Gregory
Benford is a professor of physics at the University of California,
Irvine. He is also a writer of award-winning science fiction; his latest
novel is Eater.
You are standing above
a sweeping cinnamon plain, dotted with crescent dunes beneath a pink sky.
A breeze stirs sand into dust devils. Craggy ridges far across what was
once a carved river valley point at the rising potato shape of a small
moon.
But all this you ignore,
beautiful though it is, because halfway to the rosy horizon is a splash
of yellow and brown. The possible site of an ancient thermal vent, or so
the satellite pictures say.
With a touch of your thumb
you send the robot rover ahead, while you climb back into your dune buggy.
If the yellow stain signals sulfur, this might well be an entrance into
the mysterious underground of Mars.
Once, lava and water probably
spewed from that opening. Your expedition's geologist says this river valley
once held a sprawling stream, when Mars was wet and warm. If life was here
once, it might have retreated below, just as the non-oxygen breathers did
on Earth long ago.
And the easiest way to
find out was to descend through the tubes where lava once flowed, into
the heart of the Red Planet. Eagerly you press on.
I used "you" in the above
little scene because it could indeed be you standing on Mars, carrying
out the most exciting and profound scientific expedition of the century
to come. We can do such wonderful things in the lifetime of most people
reading this.
This may seem a curious time
to talk about such grand ambitions. We lost
both this season's Mars missions, and NASA is under enormous pressure
to drop the faster-cheaper-better
mantra. Some say we should hold
off on Mars generally.
Nonsense. Space is tricky
and dangerous, but we knew that already. Instead of obsessing over the
embarrassing smashup
of an orbiter, plus the mysterious
vanishing of the Polar Lander -- probably due to a faulty engineering
design in the landing system -- we should look long. The purpose of
these landers and orbiters is primarily to understand the Red Planet's
deep past. But they can also give us a list of promising landing sites
for humans.
The argument that people
are essential to finding evidence of past (or present!) life is solid.
Robots cannot crawl down thermal vents and take samples, assessing them
on the spot. After dual exploratory expeditions in 2001,
2003 and 2005, NASA plans to return a small soil sample to Earth around
2007, using elementary robotic scavenging. (Even returning less than a
kilogram of Martian soil will probably cost around a billion dollars, Jet
Propulsion Lab scuttlebutt has it.)
After that, what? Settling
the big scientific issue of life on Mars will demand a crewed expedition.
Maybe we could go to Mars by offering an international prize, an idea I
used in a recent novel, The
Martian Race. But funding is only a side issue, really.
Right now, the entire space
community should demand that present operations work with this goal in
mind: human exploration before 2020.We're spending many billions on the
space station,
which NASA advertises as telling us how to "live in space" for "eventual
planetary voyages."
But mostly it will prove
what the Russians' Mir
experience underlined: there's not a lot of science to do there, and zero-g
is very bad for you.
So, we should demand that
the space station do something really useful for a Mars flight.
| Do the Math |
| For creating rotational gravity aboard a habitat bound for Mars, the likely counterweight would be the last stage of a big booster, which has already injected the habitat into a long 6-month orbit for Mars, starting from Low EarthOrbit.
The acceleration (A) of such a spinning dynamics problem is A= S2 R/1000. |
 Here A is in units of one g, so for Mars it's 0.38. S is the spin in units of revolutions/minute, and R the length of the cable in meters. For a spin rate of 3 rev/minute, R=9 meters. This is too short, for several reasons -- but then, I've left out a detail.The habitat rotates around the system's center of mass -- the length of the cable divided by (1+m/M), where m is the habitat mass and M the counterweight mass. |
 A plausible ratio m/M is 4, so the whole cable length L for the above case would be about 5R, or 50 meters.I include this level of techie detail to suggest the considerations we must work out to design a scheme to get comfortably to Mars. Some 1960s NASA ground experiments suggested that spinning does not produce dizziness until S=6 rev/minute,so there's room to maneuver. |
First, make it the first
centrifugal gravity experiment ever. It's shocking that no one has ever
done this simple, crucial task, and making gravity by rotating a habitat
suspended by a cable to a counterweight is probably the easiest way to
go to Mars.
But we really don't know
anything about compensating for zero-g in space itself. A basic theorem:
Theory is no substitute for experience.
Kubrick's 2001:
A Space Odyssey showed us a classic space station like a revolving
bicycle wheel. It's time to mount such an experiment, maybe a habitat on
a cable with a counterweight, next to the International Space Station.
Use the station as a construction
shack. Only by direct experience will we learn.
And then there's the whole
problem of a truly cyclic environment. We'll need to reprocess wastes in
air and urine to survive on dry Mars. NASA is studying this, but how does
such a system work in 0.38 g, the Mars standard? We could do a true dry
run by running a truly closed environment on a rotating centrifugal gravity
habitat, in Low Earth Orbit, next to the space station.
This is an exciting program,
with real work for the astronauts, and -- undoubtedly! -- plenty of unforeseen
problems. Real work, not just camping out in space, as the Russians spent
decades doing, fruitlessly.
Years of experience doing
this will give us a team of tough, experienced astronauts, ready to go
to Mars. They're alive right now. Maybe you could be one.
How to get to Mars? Start
now.
You are edging carefully
down the slope of the thermal vent, peering into the throat that once belched
hot mud and scalding water -- once a super-Yellowstone, billions of years
ago.
Your team partner carries
the 3D-TV camera on his shoulder. You're the biologist on this expedition,
so you have to carry the sample pouches, added mass. And it looks like
you're going to be needing them.
Knowing that all of humanity
will hang upon your words, when you transmit to Earth at the end of this
day, you say carefully, "Looks like some mottled growth on the rocks below.
Discoloration, brown and gray ... like an algae mat."
Your heart pounds. It
does indeed look...different.
You're only twenty meters
below the deserts of Mars. There might be anything below, caverns to be
searched, secrets uncovered.
"I'm going further in."
What do you think? Send your
comments to the editor.