axes are orthogonal eigenvector directions of this real symmetric tensor; in that basis it is diagonal, with entries the principal moments of inertia .
Derivatives in a rotating frame. Write in a body-fixed orthonormal basis. Each basis vector rotates according to . Differentiating the components and basis separately proves the rotating-frame derivative formula,
The body derivative differentiates the scalar components in that basis. A fixed pivot can replace the centre of mass when the corresponding angular-momentum balance is valid.
Euler equations. The inertial angular-momentum equation is . Since the principal moments are constant in the body frame, substitute :
These are Euler's equations in the principal body frame.
Linear perturbation of free rotation. After the impulse, . Let to leading order and be small. The third Euler equation changes only at quadratic order, so the linear transverse equations are
For and , eliminate from
This gives
Its units are inverse square seconds. Positive gives a growing real exponential; negative gives bounded oscillatory perturbations.
Distributed line parameters. The geometry is the wide parallel-plate transmission line described in the question, with absolute permittivity . A length has charge and field , giving
The opposed plate currents have sheet density and confine the leading magnetic field between the plates. The magnetic energy per unit length is , so
Here and are per unit length, in and , not lumped component values. Internal conductor fields and edge corrections are neglected.
Voltage and current evolution. The current entering a short length minus that leaving it is the rate of increase of its plate charge:
The voltage drop across that length is its inductive drop, . Dividing by gives the lossless Telegrapher's equations,
Propagation speed. Differentiate these equations once more and eliminate the other variable:
The wave equation speed is
Travelling-wave impedance. For a forward wave , take . Substitution into gives , hence the characteristic impedance
The backward-wave current has the opposite sign relative to its voltage; the fixed ratio above applies to one travelling direction.
Matching the antenna. The voltage reflection coefficient is . No reflection requires . With , , and ,
The resulting is consistent with the wide-plate approximation.
Both transverse forces. The matched transverse electromagnetic mode has electric attraction and magnetic repulsion. For time-averaged power ,
The force on one plate excludes its own field. Thus the average electric attraction and magnetic repulsion per unit length are respectively
The electric and magnetic pressure cancellation in a matched TEM line follows directly from :
The equality also holds instantaneously for a single travelling wave. Quoting either alone would omit the opposing contribution. This is the ideal electromagnetic force in the stated lossless uniform-dielectric model; a standing wave would not generally have the same cancellation.
Effective permittivity. Use peak phasors with time dependence . The Ampere-Maxwell law is
The conductive contribution to complex permittivity is therefore
Here is the source's effective relative permittivity, not just the real part of a complex response. The positive imaginary term is the loss sign appropriate to this time convention.
The penetrating electric wave. Combine this equation with Faraday's law of induction. In a uniform source-free medium the transverse phasor satisfies
For a good conductor of electrical conductivity , , so . The root which decays into is
Choose the surface phasor amplitude real. Taking the real part of gives
The skin depth is an amplitude-decay distance in metres.
The magnetic wave and phase. The curl of an -polarized field varying in is in the direction. Since ,
Thus
The phase sign follows the specified convention. Equivalently the surface impedance of a good conductor is .
How the fields differ from those in vacuum. The two metal fields have the same exponential envelope and spatial period , but their phase arguments differ by .
Figure 1.
Original normalized electric and magnetic field profiles inside a good conductor at one instant, showing their common decay envelope and quarter-of-a-right-angle phase difference
. Details.
An individual travelling wave in the lossless exterior has no attenuation, real wave impedance and in-phase electric and magnetic fields. The exterior total field also includes the reflected wave and may show interference, so it need not share that simple phase relation everywhere. At the interface the tangential fields match; is the field just inside the metal, not necessarily the incident amplitude. A good conductor reflects strongly and its wave impedance is much smaller than the vacuum impedance.
Average inward energy flux. For peak phasors, the Poynting vector averaged over a cycle is . The fields give
Consequently the constant in the question is
The flux is in the direction and has units .
Local energy conservation. The Poynting flux and local heating in a skin layer satisfy
The decrease becomes Joule heating in each layer. The Poynting theorem includes this transfer from field energy to the metal; averaged electromagnetic energy storage has zero time derivative in the periodic state, so no energy is lost from the complete balance.
The field law. In the Biot-Savart law, is the contribution to the magnetic flux density at the observation point from a directed wire element carrying steady conventional electric current . The vector points from that element to the observation point, , and . The constant is the vacuum permeability; the cross product sets the direction by the right-hand rule. Integrating the elements gives the total field, in teslas.
The moment of the shown loop. The arrows in the original PDF run counterclockwise viewed from . Thus the magnetic dipole moment is
Its units are . Reversing the current reverses both this moment and the field.
The boundary-value method. In a charge-free region, the electric potential obeys the Laplace equation, , and . Conductors impose equipotential boundaries, with specified voltages or charges, and a far-field condition fixes the remaining behaviour. The Uniqueness of the Dirichlet problem guarantees that a solution meeting the prescribed conductor potentials is the physical one. To see why, the difference of two candidate solutions is harmonic and vanishes on the boundaries; integration by parts gives , hence no difference in their fields. An exterior problem also needs the appropriate condition at infinity.
Two axisymmetric harmonic functions. For in spherical coordinates, the Laplacian reduces to
For , the bracket is . For , it is . Therefore
The second function is singular at the origin, which is allowed here because that point lies inside the excluded conductor. The printed spherical Laplacian has a typo in its azimuthal term: its denominator should be . Both functions are axisymmetric, so that term vanishes and the typo does not affect these calculations.
Potential and field geometry. Set the lower conductor to zero potential and the distant upper plate to . The small boss sees approximately uniform background field , where . Combining the two harmonic functions to make on gives the conducting hemispherical protrusion in a uniform field,
It also vanishes on the surrounding plane . The electric field components are
Equipotentials crowd near the apex, and field lines meet the conductor normally.
Figure 1.
Original calculated local equipotentials and electric-field lines above the hemispherical boss; this is the small-boss approximation rather than an exact finite-gap solution
. Details.
The formula has the correct uniform far field but does not exactly impose a flat upper equipotential at finite . It is the leading approximation justified by ; an exact finite-gap solution would include further corrections.
Apply equal compressive pressure in all directions; here denotes Poisson's ratio. The three principal normal stresses are . For an isotropic linearly elastic material, Hooke's law gives
and similarly for . At small strain, the fractional volume change is the sum of these normal strains:
The bulk modulus is , giving the isotropic elastic modulus relation,
The result assumes linear elasticity and fixed isotropic moduli. In the incompressible limit with finite Young's modulus, the bulk modulus tends to infinity.
The conventional electron plasma frequency is
Use , , and . Then
The equal proton density ensures charge neutrality; it does not double the electron density in this formula. Protons have their own plasma frequency,
If both cold species are allowed to move in the relative charge-separation oscillation, its squared frequency is . This gives , only about above the electron-only answer, because .
A large gas volume can reduce the effective mass density of the water surrounding the hull. In the simple quasihydrostatic model for the buoyancy of an aerated liquid, gas void fraction gives
By Archimedes' principle, a boat displacing volume then has buoyant force . To support the same boat mass , it needs a larger displaced volume , so its draft increases. If that exceeds the available watertight displacement, it can lose flotation or become swamped:
Uneven aeration and strong plume motion can also disturb stability. This explains a possible hazard, not a claim that any bubble plume must sink a boat: upward water flow, turbulence and the distribution of bubbles can exert substantial additional forces.
Let the signed axial velocity on the axis be . Smooth axisymmetric flow has and regular radial velocity at . The incompressible flow condition in cylindrical coordinates is
To leading order near the axis, integrate from zero to . The integration constant vanishes by regularity, giving the near-axis radial velocity in incompressible axisymmetric flow,
With the usual signed interpretation ,
For this is outward: the outward axial flow slows as its distance from the origin grows, and incompressibility requires radial spreading. Here has units , so the answer is a speed.
The source specifies a magnitude rather than an unambiguous signed component. On , reversing the axial flow while keeping its magnitude would reverse the radial answer. The general relation makes that dependence explicit; the boxed expression adopts , outward on both halves of the axis.
An infinite sheet of surface charge density gives an electric field of magnitude on either side, normal to the sheet and directed away from positive charge. Use the superposition principle for the two sheets. Choose normals for and for . Away from the charged planes,
The minus sign on the second contribution makes its field point toward the negatively charged sheet. Each sector has a uniform electric field; its direction changes on crossing a sheet.
Figure 1.
Original calculated electric-field directions for the intersecting positive and negative charge sheets; arrows retain the relative field magnitudes in the four sectors
. Details.
For example, above both sheets the field points right and slightly upward, whereas in the sector but it points left and steeply upward. The other two sectors follow by inversion through the origin. The normal field jumps by the appropriate surface charge divided by ; a single field value on an ideal zero-thickness charged sheet is not required.
Molecular transport across gradients. A gas can transport momentum, thermal energy and species abundance even when its average bulk velocity is zero. Molecules arriving at a point carry properties acquired near their preceding collisions. A small gradient makes the populations arriving from opposite sides slightly different, producing transport from larger to smaller values of the carried property. A continuum transport law requires a mean free path small compared with the gradient length, and relaxation times short compared with the observation time.
For a dilute hard-sphere gas,
where is molecular collision diameter. Both speed and collision distance matter: high speed alone does not determine a transport coefficient.
A simple kinetic estimate makes the common structure explicit. For a quantity carried per particle, a molecule moving at angle to brings approximately . Expanding to first order and averaging an isotropic velocity distribution gives
since and . This mean-free-path argument estimates the coefficients; a detailed collision calculation changes their numerical prefactors and distinguishes different relaxation rates.
Momentum transport and viscosity. For a shear flow with mean velocity , the transported directed momentum per molecule is . The net flux of momentum in the direction is
Here is dynamic viscosity in . The associated shear stress on a material surface has the corresponding traction sign convention; the flux carries momentum from the faster-moving layer towards the slower-moving one. The kinematic viscosity is , with units . Viscosity smooths velocity gradients, and the lost ordered mechanical energy becomes heat.
Heat transport. Let be the thermal heat capacity per molecule, in . Substituting gives Fourier's law,
Thermal conductivity has units . For a monatomic gas, translational equipartition gives . Rotational or vibrational excitations in other gases can increase the energy carried per molecule, while collisions govern how those modes exchange energy. A temperature gradient can therefore be transported differently from directed momentum even when the dimensional estimates look similar.
Species transport. For a dilute tracer or a mixture with prescribed total density and negligible bulk flow, molecules diffuse down concentration gradients. The first-gradient number flux is Fick's first law,
The diffusivity has units ; multiplying number flux by the species mass gives mass flux. More generally one uses diffusion flux relative to the mixture's bulk velocity and specifies mass or mole fractions. The approximation is not a claim that an arbitrary pure-gas pressure gradient can remain at rest while only a Fick flux acts. In a mixture, collision cross-sections and relative molecular speeds, including the reduced mass, determine the species diffusivities.
Dependence on density and temperature. The kinetic estimates of gas transport coefficients predict, for fixed collision diameter and molecular heat capacity,
Thus dynamic viscosity and thermal conductivity are approximately density independent in the dilute continuum regime. Reducing density reduces the number of carriers but increases their mean free path in the same proportion. At fixed density all three estimates grow as ; at fixed pressure, and
Kinematic viscosity and thermal diffusivity also grow roughly as at fixed pressure in this model. Real interaction potentials make effective collision cross-sections temperature dependent, and internal excitations change . Dense-gas correlations and boundaries invalidate the simple cancellation. In particular, when the mean free path approaches the apparatus scale, transport becomes free molecular; it cannot be described by extending the same local, pressure-independent Fourier and viscosity coefficients indefinitely.
Heat diffusion equation. For a stationary gas with constant volumetric heat capacity , constant thermal conductivity and negligible compression work, the energy balance in any fixed volume is
Here is a possible heat generation rate per volume. The divergence theorem and Fourier's law yield
Thermal diffusivity has units and is of order . In a moving or compressing gas, the material derivative, pressure-volume work and viscous heating must also enter the internal-energy equation. The displayed pure diffusion equation describes the approximation in which those effects are absent or negligible.
Representative solutions. With no source, a steady one-dimensional slab between temperatures at has and uniform heat flux . Thus a constant spatial gradient transports heat without changing local temperature in time when the boundaries continually supply and remove it.
For an infinite medium and an initial sinusoidal temperature perturbation,
Short spatial wavelengths decay faster, and the characteristic smoothing length after time is . A finite slab with both ends held at has a sine expansion with factors ; its slowest relaxation time is .
An instantaneous heat input per unit transverse area at in an otherwise uniform infinite medium gives the Gaussian solution
Its integral conserves the deposited heat. The peak falls as while its width grows as ; diffusion redistributes energy instead of transporting a sharp front at a single velocity.
Finally, a semi-infinite body initially at and held at surface temperature from has
It has and approaches far from the boundary at finite time. These solutions demonstrate steady conduction, mode decay, spreading of localized heat and boundary-driven diffusion. Their idealized behaviour at extremely short times or arbitrarily long distances must be interpreted within the continuum regime rather than as an assertion of instantaneous microscopic communication.

Pinned article: Introduction to the OurBigBook Project

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    Video 3.
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