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Iron
at the core
University of Chicago researchers using the APS diamond anvil cell
found experimental evidence that the Earth’s inner core consists
largely of two exotic forms of iron instead of only one. These forms
of iron seem to be alloyed with silicon, a lighter element.
Scientists had
previously determined some of the characteristics of the iron in
the core from the way seismic waves travel through Earth from earthquakes
and explosives.
The University
of Chicago research team used a laser-heated diamond anvil cell
to expose a sample of iron to searing subsurface temperatures of
approximately 4,200 degrees Fahrenheit and crushing pressures of
840,000 atmospheres. Using the APS helped researchers identify the
samples chemical composition.
The researchers
found that the atomic structure of iron changes under intense temperatures
and pressures. A tiny iron sample may take on two different atomic
structures under conditions found 1,800 miles beneath Earths
surface.
The existence
of two exotic forms of iron in the Earth’s core could influence
the interpretation of seismic data about the core. The research
results were reported in Science.
Cleaning
up the environment
Researchers used an X-ray microprobe at the APS to examine the microbial
processes that strip zinc and other toxic metals from solutions
to produce acceptable drinking water.
The microbes
convert metal sulfates into harmless sulfides. The results show
how microbes control metal concentrations in groundwater and wetland-based
remediation systems and suggest biological routes for formation
of some low-temperature zinc sulfide deposits. The researchers are
from the University of Wisconsin
at Madison, the Australian
Geological Survey Organization, Diversion Scuba of Madison and
Argonne.
The microbes
were first discovered by recreational scuba divers from Diversion
Scuba exploring the dark, flooded tunnels of an old mine in southwestern
Wisconsin.
This evidence
can help develop strategies for creating new wetlands, rich in organic
matter and to treat acidic drainage from mines. Acid mine drainage
is a threat to surface and groundwater near mines and can contaminate
wells and other drinking water supplies.
Seeing
an important membrane protein
Proteins on cell membranes present a challenge to biologists because
they are often large and insoluble, making them difficult to examine
in detail. A team of structural biologists at Harvards
Massachusetts General Hospital, working at the APS, has overcome
these obstacles and for the first time determined the structure
of aVb3, one of the many integrin proteins.
Integrin proteins
are important because they control many cellular activities and
are believed to play a major role in tumor growth, bone maintenance
and inflammation. In addition, some viruses, including AIDS, enter
cells through the integrin.
Knowing the
structure should help scientists determine how the protein works
and help pharmaceutical companies design drugs to combat diseases.
The X-ray analysis
confirmed some suspicions about the integrin structure, but it also
contained some surprises for the researchers, showing some bending
in parts of the molecules. This bending might help explain how the
integrin transmits its signals.
Pharmaceutical
companies are already using this information in developing new drugs
aimed at the protein.
For more information,
please contact Catherine Foster.
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