National Aeronautics and Space Administration [627979]

National Aeronautics and Space Administration
A Researcher’s Guide to:
Space Environmental Effects

2This International Space Station (ISS) Researcher’s Guide is published by
the NASA ISS Program Science Office.
Authors:
Miria M. Finckenor
Kim K. de Groh
Executive Editor: Amelia Rai
Technical Editor: Neesha HoseinDesigner: Cory Duke
Cover and back cover:
a. A stronaut Stephen Robinson retrieves Materials International Space Station Experiment-1 (MISSE-1)
during the STS-114 mission, July 2005. Photo was taken during Expedition 6 on the ISS.
b. S canning electron microscopy image of the back-surface of a thin film layer of Kapton H after four
years of low-Earth orbit (LEO) ram atomic oxygen erosion while on the exterior of the ISS as part of
the MISSE-2 Polymer Erosion and Contamination Experiment (PEACE).
c. S canning electron microscopy image showing the microscopic cone texture that developed after
four years of LEO ram atomic oxygen erosion of a pyrolytic graphite sample while on the exterior of the ISS as part of the MISSE-2 PEACE Polymers experiment.

3Close-up view of the Materials International Space Station Experiment (MISSE) 6A and 6B Passive Experiment Containers
(PECs) on the European Laboratory/Columbus. Photo was taken during a flyaround of STS-123 Space Shuttle Endeavor.Soaring 250 miles above Earth, the ISS is a modern wonder of the world,
combining the efforts of 15 countries and thousands of scientists, engineers
and technicians. The ISS is a magnificent platform for all kinds of research
to improve life on Earth, enable future space exploration and understand the
universe. This researcher’s guide is intended to help potential researchers
plan experiments that would be exposed to the space environment, while
externally attached to or deployed from the ISS. It covers all the pertinent
aspects of the space environment, how to best translate ground research to flight results and lessons learned from previous experiments. It also details
what power and data are available on the ISS in various external locations.The Lab is Open

4
4

51. Microgravity, or weightlessness, alters many observable phenomena
within the physical and life sciences. Systems and processes affected by microgravity include surface wetting and interfacial tension, multiphase flow and heat transfer, multiphase system dynamics, solidification, and fire phenomena and combustion. Microgravity induces a vast array of changes in organisms ranging from bacteria to humans, including global alterations in gene expression and 3-D aggregation of cells into tissue-like architecture.
2. Extreme conditions in the ISS environment include exposure to extreme heat and cold cycling, ultra-vacuum, atomic oxygen, and high energy radiation. Testing and qualification of materials exposed to these extreme conditions have provided data to enable the manufacturing of long-life reliable components used on Earth as well as in the world’s most sophisticated satellite and spacecraft components.
3. Low Earth orbit at 51degrees inclination and at a 90-minute orbit affords ISS a unique vantage point with an altitude of approximately 240 miles (400 kilometers) and an orbital path over 90 percent of the Earth’s population.
This can provide improved spatial resolution and variable lighting conditions compared to the sun-synchronous orbits of typical Earth remote-sensing satellites.Unique Features of the ISS
Research Environment
51. Microgravity, or weightlessness, alters many observable phenomena
within the physical and life sciences. Systems and processes affected by microgravity include surface wetting and interfacial tension, multiphase flow and heat transfer, multiphase system dynamics, solidification, and fire phenomena and combustion. Microgravity induces a vast array of changes in organisms ranging from bacteria to humans, including
global alterations in gene expression and 3-D aggregation of cells into tissue-like architecture.
2. Extreme conditions in the ISS space environment include exposure to extreme heat and cold cycling, ultra-vacuum, atomic oxygen, and high energy radiation. Testing and qualification of materials exposed to these extreme conditions have provided data to enable the manufacturing of long-life reliable components used on Earth as well as in the world’s most sophisticated satellite and spacecraft components.
3. Low-Earth orbit at 51 degrees inclination and at a 90-minute orbit affords ISS a unique vantage point with an altitude of approximately 240 miles (400 kilometers) and an orbital path over 90 percent of the Earth’s population. This can provide improved spatial resolution and variable lighting conditions compared to the sun-synchronous orbits of typical Earth remote-sensing satellites.Unique Features of the ISS
Research Environment

6Unique Features of the ISS Research Environment 5
Research Priorities for Space Environmental Effects on the ISS 7
Aspects of the Space Environment 10
Vacuum 10
Atomic Oxygen 1 0
Ultraviolet Radiation 1 2
Particulate or Ionizing Radiation 1 3
Plasma 14
Temperature Extremes and Thermal Cycling (Coefficients of Thermal
Expansion [CTE] Mismatch) 14
Micrometeoroid/Orbital Debris Impact 1 5
Orientation and Location on the ISS 17
Approaches to Mitigate Contamination 18
Lessons Learned 20
Plan for Flight Recovery Contingencies 2 0
Control Samples and Preflight Testing 2 0
Understand Sample Geometry 2 1
Other Lessons Learned 2 2
Developing and Flying Research to the ISS 24
ISS External Accomodations 26
Japanese Experiment Module Exposed Facility [Japan Aerospace
Exploration Agency (JAXA)] 2 6
Multi-Purpose Experiment Platform (MPEP [JAXA]) 2 7
JEM Small Satellite Orbital Deployer (J-SSOD [JAXA]) 2 8
EXPRESS Logistics Carrier (NASA) 2 8
Columbus External Payload Facility (European Space Agency) 3 1
Russian Segment External Facilities (Russian Federal Space Agency) 3 2
Funding Opportunities 33
Citations 34
Acronyms 37Table of Contents

7Scientists and engineers have developed advanced materials for manned spacecraft
and satellites for a range of sophisticated applications in space exploration, transportation, global positioning and communication. The materials used on the exterior of spacecraft are subjected to many environmental threats that can degrade many materials and components. These threats include vacuum, solar ultraviolet (UV) radiation, charged particle (ionizing) radiation, plasma, surface charging and arcing, temperature extremes, thermal cycling, impacts from micrometeoroids and orbital debris (MMOD), and environment‑induced contamination. In terms of
materials degradation in space, the low ‑Earth orbit (LEO) environment, defined
as 200 ‑1,000 km above Earth’s surface, is a particularly harsh environment for
most non ‑metallic materials, because single ‑oxygen atoms (atomic oxygen [AO])
are present along with all other environmental components (Yang and de Groh, 2010). Space environmental threats to spacecraft components vary greatly, based on the component materials, thicknesses and stress levels. Also to be considered are the mission duration and the specific mission environment, including orbital parameters for the mission, the solar cycle and solar events, view angle of spacecraft surfaces to the sun and orientation of spacecraft surfaces with respect to the spacecraft velocity vector in LEO (Dever et al., 2005). Examples of AO erosion
and radiation ‑induced embrittlement of spacecraft materials are provided in
Figures 1 and 2.Research Priorities for
Space Environmental
Effects on the ISS
Figure 1. Preflight and postflight Long Duration Exposure Facility M0001 Heavy Ions in Space experiment, indicating
atomic oxygen erosion and ultraviolet degradation.Preflight Postflight

8Determining how long ‑term exposure to space conditions impacts various
materials and, thus, which materials are best suited for spacecraft construction
can most effectively be accomplished through actual testing in space. Although
space environment effects testing can be conducted in ground ‑laboratory facilities,
ground facilities often do not accurately simulate the combined environmental effects and, therefore, do not always accurately simulate performance or degradation observed in the space environment. The aspects of the space environment section of this document discusses each aspect of the space environment and what ground simulation methods translate best to actual flight results. However, the synergism of all the elements of the space environment is difficult to duplicate on the ground. Therefore, actual spaceflight experiments provide the most accurate spacecraft durability data. Materials spaceflight experiments to evaluate the environmental durability of various materials and components in space have been conducted since the early 1970s, including 57 experiments on the Long Duration Exposure Facility (LDEF), which was retrieved in 1990 after spending 69 months in LEO (de Groh
et al., 2011). The ISS provides an ideal platform for long ‑term space environment
effects testing, particularly as experiments can be returned to Earth for postflight analyses. The Materials International Space Station Experiment (MISSE) is a series of materials flight experiments, the first two of which were delivered to the ISS Figure 2. Space-exposure damage to Hubble Space Telescope multilayer insulation.Large radiation-induced cracks in the
outer layer of multilayer insulation after 6.8 years of space exposure (Townsend et al., 1999).Severe degradation to the aluminized-Teflon
® outer layer of multilayer
insulation after 19 years of space exposure (Yang and de Groh, 2010).

9during STS ‑105 in 2001 (de Groh et al., 2008; de Groh et al., 2009; de Groh et al.,
2011). Consisting of a pair of trays hinged together like a suitcase (called a Passive
Experiment Container [PEC]) and containing an array of individual experiments,
the PEC is attached to the exterior of the ISS, providing long ‑duration exposure
to space conditions. In the MISSE suite (MISSEs 1 through 8), 10 PECs (and one smaller tray), together containing thousands of samples, have been flown in various external locations on the ISS. With participants from NASA, the Department of
Defense, industry, and academia, MISSE is the longest running multi ‑organization
technology, development and materials testing project on the ISS. It has provided many tangible benefits for the agency and its partners, with the flight data impacting many space programs. Like LDEF , MISSE flight data have provided a great wealth of space performance and environmental durability data and many lessons learned beneficial to further investigators (Banks et al., 2008). Published MISSE data, photographs and some raw data files are being gathered in a MISSE database in the Materials and Processes Technical Information System (MAPTIS).
All prospective experimenters should register for an account on MAPTIS, found at
http://maptis.nasa.gov/. MAPTIS contains a wealth of information for designers and materials engineers, particularly the Materials Selection Database. This is a useful reference to consult before building hardware so that safety, structural,
pressure vessel and line, fracture ‑critical and contamination requirements are met.
This database is open to all registered users and holds 50 years of analyzed results of tests conducted on metallic and nonmetallic materials:
• M etals data include analyzed results of tests relevant to corrosion, crack growth,
creep rupture, flammability, fluid compatibility, fracture mechanics, frictional
heat, high ‑cycle fatigue, low ‑cycle fatigue, mechanical impact, particle impact,
pneumatic impact, promoted ignition, stress corrosion, and tensile strength. A list of manufacturers is also provided.
• N onmetals data consist of test results, including flammability, fluid
compatibility, odor, outgassing (thermal vacuum stability), toxicity (offgassing) and vacuum condensable material compatibility with optics (VCMO).
Materials data relevant to spacecraft design may also be found in Silverman (1995).
This guidebook gathered many materials experiments’ results from the LDEF , short ‑
duration shuttle flights and selected ground simulations.

10Vacuum
The hard vacuum of space (10‑6 to 10‑9 torr) will cause outgassing, which is the
release of volatiles from materials. The outgassed molecules then deposit on line ‑
of‑sight surfaces and are more likely to deposit on cold surfaces. This molecular
contamination can affect optical properties of vehicle and payload surfaces and
spacecraft performance, particularly for sensitive optics. To mitigate this problem, the ISS has specified in NASA SSP 30426, Space Station External Contamination Control Requirements, what the limits are for molecular deposition, induced molecular column densities and the release of particulates.
An investigator must compile a list of all materials used in a flight experiment
and submit this list for a timely review. NASA maintains a database of test results from ASTM E1559, Standard Test Method for Contamination Outgassing Characteristics of Spacecraft Materials, and the older ASTM E595, Standard Test Method for Total Mass Loss and Collected Volatile Condensable Materials from Outgassing in a Vacuum Environment. Material identification, location, vacuum exposed surface area, operating temperature range and condensable outgassing rate data are used by the ISS Program’s return flux model to calculate any impact to the vehicle (Soares and Mikatarian, 2003). A material known to outgas should be thermal vacuum baked for a minimum of 24 hours at a temperature above that expected in orbit or, if that is not known, at 100 °C. Assemblies may be thermal vacuum baked prior to flight.
This is one component of the space environment that translates well between
ground simulation of 10
‑6 to 10‑9 torr vacuum and flight.
Atomic Oxygen
AO is produced when short ‑wavelength UV radiation reacts with molecular
oxygen in the upper atmosphere. It is the most significant component of the space environment at ISS altitude in terms of material degradation. AO oxidizes many metals, especially silver, copper, and osmium. AO reacts strongly with any material containing carbon, nitrogen, sulfur and hydrogen bonds, meaning that many polymers react and erode. Polymers containing fluorine, such as Teflon®, react synergistically, meaning that the reactivity to AO increases with longer exposure to UV radiation (Pippin et al., 2004). Even materials with AO protective coatings can degrade because of AO undercutting erosion at protective coating defect sites (Figure 3; Banks et al., 2004).Aspects of the Space
Environment

11The AO exposure, characterized by the fluence (atoms/cm2) to an experiment will
depend not only on the orientation and spacecraft altitude but also on the solar
activity at the time of flight. There can be an order of magnitude difference in AO flux between solar maximum (higher flux) and solar minimum (lower flux). The current solar cycle at time of publication, Solar Cycle 24, promises to be the least active cycle in the last hundred years (Hathaway, 2013). An experiment to determine AO reactivity, also known as erosion yield (cm
3/atom), of materials needs
an exposure that is long enough for measureable erosion to occur. Software such as the Mass Spectrometer Incoherent Scatter (MSIS) Model can be used to estimate the AO fluence for a particular mission, which is then used to determine if the experiment will receive a high enough level of AO for the desired measurements and also whether the sample thickness is sufficient if the expected fluence is high.
T ranslating ground simulation results to flight depends heavily on the source of
AO used in the laboratory. AO in orbit is ~5.2 ‑eV energy, principally as a result of
the ISS orbital velocity. Plasma ashers create AO but also produce heating, intense
Lyman ‑alpha UV radiation and a significant percentage of ions rather than just
neutral atoms. In addition, the arrival direction of AO may vary more than in
space. These differences may give erroneous results, particularly for polymers with low glass transition temperatures. Stambler (2011) compared ground simulation
to flight results for 40 different polymers, and the erosion yield in the plasma
asher was higher than that in space for every material. Thermal energy AO sources eliminate the heating problem but do not have the necessary energy to break some chemical bonds and may need a much higher fluence to replicate the same erosion in orbit.
AO beam facilities may use laser ‑detonation or microwave sources to generate AO
at energies close to that at ISS altitude. For polymers that do not contain fluorine, simulations in these facilities are generally close to flight, with the AO reactivity
Figure 3. Image shows atomic oxygen undercutting degradation of the solar array wing blanket box cover on the International
Space Station after one year of space exposure.

12being ±10 percent. Polymers with fluorine are more sensitive to the UV generated
simultaneously with the AO and consequently have a higher reactivity in the beam facility than observed in orbit.
In general, laboratory results are normalized to flight results by flying materials
with known reactivity to AO in addition to the test samples. Kapton® H and Kapton® HN polyimide are the most common materials selected for this purpose; polyethylene, polypropylene, and pyrolytic graphite have also been used. Following ASTM E2089, Standard Practices for Ground Laboratory Atomic Oxygen Interaction Evaluation of Materials for Space Applications, can reduce variability in results.
Ultraviolet Radiation
Earth’s atmosphere filters out most of the sun’s damaging light, but ISS materials bear the brunt of solar photon damage. While AO may bleach materials, UV generally darkens them (Figure 4), particularly in the presence of contamination.
UV radiation also damages polymers by either cross ‑linking (hardening) or chain
scission (weakening). UV under high vacuum can also create oxygen vacancies in oxides, leading to significant color changes.
Normalizing ground simulations to flight results is very dependent on the material
and the type of lamp used, whether deuterium, mercury, or mercury ‑xenon and
the intensity of the lamp (number of suns). Accelerated UV testing may also cause
material heating, so the accuracy of a simulation may depend on whether the sample temperature is controlled or not. Any UV exposure on the ground should be done
with the samples in vacuum. Also, any near ‑UV source such as a mercury ‑xenon
Figure 4. Preflight and postflight images of the Optical Properties Monitor shown with ultraviolet-darkened insulation
after nine months of exposure on the Mir Space Station.Preflight Postflight

13lamp that is not integrated into the vacuum system should illuminate the samples
through a UV ‑ grade window. For exposure of metal oxides, consider the ability
to make in ‑situ reflectance measurements after vacuum UV ground exposures, as
atmospheric oxygen has been observed to reverse the effects of oxygen vacancies.
Particulate or Ionizing Radiation
The three main sources of charged particle radiation naturally occurring in space
are galactic cosmic rays, solar proton events, and the trapped radiation belts. For most materials on the ISS, the effects of AO and UV can overshadow any effects by particulate radiation. Depending on the polymer, particulate radiation can result
in cross ‑linking or chain scission, similar to damage by UV, resulting in polymer
embrittlement. A greater effect is seen in avionics, namely single ‑event upsets,
bit errors and latchups. This can be mitigated by selecting avionics that are “rad hard” or by placing shielding around the electronics. Radiation effects may also
be alleviated by using error ‑correction circuitry and triple ‑module redundancy,
where two good process results “outvote” a corrupted one. Most of the particulate radiation dose to the ISS occurs when flying through the South Atlantic Anomaly (Figure 5) and is in the form of electrons, although proton dose can be significant for some materials and components.
Laboratory results can be normalized to flight results by understanding the dose ‑
depth profile of radiation for the maximum effect on that material. For example, radiation testing of a thermal control coating that is 3 to 5 mil thick could include
electrons and protons in the 40 ‑ to 700 ‑keV range. Particles in this energy range
would have the most effect on optical properties and coating chemistry, while higher energy particles would pass through the coating and affect the substrate.
Figure 5. Charged particle map shows the South Atlantic Anomaly. [Credit: S.L. Snowden, http://heasarc.gsfc.nasa.gov/
docs/rosat/gallery/misc_saad.html]

14Conversely, higher ‑energy particles (in the 1 ‑ to 70 ‑MeV range) have been used to
study single ‑event upsets (Swank et al., 2008), whereas the lower ‑energy particles
would not have much of an effect.
Plasma
Similar but separate from the higher energy particulate radiation is the space
plasma. The plasma environment around the ISS is composed of approximately equal amounts of positively charged oxygen ions (O+) and free electrons and varies with solar activity and altitude. Because of the differences in spacecraft velocities, ion thermal energy and electron thermal energy, electrons can impact any spacecraft surface, while ions can only impact ram (leading edge) surfaces. This can lead to a negative charge buildup, which can lead to ion sputtering, arcing and parasitic currents in solar arrays, as well as reattraction of contamination (James et al., 1994).
Examples of experiments that would be affected by the plasma environment would
be high ‑voltage solar arrays and conductive coatings designed to bleed off static
charge on a spacecraft. A principal investigator for such an experiment would need
to work in conjunction with the Spacecraft Charging Assessment Team at NASA’s Johnson Space Center (JSC). Specific information about the plasma environment around the ISS can be provided through operation of the Floating Potential Measurement Unit. ISS plasma conditions may be modeled in the laboratory with
a hollow cathode plasma source to create a low ‑density (106/cm3), low ‑temperature
(≤1‑eV electron temperature) plasma. Argon is often used, but some sources may
use xenon, oxygen or helium.
Temperature Extremes and Thermal Cycling (Coefficients of
Thermal Expansion [CTE] Mismatch)
As the ISS moves in and out of sunlight during its orbit around Earth, the degree
to which a material experiences thermal cycling temperature extremes depends on
its thermo ‑optical properties (solar absorptance and thermal emittance), its view of
the sun, its view of Earth, its view of other surfaces of the spacecraft, durations of
time in sunlight and in shadow, its thermal mass and the influence of equipment or components that produce heat (Dever et al., 2005). A rule of thumb for these
cyclic temperature variations is ‑120 °C to +120 °C, but high solar absorptance with
low infrared emittance will contribute to greater temperature swings. Large areas of material with poor thermal properties may not be allowed on the ISS because of exceeding touch temperature limits for the astronauts’ gloves.

15Protective coatings may degrade in the ISS environment if there is a mismatch in
CTE between the coating and the substrate. Sixteen thermal cycles a day (the ISS orbits Earth approximately once every 92 minutes) may lead to cracking, peeling, spalling or formation of pinholes in the coating, which then allows AO to attack the underlying material (Figure 6).
Micrometeoroid/Orbital Debris Impact
All areas of a spacecraft may be impacted by micrometeoroids traveling as fast as 60 km/s. Surfaces facing the ram direction are more likely than those in the wake direction to be hit with space debris, traveling at an average velocity of
10 km/s. Space debris varies with the solar cycle: as the Sun’s activity increases, the
atmosphere heats up, increasing the drag on space debris in orbit. Large space debris is tracked so that the ISS can perform avoidance maneuvers, but there is no current way to avoid small debris impacts. Most of the impacts on returned experiments
have been small, creating ≤0.5 ‑mm diameter craters. The first two Materials
International Space Station Experiments (MISSE ‑1 and MISSE ‑2) averaged less
than two impacts/ft2/year (Pippin 2006), with a much smaller shielding factor
from the then ‑incomplete ISS structure. As more space debris is added to the
Figure 6. Postflight photograph displays thin film samples from the Materials International Space Station Experiment-4
with catastrophic failure of both coatings related to combined thermal cycling and atomic oxygen erosion.

16environment, however, the impact risk changes. For example, the deliberate
fragmentation of the Fengyun 1 ‑C spacecraft in 2007 and the collision between the
Iridium 33 and Cosmos 2251 satellites in 2009 increased the trackable space debris
by 60 percent. As a result of these two events, the number of untrackable particles may have increased by 250,000 or more (Orbital Debris Quarterly News, 2010).
Micrometeoroid or space debris impacts on an experiment may crater the material,
spall off a coating (Figure 7) or short out a solar cell. It would be difficult to shield an experiment from impacts and still have it exposed to the rest of the space environment, but the debris environment (at time of publication) is relatively benign as it typically affects a very small area of exposure. By the same token, if an experiment will be testing various space debris shielding designs, it needs a large, unshielded area in space for a long time. Laboratory testing is usually conducted with slower velocities (<8 km/s) than those found in orbit, so it may not model vaporization, spalling or penetration accurately. Analysis tools such as the Smooth Particle Hydrodynamic Code are available and used to predict impact effects. These tools have been verified only to the velocity limit of current ground test facilities.
Figure 7 . A micrometeoroid or orbital debris impact results in a 0.6-mm diameter crater and approximately 3-mm
diameter spall (loss of the coating). 2.54 cm diameter Tiodize coating on titanium flown on the Long Duration Exposure Facility A01 71 experiment.

17The orientation of materials experiments are typically in the ram, wake, zenith and/
or nadir directions. Ram refers to the velocity vector of the vehicle and has the greatest fluence of AO. Zenith, which points into space in the opposite direction of Earth, has the most solar illumination. Wake and nadir are the opposing faces of ram and zenith, respectively. The wake direction is good for studying UV effects with typically an order of magnitude less AO as the ram direction, and
some experimenters may wish to fly duplicate samples (ram ‑ and wake ‑facing) to
differentiate between AO and UV effects. A nadir orientation is desired for Earth ‑
viewing experiments.
Note that the wake direction does not mean “no AO.” During a nominal orbit, the
ISS currently flies in what is called a local vertical, local horizontal (LVLH) frame,
with the X ‑axis in the velocity vector (+XVV; Figure 8, NASA SSP 50699 ‑03, ISS
Certification Baseline Volume 3: Flight Attitudes). Pitch, yaw and roll are all held
at zero, so the pressurized mating adapter 2 (PMA ‑2) always faces exactly forward
along the velocity vector. During Soyuz and Progress dockings and undockings, the
ISS may be pitched ‑90° so PMA ‑2 faces exactly nadir and, during this orientation,
wake surfaces can receive AO flux. Orientation and
Location on the ISS
Figure 8. +XVV Z nadir flight attitude.

18Contamination in both molecular and particulate form can compromise numerous
types of experiments (materials, optical devices, etc.), as well as affect line ‑of‑sight
surfaces on the ISS. As mentioned earlier, the ISS has specified in NASA SSP 30426
what the limits are for molecular deposition, induced molecular column densities and the release of particulates. The MAPTIS database for thermal vacuum stability (TVS) may assist in choosing materials with low outgassing rates.
If there is no substitute for a higher outgassing material, a thermal vacuum bakeout
may be performed during assembly to meet ISS outgassing requirements. The bakeout should be at a higher temperature than expected in orbit, in a vacuum of 10
‑6 torr or better and for at least 24 hours or until a temperature ‑controlled quartz
crystal microbalance (TQCM) in the vacuum chamber indicates no more evolving
material. Silicone materials that have not been vacuum ‑baked can frequently
contain short chain molecules that are volatile and readily transported onto neighboring surfaces. When these contaminated spacecraft surfaces are exposed to AO in LEO, the silicones oxidize to form silica (or silicates). Hydrocarbons can also be trapped on the surface during this process. The resulting deposit can form
an AO ‑protective coating that can darken as a result of further solar radiation
exposure. This contamination can also skew erosion yield measurements, increase solar absorptance and irreparably damage optical materials. One such case was Approaches to Mitigate
Contamination
Figure 9. Postflight photograph shows an room temperature vulcanization sample from the Long Duration Exposure Facility
A0171 experiment with deposited silicone contaminant on baseplate and sample. Also note oxidized silver fastener.

19the room temperature vulcanization (RTV) 511 samples of an LDEF experiment
(Figure 9). The sheet of RTV was baked out for a short time, which was inadequate, and then the samples were cut out of the sheet, exposing fresh material. The holes drilled for fastening also exposed new material, with outgassed deposits seen in rings on top of the sample.
Along with thermal vacuum bakeout and proper materials selection, another
approach to mitigate contamination is to be aware of line ‑of‑sight to sensitive
optics and to design vent paths accordingly. If purges or dumps are necessary to
an experiment, they must not cause any damage to the ISS surfaces from either direct or subsequent orbital impingement. NASA SSP 30426 also specifies that the
limit on particulate generation from an experiment is to be 1 particle (≥100 ‑µm
diameter) per orbit per 1×10–5 steradian field of view as seen by a 1 ‑m diameter
aperture telescope. This particulate generation requirement also applies to moving parts and vents.

20Plan for Flight Recovery Contingencies
The biggest lesson learned for passive experiments is that, historically, few materials
experiments have been returned to Earth after exactly the time planned. The LDEF
was planned for a 9 ‑ to 12 ‑month mission; the Challenger accident left it in orbit
for 5.8 years. MISSEs ‑1 and ‑2 were expected to fly for one year; the Columbia
accident extended that to nearly four years. Planning for every contingency may not be possible, but samples should be chosen to provide the needed science, even if return is significantly delayed.
Control Samples and Preflight Testing
The second biggest lesson learned is to perform as much preflight analyses as possible on duplicate sets of flight and control samples. It may not be possible to have a control sample for every flight sample, but there should be at least one control sample retained for each material, orientation and surface treatment, etc. The control samples should be maintained appropriately during the experiment flight, e.g., bagged in nitrogen or held in a desiccator out of direct sunlight. Many polymers, such as Kapton®, are hygroscopic (absorbing up to two percent of their weight in moisture) and can fluctuate in mass with humidity and temperature. Therefore, for accurate mass loss measurements to be obtained, it is necessary that the samples be fully dehydrated immediately before measuring the mass
both Preflight and postflight. Ideally, this is done by dehydrating the samples
in a vacuum desiccator maintained at a pressure of ≤13.3 Pa (≤100 mtorr)
with a mechanical roughing pump for a minimum of 72 hours. Four days are
recommended. Samples should be removed one at a time and the desiccator
pumped back down after a sample is removed to keep other samples under
vacuum. Records should be kept of the following: the sequence of sample weighing,
the number of samples in each set (if a multilayered sample), the time under vacuum before weighing, the temperature and humidity in the room, the time air was let into the desiccator and the time a sample was taken out of the desiccator, the time of each weighing (with a minimum of three measurements taken as
quickly as possible) and the mass. T ypically, the measurements are averaged, or
they can be back ‑extrapolated to time zero (when air is first introduced into the
desiccator). A balance with at least 0.01‑mg readability is needed. A faster method is to place one sample at a time in a vacuum desiccator and pump down to a pressure
of exactly 6.67 Pa (50 mtorr). When 6.67 P a is reached, the timer is started at the
same moment the chamber is vented. The sample is quickly removed from the
chamber and placed on the balance. Mass measurements are taken every 30 seconds Lessons Learned

21for 5 minutes; then regression analysis is used to calculate the mass at time zero.
This method should be used only with a small vacuum chamber that can be vented
quickly and opened easily. The same procedure and sequence should be repeated
with the same samples postflight.
In addition to dehydrated mass measurements, some suggested preflight analyses
include normal and black ‑light photography, thickness measurements for erosion
yield calculations, surface roughness, bi ‑directional reflectance distribution function
(BRDF), transmission, ellipsometry, solar absorptance, infrared emittance, electrical
conductivity and solar cell current ‑voltage curves. These non ‑destructive tests can
then be repeated postflight, minimizing any uncertainties related to equipment
calibration or even use of different equipment after flight. Experiments that are not well planned or that occur at the last minute risk yielding poor data, so designs, materials selections and analyses should be completed well in advance of experiment integration activities.
Understand Sample Geometry
The geometry of sample holders can influence the flux of AO. Commonly used passive Evaluation of Oxygen Interaction with Materials (EOIM)/MISSE sample trays have chamfered circular apertures that allow AO to scatter from the chamfered surfaces onto the samples, thus locally increasing the flux impacting the samples, as
shown in Figure 10 (Banks et al., 2008). A consequence of the perimeter ‑scattered
AO is that the erosion around the sample perimeter is greater than in the central area. If the AO is arriving off normal, then there will be a variation in flux around the perimeter of each sample, depending on the scattering geometry. As can be
seen in Figure 11 (de Groh et al., 2008; Banks et al., 2008), two MISSE ‑2 samples
peeled up from their lower left edges, and AO was found to be arriving at 8° from
normal and coming from the upper right direction. Thus, there appears to be a flux concentration near the perimeter of the samples from the AO that was deflected off the chamfered surface.
For the MISSE ‑2 trays with circular
2.54‑cm‑diameter samples, the chamfer
was at 45o, and the lip was 0.763 mm
thick. The maximum possible additional
fluence for 2.54 ‑cm‑diameter samples Figure 10. Flux concentration from chamfered Evalution
of Oxygen Interaction with Materials/Materials Interna –
tional Space Station Experiment sample holders.

22caused by AO scattering would be about15 percent but is more likely around 3.3
percent. Therefore, the concern is not of a higher average fluence but rather of sample peeling and potential release before full sample erosion, which could lead to incorrect erosion yields.
The problem of flux concentration and premature peeling could be eliminated if a
reverse chamfer were used on the sample holders, which would not allow scattering of AO onto the surface of the samples. A potential disadvantage of this would be the loss of intimate contact at the edge of the sample for profiling purposes, but this would not be a concern for mass loss measurements.
Other Lessons Learned
Written instructions and procedures used for mounting and assembly of spaceflight hardware are almost always necessary to properly integrate an experiment as specified by quality assurance and flight documentation requirements. This step
Figure 11. The Materials International Space Station Experiment-2 Polymer Erosion and Contamination
Experiment tray is seen with samples peeling up on their lower-left sides.

23occasionally is glossed over by those tasked with final installation. Be clear about
experiment or sample orientation (“this side faces space”) and properly label in red any “REMOVE BEFORE FLIGHT” covers.
Another lesson learned is that an experiment should be able to withstand the
corrosive salt environment of Cape Canaveral or the Mid ‑Atlantic Regional
Spaceport while waiting for launch. The experiment should also be able to
withstand the power being off, both on the ground and in space.
Some materials should not be flown in LEO. NASA ‑STD ‑6012, Corrosion
Protection For Space Flight Hardware, section 4.6.2, states that cadmium plating and zinc plating shall not be used because of contamination concerns. Silver and osmium react strongly with AO and should not be used without a protective coating.
Some commercial off ‑the‑shelf electronics may use “lead ‑free” or pure tin
components and soldering. This may lead to tin pest (tin plague) or tin whisker growth in orbit, potentially adversely affecting the electronics through the release of conductive particulate.
More lessons learned can be found in Banks et al. (2008) and on the NASA Lessons
Learned database located at http://llis.nasa.gov/llis/search/home.jsp.

24The current external sites on the ISS for research include:
• Columbus E xternal Payload Facility (EPF) (European Space Agency [ESA])
• EXpedite the PR ocessing of Experiments to the Space Station (EXPRESS)
Logistics Carrier (ELC [NASA])
• J apanese Experiment Module (JEM) External Facility (JEM EF) (Japan
Aerospace Exploration Agency [JAXA])
• JEM S mall Satellite Orbital Deployer (J ‑ SSOD [JAXA])
• U niversal workstations with capabilities for re ‑ equipping (URM ‑ Ds), biaxial
pointing platforms, magnetomechanical anchors/locks and portable working
platform (Roscosmos).
More information about these facilities can be found in the section on ISS External Accomodations.
An experiment setup will depend on what the principal investigator wants to
study. Issues to consider include: whether the experiment needs to be returned to Earth for analysis; if a power source and data downlink are required, i.e., for active experiments, such as testing solar cells; can the experiment be robotically deployed through the JEM airlock? Spacewalks will be limited in the future, so deployment by an astronaut might not be possible. Which environment is better suited for the experiment: ram for the most AO; zenith for the most UV radiation; wake for
UV and little AO; nadir for Earth ‑observing? How sensitive is the experiment to
contamination? Table 1 shows the large variation in silica ‑based contamination on
surfaces from experiments placed at different locations on the ISS (Dever et al.,
2006; Steagall et al., 2008). The ram ‑facing surface of MISSE ‑2 had two orders
of magnitude less contaminant thickness than the three JAXA experiment units attached to the Russian Service Module. This is probably related to differences in the total arrival of silicones based on each experiment’s respective view of, and distance from, contaminant sources on the ISS.
Care must be taken to avoid self ‑contamination of the experiment, as well as to
ensure that the experiment is out of the view of sources of silicone to be sure that AO does not produce silica deposits that can affect erosion yields or cause changes in solar absorptance.Developing and Flying
Research to the ISS

25Location Contaminant thickness (nm) Duration of exposure (yr) Contaminant thickness/
year (nm)
MISSE-2, Tray 1:
Ram facing1.3 – 1.4 3.95 0.326 – 0.351
JAXA:Unit 1, Ram facingUnit 2, Ram facingUnit 3, Ram facing30.0
75.093.50.8632.373.8434.831.724.3
Table 1. Silica-Based Contamination on International Space Station Experiment Surfaces.
The experiment will need to be strong enough to survive the launch loads but not
overdesigned with excess weight. Vibration and shock tests must be performed on the flight hardware, with the test levels dependent on the launch vehicle. Hardware
must pass sharp ‑edge inspection to ensure the hardware poses no snagging danger
to a gloved and/or tethered astronaut on an Extravehicular Activity (EVA). Active experiments will have to meet electromagnetic interference/electromagnetic compatibility (EMI/EMC) and grounding requirements so as not to interfere with the avionics and communications on the ISS. In addition, experiments will need to
undergo a thermal ‑vacuum bake ‑out prior to flight.
Experiments should have adequate internal data storage capacity, as no data storage capacity is available from the ISS. Some compression within the experiment may be needed for transmission of high volumes of data.
Pictures taken at various time intervals throughout the duration of the experiment
can also provide valuable information as to experiment function and material
degradation. For example, images taken of MISSE ‑1 and MISSE ‑2 experiments
showed deterioration of certain samples early in the mission and years before the experiment was retrieved. In Figure 12, near the center, the Dyneema tether has failed in tension, as has the dielectric foam sample
above and to the right. T o the right
of the tethers experiment, one sample of Kapton® has already eroded away, while the adjacent sample of Kapton® with aluminum acetylacetonate is still
intact. Along the right edge, part of
a beta cloth experiment has already
turned brown. This was with only a
little more than 6 months’ exposure,
and MISSE ‑2 would stay in orbit for
nearly four years.Figure 12. Image shows sample deterioration on Materials
International Space Station Experiment-2 after six months
in orbit.

26This section gives an overview of existing ISS External Facilities (EF) that are
multidisciplinary in nature (Figure 13), provide access to multiple sites that are exposed to the space environment and include structural attachment points and utility interfaces.
Japanese Experiment Module Exposed Facility
(Japan Aerospace Exploration Agency [JAXA])
The JEM Exposed Facility (EF) is an unpressurized, multipurpose pallet structure
attached to the JEM, or “Kibo,” meaning “hope” in Japanese (Figure 14). This external platform is used for research in the areas of communications, space science, engineering, technology demonstration, materials processing and Earth observation. Experiments can be monitored by six video cameras, two located on the JEM EF , two located externally on the JEM Pressurized Module and two on the JEM Remote Manipulator System (RMS).
The JEM EF is accessible from the internal pressurized volume of the ISS via the
JEM Airlock. Articles interfacing with this structure are grappled and moved using the JEM Remote Manipulator System (RMS). The JEM EF is roughly 5.7 m x 5.0 m x 3.8 m, weighs approximately 4,000 kg, and includes utilities at each of the 12 attachment sites (Figure 13). The JEM EF specification and available resources are listed below:ISS External
Accommodations
Figure 13. Kibo Exposed Facility. The yellow and black numbers show the payload attach points.

27• M ass: 500 kg (10 standard sites, mass includes payload interface unit [PIU]);
2,500 kg (two heavy sites, mass includes PIU)
• Size: 1.85 m x 1 m x 0.8 m
• Power: 3 kW or 6kW for each payload, and 11kW max in total, 120 VDC• Thermal: Active thermal control (fluid loop)
• D ata: Low Rate – 1 mbps MIL ‑ STD ‑ 1553; High Rate – 43 mbps (shared);
Ethernet – 100Base ‑TX. Downlink and uplink are available through NASA
communication system or the Japanese Inter ‑orbit Communication System(ICS).
Multi-Purpose Experiment Platform (MPEP [JAXA])
Multi ‑Purpose Experiment Platform (MPEP) (Figure 15) is available for the
medium ‑sized space ‑exposed experiment, which aims for the monitor of space
environment for Earth observation. MPEP accommodates up to a 100 kg
experiment, and it provides the appropriate attitude and position for payloads by the support of JEM RMS. Available resources for payloads on MPEP are power, communication and video interface.
One of the applications includes the JEM Small Satellite Orbital Deployer
(J‑SSOD) in the next section.
Figure 14. Multi-Purpose Experiment Platform installed on the Japanese Experiment Module Slide Table.

28JEM Small Satellite Orbital Deployer (J-SSOD [JAXA])
The J ‑SSOD (Figure 15) holds up to three small one ‑unit (1U; 10 cm x 10 cm x 10
cm) CubeSats per satellite ‑install case (six total), though other sizes (up to 55 cm x
55 cm x 35 cm) can be used from 2015 (Figure 16). Weight limit is 1.33 kg per 1U,
8 kg total. Crew members unpack and install the satellite ‑install case onto the Multi ‑
Purpose Experiment Platform (MPEP), which is on the JEM Slide Table. The small
satellites are then transferred out through the JEM Airlock and deployed by the JEM RMS. Nine satellites were successfully deployed in two missions since 2012.
EXPRESS Logistics Carrier (NASA)
The ELC is a pallet designed to support external research hardware and store external spares (Orbital Replacement Units [ORUs]) needed over the life of the ISS. Currently, four ELCs are mounted to ISS trusses, providing unique vantage points for space, technology and Earth observation investigations. T wo ELCs are attached to the integrated truss segments starboard truss 3 (ITS‑S3) and two ELCs to the
integrated truss segments port truss 3 (ITS ‑P3). By attaching at the S3/P3 sites,
a variety of views such as zenith (deep space) or nadir (Earthward) direction with a combination of ram (forward) or wake (aft) pointing allows for many possible viewing opportunities. The ELC Adapter capabilities are listed below:
• M ass: 227 kg (8 sites across four ELCs; not including adaptor plate)
• Volume: 1.2 m3
• Size: 0.8 m x 1.2 m x 1.2 m
• Power: 750 W, 113 ‑126 VDC; 500 W, 28 VDC
• D ata: Low Rate: 1 Mbps MIL ‑ STD ‑ 1553 Medium Rate: 6 Mbps (shared)Figure 15. The Japanese Experiment Module Small
Satellite Orbital Deployer (J-SSOD).Figure 16. CubeSats deployed from the J-SSOD and photographed against an ISS solar array background.

29MISSE ‑7, consisting of PECs, called MISSE ‑7A and MISSE ‑7B and later MISSE ‑8,
were located on ELC 2, Site 3, as shown in Figure 17. MISSE ‑7A was flown in
a zenith/ram orientation, and MISSE ‑7B was flown in a ram/wake orientation.
MISSE ‑8, along with a small passive sample tray called the Optical Reflector
Materials Experiment III (ORMatE III), were deployed in the same location as
MISSE ‑7A and ‑7B, respectively, (Figure 18). MISSEs 1 through 5, 6A and 6B were
located in various other (non ‑permanent) external locations on the ISS.
Figure 17 a. Materials International Space Station Experiment-7 on EXPRESS Logistics Carrier 2, Site 3 shortly after
deploy during STS-129 in November 2009.
Figure 17 b. Photo of the zenith facing surface of Materials International Space Station Experiment (MISSE) 7A (left) and the ram facing surface of MISSE-7B (right) during STS-130 in February 2010.

30Figure 18 b. Materials International Space Station Experiment-8 (left) and ORMatE III (lower center) on EXPRESS Logistics
Carrier 2, Site 3. Images in both 18a & 18b were taken in July 2011 during STS-135.
Figure 18 a. Closeup of the zenith-facing surface of Materials International Space Station Experiment-8.

31
Figure 19. European Space Agency Columbus External Payload Facility.External
Payload
FacilityColumbus External Payload Facility (European Space Agency)
The EPF (Figure 19) has four powered external attachment site locations for scientific
payloads or facilities. To date, the EPF has been used by ESA and NASA. Each of the four attachment sites may hold a mass of up to 290 kg, and each is provided utility connections for power and data. The EPF capabilities are listed below:
• M ass: ≤ 290 kg per site (4 sites; uses Columbus External Payload Adapter
[CEPA])
• Volume: 1.39 m3
• Size: 0.864 m x 1.168 m x 1.375 m
• P ower: 1,250 W (total limited to 2,500 W for all four external payloads), each
external facility is connected to 2 – 120 VDC power feeds. Note: equipment can only be radiatively passively cooled.
• D ata: Low Rate: up to 100 Mbps

32Russian Segment External Facilities (Russian Federal
Space Agency)
Russian Segment External Facilities [Roscosmos] consists of a whole host of
multi ‑user external Facility interface locations and support structures. There are
two external mounting platforms (URM ‑D) on the Service Modulus (SM), also
known as Zvezda, located on the starboard and port sides. The URM ‑D provides
power and data connection to the payloads. Passive experiments can be flown in
the Replaceable Cassette ‑Container (SKK or CKK) and can be attached to Zvezda,
the Poisk MRM, or the Pirs Docking Compartment ‑1 (Figure 20). Payloads are
installed and removed by the crew during an EVA.Figure 20. Russian Replaceable Cassette-Container on the Russian Service Module.

33NASA and the National Science Foundation fund a variety of research efforts
through grants, fellowships, contracts, interagency transfers and cooperative agreements. The NASA Solicitation and Proposal Integrated Review and Evaluation System (NSPIRES; http://nspires.nasaprs.com/) lists the solicitations and research opportunities. A guidebook for responding to NASA Research Announcements (http://www.hq.nasa.gov/office/procurement/nraguidebook/) guides the reader through notice of intent to propose, preparation of proposals, conduct of the research itself and the sharing of new knowledge through publications, public outreach and education. Research proposals are peer reviewed and should meet national research objectives.
NASA receives thousands of research proposals every year and may only fund a
limited number. However, in accordance with Federal statutes and NASA policy, no eligible applicant is to be excluded from participation or be denied the benefits of or be subjected to discrimination under any program or activity receiving financial assistance from NASA on the grounds of race, color, creed, age, sex, national origin or disability. Proposals from all qualified sources are welcome. Historically Black Colleges and Universities (HBCUs), Other Minority Universities (OMUs), small
disadvantaged businesses (SDBs), veteran ‑owned small businesses (VOSBs), service ‑
disabled veteran ‑owned small businesses (SDVOSBs), Historically Underutilized
Business Zone (HUBZone) small businesses and women ‑owned small businesses
(WOSBs) are encouraged to submit proposals. Funding Opportunities

34ASTM E595, Standard Test Method for Total Mass Loss and Collected Volatile
Condensable Materials from Outgassing in a Vacuum Environment.
ASTM E1559, Standard Test Method for Contamination Outgassing
Characteristics of Spacecraft Materials.
ASTM E2089, Standard Practices for Ground Laboratory Atomic Oxygen
Interaction Evaluation of Materials for Space Applications.
Banks, B. A., K. K. de Groh, and S. K. Miller. “Low Earth Orbital Atomic
Oxygen Interactions with Spacecraft Materials.” 2004 Materials Research Society
Fall Meeting, Boston, MA, November 29 ‑December 3, 2004, Materials Research
Society Symposium Proceedings 2004, NN8.1. New York: Cambridge University
Press, 2004. Also published as NASA/TM ‑2004 ‑213400 (Nov. 2004).
Banks, B. A., K. K. de Groh, S. K. Miller, and D. L., Waters. “Lessons Learned from Atomic Oxygen Interaction with Spacecraft Materials in Low Earth Orbit.” Proceedings of the 9th International Conference: Protection of Materials and Structures from Space Environment, Toronto, Canada, 20–23 May 2008. Melville,
NY: American Institute of Physics. Also published as NASA/TM ‑2008 ‑0215264,
July 2008.
de Groh, K. K., B. A. Banks, C. E. McCarthy, R. N. Rucker,, L. M. Roberts, and
L. A. Berger. “MISSE ‑2 PEACE Polymers Atomic Oxygen Erosion Experiment on
the International Space Station.” High Performance Polymers 20 (2008): 388 ‑409.
de Groh, K. K., D. A. Jaworske, W. H. Kinard, H. G. Pippin, and P . P . Jenkins.
“Tough Enough for Space: Testing Spacecraft Materials on the ISS.” Technology
Innovation 15, no. 4 (2011): 50 ‑53.
de Groh, K. K., B. A. Banks, J. A. Dever, D. J. Jaworske, S. K. Miller, E. A Sechkar, and S. R. Panko. “NASA Glenn Research Center’s Materials International Space
Station Experiments (MISSE 1 ‑7).” Proceedings of the International Symposium on
“SM/MPAC&SEED Experiment,” Tsukuba, Japan, March 10 ‑11, 2008. JAXA ‑SP‑
08‑015E, March 2009, pp. 91 – 119. Also published as NASA TM ‑2008 ‑215482,
December 2008.
Dever, J. A., B. A. Banks, K. K. de Groh, and S. K. Miller. “Degradation of Spacecraft Materials.” In Handbook of Environmental Degradation of Materials,
edited by Myer Kutz, 465 ‑501. Norwich, NY: William Andrew Publishing, 2005. Citations

35Dever, J. A., S. K. Miller, E. A. Sechkar, and T. N. Wittberg. “Preliminary
Analysis of Polymer Film Thermal Control and Gossamer Materials Experiments
on MISSE ‑1 and MISSE ‑2,” Proceedings of the 2006 National Space & Missile
Materials Symposium in conjunction with the 2006 MISSE Post ‑Retrieval
Conference, June 26 ‑30, 2006, Orlando, FL.
Hathaway, David H. “Solar Cycle Prediction.” http://solarscience.msfc.nasa.gov/predict.shtml (accessed April 30, 2013).
NASA SSP 30426, Space Station External Contamination Control Requirements.
NASA SSP 50699 ‑03. ISS Certification Baseline Volume 3: Flight Attitudes
James, Bonnie F ., O. W. Norton, and Margaret B. Alexander. “The natural space
environment: Effects on spacecraft.” NASA STI/Recon Technical Report N 95 (1994): 25875.
Pippin, H. G., E. Normand, S. L. B. Woll, and R. Kamenetzky. “Analysis of
Metallized Teflon™ Thin ‑Film Materials Performance on Satellites.” Journal of
Spacecraft and Rockets 41, no. 3 (May 2004): 322 ‑325.
Pippin, Gary. Summary Status of MISSE ‑1 and MISSE ‑2 Experiments and Details
of Estimated Environmental Exposures for MISSE ‑1 and MISSE ‑2, AFRL ‑ML‑
WP‑TR‑2006 ‑4237, Air Force Research Laboratory: OH July 2006.
Schwank, James R., Marty R. Shaneyfelt, and Paul E. Dodd. “Radiation Hardness
Assurance Testing of Microelectronic Devices and Integrated Circuits: Radiation Environments, Physical Mechanisms, and Foundations for Hardness Assurance.”
Sandia National Laboratories Document SAND ‑2008 ‑6851P . 21 May 2013. http://
www.sandia.gov/mstc/services/documents/Sandia_RHA_Foundations_FINAL.pdf.
Silverman, E. M. Space Environmental Effects on Spacecraft: LEO Materials
Selection Guide. NASA CR 4661, Part 1, TRW Space & Electronics Group: Redondo Beach, CA. August 1995.
Soares, C. and R. Mikatarian. “Understanding and Control of External
Contamination on the International Space Station.” ESA SP ‑540 Proceedings of the
9th International Symposium on Materials in a Space Environment, June 16 ‑20.
2003, Noordwijk, The Netherlands. Noordwijk: ESA. September 2003.

36Stambler, A. H., K. E. Inoshita, L. M. Roberts, C. E. Barbagallo, K. K. de Groh,
and B. A. Banks. “Ground ‑Laboratory to In ‑Space Atomic Oxygen Correlation for
the PEACE Polymers.” Proceedings of the 9th International Conference Protection
of Materials and Structures from Space Environment, May 19 ‑23, 2008, Toronto,
Canada. Ed. J .I. Kleiman, AIP Conference Proceedings 1087, pp. 51 ‑66, 2009.
Also NASA TM ‑2011 ‑216904..
Steagall, C., K. Smith, A. Huang, C. Soares, and R. Mikatarian, “Induced
Contamination Predictions for JAXA’s Micro ‑Particles Capturer and Space
Environment Exposure Devices,” Proc. Int. Symp. on SM/MPAC&SEED
Experiment, Japan, 2008 (JAXA ‑SP‑08‑015E, 2009), pp. 19 ‑25.
Townsend, J. A, P . A, Hansen, M. W. McClendon, K. K. de Groh, and B. A, Banks.
“Ground ‑Based Testing of Replacement Thermal Control Materials for the Hubble
Space Telescope” High Performance Polymers 11 (1999): 63 ‑79.
“Update on Three Major Debris Clouds.” Orbital Debris Quarterly News 14. 2
(April 2010). 14 May 2013 <http://orbitaldebris.jsc.nasa.gov/newsletter/pdfs/ODQNv14i2.pdf>.
Visentine, J., W. Kinard, R. Pinkerton, D. Brinker, D. Scheiman, B. Banks, J.
Zwiener, K. Albyn, T. Farrell, S. Hornung, and T. See. “Mir Solar Array Return
Experiment”, AIAA Paper 99 ‑0100 presented at the 37th AIAA Aerospace Sciences
Meeting, Reno, NV, Jan. 11 ‑14, 1999.
Yang, J. C. and K. K. de Groh. “Materials Issues in the Space Environment.” MRS
Bulletin 35 (January 2010): 12 ‑19.

37AO Atomic Oxygen
BRDF Bi-Directional Reflectance Distribution Function
CEPA Columbus External Payload Adapter
CKK Replaceable Cassette-Container
CTE Coefficients of Thermal Expansion
EF External Facility
ELC EXPRESS Logistics Carrier
EMI/EMC Electromagnetic Interference/Electromagnetic Compatibility
EOIM Evaluation of Oxygen Interaction with Materials
EPF External Payload Facility
ESA European Space Agency
EVA Extravehicular Activity
EXPRESS EXpedite the PRocessing of Experiments to the Space Station
HBCUs Historically Black Colleges and Universities
HUBZone Historically Underutilized Business Zone
ISS International Space Station
ITS-S3 Integrated T russ Segments Starboard Truss 3
ITS-P3 Integrated T russ Segments Port Truss 3
JAXA Japan Aerospace Exploration Agency
JEM Japanese Experiment Module
J-SSOD JEM Small Satellite Orbital Deployer
LDEF Long Duration Exposure Facility
LEO Low-Earth Orbit
LVLH Local V ertical, Local Horizontal
MAPTIS Materials and Processes T echnical Information System
MISSE Materials International Space Station Experiment
MMOD Micrometeoroids and Orbital Debris
MPEP Multi-purpose Experiment Platform
MRM2 Mini Research Module 2
MSIS Mass Spectrometer Incoherent Scatter
NSPIRES NASA Solicitation and Proposal Integrated Review and Evaluation System
OMUs Other Minority Universities
PEACE Polymer Erosion and Contamination Experiment
PEC Passive Experiment Container
PIU Payload Interference Unit
PMA-2 Pressurized Mating Adapter 2
RMS Remote Manipulator System
Roscosmos Russian Federal Space Agency
RTV Room T emperature Vulcanization
SDBs Small Disadvantaged Businesses
SDVOSBs Ser vice-Disabled Verteran-Owned Small Businesses
SKK Replaceable Cassette-Container
TQCM T emperature-Controlled Quartz Crystal Microbalance
TVS Thermal V acuum Stability
URM-Ds Universal W orkstations with Capabilities for Re-Equipping
UV Ultraviolet
VCMO V acuum Condensable Material Compatibility with Optics
WOSBs W omen-Owned Small Businesses
+XVV X-axis in the V elocity VectorAcronyms

38
The Complete ISS Researcher’s
Guide Series
1. A cceleration Environment
2. C ellular Biology
3. C ombustion Science
4. E arth Observations
5. Fl uid Physics
6. F ruit Fly Research
7 . F undamental Physics
8. Hu man Research
9. M acromolecular Crystal Growth
10. Mi crobial Research
11. M icrogravity Materials Research
12. P lant Science
13. R odent Research
14. S pace Environmental Effects
15. T echnology Demonstration
38

39
For more information…
Space Station Science
http://www.nasa.gov/iss-science
Facilities
http://www.nasa.gov/mission_pages/station/research/facilities_category.html
ISS Interactive Reference Guide:
http://www.nasa.gov/externalflash/ISSRG/index.htm
Researchers/Opportunities
http://www.nasa.gov/mission_pages/station/research/ops/research_information.html
ISS Research Customer Helpline
JSC-ISS-research-helpline@mail.nasa.gov281-244-6187
39

40
National Aeronautics and Space Administration
Johnson Space Center
http://www.nasa.gov/centers/johnson
www.nasa.gov
NP-2015-03-015-JSC