From: William Mook on
On Feb 15, 9:48 pm, OM <o...(a)sci.space.history> wrote:
> On Mon, 15 Feb 2010 16:52:55 -0800 (PST), "Scott M. Kozel"
>
> <koze...(a)comcast.net> wrote:
> >I can see that you have put a lot of thought into this
>
> ...Most of it the result of years of substance abuse, especially
> sniffing paint fumes from a paper bag while high on really poorly made
> acid.
>
>                                OM
>
> --
>
>   ]=====================================[
>   ]   OMBlog -http://www.io.com/~o_m/omworld  [
>   ]        Let's face it: Sometimes you *need*         [
>   ]          an obnoxious opinion in your day!           [
>   ]=====================================[

That's libel OM. Naughty naughty.
From: Alain Fournier on
Pat Flannery wrote:

> Temperature at 4.1 million miles is 2,160F according to the above
> article, so assuming halving the distance increases the temperature four
> times over (I think that's how it works, though the large solar radius
> may screw this up; it's going to at least double) that makes the temp it
> could be facing over 8,000 F.

Yes the large solar radius does screw this up. The correct way to compute
this is to measure the solid angle that the sun covers at a given distance.
For something far away, when you double the distance the solid angle
is divided by four. But when you are close to the sun the the squaring
law no longer applies. Very close to the surface of the sun, the temperature
will basically be constant, because whether you are 100 km from the surface
or 200 km makes little difference, the sun basically fills half the sky
in both cases.


Alain Fournier
From: William Mook on
On Feb 16, 2:49 pm, David Spain <nos...(a)127.0.0.1> wrote:
> William Mook <mokmedi...(a)gmail.com> writes:
> > I believe my experience exceeds yours at this point.  I understand
> > that you are clueless.  That does not mean I am.
>
> You seem to understand little, I await your SPS on orbit.
>
> Dave

Alright.
From: William Mook on
On Feb 16, 9:01 pm, Alain Fournier <alain...(a)sympatico.ca> wrote:
> Pat Flannery wrote:
> > Temperature at 4.1 million miles is 2,160F according to the above
> > article, so assuming halving the distance increases the temperature four
> > times over (I think that's how it works, though the large solar radius
> > may screw this up; it's going to at least double) that makes the temp it
> > could be facing over 8,000 F.
>
> Yes the large solar radius does screw this up. The correct way to compute
> this is to measure the solid angle that the sun covers at a given distance.
> For something far away, when you double the distance the solid angle
> is divided by four. But when you are close to the sun the the squaring
> law no longer applies. Very close to the surface of the sun, the temperature
> will basically be constant, because whether you are 100 km from the surface
> or 200 km makes little difference, the sun basically fills half the sky
> in both cases.
>
> Alain Fournier

This is correct when adjusting for energy. Inverse law doesn't
strictly apply because the sun subtends some area. Another way of
saying this is that the inverse square curve doesn't go to infinity at
zero radius. It goes to the temperature of the solar surface at the
solar surface. This makes the energy rise less than the inverse
square would suggest - and the correction SUBTRACTS from that curve.
(infinity is bigger than any large finite number)

At 3.5 million km its something like 27 degrees of the sky. The
entire sky covers 4 pi steradians. Think about a ball that has a unit
radius. It has an area of 4 pi square units. Now a circle with a
radius of 13.5 degrees on the surface of this sphere 13.5 / 57.3 =
0.24 units radius - having an area of 0.18 square units (pi*0.24^2)
which is 1.43% of the entire sky.

So, there is a slight adjustment at 3.5 million km from the sun, but
not much - due to the fact that the light is coming from a sensible
surface not a point at zero radius. This diffuses the light.

The big issue is though, that even at 3.5 million km the inverse
square law, which over-estimates energy levels, provides only a slight
over-estimate.

In the end, this nuance should not be confused with the fact that in a
vacuum energy is exchanged by radiant transfer. So, radiant energy
in, versus radiant energy out.

Imagine a gray shell of titantium 1,128.4 mm in diameter that absorbs
perfectly 50% of energy incident on it, and reflects away 50% of the
energy incident on it sitting at a point that has an energy flux of 2
million watts per square meter.

This ball has a projected area of 1 square meter and a total surface
area of 4 square meters.

It reflects away 1 million watts of energy and absorbs 1 million watts
of energy which raises its temperature to the point where it glows at
an intensity where that 1 million that gets absorbed is radiated away
as well.

Since the entire surface is glowing, and 1 million watts is coming in
then 1 million watts must be going out to balance it. Since the
entire area is 4 square meters, the flux per unit area is 250,000
watts/m2

What must this temperature be?

Well, Stephan Boltzmann tells us

j* = 5.67e-8 * T^4

Re-arranging

T = (j*/5.67e-8)^(0.25) = 1,449.1 Kelvin

Which is well below the melting point of Titanium.

If the Titanium shell is 10 mm thick, we can see that the shell has a
volume of 40 liters and a mass of 181.6 kg. And with a heat capacity
of 597.5 J/kg-K we can see that it will take no less than 2.4 minutes
to reach that temperature at this distance. (imagining that it is
removed from behind a highly reflective screen) depending on rate of
rotation.

This is how its done. You need to know the rate of energy coming into
each unit of projected area. You need to know the reflectivity of
those surfaces. You then have to calculate the temperature using
Stephan Boltzman to see what the temperature must be to balance the
heat load. You then look at the temperature, the materials, and their
physical properties to get an idea of what will happen in that
location.

Numerical modelling is best, especially with ray tracing to get
accurate heat flows. For example, consider a panel with hairlike
fibers on the back side, that are fairly efficient heat pipes. It
turns out that with fairly efficient geometries, you can have pretty
cool systems even with high heat flows. Add in the ability to reflect
wavelengths and to operate refrigeration cycles to radiant emitters
(with hair) and you can see that challenging as this engineering is,
its perfectly amenable to careful analysis and creative thought.

To achieve remarkable results.

A started this conversation detailing how two 10 ton satellites, one
in GEO and one 3.5 million km from the sun, can displace ALL the
nuclear power plants in the USA for less than the cost of TWO nuclear
power plants. Once the system is up and running, and proven, 20
satellite pairs can displace ALL power plants in the USA for the cost
of four more nuclear power plants. 140 satellite pairs can displace
ALL PRIMARY ENERGY USE IN THE WORLD TODAY! for the cost of four more
power plants (the power of mass production)

So, for the same cost as 10 new nuclear plants, the USA using its
existing space faring infrastructure could supply 100% of the world's
energy from space, and continue to support agressive industrial
expansion thereafter - earning $2 trillion per year - and growing in
30 years to $30 trillion while the world economy grows from $70
trillion today to $1 quadrillion.

Of course, if 20% of the revenue goes into expanding our space faring
infrastructure, this would be $400 bililion per year - we could do
other amazing things - if we combine the skill and creativity to think
of them.

From: William Mook on
On Feb 17, 1:28 am, Pat Flannery <flan...(a)daktel.com> wrote:
> Alain Fournier wrote:
> > Yes the large solar radius does screw this up. The correct way to compute
> > this is to measure the solid angle that the sun covers at a given distance.
> > For something far away, when you double the distance the solid angle
> > is divided by four. But when you are close to the sun the the squaring
> > law no longer applies. Very close to the surface of the sun, the
> > temperature
> > will basically be constant, because whether you are 100 km from the surface
> > or 200 km makes little difference, the sun basically fills half the sky
> > in both cases.
>
> What makes it tricky to figure out is that this isn't just a case of the
> object in orbit being bombarded by the sunlight and heating up that way,
> but it actually being in the tenuous outer atmosphere of the Sun.
> At its hottest points the corona can get up to between 8 and 20 million
> degrees Kelvin.
>
> Pat

Well, this isn't tricky at all. What you are saying is that you are
NOT in a perfect vacuum. You have some sort of conduction going on
from a hot body to a cooler one. Its still the same heat balance
equation. So, you add to the radiant transfer the conductive
transfer.

Now, you're still in pretty much a vacuum. That's important to
remember. You're not in a water bath at 8 million degrees. You're in
a vacuum where the particles that strike your vehicle are at 8 million
degrees. How many? That's the key question. Because we'll assume
for arguments sake that anything at 8 million degrees will pretty much
give up all its energy to whatever it hits. This isn't precisely
accurate, but accurate enough for engineering work.

Alright, so, how mch?

The parts of the Sun above the photosphere are referred to
collectively as the solar atmosphere. They can be viewed with
telescopes. There are five principal zones:

1) the temperature minimum,
2) the chromosphere,
3) the transition region,
4) the corona, and
5) the heliosphere.

The heliosphere, which may be considered the tenuous outer atmosphere
of the Sun, extends outward past the orbit of Pluto to the heliopause,
where it forms a sharp shock front boundary with the interstellar
medium.

The chromosphere, transition region, and corona are much hotter than
the surface of the Sun. The reason has not been conclusively proven;
evidence suggests that Alfvén waves may have enough energy to heat the
corona.

The coolest layer of the Sun is a temperature minimum region about 500
km above the photosphere, with a temperature of 4,100 K. This part of
the Sun is cool enough to support simple molecules such as carbon
monoxide and water, which can be detected by their absorption spectra.

Above the temperature minimum layer is a layer about 2,000 km thick,
is the chromosphere. The temperature in the chromosphere increases
gradually with altitude, ranging up to around 20,000 K near the top.

Above the chromosphere there is a thin (about 200 km) transition
region in which the temperature rises rapidly from around 20,000 K in
the upper chromosphere to coronal temperatures closer to one million
kelvins. The temperature increase is facilitated by the full
ionization of helium in the transition region, which significantly
reduces radiative cooling of the plasma.

So, you can see how important radiative transport of energy is.

The transition region does not occur at a well-defined altitude.
Rather, it forms a kind of cloud layer around chromospheric features
such as spicules and filaments, and is in constant, chaotic motion -
like weather on Earth - only a lot hotter!

The transition region is not easily visible from Earth's surface, but
is readily observable from space by instruments sensitive to the
extreme ultraviolet portion of the spectrum.

The corona is the extended outer atmosphere of the Sun, which is much
larger in volume than the Sun itself. The corona continuously expands
into the space forming the solar wind, which fills all the Solar
System.

So, saying that the satellite is in the corona at 3.5 million km
doesn't really bother me - and it shouldn't bother you. All you must
do is figure out what the heat balance is to get an accurate read on
temperature.

The low corona, which is very near the surface of the Sun, has a
particle density around 1e+11 particles per cubic meter at 700,000 km
from the center - the Earth's atmosphere has 2e+25 by comparison.
Density falls off as the inverse square of distance once the solar
wind is established, but that doesn't occur until we reach the base of
the heliosphere at 15 million km.. So, at 3.5 million km the effect
is dominated by an exponential function called density lapse rate. At
the high end density would be around 4e+9 particles per cubic meter.
At the low end, density would be about 1e+7 particles per cubic
meter.

The average temperature of the corona and solar wind is about 1
million–2 million kelvins, however, in the hottest regions it is 8
million–20 million kelvins as stated. We are dealing with the
average.

The heliosphere, which is the cavity around the Sun filled with the
solar wind plasma, extends from approximately 20 solar radii (0.1 AU)
to the outer fringes of the Solar System. Its inner boundary is
defined as the layer in which the flow of the solar wind flows faster
than the speed of Alfvén waves. Turbulence and dynamic forces outside
this boundary cannot affect the shape of the solar corona within,
because the information can only travel at the speed of Alfvén waves.
The solar wind travels outward continuously through the heliosphere,
forming the solar magnetic field into a spiral shape, until it impacts
the heliopause more than 50 AU from the Sun.

In December 2004, the Voyager 1 probe passed through a shock front
that is thought to be part of the heliopause. Both of the Voyager
probes have recorded higher levels of energetic particles as they
approach the boundary.

So that's the information.

Now, temperature is a measure of particle energy. The AVERAGE is 1
milion to 2 million K. The particles are largely protons. This makes
calculating their average energy easy. A proton at 7.24e+22 Kelvins
contains 1 Joule. Its a linear relationship since temperature is a
measure of energy.

http://physics.nist.gov/cgi-bin/cuu/Value?jk

2 million K = 2e+6 K

So, each particle has

2e+6/7.24e+22 = 2.76e-17 J

per poton.

Even if we were flying at the base of the corona, where density is
highest (1e+11) we'd have contained in each cubic meter of space

1e+11 * 2.76e-17 J = 2.76 micro-joules

And its likely to be 1/100th this level at the altitude we're
flying.

To get a power rating we have to plug in the speed of things. Like a
care driving down the highway thorugh a snowstorm, the speed of the
car dominates all the other speeds - so, our spacecraft flying at 3.5
million km radius is moving at 120,000 m/sec. So, we're getting
energy dumped in for each square meter of projected area (along the
line of motion) of;

2.,76e-6 J/m3 * Area (1 for our sphere) * 120,000 m/sec = 0.54
watts per square meter.

Compare this to the 1 million watts per square meter coming from
sunlight.

Increasing the temperature to 20 million K increases the rate to 5.4
watts per square meter.

Which has very little impact on the temperature - it is a correction
factor in a system dominated by radiant energy.