Generator

Reflection against the thickness of the boundary

One function in the waves library, called 44 times across 8 essays. Below: what it draws at its defaults, what it draws at every branch an essay asks for, whether the site's own gate puts a claim to it, and everywhere it is called.

At its defaults it draws reflection against the thickness of the boundary. How much of the wave comes back, against the width of the transition between media of wavenumber 1 and 2.2, on a logarithmic scale. At zero width the curve reaches 1.406e-1, which is the abrupt-interface value computed from the two end values and nothing else — so the smooth calculation contains the sharp one as a limit rather than contradicting it. Past a width of about a wavelength the fall is a straight line on this scale, of measured slope -12.551 per unit width against the -12.566 the asymptotic form gives, which is 4π times the smaller of the two wavenumbers. Exponential, not merely small: three wavelengths of transition costs eight decades of reflection. The circles are the same quantity computed by slicing the profile into uniform layers, agreeing with the curve to a factor of 1.0115.

gradient-reflection is one function in lib/figures/waves.js — travelling, standing, adding and shifting. Everything below came out of it during this build, at parameters taken from the essays rather than invented for this page. A figure here is the figure a reader meets in an essay, and if the generator changes, this page changes with it.

At its defaults

Drawn even though every essay passes options, because a default nothing exercises is a trap for the next essay to call this with none — which has happened here twice.

Reflection against the thickness of the boundary. How much of the wave comes back, against the width of the transition between media of wavenumber 1 and 2.2, on a logarithmic scale. At zero width the curve reaches 1.406e-1, which is the abrupt-interface value computed from the two end values and nothing else — so the smooth calculation contains the sharp one as a limit rather than contradicting it. Past a width of about a wavelength the fall is a straight line on this scale, of measured slope -12.551 per unit width against the -12.566 the asymptotic form gives, which is 4π times the smaller of the two wavenumbers. Exponential, not merely small: three wavelengths of transition costs eight decades of reflection. The circles are the same quantity computed by slicing the profile into uniform layers, agreeing with the curve to a factor of 1.0115.

How much of the wave comes back, against the width of the transition between media of wavenumber 1 and 2.2, on a logarithmic scale. At zero width the curve reaches 1.406e-1, which is the abrupt-interface value computed from the two end values and nothing else — so the smooth calculation contains the sharp one as a limit rather than contradicting it. Past a width of about a wavelength the fall is a straight line on this scale, of measured slope -12.551 per unit width against the -12.566 the asymptotic form gives, which is 4π times the smaller of the two wavenumbers. Exponential, not merely small: three wavelengths of transition costs eight decades of reflection. The circles are the same quantity computed by slicing the profile into uniform layers, agreeing with the curve to a factor of 1.0115.

Nine slabs, no symmetry, and one transmission

The options are the ones Swap the ends and nothing changes passes. A branch drawn at its own defaults instead would be a picture no essay asked for and no assertion has been run against.

Nine slabs, no symmetry, and one transmission. A stack of 9 slabs of random wavenumber and random thickness, with no symmetry anywhere in it. Send a wave in from the left and the amplitude that emerges on the right is 0.6694240937; turn the stack round and send it in from the right and the amplitude is 0.6694240937. The two agree to every digit the arithmetic has. This is not a property of the stack — it survives any arrangement, any number of layers, any amount of internal reflection — but of the equation, which is unchanged when the sign of time is reversed, and the phase is protected as well as the modulus, which is the stronger statement and the one an interferometer would notice. The reflections are a different matter. Their moduli are equal too, at 0.742880, but only because nothing here absorbs; their phases differ by 1.621 radians, because the wave meets a different first surface from each side. What the theorem protects is the pair of ends, and not what the wave does on its way between them.

A stack of 9 slabs of random wavenumber and random thickness, with no symmetry anywhere in it. Send a wave in from the left and the amplitude that emerges on the right is 0.6694240937; turn the stack round and send it in from the right and the amplitude is 0.6694240937. The two agree to every digit the arithmetic has. This is not a property of the stack — it survives any arrangement, any number of layers, any amount of internal reflection — but of the equation, which is unchanged when the sign of time is reversed, and the phase is protected as well as the modulus, which is the stronger statement and the one an interferometer would notice. The *reflections* are a different matter. Their moduli are equal too, at 0.742880, but only because nothing here absorbs; their phases differ by 1.621 radians, because the wave meets a different first surface from each side. What the theorem protects is the pair of ends, and not what the wave does on its way between them.

One change of medium, at three thicknesses

The options are the ones Swap the ends and nothing changes passes. A branch drawn at its own defaults instead would be a picture no essay asked for and no assertion has been run against.

One change of medium, at three thicknesses. The wavenumber against position for a medium changing from 1 to 2.2, over transition widths of 0.02, 0.2, 0.6 in the same units — that is, 0.003, 0.032, 0.095 wavelengths of the longer wave. The three profiles have identical ends and differ only in how quickly they get from one to the other. The reflectances are 1.39e-1, 5.09e-2, 5.20e-4, a range of 2.7e+2 to one, computed by slicing each profile into thin uniform layers and multiplying their transfer matrices. Nothing about the two media has changed between the curves. The only thing that has changed is a length, and the length is not in the Fresnel expressions at all.

The wavenumber against position for a medium changing from 1 to 2.2, over transition widths of 0.02, 0.2, 0.6 in the same units — that is, 0.003, 0.032, 0.095 wavelengths of the longer wave. The three profiles have identical ends and differ only in how quickly they get from one to the other. The reflectances are 1.39e-1, 5.09e-2, 5.20e-4, a range of 2.7e+2 to one, computed by slicing each profile into thin uniform layers and multiplying their transfer matrices. Nothing about the two media has changed between the curves. The only thing that has changed is a length, and the length is not in the Fresnel expressions at all.

The only thing that breaks it, and the instrument that reads the difference

The options are the ones Swap the ends and nothing changes passes. A branch drawn at its own defaults instead would be a picture no essay asked for and no assertion has been run against.

The only thing that breaks it, and the instrument that reads the difference. Transit-time difference between an upstream and a downstream pulse, against flow speed, for a 10 cm path in water. Reciprocity is a consequence of the wave equation being unchanged when the sign of time is reversed, so no arrangement of materials can break it — and a medium that is itself moving does break it, because reversing time reverses the flow as well. The downstream pulse arrives sooner and the upstream one later, by 2vL/c² to a part in 1e+5 across this range: 18 ns at 0.2 m/s, 46 ns at 0.5 m/s, 91 ns at 1 m/s, 183 ns at 2 m/s, 365 ns at 4 m/s. That difference is the whole of a transit-time flowmeter, and it is why the instrument needs a clock good to a nanosecond rather than a sensor in the pipe. The other thing that breaks reciprocity is a magnetic field, through the same loss of time-reversal symmetry — and neither breaks it by attenuating anything, which is why an optical isolator is a rotator and a polariser: the magnet supplies the non-reciprocity and the polariser turns it into a one-way door.

Transit-time difference between an upstream and a downstream pulse, against flow speed, for a 10 cm path in water. Reciprocity is a consequence of the wave equation being unchanged when the sign of time is reversed, so no arrangement of materials can break it — and a medium that is itself moving does break it, because reversing time reverses the flow as well. The downstream pulse arrives sooner and the upstream one later, by 2vL/c² to a part in 1e+5 across this range: 18 ns at 0.2 m/s, 46 ns at 0.5 m/s, 91 ns at 1 m/s, 183 ns at 2 m/s, 365 ns at 4 m/s. That difference is the whole of a transit-time flowmeter, and it is why the instrument needs a clock good to a nanosecond rather than a sensor in the pipe. The other thing that breaks reciprocity is a magnetic field, through the same loss of time-reversal symmetry — and neither breaks it by attenuating anything, which is why an optical isolator is a rotator *and* a polariser: the magnet supplies the non-reciprocity and the polariser turns it into a one-way door.

The ripple a reflection leaves on the incoming side

The options are the ones Swap the ends and nothing changes passes. A branch drawn at its own defaults instead would be a picture no essay asked for and no assertion has been run against.

The ripple a reflection leaves on the incoming side. The amplitude of the wave through the transition, for the sharpest and the smoothest of the profiles. On the incoming side each curve is the incident and the reflected wave together, so it ripples, and the depth of the ripple is a direct measurement of how much came back: a visibility of 0.3559 for L = 0.02, against a reflection amplitude of 0.3728; and a visibility of 0.0228 for L = 0.6, against a reflection amplitude of 0.0228. The smooth transition's incoming side is almost flat — the wave passes as though nothing were there — while the sharp one's ripples visibly. Both fields are integrated from the far side, where the solution is a pure outgoing wave by construction, so the reflection is an output of the integration rather than an input to it.

The amplitude of the wave through the transition, for the sharpest and the smoothest of the profiles. On the incoming side each curve is the incident and the reflected wave together, so it ripples, and the depth of the ripple is a direct measurement of how much came back: a visibility of 0.3559 for L = 0.02, against a reflection amplitude of 0.3728; and a visibility of 0.0228 for L = 0.6, against a reflection amplitude of 0.0228. The smooth transition's incoming side is almost flat — the wave passes as though nothing were there — while the sharp one's ripples visibly. Both fields are integrated from the far side, where the solution is a pure outgoing wave by construction, so the reflection is an output of the integration rather than an input to it.

Reflection against the thickness of the boundary

The options are the ones Swap the ends and nothing changes passes. A branch drawn at its own defaults instead would be a picture no essay asked for and no assertion has been run against.

Reflection against the thickness of the boundary. How much of the wave comes back, against the width of the transition between media of wavenumber 1 and 2.2, on a logarithmic scale. At zero width the curve reaches 1.406e-1, which is the abrupt-interface value computed from the two end values and nothing else — so the smooth calculation contains the sharp one as a limit rather than contradicting it. Past a width of about a wavelength the fall is a straight line on this scale, of measured slope -12.551 per unit width against the -12.566 the asymptotic form gives, which is 4π times the smaller of the two wavenumbers. Exponential, not merely small: three wavelengths of transition costs eight decades of reflection. The circles are the same quantity computed by slicing the profile into uniform layers, agreeing with the curve to a factor of 1.0115.

How much of the wave comes back, against the width of the transition between media of wavenumber 1 and 2.2, on a logarithmic scale. At zero width the curve reaches 1.406e-1, which is the abrupt-interface value computed from the two end values and nothing else — so the smooth calculation contains the sharp one as a limit rather than contradicting it. Past a width of about a wavelength the fall is a straight line on this scale, of measured slope -12.551 per unit width against the -12.566 the asymptotic form gives, which is 4π times the smaller of the two wavenumbers. Exponential, not merely small: three wavelengths of transition costs eight decades of reflection. The circles are the same quantity computed by slicing the profile into uniform layers, agreeing with the curve to a factor of 1.0115.

What checks it

physicscheck asserts something about gradient-reflection that could fail — it draws it and measures the result against a value reached some other way.

Across the library: 100 interrogated, 2 exercised only, 1 untouched, of 103. Read out of the gate's source by the gate's own two patterns — and the gate's last claim fails the build if that read disagrees with what it was handed while running.

Where it is called

Changing this generator changes every figure on this list. That is what makes the list worth publishing rather than keeping in a check script.

Waves

Swap the ends and nothing changes

Put a source at one end of the most complicated arrangement of materials anybody can build and a detector at the other, then exchange them. The reading is identical — not approximately, not on average, but to every digit the arithmetic has. Two things in physics break it, and neither of them is a shape.

Waves

The equation that lets a shape travel

Newton's second law applied to a piece of string a millimetre long gives T·y″ = µ·ÿ, and the derivation never once asks what the string is made of. Two things fall out immediately: the speed is √(T/µ) and belongs to the medium, and the general solution holds two arbitrary functions rather than one. The second of them is the reflection, which is why a boundary condition can be met at all.

Waves

The layer that makes a reflection vanish

A wave meeting a step in impedance reflects, and nothing can be done about the step. Put a third medium between the two, a quarter of a wavelength thick and of exactly the intermediate impedance, and the reflection stops existing — not reduced, cancelled.

Waves

The mismatch no network can remove

A quarter-wave layer or a taper can match a resistance to a resistance as well as anyone likes. Put a capacitance across the load and that stops being true for every network that could ever be built from lossless parts: Bode and Fano proved that the total amount of match available is fixed by the load's resistance and capacitance, so a network can only move it about — and a flat match across a band can never be better than e to the minus π over the load's time constant times the band.

Waves

The node that is not standing still

A wave meeting a perfect reflector makes a standing wave with real nodes. A partial reflection makes something that looks the same and is not: the minima are not zeros, energy flows steadily through them, and the depth of the pattern is a measurement of the load that caused it.

Waves

The taper that matches every note

A quarter-wave layer cancels a reflection at one wavelength and only near it. Spread the same change of impedance over a distance instead, and the reflection vanishes for every wavelength shorter than about twice that distance — not by cancelling one echo against another, but by leaving no step anywhere for an echo to come from.

Waves

The wave a surface is enough to hold

A pipe guides with walls and a fibre guides with a slower core. A solid needs neither: one free surface binds a wave that is not a bulk wave bouncing but a separate solution, travelling slower than any wave in the material, dying away exponentially into it, and carrying its energy round a circle instead of over a sphere — which is why it is the part of an earthquake that knocks buildings down.

Waves

What happens where the medium changes

Two conditions at a join — the displacement is continuous, and so is the transverse force — fix the reflected and transmitted amplitudes completely. What decides them is one quantity, the impedance, and not the stiffness or the density separately: two quite different media with the same impedance are, to a wave, the same medium.

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