RESEARCH AND DEVELOPMENT AT NASA
The Vision for Space Exploration marks the next segment
of NASA’s continuing journey to find answers to
compelling questions
about the origins of the solar system, the existence
of life beyond Earth, and the ability of humankind
to live on other worlds.
The success of the Vision relies upon the ongoing
research and development activities conducted at
each of NASA’s 10 field centers. In an effort to
promote synergy across NASA as it works to meet
its long-term goals, the Agency restructured its
Strategic Enterprises into four Mission Directorates
that align with the Vision. Consisting of Exploration
Systems, Space Operations, Science, and Aeronautics
Research, these directorates provide NASA Headquarters
and the field centers with a streamlined approach
to continue exploration both in space and on Earth.
EXPLORATION SYSTEMS
The Exploration Systems Mission Directorate creates
capabilities and supporting technologies that will
permit sustainable and affordable human and robotic
exploration. It includes the biological and physical
research necessary to ensure the health and safety
of crews during long-duration space flight. Led
by Associate Administrator Rear Admiral Craig Steidle,
USN (Ret.), the directorate actively supports the
Vision for Space Exploration, ensuring that it
is both achievable and affordable. The directorate
will guide NASA’s development of new systems for
safe human missions to the Moon, Mars, and beyond.
JUPITER ICY MOONS ORBITER
The mission design requirement document for a proposed
mission to Jupiter and its three icy moons was
the first product formulated by NASA’s new Exploration
Systems Mission Directorate. The
Jupiter Icy Moons
Orbiter (JIMO) is a spacecraft with an ambitious
proposed mission that would orbit the three planet-size
moons of Jupiter (Callisto, Ganymede, and Europa),
which may harbor vast oceans beneath their icy
surfaces. The mission would be powered by nuclear
fission and launched sometime in the next decade.
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The image shows a region of Europa’s crust made up of blocks which are thought
to have broken apart and “rafted” into new
positions. These features provide geologic
evidence that Europa may have had a subsurface
ocean at some time in its past. Combined
with the geologic data, the presence of a
magnetic field leads scientists to believe
an ocean is most likely present on Europa
today.
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Managed by NASA’s Jet Propulsion Laboratory (JPL),
the JIMO mission is part of NASA’s Project Prometheus,
a program studying a series of initiatives to develop
power systems and technologies for space exploration.
The JIMO endeavor would be the first NASA exploration
mission utilizing nuclear electric propulsion,
which would enable the spacecraft to orbit each
of these icy worlds to perform extensive investigations
of their makeup, history, and potential for sustaining
life.
According to Steidle, “The Jupiter Icy Moons Orbiter
requirements represent our new way of doing business,
tracing exploration strategies to the technology
maturation programs that will enable this exciting
mission and the other missions that make up Project
Constellation.” Just as the Apollo Program encompassed
NASA’s efforts to reach the Moon in the 1960s,
Project Constellation embodies the Agency’s new
initiatives to fulfill the Vision for Space Exploration.
LIFEGUARD SYSTEM
While NASA field centers such as JPL strive to
develop more effective ways to safely power, propel,
and maneuver spacecraft to explore worlds currently
beyond our reach, other centers are preparing the
technologies that will enable human beings to visit
these worlds. An astrobionics team at NASA’s Ames
Research Center has focused on physiological monitors
for the past decade, conducting research that supports
the goals of the Exploration Systems Mission Directorate
and the Vision for Space Exploration. The scientists
recently developed the
LifeGuard system , a lightweight,
portable device enabling physicians to monitor
the health and safety of explorers in remote locations
on Earth. The system may eventually be used in
space to monitor astronauts during space travel.
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The LifeGuard system, which may eventually be used in space to monitor astronauts
during space travel, recently monitored the
vital signs of expedition members sampling
soils and water from the world’s highest
alpine lake.
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The wireless LifeGuard system watched over the
vital signs of several expedition members who sampled
soils and water from the world’s highest alpine
lake, nearly 20,000 feet up the Licancabur volcano,
on the border between Chile and Bolivia late in
2003. The LifeGuard units sent real-time vital
signs from the members at the volcano to scientists
at Ames by satellite. This proved the monitor’s
potential to work in an extreme environment. The
test also demonstrated the enhanced ability for
doctors to practice telemedicine over long distances
on Earth or potentially in space.
The LifeGuard system allows real-time monitoring
of vital parameters such as heart rate, blood pressure,
electrocardiogram (EKG), breathing rate, and temperature.
It can also measure human movements in three dimensions.
The LifeGuard’s button sensors stick to the skin
to measure a person’s EKG and breathing rate, and
the device uses an arm cuff to measure blood pressure.
The data logger connects to a sensor clipped or
wrapped on an index finger to measure oxygen in
the blood and pulse rate.
“The data logger part of the system that collects
data from body sensors is about the size of your
palm and weighs about 166 grams (6 ounces),” explains
Carsten Mundt, an engineer who is developing LifeGuard
at Ames. According to Mundt, “The sensors we use
are quite easy to apply and comfortable to wear.”
In addition to potentially monitoring the health
of astronauts on long-term spaceflights, the LifeGuard
system may provide several applications on Earth.
LifeGuard could be used by physicians on Earth
to transmit a patient’s vital signs during transfer
to the hospital, and it could also be worn to monitor
patients at home to diagnose sleep disorders, heart
disease, or unsteady gait in the elderly. Firefighters
and hazardous material workers could also wear
the device to monitor their health during dangerous
activities.
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MOBILE AGENT SOFTWARE
In the spring of 2004, NASA scientists began testing
“mobile agent” software that eventually may help
astronauts on Mars talk with mission control on
Earth. The mobile agent software project, based
at Ames Research Center, called upon researchers
to play the role of astronauts during tests in
Utah’s Southeast Desert. The “explorer astronauts”
carried backpacks containing “smart” laptop computers
that were loaded with the mobile agent software.
The software, which scientists say may improve
communications between human planetary explorers,
robots, and mission support on Earth, comes in
several types, including “personal agent” software—software
to which people can speak—and “com” software, which
links software and hardware devices.
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NASA scientists tested the mobile agent system while the explorer astronauts
conducted real exploration in the desert.
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The main objective of the effort was to test the
mobile agent system while the explorer astronauts
and a robotic assistant conducted real exploration
in the desert. During the tests, each person’s
laptop computer was equipped with personal agent
software that could literally speak with them.
NASA’s Glenn Research Center provided the satellite
communications link from the Utah site to the NASA
Research & Education Network located at Glenn. During the field work, the explorers used
the mobile agent system to conduct real science,
looking for geological evidence of past water in
the desert as well as fossils from the Jurassic
period.
During the tests, the explorers talked with the
computer mobile agent software about science observations
being made. They needed to relay the name of the
location and identify which bag was being used
to collect samples, while narrating the contents
of the bag and the geologic context. The helper
robot that took part in the tests, called the Extravehicular
Activity (EVA) Robotic Assistant, followed along
with the human explorers.
Developed at NASA’s Johnson Space Center, the EVA
Robotic Assistant responds to voice commands. The
explorer astronaut speaks through a microphone
to the personal agent software, which relays commands
to the robot’s personal agent software. This software
activates computer programs that direct the robot
to follow the explorer astronauts, take photographs,
or carry samples.
During future planetary exploration, data will
be relayed by personal agent software to others
on the science team, both on the planet’s surface
and back on Earth. Information will be stored in
a database in a Mars or planetary human habitat.
The personal agent software will send these data
via e-mail to the Earth-bound science team. The
software will also automatically transmit images
taken by the astronauts to their planetary habitat
and to Earth. The computer that astronauts will
carry will include a global positioning system
device, enabling the software agent to stamp the
collected data with time and location.
The astronauts will also be able to tell the software
agent what activity they are going to do next by
choosing activities from a menu of potential planned
subjects. The chosen activity sets up expectations
for the personal agent software describing where
the explorer should be and how long the activity
should continue. If the astronaut deviates from
the plan or the planned location, or stays too
long, the personal agent software will verbally
warn the astronaut. At the same time, the computer
agent also will send e-mail to the support team
on Earth and to another computer agent in the habitat,
which will announce on the habitat’s loudspeaker
that there is a possible problem.
During a mission, the astronauts will wear biosensors,
possibly such as the ones designed for the LifeGuard
system, which will detect and transmit human vital
signs to his or her personal agent software. If
vital signs are not normal, the agent software
will send e-mail to Earth and broadcast a warning
on the loudspeaker.
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ARTIFICIAL INTELLIGENCE SOFTWARE
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This miniature antenna was developed using a NASA artificial intelligence software
program that creates designs faster than
a human being.
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Other current research and development activities
supporting the Exploration Systems Mission Directorate
are exploring the ways that artificial intelligence
(AI) can help engineers design advanced components
for long-term spaceflight. Funded by the directorate,
four computer scientists at Ames Research Center
wrote the AI evolutionary program, which can create
designs faster than a human being. The software,
which operates on 120 personal computers, can plan
devices that are smaller, lighter, stronger, and
consume less power—characteristics that meet spaceflight
requirements.
The AI software’s first task involved designing
a satellite antenna scheduled to orbit Earth in
2005. The antenna, able to fit into a 1-inch space,
can receive commands and send data to Earth from
the Space Technology 5 satellites. The three satellites—each
no bigger than an average television set—will help
scientists study magnetic fields in Earth’s magnetosphere.
According to project lead Jason Lohn, a scientist
at Ames, “The AI software examined millions of
potential antenna designs before settling on a
final one.” The software started with random antenna
designs and refined them through the evolutionary
process. It adapted existing designs quickly to
meet changing mission requirements. Scientists
also can use the evolutionary AI software to invent
and create new structures, computer chips, and
even machines. Lohn explains, “We are now using
the software to design tiny microscopic machines,
including gyroscopes, for spaceflight navigation.”
SPACE OPERATIONS
NASA’s new Space Operations Mission Directorate
is supported by Johnson Space Center, Kennedy Space
Center, Stennis Space Center, and Marshall Space
Flight Center. The directorate, led by Associate
Administrator William F. Readdy, directs space
flight operations, space launches, and space communications,
as well as the operation of integrated systems
in low-Earth orbit and beyond.
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Researchers record data as the hazardous gas detection system is used to analyze
the toxic gases produced by active vents,
called fumaroles, in the Turrialba volcano
in Costa Rica.
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Johnson manages the development, testing, production,
and delivery of all NASA human spacecraft, as well
as all human spacecraft-related functions such
as life support systems, space suits, and spacewalking
equipment. Johnson also serves as the lead NASA
center for the design and implementation of the
International Space Station. Scheduled for completion
around 2010, this working laboratory will serve
as a stepping-stone to other planets by teaching
the essentials of long-term living in space.
Kennedy’s slogan, “Launching the NASA Vision,”
has never been more true or applicable as the Agency
works diligently to return to flight safely and
implement the Vision for Space Exploration. The
Center will play a major role in these endeavors,
since its dual mission includes space launch operations
and spaceport and range technology development.
The Spaceport Technology Center initiative carries
out Kennedy’s role within NASA to meet the goals
of increased safety, reduced cost of space access,
and rapid expansion of commercial markets by infusing
spaceport technologies into all facets of current
and future Space Trans-portation Systems.
VOLCANIC EMISSION MASS SPECTROMETER
A Kennedy research and development team recently
used a new hazardous gas detection system to study
volcanic emissions in Costa Rica. The new prototype
system, named the “Aircraft-based Volcanic Emission
Mass Spectrometer (AVEMS),” also will have a direct
application to the Space Shuttle Program. The AVEMS
is a step toward an advanced system that will be
able to detect toxic gas leaks and emissions in
the Space Shuttle aft, or rear, engine compartment
and the crew compartment, providing an added level
of protection for the astronauts and the vehicle.
The Kennedy team used AVEMS to analyze gases vented
from the
Turrialba volcano in Costa Rica. The tests
were conducted from the air and in the volcano’s
crater. Johnson provided the WB-57F aircraft and
support for the nine research flights in the hazardous
gas study, while Ames provided infrared and visible
photography as well as multispectral imaging on
the mission.
The study was the first to sample and quantitatively
analyze fresh volcanic gases in their natural state.
Active vents in volcanoes, called fumaroles, produce
toxic gases such as sulfur dioxide, hydrogen sulfide,
and carbon dioxide, which, if too concentrated,
can be fatal. “Hikers on the volcanoes sometimes
get cold then are attracted to the warm vents.
When a large vent is producing massive amounts
of carbon dioxide, the carbon dioxide displaces
oxygen, which could be fatal to the hikers nearby,”
explains NASA project lead, Dr. Tim Griffin.
The new system shows promise for commercial applications
in a variety of environments and industries such
as semiconductor, petrochemical, automotive, refrigeration,
and cathode ray tube. The technology could be used
for breath and blood analysis as well as for monitoring
air quality in the workplace. “Mass spectrometer
technology could be used to ensure public safety
and equipment protection in so many areas,” says
Griffin. “Previous mass spectrometer systems have
been so expensive and bulky that their use was
limited to laboratories.” The new system is small
and mobile and is able to easily and accurately
produce in-depth data.
WIRE INSULATION REPAIR
Another Kennedy research and development project
is investigating innovative methods to repair damaged
wire insulation that can lead to self-healing systems.
The wire insulation used in the Space Shuttle is
either Kapton® (a polyimide) or Teflon® (a polyfluorocarbon).
Similar to other critical applications in the aircraft
and nuclear industry, wire inspection and repair
is important in keeping these systems safe. Existing
insulation repair methods use similar repair materials,
and either wrap the damaged area with mystic tape
and secure the ends with tie-wraps or melt a fluorocarbon
polymer over the damaged area with a heat gun.
These methods result in poor adhesion to the damaged
insulation and can cause breaks at each end of
the repair.
NASA’s new repair methods for Kapton synthesize
a polyimide on the surface of the damaged insulation,
producing an excellent seal with very high adhesive
forces. In addition to using this technology on
the Space Shuttle, NASA has been awarded funding
from the Federal Aviation Administration’s aging
aircraft group and is seeking partners to co-develop
and commercialize self-healing insulation repair.
SPACE SHUTTLE MAIN ENGINE ADVANCES
Stennis Space Center is NASA’s primary center for
testing and proving flight-worthy rocket propulsion
systems for the Space Shuttle and future generations
of space vehicles. Having conducted engine testing
for 4 decades, Stennis is NASA’s program manager
for rocket propulsion testing with total responsibility
for conducting and managing all NASA propulsion
test programs.
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A Space Shuttle Main Engine undergoes a test firing on the A-1 Test Stand at
Stennis Space Center.
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The
Space Shuttle’s Main Engines (SSMEs) reached
a significant milestone on January 21, 2004, by
surpassing 1 million seconds of successful test
and launch firings during a flight acceptance test.
The engine test, conducted at Stennis, ran for
8.5 minutes, the length of time it takes the Space
Shuttle to achieve orbit. “This 1 millionth-second
test is a testimony to the NASA and contractor
team that developed, tested, and continues to improve
the SSME to safely take humans to low-Earth orbit,”
said NASA’s Miguel Rodriguez, director of the Propulsion
Test Directorate at Stennis.
Developed in the 1970s, the SSMEs are the world’s
most sophisticated reusable rocket engines. Each
powerful engine is 14 feet long, weighs about 7,000
pounds, is 7.5 feet in diameter at the end of its
nozzle, and generates nearly 400,000 pounds of
thrust. The rigorous testing used to verify that
an engine is ready to fly is critical to any flight
program. According to Michael Rudolphi, Space Shuttle
propulsion manager, “The Main Engine that flies
today has gone through major upgrades and is safer,
stronger, and more reliable than the one that flew
on STS-1 in 1981. Reaching this milestone is a
historic moment for the Space Shuttle Program.”
In another effort to return the Space Shuttle safely
to flight, engineers with Stennis’ Propulsion Test
Directorate recently modified two test stands for
Space Shuttle flow liner testing. Flow liners,
located in the Space Shuttle’s main propulsion
system fuel feed lines, protect flexible joints
from the liquid hydrogen fuel as it feeds toward
the SSME turbopumps. Small cracks have been found
in the flow liners inside the hydrogen fuel lines
aboard the NASA orbiters Atlantis, Discovery, and
Endeavour. The cracks were first found in June
2002, resulting in concern that a piece of flow
liner material may work free and enter the SSME
turbopumps, causing potential for a premature engine
shutdown in flight. After extensive testing and
analysis, the existing cracks on the orbiters’
flow liners were repaired by welding.
Stennis has reactivated the A-1 Test Stand to accommodate
additional SSME upgrade testing and the E-1 Cell
2 Test Position articles are being activated to
accommodate future flow liner testing that will
be used to gather data while simulating the actual
flight environment. The fuel duct on the A-2 Test
Stand is also being modified to support fuel flow
characterization efforts. The A-2 stand currently
supports SSME testing and certification for flight.
The A-1 stand was used for testing the SSME until
last summer, when refurbishment of the A-2 stand
was completed and all SSME test activities were
transferred there.
“We are proud of the effort that was put forth
by our A-1 Activation Team,” asserts Ronnie Rigney,
deputy project manager of the SSME Project Office
at Stennis. “Successful completion of the A-1 Activation
test demonstrated that we are ready to support
the Space Shuttle Main Engine Test Program in its
Return to Flight work.”
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FIBER-OPTIC MASS FLOW SENSOR
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The fiber-optic mass flow sensor system was originally developed to accurately
determine the flow rates and tank levels
of multi-phase cryogenic fuels used on various
NASA vehicles such as the Space Shuttle.
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Marshall Space Flight Center recently developed
a technology that both supports the Vision for
Space Exploration and offers opportunities for
commercial partnerships with private industry.
Companies can license Marshall’s new fiber-optic
mass flow sensor system, whic was originally developed
to accurately determine the flow rates and tank
levels of multi-phase cryogenic fuels used on various
NASA vehicles, including the Space Shuttle, and
in ground-based propulsion testing.
Capable of measuring multi-phase flows in a pipe,
the technology is minimally invasive, cost effective,
retrofittable, and compact. Marshall’s new technology
combines high accuracy, intrinsically safe operation,
and low-cost flow sensing for virtually any optically
transparent medium, providing a superior product
for measuring multi-phase flows. Possible applications
include oil and gas industry multi-phase flows;
industrial, automotive, and aerospace multi-phase
flows; powder spray coatings; food processing;
and chemical processing, handling, and storage.
LAB-ON-A-CHIP TECHNOLOGY
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Dr. Lisa Monaco, the project scientist for the Lab-on-a-Chip Applications Development
program, examines a lab on a chip. The small
dots are actually ports where fluids and
chemicals can be mixed or samples can be
collected for testing.
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Another current Marshall research and development
effort involves the study of “lab-on-a-chip” technology.
The technology allows chemical and biological processes—previously
conducted on large pieces of laboratory equipment—to
be performed on a small glass plate with fluid
channels, known to scientists as microfluidic capillaries.
Dr. Helen Cole, project manager for the Lab-on-a-Chip
Applications Development program, explains, “We
are studying how lab-on-a-chip technology can be
used for new tools to detect bacteria and life
forms on Earth and other planets, and for protecting
astronauts by monitoring crew health and detecting
microbes and contaminants in spacecraft.”
The Marshall team is collaborating with scientists
at other NASA centers and universities to design
chips for many applications, such as studying how
fluidic systems work in spacecraft and identifying
microbes in self-contained life support systems.
Since the chips are small, a large number of them
can be carried on a Mars rover to search for life
or carried on long-duration human exploration missions
for monitoring microbes inside lunar or Martian
habitats.
SCIENCE
NASA’s Science Mission Directorate, headed by Alphonso
V. Diaz, carries out the scientific exploration
of the Earth, Moon, Mars, and beyond; charts the
best route of discovery; and reaps the benefits
of Earth and space exploration for society. By
combining Earth and space studies, NASA is best
able to establish an understanding of the Earth
and the surrounding solar system, to assure the
discoveries made here will enhance our work there,
and vice versa.
MARS EXPLORATION ROVER MISSION
Headlining NASA’s research efforts in the areas
of science and discovery, the
Mars Exploration
Rover mission has been turning up valuable data
regarding the Red Planet’s past and present environment,
thanks to a loyal mission team managed by JPL and
two determined robotic explorers, Spirit and Opportunity.
The big science question for the mission team is
how past water activity on Mars has influenced
its environment over time. While liquid water cannot
exist for long on the surface of Mars today, the
record of past water activity on Mars can be found
in the rocks, minerals, and geologic landforms,
particularly in those that can only form in the
presence of water. That is why the rovers are specially
equipped with tools to study a diverse collection
of rocks and soils that may hold clues to past
water activity on Mars.
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Clues from a wind-scalloped volcanic rock on Mars investigated by NASA’s Spirit
rover suggest repeated possible exposures
to water inside Gusev Crater.
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Spirit and Opportunity are offering unique contributions
in pursuit of the overall Mars science strategy
to “follow the water.” Understanding the history
of water on Mars is important to meeting the four
science goals of NASA’s long-term Mars Exploration
program: Determine whether life ever arose on Mars,
characterize the climate of Mars, characterize
the geology of Mars, and prepare for human exploration.
Spirit traveled 487 million kilometers (302.6 million
miles) and nearly 7 full months to reach Mars after
its launch from Cape Canaveral Air Force Station
on June 10, 2003. On January 3, 2004, Spirit landed
on Mars and successfully sent a radio signal to
notify the mission team of its historic arrival.
NASA chose Gusev Crater as Spirit’s landing site,
based on evidence from Mars orbiters that this
crater may have held a lake long ago. A long, deep
valley, apparently carved by ancient flows of water,
leads into Gusev. The crater itself is a basin
the size of Connecticut, created by an asteroid
or comet impact early in the planet’s history.
While the rover worked to free itself from its
lander platform over the next 12 days, it did not
waste any time in taking panoramic pictures of
its new “neighborhood” to send back to Earth. The
initial images—the highest- resolution pictures
ever sent from Mars and more than 3 times as detailed
as images from Mars Pathfinder in 1997—excited
the mission’s scientists about the prospects of
exploring the region.
On January 15, Spirit rolled all six of its wheels
onto Martian soil to begin what was originally
scheduled as a 90-day adventure to explore Mars.
Research was underway the next day, as Spirit reached
out with its versatile robotic arm and examined
a patch of fine-grained soil with a microscope
at the end of the arm. One unexpected finding was
the detection of a mineral called olivine, which
does not survive weathering well. According to
the mission scientists, the lack of weathering
suggested by the presence of olivine might be evidence
that the soil particles are finely ground volcanic
material. Another possible explanation is that
the soil layer where the measurements were taken
is extremely thin, and the olivine is actually
in a rock under the soil. The most prevalent elements
detected in the soil patch were silicon and iron.
Significant levels of chlorine and sulfur were
also found, characteristic of soils at previous
Martian landing sites but unlike soil composition
on Earth. The scientists believe that the soil
may not have even originated anywhere near Spirit’s
landing site, because Mars has dust storms that
redistribute fine particles
around the planet. The next target for use of the
rover’s full set of instruments was a rock the mission team named “Adirondack,” which was more
likely to have originated nearby.
Prior to the chance to study Adirondack, Spirit
temporarily stopped communicating on January 22.
The problem was later diagnosed as a memory-management
issue. Engineers regained partial control of the
spacecraft within days and reformatted the rover’s
flash memory to prevent recurrence of the problem.
Meanwhile, NASA’s second Mars Exploration Rover,
Opportunity, successfully sent signals to Earth
during its January 25 landing in a region of Mars
called Meridiani Planum, halfway around the planet
from the Gusev Crater site. A healthy Spirit got
back to work 4 days after the arrival of its twin,
and resumed its pursuit to examine Adirondack.
Spirit grinded the rock with an abrasion tool to
reveal its interior. Mission scientists were able
to confirm from the sublayer’s properties that
Adirondack was volcanic basalt, a predominant material
found on the planet’s surface. In spite of this,
further examination of Martian rocks would turn
up more promising results.
In early March, Opportunity found strong evidence
that the region of Meridiani Planum was once wet.
A rock outcrop dubbed “Guadalupe” yielded clues
that made the case for a watery history, such as
the presence of sulfates and crystal-filled niches.
“Liquid water once flowed through these rocks.
It changed their texture and it changed their chemistry,”
says Dr. Steve Squyres of Cornell University, Ithaca,
New York, and principal investigator for the science
instruments on the two rovers. “We’ve been able
to read the tell-tale clues the water left behind,
giving us confidence in that conclusion.” On Earth,
rocks with as much salt as this outcrop of Mars
rocks either have formed in water or, after formation,
have been highly altered by long exposures to water.
Back at the Gusev Crater, Spirit found hints of
a water history in a rock—albeit a very different
type of rock than those in which Opportunity found
clues to a wet past. A dark volcanic rock dubbed
“Humphrey,” about 2 feet tall, shows bright material
in interior crevices and cracks that looks like
minerals crystallized out of water, according to
the team scientists. The amount of water suggested
by the possible crystals in Humphrey is far less
than what is indicated by the minerals and structures
that Opportunity revealed in the Guadalupe rock
outcrop, indicating that Mars is a diverse planet.
Further clues uncovered by Opportunity caused the
mission team to deduce that some rocks on Mars
probably formed as deposits at the bottom of a
body of gently flowing saltwater. “We think Opportunity
is parked on what was once the shoreline of a salty
sea on Mars,” Squyres notes. The evidence continued
to mount up in early April when Spirit grinded
down a wind-scalloped volcanic round and found
a fracture in which water may have flowed through
at one time.
Given the success of the rovers, NASA decided to
extend the mission, handing Spirit and Opportunity
up to 5 months of overtime assignments.
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AURA EARTH-OBSERVING MISSION
In searching for conditions that might support
life on other planets, one of the first things
to look for is water—as in the case of the Mars
rovers—but the thin sliver of gases and air that
make an atmosphere around a planet is just as necessary
for life to exist. On July 15, NASA launched Aura,
a next-generation, Earth-observing satellite managed
by Goddard Space Flight Center that will
supply the best information yet about the health
of Earth’s atmosphere, according to the Space Agency.
Aura will provide an essential component for understanding
changes in our climate, our air quality, and the
ozone layer that protects life from harmful solar
radiation. In doing so, it will help answer some
fundamental questions regarding climate change.
One question that researchers have asked is: “Is
the stratospheric ozone layer recovering?” International
agreements have banned ozone-destroying chemicals
like chlorofluorocarbons (CFCs), but scientists
are unclear about the effectiveness of these treaties.
Aura will accurately detect global levels of CFCs,
and their byproducts, chlorine and bromine, which
destroy the ozone layer.
Another question to which researchers need more
information is: “What are the processes controlling
air quality?” Aura will help greatly to unravel
some of these mysteries by tracking the sources
and processes controlling global and regional air
quality. When ozone exists in the lower atmosphere,
the troposphere, it acts as an air pollutant. Gasoline
and diesel engines give off gases in the summer
that create ozone and smog. Aura will help scientists
follow the sources of ozone and its precursors.
Additionally, Aura will offer insights into the
question: “How is the Earth’s climate changing?”
As the composition of Earth’s atmosphere changes,
so does its ability to absorb, reflect, and retain
solar energy. Greenhouse gases, including water
vapor, trap heat in the atmosphere. Airborne aerosols
from human and natural sources absorb or reflect
solar energy based on color, shape, size, and substance.
The impact of water vapor and aerosols on Earth’s
climate remains largely unquantified, but now Aura
will have the unique ability to monitor these agents.
Aura’s space-based view of the atmosphere and its
chemistry will complete the first series of NASA’s
Earth Observing System satellites. The other satellites
are Terra, which monitors land, and Aqua, which
observes Earth’s water cycle.
CASSINI-HUYGENS MISSION
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This image, taken with Cassini’s Ultraviolet Imaging Spectrograph instrument,
indicates that there is more ice toward the
outer part of Saturn’s rings than the inner
part.
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An extensive tour of Saturn, its majestic rings,
and its 31 known moons is currently underway, following
a nearly 7-year journey to the planet.
Launched October 15, 1997, from Cape Canaveral
Air Force Station, Cassini is the most instrumented
and scientifically capable planetary spacecraft
ever flown. It aims to fulfill the
Cassini-Huygens
mission, a cooperative project of NASA, the European
Space Agency, and the Italian Space Agency. The
4-year mission, managed by JPL, will draw upon
the spacecraft’s 18 highly sophisticated science
instruments to study the Saturnian system in detail.
Cassini’s first stop on its historical tour of
Saturn was a June 11 fly-by visit of Phoebe, Saturn’s
largest outer moon. Data collected from the fly-by
indicate that Phoebe may be a frozen artifact of
a bygone era, some 4 billion years ago, like a
woolly mammoth trapped in Arctic ice. Mission scientists
concluded that Phoebe is likely a primordial mixture
of ice, rock, and carbon-containing compounds,
and further believe bodies similar to this moon
were plentiful in the outer reaches of the solar
system long ago.
The international Cassini-Huygens mission successfully
entered orbit around Saturn on June 30 of this
year, after completing a critical 96-minute main
engine burn that was calculated to slow the spacecraft
by 626 meters per second, or 1,400 miles per hour.
According to Robert T. Mitchell, program manager
for the mission, orbit insertion is “sort of like
applying your brakes while driving your car downhill.
Although you’ve got your foot on the brakes, you
still pick up speed as a steep gravity pulls you
in.” During the orbit insertion, Cassini flew closer
to Saturn than it will at any other time during
the planned mission.
Just 2 days after Cassini entered Saturn’s orbit,
preliminary science results from breathtaking images
and scientific measurements showed a complex and
fascinating planetary system. One early result
concerns Saturn’s Cassini Division, the large gap
between the “A” and “B” rings. While Saturn’s rings
are almost exclusively composed of water ice, new
findings show the Cassini Division contains relatively
more “dirt” than ice. Further, the particles between
the rings seem remarkably similar to dark material
that scientists saw on Phoebe. These dark particles
refuel the theory that the rings might be the remnants
of a moon. Also, Cassini’s ultraviolet imaging
instrument detected the sudden and surprising increase
in the amount of atomic oxygen at the edge of the
rings. The finding leads scientists to hypothesize
that something may have collided with the main
rings, producing the excess oxygen.
Still to come, the Cassini spacecraft and its piggybacking
Huygens probe (built by the European Space Agency)
will target Saturn’s largest moon, Titan. “In the
350 years since the discovery of Titan we have
come to see it as a world with surprising similarities
to our own, yet located almost 1.5 billion kilometers
(900 million miles) from the Sun,” said Dr. Jonathan
Lunine, Huygens interdisciplinary scientist and
professor of planetary science and physics at the
University of Arizona, Tucson. “With a thick, nitrogen-rich
atmosphere and possible hydrocarbon seas, Titan
may harbor organic compounds important in the chain
of chemistry that led to life on Earth.”
On December 24—6 months after reaching Saturn—Cassini
will release the wok-shaped Huygens probe towards
Titan. The event will be by far the most distant
descent of a robotic probe on another object in
the solar system. On January 14, 2005, Huygens
will enter Titan’s atmosphere, deploy its parachute,
and begin its scientific observations of Titan.
REMOTE SCANNING ELECTRON MICROSCOPY
In another far-reaching extension of NASA’s scientific
know-how, researchers for the first time can study
laboratory specimens from thousands of miles away
by remotely operating NASA’s new “super magnifying
glass.”
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High-resolution image of the hair bundle (stereocilia and kinocilium) of a horizontal
semicircular canal hair cell in a young chicken,
taken with a scanning electron microscope
(16,250 times magnitude). The electron micrograph
was obtained during a remote collaborative
scientific activity between NASA Ames’ Visualization,
Imaging, and Simulation Technology Center
and the National Institute of Deafness and
Other Communication Disorders in Bethesda,
Maryland.
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The Remote Scanning Electron Microscopy (RSEM)
technology was developed at Ames Research Center,
and has been successfully tested to allow scientists
to help NASA solve problems encountered by astronauts
during long-duration spaceflights.
“This technology will enable multiple researchers
at locations across the country to observe and
control the scanning electron microscope, thus
allowing for remote, real-time simultaneous analysis
of tissue by several investigators,” notes Dr.
Richard Boyle, director of the
Biological Visualization,
Imaging, and Simulation Technology Center at Ames.
In contrast to conventional microscopes that use
light waves, the RSEM uses electrons to magnify
details of tissue from 10 to 100,000 times. This
“super- dissecting microscope” illuminates the
sample with a great depth of field and produces
three-dimensional, high-resolution images. All
scientists need to use the RSEM is a suitable Web
browser and network access to connect to the instrument.
A remote-control system on the microscope enables
real-time interface with the tissue researchers
are studying.
The technology is being utilized in a collaborative
project with the National Institute of Deafness
and Other Communication Disorders in an attempt
to unravel key developmental processes of structures
of the inner ear involved in hearing. “The inner
ear cells change when you are in space and this
impacts astronauts’ health,” claims NASA astronaut
and physician Dr. Yvonne Cagle. “If we understand
how these hair cells reposition themselves, we
can better understand what happens over a long
period of time in space.”
AERONAUTICS RESEARCH
The Aeronautics Research Mission Directorate, led
by Associate Administrator Dr. J. Victor Lebacqz,
is committed to developing tools and technologies
that can help to transform how the air transportation
system operates, how new aircraft are designed
and manufactured, and how our Nation’s air transportation
system can reach unparalleled levels of safety
and security. Such tools and technologies will
drive the next wave of innovation, enabling missions
to be performed in completely new ways and creating
new missions that were never before possible. The
three NASA field centers that make up the directorate
are: Dryden Flight Research Center, Glenn Research
Center, and Langley Research Center.
As NASA’s primary installation for flight research,
Dryden Flight Research Center sits on the northwest
edge of Rogers Dry Lake, at Edwards Air Force Base
in Southern California’s high desert. Since its
creation in 1946, Dryden has advanced the design
and capabilities of many civilian and military
aircraft. To demonstrate improved reliability,
capability, and enhanced safety, new technologies
and new vehicles for both aviation and space flight
require validation through flight testing. Dryden’s
workforce expertise in aeronautics and in the development
of flight research tools and techniques, coupled
with the suite of specialized laboratories and
facilities needed for flight validation, are key
to the development and maturation of new vehicles.
Dryden operates a variety of specialized aircraft
that are used to verify a technology’s performance,
validate its safety and reliability, and discover
any previously unknown problems.
Glenn Research Center, located in Cleveland, Ohio,
and founded in 1941, provides research leadership
in power and propulsion technologies for aircraft
and spacecraft applications, aerospace communications,
microgravity fluid physics and combustion, and
bioscience and bioengineering. Glenn researchers
are working to develop, verify, and transfer air-breathing
propulsion technology for subsonic, supersonic,
hypersonic, general aviation, and high-performance
aircraft and rotorcraft, along with conducting
fundamental research in propulsion-related specialties
and new technologies, such as high-temperature
nanomaterials, nanodevices, and computational intelligence.
In the area of aerospace communications, Glenn
develops communication and network architectures,
systems modeling, and enabling technologies for
global communications network connectivity and
integrated communications, navigation, surveillance,
and weather information.
Langley Research Center, located in Hampton, Virginia,
and established in 1917, is renowned for scientific
and technological expertise in aerospace research,
systems integration, and atmospheric science. Langley
leads NASA initiatives in aviation safety and security,
quiet-aircraft technology, small-aircraft transportation
systems, and aerospace vehicles systems technology.
The Center’s unique infrastructure of wind tunnels,
laboratories, and equipment arrays have enabled
researchers to develop, validate, and deliver to
the commercial sector technologies to improve the
effectiveness, capability, efficiency, and safety
of the Nation’s air transportation system. Langley
supports space programs with atmospheric research
and technology testing and development. The Center
serves a principal role in understanding our planet
through uniquely developed atmospheric missions,
measurement instruments, and climate prediction
data.
X-43A HYPERSONIC RESEARCH AIRCRAFT
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The X-43A hypersonic research aircraft and its modified Pegasus booster rocket
accelerate after launch from NASA’s B-52B
launch aircraft over the Pacific Ocean.
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In a combined research effort involving Dryden,
Langley, and several industry partners, NASA recently
demonstrated the value of its
X-43A hypersonic
research aircraft, as it became the first air-breathing,
unpiloted, scramjet-powered plane to fly freely
by itself. The March 27 flight, originating from
Dryden, began with the Agency’s B-52B launch aircraft
carrying the X-43A out to the test range over the
Pacific Ocean off the California coast. The X-43A
was boosted up to its test altitude of about 95,000
feet, where it separated from its modified Pegasus
booster and flew freely under its own power.
Two very significant aviation milestones occurred
during this test flight: First, controlled accelerating
flight at Mach 7 under scramjet power, and second,
the successful stage separation at high dynamic
pressure of two non- axisymmetric vehicles. To
top it all off, the flight resulted in the setting
of a new aeronautical speed record. The X-43A reached
a speed of over Mach 7, or about 5,000 miles per
hour faster than any known aircraft powered by
an air-breathing engine has ever flown.
Hyper-X, NASA’s multi-year experimental hypersonic
ground and flight test program for the X-43A, is
demonstrating air-breathing engine technologies
that promise to increase payload capacity—or reduce
vehicle size for the same payload—for future hypersonic
aircraft and/or reusable space launch vehicles.
As envisioned, payload capacity will be increased
by discarding the heavy oxygen and associated tanks
that rockets must carry by using a propulsion system
that uses the oxygen in the atmosphere as the vehicle
flies at many times the speed of sound. Hydrogen
fuels the X-43A’s scramjet engine, which scoops
oxygen from the atmosphere for combustion.
S-3 VIKING ICING RESEARCH AIRCRAFT
Meanwhile, at Glenn, researchers under NASA’s
Aviation
Safety and Security program are preparing to retire
a 22-year-old icing research “workhorse” in order
to accommodate a successor that will provide increased
power, speed, and range. The S-3 Viking, a former
U.S. Navy aircraft, will replace Glenn’s current
icing research aircraft, a DeHavilland Twin Otter,
with initial research flights scheduled to be performed
in 2006. The S-3 Viking arrived at Glenn in March
and is being modified by the Center’s technicians
to incorporate diagnostic tools and allow for in-flight
icing weather forecasts.
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In-flight icing research activities will soon be aided by a new addition to Glenn
Research Center. A former U.S. Navy S-3
Viking aircraft was recently transferred
to NASA and will undergo modifications
to provide a state-of-the-art flying laboratory
in 2006.
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The DeHavilland Twin Otter icing research aircraft
has helped Glenn in studying icing cloud characterization,
natural icing physics studies, full-scale iced
aircraft aerodynamics, and ice protection development.
It has also helped solve the problems of tail plane
stall and super-cooled large droplet dangers. However,
to support NASA’s new aviation safety objectives,
strategic icing research plans have identified
that icing flight research will require increased
capability in range, speed, payload, and onboard
power beyond the Twin Otter’s capabilities.
The S-3 Viking’s range and speed will enable research
flights from Cleveland to Wyoming and back in a
single day. These increased capabilities are essential
in the areas of improved aviation weather forecast
development, icing simulation tool development,
icing cloud characterization, identification and
simulation of aerodynamic effects of icing, and
continued development of education and training
materials for modern regional and general aviation/business
aircraft operators.
The NASA Aviation Safety and Security program is
a partnership with the Federal Aviation Administration,
aircraft manufacturers, airlines, and the U.S.
Department of Homeland Security that is working
to reduce the fatal aircraft accident rate and
protect air travelers and the public from security
threats.
As NASA begins its new quest to achieve the Vision
for Space Exploration, the research and development
efforts across the Agency will continue to bring
cutting-edge technologies to the American public.
These innovations will help build the future, while
protecting and improving the world today.
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