The Maxus-4 package: what goes on in microgravity

>The Maxus-4 rocket launched on 29 April carried seven experiments stacked in
five self-contained modules. They were designed to investigate phenomena in
fluid physics and materials science that are difficult or impossible to
observe on Earth.

All of them involved very clever design to squeeze the maximum amount of
information-gathering capacity within the strict limitations of space and
weight inside the rocket payload. There was a strict time limitation, too:
the microgravity environment inside the free-falling payload would last
no more than 12.5 minutes between rocket burnout and atmospheric reentry

For most people, 12.5 minutes is just about enough time for a sandwich and
a cup of coffee. But microgravity scientists have learned to make the most
of every second of their experiments’ freedom from weight.

For example, a team from the University of Leuven in Belgium used their
berth on Maxus-4 to investigate the way zeolite crystals form in near-
weightlessness. Crystals formed in microgravity usually have a more
perfect structure than those grown on Earth. But in the case of zeolites
it is not yet known whether gravity favours or hinders the formation of
crystals. By observing crystal formation without the complication of
gravity, scientists hope to learn how to grow better crystals on Earth,
too.

For the Leuven group’s experiment, ten separate furnaces, each with three
different cells, quickly heated liquid silicate solution to a range of
temperatures. A rapid-cooling system "froze" crystal formation at various
stages; when the payload returned to Earth, scientists hoped to learn a
great deal from the samples they obtained.

Colleagues from the University of Freiberg in eastern Germany also packed
two mirror furnaces aboard Maxus-4, this time to investigate a curious
effect called Marangoni convection after its 19th-century discoverer,
Italian physicist Carlo Marangoni.

Most people are familiar with normal convection: in a room with a heater,
hot air rises because it is lighter than cold air. But in microgravity,
nothing is significantly "lighter" than anything else, and such convection
is impossible. Marangoni convection does not depend on gravity, but on
surface tension effects within liquids. It interferes with the formation
of perfect crystals in microgravity, and the Freiberg team were
investigating ways of suppressing it by means of high frequency
vibrations of by a rotating electromagnetic field.

For the team, the Maxus-4 environment was almost perfect. Professor
Croll of Bergakedemie Freiberg explained: "We don’t need three days of
microgravity. It’s more important that we have a short preparation time,
and that we can perform reference experiments a couple of days before the
launch. For the ISS, you have to deliver your material six months or a
year in advance. Here, we brought our samples to Kiruna a week ago. Next
week, we can take them back."

Prof Croll and his colleagues did take them back, too, despite some
anxious moments when the Maxus-4 recovery system failed and sent the
payload package plummeting into the Arctic wilderness 80 km from the
Esrange launch site. The crash wrecked the furnace apparatus that they
had so painstakingly built and scattered its silicon contents, but the
crystal samples themselves, one of them all of 38 cm long, were still
intact.

Scientists with experiments on the remaining three Maxus modules were
equally positive. Although no one was pleased at the equipment damage,
excellent video and telemetry links during the flight, plus rugged data
storage systems, ensured that none of their precious 12.5 weightless
minutes were wasted. And once the results are analyzed, some at least of
the Maxus-4 teams will use the new information to plan experiments for
their next incursion into microgravity.

The Maxus-4 package: what goes on in microgravity

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