Shielding against radiation is considered a very difficult task. For example, a proton or alpha particle cosmic ray of "medium" energy can pass through more than a meter of aluminium, not counting the effects of secondary radiation. With this in mind, it is clear that any Martian colonists would have to take a holistic approach, reducing their radiation exposure at every possible opportunity through shielding and risk-mitigating behaviour.
In most cases, matter placed between a person (or radiation-sensitive equipment) and radiation source reduces the amount of radiation they absorb. The effectiveness of the shielding increases with the mass of the shielding and decreases with the atomic mass of the elements used for the shielding. For example, 1kg of hydrogen offers more protection then 1kg of aluminium, 2kg of aluminium offers more protection than 1kg of aluminium and 1kg of hydrogen offers more protection than 2kg of aluminium.
Mars One's solution is a thick layer of regolith on top of the settlement modules. An effective shield will require at least several hundred grams of regolith per square centimeter, according to one study. Using a regolith density estimate of 1.4 g/cm3, this means the regolith layer would need to be over 2 meters deep. For concrete with an average density of 2.4 g/cm3 the required thickness might be less.
The attenuation of radiation follows the Beer Lamberth law.
|Where:||I||=||the intensity of photons transmitted across some distance x|
|I0||=||the initial intensity of photons (or radiation in general)|
|s||=||a proportionality constant that reflects the total probability of a photon being scattered or absorbed|
|µ||=||the linear attenuation coefficient|
|x||=||distance traveled (thickness of material)|
|Absorber||100 keV||200 keV||500 keV|
the linear attenuation coefficient µ is not commonly found in the litterature, the mass attenuation coefficient µm is usually used instead. The coefficient is also dependent on the type of radiation, so a complete solution for radiation protection requires multiple analysis of the type of radiation to be protected against.
Conversion is quite simple as:
µ=µm*density of the material
List of mass attenuation coefficients can be found at the NIST website. https://physics.nist.gov/PhysRefData/XrayMassCoef/tab3.html
Another common way of evaluating radiation shielding is to use the half value, that expresses the thickness of absorbing material which is needed to reduce the incident radiation intensity by a factor of two, or Ix=Io / 2.
The Half Value Layer for a range of absorbers is listed in the following table for three gamma-ray energies:
|Absorber||100 keV||200 keV||500 keV|
The first point to note is that the Half Value Layer decreases as the atomic number increases. For example, the value for air at 100 keV is about 35 meters and it decreases to just 0.12 mm for lead at this energy. In other words 35 m of air is needed to reduce the intensity of a 100 keV gamma-ray beam by a factor of two whereas just 0.12 mm of lead can do the same thing. The Half Value Layer increases with increasing gamma-ray energy. For example, from 0.18 cm for copper at 100 keV to about 1 cm at 500 keV.
Active shielding against radiation involves a man made magnetic field which deflects ionized particles in the same manner as the Earth's. Such fields might require infeasible amounts of energy to generate and could also pose a major risk to anyone approaching the craft or base, as it would create bands of trapped particles similar to the Van Allen belts. However, the radiation exposure might be low, as traversing the magnetic shield should be a very brief event.
It might be possible to situate a base in such a location that one of the residual Martian magnetic fields offers a net benefit. Care should certainly be taken not to situate it where the fields concentrate radiation.
Also, it might be possible (assuming one could generate the required magnetic field in some way) to have the radiation belts of the habitat pass through some sort of physical barrier, which scrubs them of particles.
The possible sources of radiation on Mars are manmade sources, such as nuclear reactors or medical equipment, solar radiation, galactic cosmic radiation and naturally occuring radioactive elements on Mars.
Possible behavioural choices which minimize the risk from these include:
- Avoiding daytime EVA when there is a significan risk from solar radiation.
- Working preferentially close to natural or manmade objects, such as habitats, rovers or cliffs which provide additional (if not omni-directional) shielding.
- Entering a storm shelter when there is a high-radiation risk from solar particle events.
We can combine passive shielding with risk mitigating behavior to achieve low radiation exposure but still allow for some views of the exterior through windows. For example:
- Martian background average radiation is 240-300 mSv per year (if anyone has another number and reference would love to have it).
- If you sleep in a radiation shielded space such as underground rooms with a thick regolith cover, 8/24 hours, then the dose would be 160-200 mSv per year.
- If you spend most of your living (work, study) time in a radiation shielded space, then your dose becomes 80 to 100 mSv.
- With overhangs and a radiation proof roof, 70% of the incident radiation to a space close to windows can be stopped by geometries, than the dose is down to 20 to 25 mSv. this is about the 20 mSv per year for a 5 year period that is recommended for radiation workers.
- Part of the surface dose on Mars is solar proton events. These are predictable and detectable, and a large settlement will mostly be built of shielded areas. So during Solar Proton Events you stay away from the windows. This behavior might reduce the yearly radiation load another 25%, down to 15-18 mSv per year.
- What is the portion of the dosage from SPE? I have a weak reference that puts this at 30%. If correct, then the radiation load from large windows under a radiation proof ceiling is acceptable.
- Mars should be low in Radon because it is low in Thorium, and any thorium in the atmosphere can be separated out when the habitat atmosphere is produced. As 2 mSv on Earth comes from atmospheric radon, then this part of the yearly dose goes away.
- Even just 1/2 to 1 inches of glass reduces radiation dosage.
If the above is correct, then large windows are not really an issue. Geodesic glass domes over public spaces might be a poor choice, unless there is an understanding that you don't spend more than 2 to 4 hours per day under them.
- Operational medicine and health care delivery - J.S. Logan, in S.E. Churchill ed. Fundamentals of space life sciences, Volume 1 - 1997, ISBN 0-89464-051-8 pp. 154-156.
- Radiation biology - J.R. Letaw, in S.E. Churchill ed. Fundamentals of space life sciences, Volume 1 - 1997, ISBN 0-89464-051-8 pp. 16-17.
- Slaba, T. C., Mertens, C. J., & Blattnig, S. R. (2013). Radiation Shielding Optimization on Mars. NASA/TP–2013-217983. Retrieved from https://ntrs.nasa.gov/archive/nasa/casi.ntrs.nasa.gov/20130012456.pdf
- Kim, M. Y., Thibeault, S. A., Simonsen, L. C., & Wilson, J. W. Comparison of Martian Meteorites and Martian Regolith as Shield Materials for Galactic Cosmic Rays. NASA TP-1998-208724. Retrieved from https://ntrs.nasa.gov/archive/nasa/casi.ntrs.nasa.gov/19980237030.pdf.