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David or Jo Anne Ryeburn August 29th 03 06:31 AM

Calculus not needed (was: Reflection Coefficient Smoke Clears a Bit)
 
I've enjoyed reading this and related threads. Some comments have been
made about using calculus. Though I spent a significant portion of my
pre-retirement life attempting to teach that subject to undergraduates, I
don't believe in using calculus whenever simple geometry and/or algebra
makes it unnecessary. A proof that avoids calculus can be meaningful for
those who don't know calculus, or who haven't used it for a while.

With that said, I have a few comments to make about some of the assertions
I have read here recently, some of which have appeared without explicit
proof.

(1) The surge impedance of a (lossy) transmission line cannot have an
angle more than 45 degrees away from the real axis.

This is true. Z_0 = sqrt((R + jwL)/(G + jwC)) (here I am using "w" instead
of omega). Both the numerator and denominator lie in the first quadrant,
so their quotient lies in the right half plane (angles subtract when one
divides), and the square root of that has an angle lying between - 45
degrees and + 45 degrees. (The branch of the square root with positive
real part has to be taken; if you can find coax whose surge impedance has
a negative real component, I'll pay you good money for it.)

[Since this angle lies between - 45 degrees and + 45 degrees, peculiar
consequences deduced from calculations involving surge impedances such as
50 - j200 can be ignored.]

(2) There is a nice geometrical interpretation for the reflection
coefficient, or rather for its magnitude. Since the coefficient is (Z_L -
Z_0)/(Z_L + Z_0), its magnitude expresses how much further Z_L is from the
surge impedance Z_0 than it is from the negative, - Z_0, of the surge
impedance. If Z_L is equidistant from Z_0 and - Z_0, then the magnitude of
the reflection coefficient is 1. If Z_L is closer in the complex plane to
Z_0 than it is to - Z_0, then the magnitude of the reflection coefficient
is less than 1. If Z_L is closer to - Z_0 than to Z_0, then the reflection
coefficient's magnitude exceeds 1. Now plot the points Z_0 and - Z_0 and
draw the perpendicular bisector of the segment joining them. If Z_L is on
that perpendicular bisector, the magnitude of the reflection coefficient
is 1; if it is on Z_0's side of the bisector, the magnitude is less than
1; if it is on - Z_0's side, the magnitude exceeds 1. Of course Z_L has to
stay in the right half plane; if it didn't have to do this, you could take
Z_L very close to - Z_0 and get enormous reflection coefficient
magnitudes.

(3) Consider an ellipse having Z_0 and - Z_0 as its foci. There are
infinitely many such ellipses, including a degenerate one (just the
segment between the "foci"). All these different ellipses fill up the
complex plane, and no point in the plane is on more than one of them. On
any one such ellipse, the sum of the distances from a point on the ellipse
to the two foci Z_0 and - Z_0 is constant (definition of an ellipse), the
value of that constant depending upon which ellipse it is but the constant
has to be at least as large as the interfocal distance. We should ignore
points on the ellipse that are in the left half plane. A portion of the
ellipse will be in the same quadrant as Z_0, and a portion will be in the
quadrant that contains the conjugate of Z_0. (Remember we are ignoring the
points in the left half plane.) All of the points on the ellipse that are
in Z_0's quadrant are closer to Z_0 than to - Z_0, so they'll give
reflection coefficients with magnitude less than 1. So will those of the
points on the ellipse in the other quadrant under consideration that are
between the real axis and the perpendicular bisector. But those that are
between the perpendicular bisector and the imaginary axis will be closer
to - Z_0 than to Z_0 and thus will yield reflection coefficients with
magnitudes greater than 1. It should be obvious that, along any given
ellipse, the one for which the magnitude of the reflection coefficient is
greatest is the one on the imaginary axis, since as we move along the
ellipse towards that point, the distance to - Z_0 decreases and the
distance from Z_0 increases (remember, their sum is constant along the
ellipse). So on any *one* ellipse, the largest reflection coefficient
magnitude occurs where the ellipse meets the imaginary axis, and thus Z_L
has real part 0 and imaginary part of opposite sign to that of Z_0.

(4) Start with Z_0 real, and slowly rotate Z_0 into either the first or
fourth quadrant, but not more than 45 degrees in either direction, keeping
the same magnitude while you rotate. The segments joining Z_0 and - Z_0,
their perpendicular bisectors, and the various ellipses will all
simultaneously rotate. It's now obvious that for ellipses of any fixed
size, the one producing the largest magnitude for the reflection
coefficient will occur when Z_0 is at + 45 degrees or - 45 degrees. So if
we want to maximize the reflection coefficient magnitude, we can restrict
attention to those two cases. The - 45 degree case (capacitive surge
impedance) is the more familiar one, but the math is the same either way.
The only question is, which one of the ellipses should we use, if we wish
to maximize the magnitude of the reflection coefficient?

(5) So now we're going to assume Z_0 = k(1 - j), and thus - Z_0 = k(-1 +
j), while Z_L = ktj. It's clear that the factor k is going to cancel out
when calculating the reflection coefficient, so I will henceforth ignore
it (i.e., normalize it to k = 1 by appropriate choice of units). If you
are of a geometrical turn of mind, you can produce a geometrical argument
showing that the best one can do is to make sure the ellipse meets the
imaginary axis at the same distance from the origin as the two foci, i.e.
at j*sqrt(2). If you are of an algebraic turn of mind, you can make an
algebraic argument involving completing the square to demonstrate the same
thing. If you insist on using calculus, it's now just one variable
calculus, not multivariable calculus, since the only independent variable
is t, which will turn out to be sqrt(2) at the maximum. (Hint: don't look
at the ratio of distances; look at the square of that ratio, so as to get
rid of all those square roots.)

(6) Once all that is done, it's just a bit of algebra to show that when t
= sqrt(2) then the magnitude of the reflection coefficient is 1 + sqrt(2).
That's the best (worst?) you can do. And if you can find some coax whose
surge impedance angle is - 45 degrees, you can indeed do it.

All the above was done from first principles. I am not fortunate enough to
own a copy of Chipman, though I wish I were, but if this is what he says,
then I am in full agreement with him.

David, ex-W8EZE, willing to part with some of my pension money for a copy
of Chipman if you know where one can be found (Powell's doesn't have any
copies)

--
David or Jo Anne Ryeburn

To send e-mail, remove the letter "z" from this address.

Ian White, G3SEK August 29th 03 08:16 AM

David or Jo Anne Ryeburn wrote:

David, ex-W8EZE, willing to part with some of my pension money for a
copy of Chipman if you know where one can be found (Powell's doesn't
have any copies)

When looking for a copy yesterday, it seemed incredible that none of the
major US dealers had even one for sale.

However, copies might also have been catalogued under "Schaum" as the
author, the book being one of the Schaum's Outline series.

I only discovered this possibility when it was too late to do anything
about it, so it may be worth a second look at the US dealers.


--
73 from Ian G3SEK 'In Practice' columnist for RadCom (RSGB)
Editor, 'The VHF/UHF DX Book'
http://www.ifwtech.co.uk/g3sek

Richard Clark August 29th 03 07:43 PM

On Fri, 29 Aug 2003 08:16:35 +0100, "Ian White, G3SEK"
wrote:

David or Jo Anne Ryeburn wrote:

David, ex-W8EZE, willing to part with some of my pension money for a
copy of Chipman if you know where one can be found (Powell's doesn't
have any copies)

When looking for a copy yesterday, it seemed incredible that none of the
major US dealers had even one for sale.


Hi All,

One very reliable source gave me two other sources with multiple
copies to choose from:
http://www.bookfinder.com/search/?ac...0558_2:268:527

73's
Richard Clark, KB7QHC

Dr. Slick August 29th 03 09:46 PM

(David or Jo Anne Ryeburn) wrote in message .. .
I've enjoyed reading this and related threads. Some comments have been
made about using calculus. Though I spent a significant portion of my
pre-retirement life attempting to teach that subject to undergraduates, I
don't believe in using calculus whenever simple geometry and/or algebra
makes it unnecessary. A proof that avoids calculus can be meaningful for
those who don't know calculus, or who haven't used it for a while.


The the area within the rho=1 circle of the Smith is reserved for
passive networks. Outside rho=1, where the reflection is greater than
one, is reserved for active networks only.


Slick

Richard Clark August 29th 03 10:46 PM

On Fri, 29 Aug 2003 17:28:24 -0400, "Tom Coates"
wrote:

Search Amazon.com and www.addall.com for ISBN 0070107475.
They're my favorite book-finding tools.

Tom, N3IJ


Hi Tom,

Thanks for the new lead to a book site.

73's
Richard Clark, KB7QHC

Peter O. Brackett August 30th 03 12:32 AM

Group:

Another very good and inexpensive reference on waves that might be of
interest to this group is:

William C. Elmore and Mark A Heald, "Physics of Waves", first published in
1969, but
most recently published in paperback by Dover Publications, New York, 1985
and
generally available in reprints even today for around US$17.00. A real
bargain.
ISBN: 0-486-64926-1 LCCN: 85-10419.

Be aware, since this is a Physics book it is loaded with gratuitous partial
differential
equations.

This book is interesting because it covers the *whole* field of waves, not
just
electromagnetic waves.

Electromagnetic waves are particularly simple when compared to general wave
phenomena,
since em waves are transverse only.

This book covers waves on strings and membranes, waves in and on fluids,
waves in compressible
media such as the earth [the seismic wavefield]etc... and so covers many of
the "analogies" that
posters to this news group like to draw upon, often drawing false
conclusions.

Are ocean waves at the beach *really* analogous to em waves?

This book will explain why not.

The earth supports both transverse and compressive-dillutive waves as well
as surface seismic waves. Are compressive-dillutive waves different either
qualitatively or quantitatively from electromagnetic transverse waves, this
book answers the question.

etc, etc...

Expand your wave horizons beyond mere em waves, if you are deeply interested
in waves, this book is more than worth the price at US$17.00. It's
available from Amazon.

--
Peter K1PO
Indialantic By-the-Sea, FL


"David or Jo Anne Ryeburn" wrote in message
...
I've enjoyed reading this and related threads. Some comments have been
made about using calculus. Though I spent a significant portion of my
pre-retirement life attempting to teach that subject to undergraduates, I
don't believe in using calculus whenever simple geometry and/or algebra
makes it unnecessary. A proof that avoids calculus can be meaningful for
those who don't know calculus, or who haven't used it for a while.

With that said, I have a few comments to make about some of the assertions
I have read here recently, some of which have appeared without explicit
proof.

(1) The surge impedance of a (lossy) transmission line cannot have an
angle more than 45 degrees away from the real axis.

This is true. Z_0 = sqrt((R + jwL)/(G + jwC)) (here I am using "w" instead
of omega). Both the numerator and denominator lie in the first quadrant,
so their quotient lies in the right half plane (angles subtract when one
divides), and the square root of that has an angle lying between - 45
degrees and + 45 degrees. (The branch of the square root with positive
real part has to be taken; if you can find coax whose surge impedance has
a negative real component, I'll pay you good money for it.)

[Since this angle lies between - 45 degrees and + 45 degrees, peculiar
consequences deduced from calculations involving surge impedances such as
50 - j200 can be ignored.]

(2) There is a nice geometrical interpretation for the reflection
coefficient, or rather for its magnitude. Since the coefficient is (Z_L -
Z_0)/(Z_L + Z_0), its magnitude expresses how much further Z_L is from the
surge impedance Z_0 than it is from the negative, - Z_0, of the surge
impedance. If Z_L is equidistant from Z_0 and - Z_0, then the magnitude of
the reflection coefficient is 1. If Z_L is closer in the complex plane to
Z_0 than it is to - Z_0, then the magnitude of the reflection coefficient
is less than 1. If Z_L is closer to - Z_0 than to Z_0, then the reflection
coefficient's magnitude exceeds 1. Now plot the points Z_0 and - Z_0 and
draw the perpendicular bisector of the segment joining them. If Z_L is on
that perpendicular bisector, the magnitude of the reflection coefficient
is 1; if it is on Z_0's side of the bisector, the magnitude is less than
1; if it is on - Z_0's side, the magnitude exceeds 1. Of course Z_L has to
stay in the right half plane; if it didn't have to do this, you could take
Z_L very close to - Z_0 and get enormous reflection coefficient
magnitudes.

(3) Consider an ellipse having Z_0 and - Z_0 as its foci. There are
infinitely many such ellipses, including a degenerate one (just the
segment between the "foci"). All these different ellipses fill up the
complex plane, and no point in the plane is on more than one of them. On
any one such ellipse, the sum of the distances from a point on the ellipse
to the two foci Z_0 and - Z_0 is constant (definition of an ellipse), the
value of that constant depending upon which ellipse it is but the constant
has to be at least as large as the interfocal distance. We should ignore
points on the ellipse that are in the left half plane. A portion of the
ellipse will be in the same quadrant as Z_0, and a portion will be in the
quadrant that contains the conjugate of Z_0. (Remember we are ignoring the
points in the left half plane.) All of the points on the ellipse that are
in Z_0's quadrant are closer to Z_0 than to - Z_0, so they'll give
reflection coefficients with magnitude less than 1. So will those of the
points on the ellipse in the other quadrant under consideration that are
between the real axis and the perpendicular bisector. But those that are
between the perpendicular bisector and the imaginary axis will be closer
to - Z_0 than to Z_0 and thus will yield reflection coefficients with
magnitudes greater than 1. It should be obvious that, along any given
ellipse, the one for which the magnitude of the reflection coefficient is
greatest is the one on the imaginary axis, since as we move along the
ellipse towards that point, the distance to - Z_0 decreases and the
distance from Z_0 increases (remember, their sum is constant along the
ellipse). So on any *one* ellipse, the largest reflection coefficient
magnitude occurs where the ellipse meets the imaginary axis, and thus Z_L
has real part 0 and imaginary part of opposite sign to that of Z_0.

(4) Start with Z_0 real, and slowly rotate Z_0 into either the first or
fourth quadrant, but not more than 45 degrees in either direction, keeping
the same magnitude while you rotate. The segments joining Z_0 and - Z_0,
their perpendicular bisectors, and the various ellipses will all
simultaneously rotate. It's now obvious that for ellipses of any fixed
size, the one producing the largest magnitude for the reflection
coefficient will occur when Z_0 is at + 45 degrees or - 45 degrees. So if
we want to maximize the reflection coefficient magnitude, we can restrict
attention to those two cases. The - 45 degree case (capacitive surge
impedance) is the more familiar one, but the math is the same either way.
The only question is, which one of the ellipses should we use, if we wish
to maximize the magnitude of the reflection coefficient?

(5) So now we're going to assume Z_0 = k(1 - j), and thus - Z_0 = k(-1 +
j), while Z_L = ktj. It's clear that the factor k is going to cancel out
when calculating the reflection coefficient, so I will henceforth ignore
it (i.e., normalize it to k = 1 by appropriate choice of units). If you
are of a geometrical turn of mind, you can produce a geometrical argument
showing that the best one can do is to make sure the ellipse meets the
imaginary axis at the same distance from the origin as the two foci, i.e.
at j*sqrt(2). If you are of an algebraic turn of mind, you can make an
algebraic argument involving completing the square to demonstrate the same
thing. If you insist on using calculus, it's now just one variable
calculus, not multivariable calculus, since the only independent variable
is t, which will turn out to be sqrt(2) at the maximum. (Hint: don't look
at the ratio of distances; look at the square of that ratio, so as to get
rid of all those square roots.)

(6) Once all that is done, it's just a bit of algebra to show that when t
= sqrt(2) then the magnitude of the reflection coefficient is 1 + sqrt(2).
That's the best (worst?) you can do. And if you can find some coax whose
surge impedance angle is - 45 degrees, you can indeed do it.

All the above was done from first principles. I am not fortunate enough to
own a copy of Chipman, though I wish I were, but if this is what he says,
then I am in full agreement with him.

David, ex-W8EZE, willing to part with some of my pension money for a copy
of Chipman if you know where one can be found (Powell's doesn't have any
copies)

--
David or Jo Anne Ryeburn

To send e-mail, remove the letter "z" from this address.




Peter O. Brackett August 30th 03 02:08 AM

Roy:

[snip]
I thought this was only true for waves moving through a lossless medium
or in a lossless transmission line that supports TEM waves. Either the
electric or magnetic field isn't transverse in a hollow waveguide, and
either or both can be non-transverse in a lossy medium.

Or am I mistaken about this?

Roy Lewallen, W7EL

[snip]

Compressive-dillutive waves occur only in media that is compressible, like
the earth or the air, or springs, etc... With compressive-dillutive waves
the "vibrations" occur in the effective density of the medium.

Electromagnetic waves propagate with transversal vibrations of the E and H
fields, viz. Side to side vibrations, not shortening and lenghtening
vibrations. If an electromagnetic wave is supported in the Transverse
Electromagnetic or TEM mode then [theoretically] the E and H fields are at
right angles to each other and to the direction of propagation, in the
terminology of TEM, the term transverse referes to the orientation of the
wave with respect to it's guides, and not to it's vibration mode in the
longitudinal - transverse sense.

Visualize a long "slinky" coil attached to the wall. Shake one end up and
down to create a transverse wave in which the slinky moves up and down.
Push and pull on the end to produce compression and dilution to cause
longitudinal waves in which the slinky does not move up and down but in
which the distance between turns moves back and forth. This slinky analogy
sort of illustrates the differences. Meanwhile in electromagnetic wave
phenomena you have as well as the most common TEM mode which is only
transverse vibrations, also there exists a plethora of TM and/or TE modes,
or even in the near field, where the fields may not be at right angles to
each other or to the direction of propagation, but the vibrations are still
talways transverse, i.e. not compressive-dilutive.

Back in the mid-1800's after Maxwell produced his celebrated equations and
Heaviside improved them by expressing them in vector form most scientists
of the time noted that Maxwell's formulation provided no explicit form for a
medium for the electromagnetic waves to propagate in, and they also noted
that there were only transverse and not longitudinal [compressive-dilutive]
vibrations supported by his equations. Several eminent scientists of the
day felt that this left openings for several more discoveries and so...
Then ensued for several decades a search for the "ether". The "ether" was
supposed to be the media which supported the electromagnetic waves. During
that period several of the eminent scientists of the time proposed that the
"ether" once it was found might actually be compressible and they proposed
that Maxwell and Heaviside had left out of their formulations the
possibility of compressive-dilutive or longitudinal vibrations. Several
scientists of the time actually formulated equations which supported
compressive-dilutive em waves and actually conconcted and, to no avail,
actually conducted experiments to try to find out if such
compressive-dilutive vibrations actually occured with electromagnetic
phenomena.

As we all know, eventually the existence of the "ether" was discredited,
mainly by the Michelson-Morley experiments, and today we all know that
electromagnetic waves do not have a media or "ether" to support their
propagation and vibrations.

Electromagnetic waves propagate just fine in a complete vacuum, and a vacuum
is incompressible, and so the search for compressive-dilutive vibrations of
electromagnetic waves became moot and a search for experimental evidence of
them was abandoned by all who were interested. One can add terms to the
Maxwell-Heaviside equations to support compressive waves, and this has been
done by several theoretical physicists, but there is no sense doing so since
none have ever been discovered!

The book, I referred to above, "Physics of Waves" gives all the details of
the wave equation for media that supports compressive waves. An important
such field is the field of seismology. Indeed the field of siesmology
studies waves that vibrate in all modes, transversally and longitudinally,
as well as surface waves. Seismic waves are processed regularly with beam
forming arrays of seismometers and processed by tomographic techniques to
image the earth in all wave modes.

Seismology is a facinating field and seismologists are generally the most
sophisticated of all wave mechaics!

A good modern book on the seismic wavefield is:

B. L. N. Kennett, "The Siesmic Wavefield", Cambridge University Press, New
York, NY, 2001. ISBN: 0-521-00663-5.

But be aware it is full of gratuitous partial differential equations and
tensor analysis. The stress-strain variables of compressible-dillutive
media are expressed as tensors and the partial differential equations are
cast in tensor form.

All this to say that electromagnetic wave phenomena are a particularly
simple form of wave phenomena when compared to the most complicated types.

--
Peter K1PO
Indialantic By-the-Sea, FL.



Roy Lewallen August 30th 03 03:52 AM

Thanks for the most interesting discussion of slinkys, "ether", and
seismology. But I'm a little vague on what you mean by "vibrations".
You're describing a field whose orientation isn't necessarily at a right
angle (transverse) to the direction of propagation (as in a TE or TM
mode wave), yet whose "vibrations" are nevertheless at a right angle to
the direction of propagation. So the "vibrations" are in a different
direction than the field. I'd like to learn more about this phenomenon,
but I can't find "vibrations" in the indexes of any of my
electromagnetics texts. Do they have another name?

Roy Lewallen, W7EL

Peter O. Brackett wrote:
. . .
Visualize a long "slinky" coil attached to the wall. Shake one end up and
down to create a transverse wave in which the slinky moves up and down.
Push and pull on the end to produce compression and dilution to cause
longitudinal waves in which the slinky does not move up and down but in
which the distance between turns moves back and forth. This slinky analogy
sort of illustrates the differences. Meanwhile in electromagnetic wave
phenomena you have as well as the most common TEM mode which is only
transverse vibrations, also there exists a plethora of TM and/or TE modes,
or even in the near field, where the fields may not be at right angles to
each other or to the direction of propagation, but the vibrations are still
talways transverse, i.e. not compressive-dilutive.
. . .



W5DXP August 30th 03 05:56 AM

Peter O. Brackett wrote:
Electromagnetic waves propagate with transversal vibrations of the E and H
fields, ...


Heh, heh, not wearing the particle physics hat today, Peter? :-)
--
73, Cecil http://www.qsl.net/w5dxp



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Tdonaly August 30th 03 06:14 AM



Thanks for the most interesting discussion of slinkys, "ether", and
seismology. But I'm a little vague on what you mean by "vibrations".
You're describing a field whose orientation isn't necessarily at a right
angle (transverse) to the direction of propagation (as in a TE or TM
mode wave), yet whose "vibrations" are nevertheless at a right angle to
the direction of propagation. So the "vibrations" are in a different
direction than the field. I'd like to learn more about this phenomenon,
but I can't find "vibrations" in the indexes of any of my
electromagnetics texts. Do they have another name?

Roy Lewallen, W7EL


Yes, "vibes." I think Peter is regressing back to the '60's.
73,
Tom Donaly, KA6RUH

Peter O. Brackett August 30th 03 01:57 PM

Roy:

[snip]
"Roy Lewallen" wrote in message
...
Thanks for the most interesting discussion of slinkys, "ether", and
seismology. But I'm a little vague on what you mean by "vibrations".
You're describing a field whose orientation isn't necessarily at a right
angle (transverse) to the direction of propagation (as in a TE or TM
mode wave), yet whose "vibrations" are nevertheless at a right angle to
the direction of propagation. So the "vibrations" are in a different
direction than the field. I'd like to learn more about this phenomenon,
but I can't find "vibrations" in the indexes of any of my
electromagnetics texts. Do they have another name?

Roy Lewallen, W7EL

[snip]

Vibrations = oscillations

An instance where compressional-dilative waves might occur in
electromagnetic propagation and where those compressional vibrations terms
could be added to the Maxwell-Heaviside equations might be that of
electromagnetic propagation through "light ion" plasmas [ionized gases]
where the ions could physically respond essentially instantaeously to the
passing waves and the distance between ions and hence the media properties
becomes a function of the electromagnetic fields. The effective mu and
epsilon of the media changing instantaneously in response to the propagating
fields, in turn changing the waves, etc... just as for compression acoustic
wave propagating in a compressible gas. This effect is probably
infinitesimal for "heavy ion" plasmas and might be perceptable for "light
ion" plasmas. I wonder if any readers of this NG have any experience with
propagation in plasmas and can share with us if they use
compression-dilutive terms to augment the Maxwell-Heaviside equations in the
analysis.

I presume that the NEC code that you use in EZNEC to integrate the
Maxwellian equations does not support plasma propagation analysis. Perhaps
someone knows of a version of NEC that does. I'd guess that folks at
Lawrence Livermore and at NASA are interested in such problems. I'd be
curious to know if they use augmented versions of Maxwell-Heaviside
equations.

Another, arcane, far fetched, and impractical example of
compressional-dillutive vibrations in em waves that I can think of could be
imagined as a system wherein em waves travel in a waveguide system where the
dimensions of the system [walls of the waveguide] are such that they can
move in and out instantaneously in response to the passing waves thus
alternately confining and expanding the dimensions of the guide relative to
the wavelength of the passing waves, it might be imagined that such action
could induce a wave shortening and lengthening effect on the passing waves
which is what compression-dillution waves are.

Thoughts, comments?

--
Peter K1PO
Indialantic By-the-Sea, FL.




Peter O. Brackett August 30th 03 01:59 PM

Tom:

[snip]

Yes, "vibes." I think Peter is regressing back to the '60's.
73,
Tom Donaly, KA6RUH

[snip]

Hmmm.... I remember Angela fondly, and how we used to dance to "I just wanna
hold your hand..."

Now just where did I put those old Beatles albums?

--
Peter K1PO
Indialantic By-the-Sea, FL



W5DXP August 30th 03 07:04 PM

Peter O. Brackett wrote:
Say did you order your copy of "Entanglement" yet?


I'm going to take a look at it first at the Texas A&M library
hopefully next week.

What is Cecil's wavelength and can I get on it?


Want me to grid dip myself?
--
73, Cecil http://www.qsl.net/w5dxp



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Roy Lewallen August 30th 03 11:08 PM

Thanks for the rundown on "light ion" plasmas, plasma propagation, and
moving-wall waveguides. I only have one remaining question.

Do the "vibrations" of electromagnetic waves you referred to in your
previous post have another name?

Roy Lewallen, W7EL

Peter O. Brackett wrote:
Roy:

[snip]
"Roy Lewallen" wrote in message
...

Thanks for the most interesting discussion of slinkys, "ether", and
seismology. But I'm a little vague on what you mean by "vibrations".
You're describing a field whose orientation isn't necessarily at a right
angle (transverse) to the direction of propagation (as in a TE or TM
mode wave), yet whose "vibrations" are nevertheless at a right angle to
the direction of propagation. So the "vibrations" are in a different
direction than the field. I'd like to learn more about this phenomenon,
but I can't find "vibrations" in the indexes of any of my
electromagnetics texts. Do they have another name?

Roy Lewallen, W7EL


[snip]

Vibrations = oscillations

An instance where compressional-dilative waves might occur in
electromagnetic propagation and where those compressional vibrations terms
could be added to the Maxwell-Heaviside equations might be that of
electromagnetic propagation through "light ion" plasmas [ionized gases]
where the ions could physically respond essentially instantaeously to the
passing waves and the distance between ions and hence the media properties
becomes a function of the electromagnetic fields. The effective mu and
epsilon of the media changing instantaneously in response to the propagating
fields, in turn changing the waves, etc... just as for compression acoustic
wave propagating in a compressible gas. This effect is probably
infinitesimal for "heavy ion" plasmas and might be perceptable for "light
ion" plasmas. I wonder if any readers of this NG have any experience with
propagation in plasmas and can share with us if they use
compression-dilutive terms to augment the Maxwell-Heaviside equations in the
analysis.

I presume that the NEC code that you use in EZNEC to integrate the
Maxwellian equations does not support plasma propagation analysis. Perhaps
someone knows of a version of NEC that does. I'd guess that folks at
Lawrence Livermore and at NASA are interested in such problems. I'd be
curious to know if they use augmented versions of Maxwell-Heaviside
equations.

Another, arcane, far fetched, and impractical example of
compressional-dillutive vibrations in em waves that I can think of could be
imagined as a system wherein em waves travel in a waveguide system where the
dimensions of the system [walls of the waveguide] are such that they can
move in and out instantaneously in response to the passing waves thus
alternately confining and expanding the dimensions of the guide relative to
the wavelength of the passing waves, it might be imagined that such action
could induce a wave shortening and lengthening effect on the passing waves
which is what compression-dillution waves are.

Thoughts, comments?

--
Peter K1PO
Indialantic By-the-Sea, FL.





Peter O. Brackett September 1st 03 04:31 AM

Roy:

[snip]
Do the "vibrations" of electromagnetic waves you referred to in your
previous post have another name?

Roy Lewallen, W7EL

[snip]

Oscillations perhpaps?

I don't really understand your question... do you object to the term
"vibrations"? What would you prefer, oscillations, or...

It is well known by Physicists that lectromagnetic waves [at least in free
space and isotropic media] are generally consist of only transverse
vibrations,. this type of vibration is inherent in the formulation and
solutions to the Maxwell-Heaviside equations.

For examples of longitudinal or compressive vibratons for instance in a
taught wire like a guitar string, transverse vibrations or oscillations are
side to side, but longitudinal or compressional vibrations would be the very
tiny vibrations in the length of the guitar string. In systems where
longitudinal vibrations are supported, generally the velocity of propagation
of longitudinal vibrations will not be the same as that of transverse
vibrations.

For a detailed explantation of compressional-dilutive or longitudinal waves
in a variety of physical systems, cfr:

William C. Elmore, and Mark A. Heald, "Physics of Waves", McGraw-Hill, New
York, 1969.

--
Peter K1PO
Indialantic By-the-Sea, FL.




Roy Lewallen September 1st 03 09:33 AM

No, I'm just trying to figure out how an EM wave can have E and/or H
fields whose directions aren't transverse to the direction of
propagation (as in a lossy medium or in a hollow waveguide) can have
another property of "vibrations" or "oscillations" that *are* always
transverse. The properties of E and H fields that I'm familiar with
include orientation of the field in space, and change in amplitude with
time (which is what I'd normally call oscillations). And, of course, the
orientation can change in time also, as in elliptically or circularly
polarized waves. The property of "vibrations" or "oscillations" that
have a direction different from the direction of the field is new to me.

I notice that you're now qualifying your statement to free space and
isotropic media. Does this perhaps leave open the possibility that waves
in a lossy medium, or bounded within a hollow waveguide, could have
"vibrations" that *aren't* transverse to the direction of propagation?
My original question was in response to your statement that EM waves
were always transverse, regardless of the medium.

Do you perhaps have Krus' _Electromagnetics_, or electromagnetics texts
by Holt, Johnk, Skilling, Magid, Magnusson, or Jordan & Balmain? If so,
perhaps you could direct me to a section which addresses this.

Roy Lewallen, W7EL

Peter O. Brackett wrote:
Roy:

[snip]

Do the "vibrations" of electromagnetic waves you referred to in your
previous post have another name?

Roy Lewallen, W7EL


[snip]

Oscillations perhpaps?

I don't really understand your question... do you object to the term
"vibrations"? What would you prefer, oscillations, or...

It is well known by Physicists that lectromagnetic waves [at least in free
space and isotropic media] are generally consist of only transverse
vibrations,. this type of vibration is inherent in the formulation and
solutions to the Maxwell-Heaviside equations.

For examples of longitudinal or compressive vibratons for instance in a
taught wire like a guitar string, transverse vibrations or oscillations are
side to side, but longitudinal or compressional vibrations would be the very
tiny vibrations in the length of the guitar string. In systems where
longitudinal vibrations are supported, generally the velocity of propagation
of longitudinal vibrations will not be the same as that of transverse
vibrations.

For a detailed explantation of compressional-dilutive or longitudinal waves
in a variety of physical systems, cfr:

William C. Elmore, and Mark A. Heald, "Physics of Waves", McGraw-Hill, New
York, 1969.

--
Peter K1PO
Indialantic By-the-Sea, FL.





Peter O. Brackett September 2nd 03 03:06 AM

Roy:

[snip]
"Roy Lewallen" wrote in message
...
The property of "vibrations" or "oscillations" that
have a direction different from the direction of the field is new to me.

[snip]

That's fine, there are lots of things new to me as well. :-)

These are called longitudinal or compressive-dilutive waves. Such
vibrations do not [usually] occur
with electromagnetic fields, and in the early days of em theory scientists
did wonder if such were
possible, as I have noted in prior postings. However there are numerous
physical systems described
by wave equations which do support both transverse and longitudinal
vibrations of the constituient fields.
I gave several examples in prior postings and you will find lots of such
examples in "Physics of Waves".

[snip]
I notice that you're now qualifying your statement to free space and
isotropic media. Does this perhaps leave open the possibility that waves
in a lossy medium, or bounded within a hollow waveguide, could have
"vibrations" that *aren't* transverse to the direction of propagation?

[snip]

The point is not that the waves have "vibrations" that are transverse to the
direction
of propagation. Of course, guided em waves have vibrations which are not
perfectly
perpendicular to the direction of propagation. The TEM mode would not exist
and
TEM waves would not propagate if there were not some potential driving the
waves
forward, meaning that both the E and H fields have some tiny component in
the direction
of propagation. All of this to establish that I do understand em wave
propagation, and to
say that... this has nothing whatsoever to do with longitudinal or
compressive-dilutive
vibrations. The fact that E and H fields "lean" slightly in the direction
of propagation
in a wave guide is not a compressive-dillutive effect on the fields. For
longitudinal
field vibrations to occur the wavelength of the propagating fields has to
change as
it propagates. This does not occur in "normal" em propagation. I
conjecture that
there may however be some exceptions to this, e.g. plasmas, etc... I just am
not
aware of them. Perhaps some other newsgroup reader/poster is more familiar
with any possible longitudinal vibrations of em waves.

[snip]
My original question was in response to your statement that EM waves
were always transverse, regardless of the medium.

[snip]

Roy, I believe that you may be reading too much into the word "transverse",
it
can be used in several contexts. Tansverse vibrations are not compressive
vibrations. With compressive vibrations, the wavelength of the waves
actually
changess it propagates. While in transverse vibrations no such wavelength
changes occur. In this usage the word "transverse" does not refer to
directionality
with respect to direction of propagation, but rather to the fact that the
waves
maintain their wavelegth during propagation. As a "real" example, some
seismic
waves [the so called "S-Waves" in the earth actually change their wavelength
as
they propagate..

[snip]
Do you perhaps have Krus' _Electromagnetics_, or electromagnetics texts
by Holt, Johnk, Skilling, Magid, Magnusson, or Jordan & Balmain? If so,
perhaps you could direct me to a section which addresses this.

[snip]

Roy, yes indeed I have two editions of "Kraus" and I took a course from
Keith Balmain
using his first edition text when I was at U of T.

And...

I can tell you here and now that neither of those two august gentlemen
address the issue
of longitudinal vibrations anywhere in their texbooks! Simply because, as I
have stated in
other postings, Maxwell-Heaviside equations do not support longitudinal
vibrations, and so
why would a text on em waves even discuss such vibrations? The fact that
Kraus and Balmain
do not discuss such things does not surprise me, nor should it you, since
electromagnetic wave
propagation and the Maxwell-Heaviside equations are a particularly simple
example of wave
motion.

Roy if you wish to deeply understand wave equations and wave motions and to
understand
the wider ramifications of wave motion, you just gotta read more widely in
the "Waves"
literature.

Kraus and Balmain are very narrow in scope, being confined strictly to em
waves!

If they had attempted to include any "early" history of em research from
around the middle
of the 1800's then they would have outlined some of the early speculations
by contemporaries
of Maxwell, such as Kelvin, Heaviside and others as to the possibility that
Maxwell might have
left longitudinal terms that might have proved significant, of course they
were found never to be
needed. However even back in those times most Natural Philosophers [They
were'nt called
Physicists in those days] and Electricians like Heaviside were more widely
schooled than
today's Engineers and they knew and studied wave equations in their full
glory... longitudinal
vibrations included. These days however our electrical engineering
education is far too narrrow
and does not expose folks to the wider view of the world. Thus we often
find em wave
mechanics who don't understand longitudinal waves. Until I became involved
in underwater acoustics and seismic propagation problems and saw the wave
equations in
their full glory, I too had a narrow view of wave mechanics.

I don't know if Kraus or Balmain ever encountered the "full" wave equations,
but in any
case their texts are directed at em specialists and so their narrow view is
not surprising.

As I posted before, if you are interested in such things, check out:

Elmore and Heald, "Physics of Waves" and say, Kennett's, "The Seismic
Wavefield" among
others to help you to broaden your horizons on these issues of longitudinal
waves.

--
Peter K1PO
Indialantic By-the-Sea, FL.



pez December 13th 03 10:48 AM

Dear Professor David or Jo Anne Ryeburn,

Finally,
I accomplished the study
of this most interesting article...

But, with your permission,
I can not resist to notice that
the key-point of the surprising,
at least to me, introduction
of an ellipse at step (3),
it looks somehow artificial
and in some way opposite
to the intentions of the introduction:

| ...
| don't believe in using calculus
| whenever simple geometry and/or algebra
| makes it unnecessary.
| A proof that avoids calculus can be meaningful for
| those who don't know calculus,
| or who haven't used it for a while
| ...

In all other respects
and as far as I could say something more,
then it is, at least for me,
a perfect argument, indeed!

Sincerely yours,

pez
SV7BAX
TheDAG




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