Nothing seems more down-to-Earth than dirt, but scientists are going to
space to understand how earthquakes and related strains and stresses disturb
soil and sand.

When Space Shuttle Columbia lifts off in January, it will carry the
Mechanics of Granular Materials (MGM) experiment, which studies soil
behavior under conditions that cannot be duplicated on Earth — the
microgravity, or low-gravity created as the Shuttle orbits Earth.

Results from this granular mechanics research can lead to improved
foundations for buildings, management of undeveloped land, and handling of
powder or granular materials used in chemical, agricultural and other
industries.

“Even in North Alabama, we experienced an earthquake tremor last year,” said
Buddy Guynes, the experiment’s project manager at NASA’s Marshall Space
Flight Center in Huntsville, Ala. ” This experiment is relevant to our lives
on Earth. At NASA, we also want to know how soil behaves at different
gravity levels, so one day crews can safely build habitats on Mars and the
Moon.”

How do earthquakes and other geological activities, like mining, impart
stress to soil causing it to literally become shifting sand? As an
earthquake strikes, it deforms the soil, changing the volume of the soil. If
water is present, water pressure may build up in the pore space between the
soil grains. What was once a solid foundation begins to flow like a liquid,
a process called soil liquefaction. As the soil moves, foundations become
unstable, and Earth’s gravity wins out — collapsing buildings, bridges and
other structures.

Earth’s gravity also makes it difficult for scientists to study the precise
physics of granular mechanics and soil liquefaction.

“On Earth, gravity-induced stresses quickly change the amount of weight, or
loads, a foundation can support,” said Dr. Stein Sture, the experiment’s
principal investigator at the University of Colorado at Boulder. “We can use
space-based research to perform detailed analyses to understand the physics
that causes water- saturated, but initially firm foundation soil, to
suddenly flow like water.”

The strength of sand or any particulate material depends on how the granular
assembly is packed together and interlocked. Moisture or air trapped within
or external loads on the site help determine its weakness or softness.
Cyclic loading and instabilities can cause the soil to loosen and collapse
under the stress of earthquakes or other pressures.

“Computer tomography scans will produce a series of images that help us
study the minute details of individual grains of sand and how they interact
with each other,” said Sture. “We can examine the particle arrangement and
structure of soils and learn about the strength, stiffness and volume
changes that occur when low pressures are applied to granular materials.”

For the STS-107 experiment, three sand columns held inside latex sleeves
will be used for nine experiment runs. Ottawa sand — natural quartz sand
with fine grains widely used for civil engineering experiments — will be
saturated with water to resemble soil on Earth. Each column holds about 1.3
kilograms (2.8 pounds) of Ottawa F-75 banding sand.

The flight crew will use a laptop computer to send commands to the
experiment, causing the sand to be compressed between two tungsten metal
plates. As the sand is compressed and relaxed, a load cell will measure the
applied force, and three CCD cameras will record changes in shape and
position of the soil inside the column. This compression and relaxation will
simulate the loads that might be imparted to soil via earthquakes and other
external forces.

The three columns will be used for nine tests or observations periods. Upon
completion of each run, the samples will be expanded and stretched back to
their original length to create a homogenous mix of sand and water at the
start of each run.

When the Shuttle lands, the sand columns will be imaged using computer
tomography at laboratories at NASA’s Kennedy Space Center in Florida. Then,
they will be injected with epoxy, and the columns will be sawed into thin
disks. These will be sent to experiment investigators in Colorado and
Louisiana for inspection under an optical microscope.

“Our earlier flights showed gravity masked measurements of friction between
grains of sand,” said Dr. Khalid Alshibli, project scientist for the
experiment and professor of civil engineering at Louisiana State University
and Southern University in Baton Rouge. “This is an important factor in
determining the amount of weight the soil can support.”

The Mechanics of Granular Materials experiment has flown twice — on Space
Shuttle missions STS-79 in 1996 and STS-89 in 1998. These investigations
revealed soil specimens were two-to-three-times stronger and much stiffer
than scientists had predicted. The 16-day STS-107 flight aboard Columbia
gives scientist an opportunity to perform longer, more complex experiments.
Future experiments will benefit from extended tests aboard the International
Space Station, including experiments under simulated lunar and Martian
gravity in a science centrifuge.

“We anticipate valuable results from the STS-107 experiments,” said
Alshibli. “We are using a novel specimen reformation technique that enables
us to use the same specimen for more than one experiment run. This lays the
foundation for more extensive, long-term soil research that can be carried
out on the International Space Station.”

In addition to the Mechanics of Granular Materials experiment, Columbia will
carry 29 more investigations sponsored by NASA’s Office of Biological and
Physical Research. These peer-reviewed and commercial experiments will
advance knowledge in medicine, fundamental biology, fluid physics, materials
science and combustion. The STS-107 mission is a dedicated science mission
recommended by the National Research Council and approved by the U.S.
Congress. With more than 80 investigations, it builds on prior
multidisciplinary Shuttle science missions and serves as a prelude to
long-duration investigations that will be possible as science capabilities
grow on the International Space Station.