LIFA: Lightweight Fiber-based Antenna for Small Sat-Compatible Radiometry

LIFA: Lightweight Fiber-based Antenna for Small Sat-Compatible Radiometry

2 min read

Preparations for Next Moonwalk Simulations Underway (and Underwater)

Artist rendition of a satellite above the earth with communication beams.
Graphic depiction of LIFA: Lightweight Fiber-based Antenna for Small Sat-Compatible Radiometry
Beijia Zhang

Zhang, Beijia Zhang, Beijia
Massachusetts Institute of Technology (MIT), Lincoln Lab

Very large space-based RF antennas can be large and expensive to manufacture and deploy. These problems become more challenging for cases when an array of antennas are needed such as for correlation interferometers that provide high spatial resolution of Earth and space. The proposal will specifically examine the potential applicability of novel fiber-based antennas to L-band radiometry for the purpose of generating high resolution soil moisture and sea surface salinity data. Initial estimates indicate that a x10 improvement on resolution may be possible with long fiber-based antenna arrays. Lincoln Laboratory has been investigating the ability to produce large flexible RF antenna arrays embedded in polymer fibers. These lightweight fibers are flexible enough to be coiled and uncoiled, thus facilitating transport and deployment. The metal that forms the antenna structure and other conductive elements is embedded inside a polymer boule that is heated and drawn to form a novel type of fiber. The resulting fiber thus has multiple materials embedded inside for the ability to support sensing capabilities and other functionalities. Thus, this fiber fabrication process may also lead to a cost-effective means to create very large antennas. This work will include analysis of the required antenna performance and the ability of fiber-based antennas to meet those requirements, deployment strategies, satellite specifics, space tolerance of components and materials, a preliminary system-level design, and concept of operations.

2024 Phase I Selection

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Loura Hall

Swarming Proxima Centauri: Coherent Picospacecraft Swarms Over Interstellar Distances

Swarming Proxima Centauri: Coherent Picospacecraft Swarms Over Interstellar Distances

4 min read

Preparations for Next Moonwalk Simulations Underway (and Underwater)

Labeled diagram of the Swarming Proxima Centauri
Graphic depiction of Swarming Proxima Centauri: Coherent Picospacecraft Swarms Over Interstellar Distances
Thomas Eubanks

Thomas Eubanks
Space Initiatives, Inc.

Tiny gram-scale interstellar probes pushed by laser light are likely to be the only technology capable of reaching another star this century. We presuppose availability by mid-century of a laser beamer powerful enough (~100-GW) to boost a few grams to relativistic speed, lasersails robust enough to survive launch, and terrestrial light buckets (~1-sq.km) big enough to catch our optical signals. Then our proposed representative mission, around the third quarter of this century, is to fly by our nearest neighbor, the potentially habitable world Proxima b, with a large autonomous swarm of 1000s of tiny probes.

Given extreme constraints on launch mass (grams), onboard power (milliwatts), and coms aperture (centimeters to meters), our team determined in our work over the last 3 years that only a large swarm of many probes acting in unison can generate an optical signal strong enough to cross the immense distance back to Earth. The 8-year round-trip time lag eliminates any practical control by Earth, therefore the swarm must possess an extraordinary degree of autonomy, for example, in order to prioritize which data is returned to Earth. Thus, the reader will see that coordinating the swarming of individuals into an effective whole is the dominant challenge for our representative mission to Proxima Centauri b. Coordination in turn rests on establishing a mesh network via low-power optical links and synchronizing probes’ on-board clocks with Earth and with each other to support accurate position-navigation-timing (PNT).

Our representative mission begins with a long string of probes launched one at a time to ~0.2c. After launch, the drive laser is used for signaling and clock synchronization, providing a continual time signal like a metronome. Initial boost is modulated so the tail of the string catches up with the head (“time on target”). Exploiting drag imparted by the interstellar medium (“velocity on target”) over the 20-year cruise keeps the group together once assembled. An initial string 100s to 1000s of AU long dynamically coalesces itself over time into a lens-shaped mesh network #100,000 km across, sufficient to account for ephemeris errors at Proxima, ensuring at least some probes pass close to the target.

A swarm whose members are in known spatial positions relative to each other, having state-of-the-art microminiaturized clocks to keep synchrony, can utilize its entire population to communicate with Earth, periodically building up a single short but extremely bright contemporaneous laser pulse from all of them. Operational coherence means each probe sends the same data but adjusts its emission time according to its relative position, such that all pulses arrive simultaneously at the receiving arrays on Earth. This effectively multiplies the power from any one probe by the number N of probes in the swarm, providing orders of magnitude greater data return.

A swarm would tolerate significant attrition en route, mitigating the risk of “putting all your eggs in one basket,” and enabling close observation of Proxima b from multiple vantage points. Fortunately, we don’t have to wait until mid-century to make practical progress – we can explore and test swarming techniques now in a simulated environment, which is what we propose to do in this work. We anticipate our innovations would have a profound effect on space exploration, complementing existing techniques and enabling entirely new types of missions, for example picospacecraft swarms covering all of cislunar space, or instrumenting an entire planetary magnetosphere. Well before mid-century we foresee a number of such missions, starting in Earth or lunar orbit, but in time extending deep into the outer Solar system. For example, such a swarm could explore the rapidly receding interstellar object 1I/’Oumuamua or the solar gravitational lens. These would both be precursors to the ultimate interstellar mission, but also scientifically valuable in their own right.

2024 Phase I Selection

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Loura Hall

Detoxifying Mars: the biocatalytic elimination of omnipresent perchlorates

Detoxifying Mars: the biocatalytic elimination of omnipresent perchlorates

3 min read

Preparations for Next Moonwalk Simulations Underway (and Underwater)

Artist rendition of a bottle of H2O, Bioreactor and H2O with a planetary surface in the background.
Graphic depiction of Detoxifying Mars: the biocatalytic elimination of omnipresent perchlorates
Lynn Rothschild

Lynn Rothschild
NASA Ames Research Center (ARC)

Water is the lifeblood of human survival and civilization and is critical for our sustained exploration beyond Earth. Fortunately, Mars has plenty of water to sustain our aspirations in the form of subsurface ice. Unfortunately, it is not clean water – it is contaminated by toxic perchlorates. Perchlorate and chlorate are potent oxidizers that cause equipment corrosion and are hazardous to human health even at low concentrations. It is therefore critical that Martian water be detoxified to remove these contaminating solutes before it can be used in propellant production, food production, or human consumption. The scale of anticipated water demand on Mars highlights the shortcomings of traditional water purification approaches, which require either large amounts of consumable materials, high electrical draw, or water pretreatment.

What if we could make the perchlorates just vanish? This is the innovative solution we propose here, taking advantage of the reduction of chlorate and perchlorate to chloride and oxygen being thermodynamically favorable, if kinetically slow. This is the promise of our regenerative perchlorate reduction system, leveraging synthetic biology to take advantage of and improve upon natural perchlorate reducing bacteria. These terrestrial microbes are not directly suitable for off-world use, but their key genes pcrAB and cld, which catalyze the reduction of perchlorates to chloride and oxygen, have been previously identified and well-studied. This proposed work exploits the prior work studying perchlorate-reducing bacteria by engineering this perchlorate reduction pathway into the spaceflight proven Bacillus subtilis strain 168, under the control of a robust, active promoter. This solution is highly sustainable and scalable, and unlike traditional water purification approaches, outright eliminates perchlorates rather than filtering them to dump somewhere nearby.

For Phase I we will explore whether this approach is feasible through these objectives:

  1. Engineer the genes PcrAB and cld into B. subtilis 168 under the control of the strong promoter pVeg and test and quantify the efficacy of perchlorate reduction under the modeled conditions.
  2. Develop B. subtilis strains that secrete the enzymes to test intra- vs extracellular efficacy.
  3. Perform a trade study comparing the performance of biological water detoxification from Objs. 1 & 2 to traditional engineering approaches in terms of mass, power, and crew time.
  4. Delineate a plan to infuse this technology in human Mars missions. Development of our detoxification biotechnology will also lead to more efficient solutions to natural and particularly industrial terrestrial perchlorate contamination on Earth. It will also shine a spotlight on the potential of using life rather than only industrial solutions to address our environmental problems, which may spur further innovations for other terrestrial environmental challenges such as climate change. The system will be launched as inert, dried spores stable at room temperature for years. Upon arrival at Mars, spores will be rehydrated and grown in a bioreactor that meets planetary protection standards. Martian water will be processed by the bioreactor to accomplish perchlorate reduction. Processed water can then be used or further purified as required.

2024 Phase I Selection

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Loura Hall

Add-on to Large-Scale Water Mining Operations on Mars to Screen for Introduced and Alien Life

Add-on to Large-Scale Water Mining Operations on Mars to Screen for Introduced and Alien Life

4 min read

Preparations for Next Moonwalk Simulations Underway (and Underwater)

Artist rendition of labled Water mining ISRU missins on a lunar surface.
Graphic depiction of Add-on to large-scale water mining operations on Mars to screen for introduced and alien life
Steven Benner

Steven Benner
Foundation For Applied Molecular Evolution

As noted at NASA’s 2019 Carlsbad Conference we have good reason to think that:

  • Life started on Mars using the same geo-organic chemistry that started life on Earth.
  • Martian life persists today on Mars, in near-surface ice, low elevations, and caves, all with transient liquid brines, environments that today on Earth host microbial life.
  • Martian life must use informational polymers (like DNA); Darwinian evolution requires these, and Darwinian evolution is the only way matter can organize to give life.
  • While Martian “DNA” may differ (possibly radically) in its chemistry from Terran DNA, the “Polyelectrolyte Theory of the Gene” limits the universe of possible alien DNA structures.
  • Those structures ensure that Martian DNA can be concentrated from Martian water, even if very highly diluted, and even if Martian “DNA” differs from Earth DNA.
  • On Mars as it exists today, information polymers cannot be generated without life (unlike other less reliable biosignatures such as methane), ensuring that life will not be “detected” if it is not present (the “false positive problem”). Nevertheless, as noted by Rummel and Conley, “the Mars community is not convinced that a mission to attempt detection of extant Martian life has a high priority.” Thus, NASA’s current flagship mission to Mars, derived from its 2012 Decadal Survey, involves pedestrian collection of old dry rocks to be cached, eventually to be returned to Earth to study for evidence of past life.

The purpose of this NIAC project is to change this view, and to do so before human arrival planned by NASA, the Chinese National Space Agency, and SpaceX, “by 2040”, “in 2033”, and “before 2030”, according to their respective statements. Human arrival will undoubtedly complicate the search for indigenous Martian life. Thus, from an astrobiological perspective, these planned crewed missions to Mars put a very strict deadline on the search for life on a pristine Mars. However, crewed missions also offer an opportunity that we will exploit. Crewed missions to Mars will use materials found on Mars itself, “in situ”, in particular, near surface water ice. Propellant (methane and oxygen) will be generated from that water and

atmospheric carbon dioxide for the return trip back to Earth. That water ice will be mined on the scale of tens to hundred tons. Further, to maximize the likelihood of safe return of the crew to Earth, robotic operations that mine tons of near surface water-ice will be in place before the first human astronauts arrive. Thus, water mined in preparation for human arrival is correctly seen as an extremely large-scale astrobiological sample, far larger than dry cached rocks. As the mined water-ice is delivered with dust that, through dust storms, survey the entire accessible surface, this humongous sample will effectively enable a highly sensitive survey of the entire accessible Mars surface for life. This NIAC project will provide an “agnostic life finding” (ALF) system capable of extracting genetic polymers (DNA or alien) from

these large ISRU water samples. ALF is agnostic because it exploits what synthetic biology taught us about the limited kinds of Darwinian genetic molecules. ALF also offers tools to partly analyze the polyelectrolytes in situ.

As an add-on system, ALF creates a negligible additional burden (regarding mass and energy consumption) compared to the investment in the water mining operation at this scale. Although small and low cost, this instrument will allow science to place a severe lower limit on the amount of biosphere on the accessible Martian surface. And it will do so before Homo sapiens becomes a multiplanetary species. And “multiplanetary” is the correct term. This add-on ALF system can be used on all celestial bodies where water will be mined to search for and analyze life, indigenous or introduced, Earth-like or alien. This includes Europa, Enceladus, the Moon, and exotic locales on Earth.

2024 Phase I Selection

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Loura Hall

Mars Aerial and Ground Global Intelligent Explorer (MAGGIE)

Mars Aerial and Ground Global Intelligent Explorer (MAGGIE)

2 min read

Preparations for Next Moonwalk Simulations Underway (and Underwater)

Artist rendition of MAGGIE above a planetary surface
Graphic depiction of Mars Aerial and Ground Global Intelligent Explorer (MAGGIE)
Ge-Cheng Zha

Ge-Cheng Zha
Coflow Jet, LLC

We propose to develop a novel global mobility Mars exploration platform , Mars Aerial and Ground Intelligent Explorer (MAGGIE). MAGGIE is a compact fixed wing aircraft with ultra-high productivity efficiency powered by solar energy to fly in the Martian atmosphere with vertical take-off/landing (VTOL) capability, which is enabled by advanced deflected slipstream technology with CoFlow Jet (CFJ). The cruise Mach number of MAGGIE is 0.25 with a cruise lift coefficient CL of 3.5, nearly an order of magnitude higher than conventional subsonic aircraft to overcome the low density of the Martian atmosphere. The ultra-high cruise CL with CL/CDc of 9 is made possible by CFJ that overcomes the low Reynolds number effect on Mars. The range of MAGGIE for a fully charged battery per 7.6 sol is 179 km at altitude of 1,000 m. The total range of MAGGIE per Martian year is 16,048 km. The representative mission for MAGGIE presented would conduct three atmospheric and geophysical investigations, all supporting different timescales of the Dynamic Mars science theme. These include a study of the origin and timing of the Martian core dynamo from the weak magnetic fields found in the large impact basins, a regional investigation of the source of methane signals detected by the Tunable Laser Spectrometer on the Mars Science Laboratory in Gale crater, and mapping of subsurface water ice at high resolution in the mid-latitudes where it has been observed from orbit. The conceptual MAGGIE system study indicates that the concept appears to be feasible, but need to be further investigated, designed, and verified under Martian atmospheric conditions in Phase I. MAGGIE would be able to perform the first global-scale atmospheric mission at Mars and revolutionize our capability of exploring almost the entirety of the Martian surface. It is the first concept to enable ongoing exploration of this region of Mars and would provide a substantial leap in capability for NASA’s exploration of the Red Planet. The attractiveness of airborne missions on Mars has been amply demonstrated by the Ingenuity helicopter. MAGGIE would be similarly engaging to the public, both in its audacity, and in the variety of environments it could explore, study, and image. The technology would also enhance VTOL aircraft technology on Earth and other planets.

2024 Phase I Selection

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Loura Hall