In a word, probably
not.
The mechanics required for steady flight are illustrated in Figure
1 below. Basically, lift must balance weight, and thrust must balance drag. For clarity,
the moment balance about the center of gravity is not depicted.
Lift and drag are both proportional to the wind pressure and
the wing area. The coefficients of
proportionality are the lift and drag coefficients. Control of lift is by angle of attack
(AOA), and the usable lift coefficient
only varies between zero and the stall value (a bit over 1). For control purposes, the same basic lift coefficient values must
be used on Mars as on Earth.
The wind pressure (q, the dynamic pressure) is proportional
to density and to velocity squared.
The density can be calculated as a density ratio (σ)
multiplied by a standard density value (ρo). Earth sea level density on a standard day is
the usual value used for that standard density.
Values are shown.
Under ideal gas assumptions (P = ρ Runiv T/MW), the density ratio pretty much anywhere is the
pressure ratio to Earth standard pressure, multiplied by the molecular weight ratio to
standard, and divided by the absolute-scale
temperature ratio to standard. For
typical pressures and temperatures on Mars,
density ratio is near 1% of Earth sea level, but this is quite variable since the “air”
pressure there is quite variable. An
average value is shown. Surface gravity
on Mars is 38% that on Earth.
To design aircraft for Mars,
we need the surface density ratio divided by the surface gravity
ratio. The net effect is that the levels
of the aerodynamic forces acting on a reduced weight on Mars, are about factor
35 smaller than here on Earth, at
otherwise the same AOA’s! That factor
can increase either the wing area or the square of the velocity, or some of both, to get the same balance for steady flight on
Mars.
Note that if you make the wing bigger, it will be more massive in proportion to that
increased area, and therefore
heavier, even in the lower gravity of
Mars. The weight increase of more wing
area will act toward overcoming any lower speed benefit. That is because the density effect is much
larger than the reduced gravity effect,
on Mars.
Velocity squared factored up by 35 is the same as
velocity factored up by almost 6. Example:
if landing and takeoff speed for some airplane design was about 100 mph
on Earth, it would be almost 600 mph on
Mars for the same wing area as on Earth.
Such speeds that close to the surface are quite dangerous. That is just not something to be attempted
voluntarily.
Double the pressure to 12 mbar in the Hellas Basin, and the over-100 density reduction factor
halves. That density ratio divided by
the gee ratio is now closer to 17 than 35,
and its square root is a velocity ratio a bit over 4. It’s still a bigger, heavier (and impractical) wing by a factor of
17 on wing area, or else a speed near
the surface exceeding 400 mph. Or
something in-between, with an
impractically-large wing and a speed that is still too high close to the ground
to be safe. Not at all safe to attempt. Plus, you cannot fly it anywhere except down in
that basin.
The same basic aerodynamic and weight-carried factors act on
helicopter rotors in pretty much the same way.
This is why I think the use of airplanes (or helicopters) as we
know them here on Earth, at a size scale
suitable for transporting freight or people,
are simply not technologically feasible in the extremely thin “air” of
Mars, despite the lower gravity.
Not absolutely impossible, but a practical design configuration is pretty much unimaginable.
Figure 1 – First Cut Exploration of Aircraft Design
Requirements for Mars
Second, Closer
Look:
Now, looking at this
issue a bit more closely, let us explore
landing and takeoff speeds that are practical,
and at lift coefficients that are high,
but with adequate stall margin,
sort of like what is required by the FAR’s here on Earth. For that,
I presume 120 mph = 176 ft/sec = 53.6 m/s, and a max lift coefficient at takeoff and
landing of 1.0. I also looked at high
altitudes on Earth, and at higher
pressure in the Hellas Basin on Mars. I
did this with a spreadsheet, as
illustrated in Figure 2 below.
Those numbers for Mars might not seem too bad, until you try to sketch what that kind of a change
to an aircraft design might look like. I
did that in Figure 3 below,
holding the fuselage size constant,
and just up-sizing the wings and tails.
There is no way to get the required tail arm lengths for stability
and control, without also up-sizing
the fuselage, which drives up mass even
further! It would be the same with a
swept-wing design for higher cruise speeds:
you still have to land and take off!
That should indicate just how impractical it will always
prove to be, to design conventional
airplanes capable of safe and practical flight on Mars, regardless of the propulsion. That “air” is just too thin!
Figure 2 – Sizing Wings for 120 mph Takeoff/Landing Speeds
on Mars
Figure 3 -- Upsizing
Aerosurfaces for Fixed Fuselages For Mars
Sounds like you'd need rocket propulsion with vertical take off and landing by rocket, and high flight speeds, maybe even supersonic. I wonder how the range would work out. Hmm.. I am no chemist, and I don't know anything about lithium nitride, but it keeps coming up in searches as something that reacts energetically with CO2. Maybe a jet engine that's sort of like a hybrid rocket, i.e. with solid fuel? No doubt there are MANY things wrong with this, and I'd probably learn them if I got on the right part of the Mars forum.
ReplyDeleteI'm no chemist, either. Li3N is a crystalline solid with a high meltpoint (over 800 C) that reacts exothermically with both CO2 and H2O. I think you'd have to burn it from the solid phase, like coal. It would have to be shipped from Earth to Mars, quite a dangerous thing. Why not instead just build a rocket hopper instead of attempting jet airplanes on Mars? They fly ballistic trajectories sort of like artillery shells. -- GW
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