0.220977648
0.258184299
0.235861829
0.254216997
0.246889605
As I recall, Hector posted some chord factors, but probably only to 4
decimal places. I probably then used these to establish the spherical
coordinates and chord factors to greater accuracy using iteration. I
found some old records of the Domelist discussion group that used to
be run by a company called Hoflin.That group eventually reestablished
itself as the Yahooo Domelist, moderated by Sal Cerda. Most of the
exchanges between me, Hector and two others took place in late
September and early October 2006. At that time, one of the other
people, from Texas, also remarked that Hector had come up with a new
breakdown method that gives results slightly different from method 2,
and with fewer chord factors. (I wish now I had remembered that
exchange.) i will send you some notes and messages exchanges in a few
days.
Gerry in Quebec
P.S. Did you take a look at solution 10b for the 6v icosa, in the
files section?
On Feb 10, 4:53 pm, TaffGoch <taffg...@gmail.com> wrote:
> The discussion thread, where the "Mexican" subdivision was introduced (by
> Gerry,) really deserves it's own thread.
> (You can catch-up:http://groups.google.com/group/geodesichelp/browse_thread/thread/a7ee...
> )
>
> Gerry attributed the "Mexican" subdivision method to professor Hector
> Hernandez, at the University of Sonora. This is what I could find, on
> Google, for Dr. Hernandez:
>
> Héctor Alfredo Hernandez Hernandez
> email: hector(at)gauss.mat.uson.mx
>
> Universidad de Sonora
> Departamento de Matemáticashttp://www.mat.uson.mx/personalacademicos.htmhttp://www.mat.uson.mx/hector/indexA.html
> Mexican6.png
> 155KViewDownload
>
> Mexican5.png
> 59KViewDownload
Here they are to 9 decimal places...
Did you take a look at solution 10b for the 6v icosa, in the files section?
On Feb 10, 10:45 pm, TaffGoch <taffg...@gmail.com> wrote:
> This one was, comparatively, much easier, and quicker:
>
> The "Mexican" subdivision method, class-I, frequency-4v, icosa chord factors
>
> Mexican4.png
> 47KViewDownload
On Wed, 10 Feb 2010, TaffGoch wrote:
> While the concept is simple, I'm not so sure that can be said of the
> underlying mathematics. Perhaps, someone else, more proficient at spherical
> geometry, can more easily transition from the physical model to the
> descriptive math.
Here is a long-winded way to find the chord factor
http://www.antiprism.com/misc/geo_i_4_edges_calc.jpg
The object is to find l.
You can solve a triangle using spherical trigonometry if you
know any three values from its sides or edges.
Triangle ABC has angles pi/2, pi/3 and pi/5. You can use
this to find a (opposite A) and d. Knowing d and C you can
find j in terms of l. In the small triangle by B (sixth of
the brown equilateral triangle) you know two of the angles
and can find k in terms of l.
Finally, you have a = j + k. This looks like a quartic
in, say, cos(l), which can be solved with the quartic
formula and can be used to give an expression for the
chord factor. I guess it would take half a side of A4
or more to write this expression down.
However, it may be that there is an angle substitution
to simplify the quartic and produce a more reasonable
final expression.
Adrian.
--
Adrian Rossiter
adr...@antiprism.com
http://antiprism.com/adrian
... any three values from its sides and angles.
I'd love to know the math behind this Mexican layout, but I fear it's
beyond my 1960s high school trig.
Cheers,
Gerry
On Feb 12, 6:20 pm, TaffGoch <taffg...@gmail.com> wrote:
> "Mexican" subdivision method, class-I, frequency-8v, icosa chord factors:
>
> Mexican8.png
> 144KViewDownload
On Fri, 12 Feb 2010, TaffGoch wrote:
> In the past 30+ years, I've used reams of paper to resolve multivariate
> calcs, but I can't seem to justify the time to do so, nowadays. (And
> here, I thought that, when I retired, I'd have MORE time for this sort of
> thing!) I'm not unfamiliar with the spherical-geometry concepts or formulae.
> It's simply faster for me to "build" it by manipulation, in the modeling
> environment.
I was solving the Johnson polyhedra last year, and did some of
them like this. I found coordinates for them iteratively first,
and then switched to exact expressions as I worked them out.
I still have three left
http://en.wikipedia.org/wiki/Sphenomegacorona
http://en.wikipedia.org/wiki/Hebesphenomegacorona
http://en.wikipedia.org/wiki/Disphenocingulum
The calculations for these look like they are going to be
really long. I've left them for now in the hope of coming
up with a different approach!
As regards a general method for solving the Hernandez method
geodesic spheres, if the long-winded method didn't simplify
then it is probably impractical. But, if there is a method,
like an angle substitution, that simplifies the equations
in the lower frequency sphere then maybe the simplification
also generalises. It would probably be hard to get an idea
Without actually working through the equations and
experimenting a bit.
For other approaches, I wondered whether a path of equal
length edges would have its vertices lying on a curve
that depended only on how far along the base triangle
edge the path was attached to. For example, could the
red path in your mexican4 be the same as the yellow
path in mexican8? The sum of the central angles across
both these paths is very close. Comparing twice the
yellow edge angle to the red edge angle
2*2*asin(0.149584/2) = 0.299448
2*asin(0.298311/2) = 0.299428
So the path length change is minimal, and the difference
may be completely explained by the fact that the red
edge cuts across the slight angle that will be between
two adjacent yellow edges.
For comparison, these figures are for the first edge on
the spherical division I use (average of where the three
coordinating great circles meet)
0.2981066 (F8, 2*first edge on second path from vertex)
0.2989018 (F4, first edge on first path from vertex)
The numbers are close, but differ by considerably more than
the numbers in the Hernandez method. What is more significant
though is that this time the sum of the two smaller angles
in the F8 is *less* than the larger angle of the F4.
Another thought I had is that using the method to
divide up an extreme triangle whose three edges were
a great circle may suggest something about the shapes
of the paths by exaggerating them.
For other approaches, I wondered whether a path of equal
length edges would have its vertices lying on a curve
that depended only on how far along the base triangle
edge the path was attached to. For example, could the
red path in your mexican4 be the same as the yellow
path in mexican8?
> AniMexican8.gif
> 137KViewDownload
On Mon, 15 Feb 2010, TaffGoch wrote:
> I had to be making mistakes, or there was an unrevealed error or
> misunderstanding in the general principle. By repeated, meticulous modeling
> of the 6v subdivision, solving for vertices in different orders, I
> discovered the problem -- the general concept DOESN'T WORK !
...
> I've identified the discrepency to my satisfaction, and would like to be
> able to better explain it in words. Basically, the ORDER in which you solve
> for vertex positions, and the resultant chords, DOES make a difference.
I've just had a quick look at doing this iteratively, and have
found the same problem.
On each iteration I run through the edges trying to make each
edge closer to the average length for its colour, and in no
particular order (not by colour order) although always in the
same order.
Here are some results. 0 is an icosahedron edge path, 1 is the path
of edges next to that, ..., 5 are the single edges next to
an icosahedron vertex. The values are the shortest edge on
a path, the average edge, the longest edge, and the difference
between the longest and shortest edge
0: min=0.184263107796267, avg=0.184263107796267, max=0.184263107796267, diff=0.000000000000000
1: min=0.194845862377352, avg=0.194845866183443, max=0.194845867645556, diff=0.000000005268204
2: min=0.203190330893239, avg=0.203191083873434, max=0.203191836870035, diff=0.000001505976796
3: min=0.209348363305264, avg=0.209349831372071, max=0.209350565442586, diff=0.000002202137322
4: min=0.213451180983742, avg=0.213451180983881, max=0.213451180983982, diff=0.000000000000240
5: min=0.215692980245839, avg=0.215692980245839, max=0.215692980245839, diff=0.000000000000000
You can see that the greatest discrepency between two edges in
a path is around 0.0000022
This solution is only locally optimal. If I continue to run my
program, making only the tiniest adjustments, the discrepency
increases. It may be that if I ran the program for longer, or
differently, that it would converge on a solution.
I can easly see how my approach can fail. The paths have
minimal kinks in them. If the algorithm puts the kink on the
wrong side then it is possible that may never be corrected.
I should try to run my program for a long time using very
small changes.
Here are the chord factors:
0.275904484255
0.321244071280
0.313239424221
0.298310757694
Gerry
> Mexican5_precision9.png
> 63KViewDownload
By referring to vertices by their colour combinations, can you
identify which vertices you're talking about for the 0.999961680
radius and the 1.000004591 radius? I realize that this doesn't matter
for construction purposes, but it would be good to keep the Excel
model "true".
Thanks,
Gerry
P.S. Most of the Excel models I've done in recent years allow for
non-1 radii -- so they can handle some ellipsoids, the duals of the
archimedean solids, and other special cases.
> Mexican7_precision9.png
> 68KViewDownload
Example dome, of 10 meter radius (a fairly large conduit dome)
3 radial measurements will be off by -0.38200 mm
6 radial measurements will be off by +0.04591 mm
These disparities easily "pale in comparison" with construction-errror
tolerances. In other words, slight compounded errors in drilling
vertex holes, or metal strut thermal expansion/contraction, are likely
to be greater than the derived radial disparities observed in the
"pure" mathematical model.
As a physicist and mathematician, I appreciate the elegant "purity" of
6-decimal precision. For real-world application, however, I'd have to
acknowledge that a half-a-millimeter radial variance in a 65-foot
diameter dome would be impossible to detect or measure.
Seven unique strut lengths, for a 7v dome, has, itself, a certain
elegance -- worth appreciating, in it's own right.
Taff
In any case, your 7v numbers work perfectly. A tiny change in some
radii yields the same path-specific equality of chord lengths that you
get in the lower frequencies. I'm curious to know what might happen at
higher frequencies.
This Mexican (Hernandez) layout has something in common with the Class
II, Method 3 described in Domebook 2 and Kenner's Geodesic Math. In
each case, the number of unique edge lengths equals the frequency
(even frequencies in class II).
Again, thanks for posting your work on this.
Cheers,
Gerry
> Mexican7_radii.png
> 92KViewDownload
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The Desert Domes strut lengths for the 4 frequency and 6 frequency
icosa yield domes that sit flat as hemispheres (i.e., at the
"equator"), but not at any other useful truncation. The 6 frequency
Mexican layout, while having only 6 strut lengths rather than 9, does
not sit flat at any useful truncation. So you would have to introduce
more strut types (unique lengths) in the bottom row of triangles to
make the dome sit flat -- if of course having a flat base is of
importance for the particular job you have in mind.
Is it a hub-&-strut dome, a pipe dome or a wooden panel dome?
Good luck,
Gerry in Quebec
On Feb 20, 1:58 pm, TaffGoch <taffg...@gmail.com> wrote:
> 6v primary icosa triangle:
>
> Mexican6v.png
> 71KViewDownload
I’ve uploaded a jpg image to the files section, showing the two sets
of radii and chord factors side by side: 6v-icosa-Mexican-2-
solutions.jpg.
Taff, using the SketchUp models from your catalog of class 1
subdivisions, in the 3D warehouse, is there any way to measure radii
at a given vertex? I couldn’t figure out how to do this in SketchUp.
The measuring tape won’t let me measure from north pole to south pole
through the model.
Gerry in Quebec
> http://sketchup.google.com/3dwarehouse/details?mid=9f5cb5daa0e99215d7...
>
> Taff
>
> Geodesic_Class_I_Library.png
> 391KViewDownload
In my earlier post, I mentioned that some of the radii in the two
different versions of the 6v Mexican layout were "a little bit more
than zero" and some "a little less than zero". I should have said
"one", of course, not zero. Looks like I've contracted some sort of
binary disorder -- and I'm not even a computer geek!
Are you familiar with the Small Stella and Great Stella programs, by
Rob Webb in Australia? I have been using Small Stella for several
years and find it has been a great learning tool for polyhedral
geometry. Some of its graphics display features are similar to
SketchUp's.
Gerry in Quebec
On Mar 6, 4:36 pm, TaffGoch <taffg...@gmail.com> wrote:
> My apologies, Gerry, I forgot to update that model with center guidepoints.
> I've corrected the oversight, and uploaded the modified model file to the 3D
> Warehouse:http://sketchup.google.com/3dwarehouse/details?mid=9f5cb5daa0e99215d7...
>
> If you download it again, you'll be able to measure from the centers. Turn
> on the "X-Ray" mode, and both the "Line" and "Tape Measure" tool cursors can
> snap to the center, through the exterior faces (rather than to the
> semi-transparent faces.)
>
> If you start a new line at the center guidepoint, you can read the lengths
> to each vertex, one-after-another, as long as you DON'T click on the vertex
> (thereby, completing the line.) Just let the cursor "snap" to the vertex,
> and read the value in the VCB (value control box.) The tape-measure will do
> the same thing, so you can use either one. I regularly use the line tool,
> because I remember the keyboard shortcut, "L" (but forget the "T" shortcut
> for the tape measure.)
>
> Taff
>
> Geodesic_Class_I_LibraryB.png
> 131KViewDownload
The discussion thread, where the "Mexican" subdivision was introduced (by Gerry,) really deserves it's own thread.(You can catch-up: http://groups.google.com/group/geodesichelp/browse_thread/thread/a7eec9697e55d700?hl=en )Gerry attributed the "Mexican" subdivision method to professor Hector Hernandez, at the University of Sonora. This is what I could find, on Google, for Dr. Hernandez:Héctor Alfredo Hernandez Hernandez
email: hector(at)gauss.mat.uson.mxUniversidad de Sonora
Departamento de Matemáticas__________________________________________Conceptually, this method appears pretty basic, so I would not be at all surprised to learn that Dr. Hernandez is not the originator. I have a strong inkling that the method must have been conceived, developed and evaluated by geodesic developers, sometime in the past 5-6 decades.While the concept is simple, I'm not so sure that can be said of the underlying mathematics. Perhaps, someone else, more proficient at spherical geometry, can more easily transition from the physical model to the descriptive math.I'll be cleaning up my SketchUp models that I've been using for development and experimenting, so that I can post those, as well. With a 3D computer model to examine, the underlying concept is obvious (but a bit deceptive.) Arc centers are not coincident with either the sphere's center, or with any of the other arcs. Also, the arcs are not quite planar (but are very, VERY close.) Even so, I've been able to manipulate the arc segments (chords,) with SketchUp's tools, to arrive at 5-6 decimal accuracy -- surely precise enough for "real world" construction, at pretty large scales.I've attached two diagrams. (I'm working on other frequencies, and will append to this thread.) We've discussed the 6v division previously, and I've replicated that chord-factor diagram below. Today, I developed the 5v chord-factor model & diagram (also attached.)__________________________________________Gerry, I recall that you mentioned developing the 5v chords, yourself. Do the chord factors in the attached 5v diagram positively correlate with your results?Taff
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