Commercial activities and a fly-by

Credit: Polaris Dawn

August 27th is due to see the launch of a ground-breaking flight into space which is both daring and possibly questionable. Entitled Polaris Dawn, it is slated to be the first private-venture / commercial spaceflight to feature an EVA – “spacewalk” – and a flight that will carry humans the farthest from Earth since Apollo.

The mission is due to lift-off from Kennedy Space Centre at 07:38 UTC on the morning of August 27th, carrying four “citizen astronauts” into a highly elliptical orbit around the Earth. This will reach a maximum apogee of 1,400 km, putting the crew inside the Van Allen radiation belts, thus providing one of the medical goals for the mission.

Polaris Dawn is one of three such missions that are being led and paid for by billionaire Jared Isaacman. It will mark his second flight into orbit; the first being in 2021, when he paid for and led the Inspiration4 private mission also using SpaceX. This mission flew a crew of paying private citizens around the Earth as part of a multi-million dollar fund-raiser for St. Jude Children’s Research Hospital in Memphis, Tennessee (and for whom Polaris Dawn is continuing to raise money). However, Polaris Dawn is far more ambitious.

The Polaris Dawn crew. Credit: Polaris Dawn

Following launch, the Crew Dragon vehicle, comprising the capsule Resilience – also the craft used for the Inspiration4 mission – and a power and propulsion service module (“trunk” in SpaceX parlance) will be placed into an orbit with an apogee of 1,200km, which all then be raised to 1,400 over a number of orbits. These initial orbits will repeatedly pass through South Atlantic Anomaly, exposing the crew to the same amount of radiation in just a few orbits as a crew on the ISS would experience in some 3 months in space. The purpose of this is for researchers to gain, “Valuable research into the health effects of space radiation and spaceflight on the human body.”

On the second day of the flight, the orbit will be lowered and circularised at 750 km as on-board experiments are carried out, including testing the viability of the SpaceX Starlink system for use in crewed missions “to the Moon, Mars and beyond”. Then, on flight day 3, the EVA will be carried out with two of the crew carrying out the spacewalk in a manner harking back to the early days of spaceflight.

In the modern era, EVA – extra vehicular activities – are carried out in self-contained suits complete with life support systems – backpacks, if you will – to supply them with breathable air and vital cooling. The suits the Polaris Dawn crew will be using aren’t self-contained per se; they have no backpacks but instead rely on an umbilical connected to the spacecraft to provide the wearer with air and cooling. This is where some has raised concerns about the flight, together with the manner in which it must be carried out. Resilience does not have an airlock through which EVAs can be made; instead, the entire vehicle will have to be depressurised and the forward hatch (normally fitted with the mating mechanism for docking with the International Space Station) opened., exposing the craft’s entire interior to the vacuum of space.

A tale of two Dragons: The Polaris Dawn Crew Dragon Resilience (l) and the Crew 9 Dragon Freedom being prepared for launch at the SpaceX facilities at Cape Kennedy. Credit: SpaceX

This means the vehicles electrical and power systems have had to be specially updated for the flight. As there is no airlock, it further means that all four crew must be in EVA suits for the spacewalk to take place. As space suits work at a lower atmospheric pressure than the human body is used to, any EVA generally requires the astronauts spend time within an airlock pre-breathing an oxygen mix to remove nitrogen from their blood and organs – which might otherwise cause decompression sickness (also called “the bends”) when returned to a normal atmospheric pressure.

However, as Resilience doesn’t have an airlock, the entire crew will commence pre-breathing roughly an hour into the mission and continue to do so over the first two days of the mission as the pressure within the craft is reduced from 100.0 to 59.6 kPa (14.5 psi to 8.65psi), and enriched with oxygen, meaning all four crew with have to go through decompression after the EVA and prior to their return to Earth – the overall mission elapsed time expected to be around 5 days.

The 15-20 minute spacewalk itself will be carried lout by Isaacman and a Sarah Gillis, the senior space operations engineer at SpaceX, with retired US Air Force pilot Scott Poteet (mission pilot) and SpaceX lead space operations and a mission director Anna Menon remaining in the main capsule ready to provide assistance. The purpose is ostensibly to test the new SpaceX EVA suit – an evolution of the suits used by crews flying to the ISS aboard Crew Dragon, but featuring improved insulation and thermal protection (adapted from elements of the spacecraft’s own thermal insulation), improved mobility and helmets equipped with heads-up displays.

The new SpaceX IVA (intravehicular activity) / EVA suit, to be tested by Polaris Dawn. Credit: SpaceX / Polaris Dawn

Polaris Dawn is a fascinating venture, although it might be argued that several of its goals might be achieved just as well through other means. It’s also something of a high-risk venture for those directly involved as crew and for private-sector spaceflight as a whole. If successful (as I hope it will be), it could open the doors wide for more private-sector activity in space; however, if it fails, it has been claimed it could have major repercussions on commercial spaceflight, up to and including plans by Axiom and Blue Origin / Sierra Space and others to operate orbital facilities intended to replace the ISS.

Starliner Update: A Tale of Two Returns

On August 24th, NASA provided an update on the overall status of the Boeing Starliner CST-100 Crew Flight Test.

Originally stated to last a little over a week in early June 2024, the flight – with astronauts Barry “Butch” Wilmore and Sunita “Suni” Williams – has experienced a series of issues relating to the propulsion / manoeuvring systems on the Starliner’s service module, forcing it to remain at the ISS.

Boeing had thought they’d found a way to address the core issues as a result of a series of comparative “hot fire” tests on Earth and aboard the vehicle at the space station, however, a detailed review of the data from the last set of tests carried out at the end of July revealed what appears to be wear-and-tear on valves within the system might might also impact the reliability of the vehicle’s thruster systems during critical manoeuvring prior to the service module being jettisoned during a return to Earth.

Barry “Butch” Wilmore and Sunita “Suni” Williams will remain abord the ISS through until early 2025 and return to Earth aboard the Crew 9 mission vehicle. Credit: NASA

While Boeing has remained adamant the vehicle can make a crewed return to Earth, after seeking input from multiple internal teams, and with the shadows of the Challenger and Columbia disasters ever-present, NASA has made the decision not to use Starliner to return Wilmore and Williams to Earth. Instead, they will now return to Earth aboard the SpaceX Crew 9 / NASA Expedition 72 Crew Dragon, something I’d speculated might be the case when last reporting on this situation back on August 11th:

The most likely scenario for this would launching the Crew 9 mission with only two people on board – most likely Commander Zena Cardman and Pilot Nick Hague, leaving 2 seats free for Williams and Wilmore (although their space suits are different to those used by SpaceX, so this would have to be worked through). Wilmore and Williams would then remain aboard the ISS as a part of the Crew 9 rotation (Expedition 72), returning to Earth with Cardman and Hague in March 2025.

– This column, August 11th, 2024

(side note: One small adjustment to the above statement is that it appears as if cosmonaut Aleksandr Gorbunov will fly the mission in order for NASA to maintain its seating agreement with Roscosmos.)

This means Starliner will now make an automated return to Earth some time ahead of the Crew 9 launch, currently slated for no earlier than September 24th. As I also noted in my August 11th piece, Starliner can in theory do so; unlike Crew Dragon, it is fully capable of fully automated flight, the system being tested during the unscrewed Orbital flight Test-2 in May 2022. The wrinkle here being that OFT-2 used the Starliner SP2 capsule, not Calypso, and so the latter doesn’t have the necessary flight software aboard; instead, Boeing will have to configure, test and upload it, a process which will take a number of weeks.

Whilst NASA management remain convinced Boeing and Rocketdyne will overcome the issues with the thruster systems on Starliner, the entire matter is embarrassing for the US agency, and particularly for Boeing, which has already seen direct losses in share value directly as a result of Starliner’s issues. Boeing have also faced penalties and the need to cover the additional costs involved in having to fly a second Orbital Flight Test mission – and may yet need to meet those of a second Crew Flight Test; NASA has left the need to fly such a mission open, and will decide on it once Boeing are in a position to demonstrate the underpinning problems with the Starliner propulsion systems have been resolved.

RFA Core Stage Explodes at SaxaVord

Britain’s first vertical space launch facility, the SaxaVord Spaceport, located at the northern end of the Isle of Unst in the Shetlands, became the focus of attention on August 19th, albeit for the wrong reasons.

A private venture, SaxaVord was licensed for up to 30 rocket launches a year at the end of 2023, and operations were due to commence this summer via Rocket Factory Augsburg AG (RFA). A German commercial space launch start-up founded in 2018 with the aim of providing a smallsat launch vehicle called RFA One, capable of lifting a maximum payload of 1.6 tonnes to LEO, 450 kg to geostationary transfer orbit (GTO) and a maximum of 150 kg to geostationary Earth orbit (GEO), RFA have the stated goal of producing the RFA-One via a production line process “like a car”, enabling them to provide a rapid launch provisioning service out of SaxaVord and other commercial launch locations.

The core stage of the rocket – which overall will be a 3-stage vehicle some 30 metres tall with a 2 metre diameter and feature two sub-orbital stages and an upper stage called Redshift, which doubles as an orbital transfer vehicle (OTV) – has been undergoing a series of tests at SaxaVord over the past few months in readiness for the first launch.

The first indications of problems for the RFA One test, August 19th, at SaxaVord Spaceport. Note the plume of ignited gases on the left of the vehicle’s base. Credit: RFA / SaxaVord Spaceport CCTV

However, on August 19th, during the latest hot fire test with the stage, something went wrong. Intended to be a hot-fire burn of all nine of the stage engines – only four having thus far being fired in any single test, some was seen to go wrong within seconds of motor ignition, While the majority of exhaust gas and flame was being directed down though the elevated launch stand, a powerful jet of ignited exhaust gases could be seen leaving the base of the rocket horizontally.

The motors all rapidly shut down, but the base of the rocket and its launch mount were by that time – around 6 seconds into the test – already on fire, and ignited gases continued to stream from the side of the stage, causing a fire on the launch stand itself. At some 38 seconds after ignition, the lower portion of the rocket was on fire and fames quickly engulfed it and the launch stand prior to the rocket collapsing and exploding.

Following preliminary analysis of data and footage of the event, RFA stated on August 24th that the most likely cause of the incident was the failure of an oxygen pump within one of the motors which started a fire beneath the stage that quickly spread to other propellant lines despite the automatic shut-down of the motors. Fire suppression systems on the stage and the launch mount were then overwhelmed, leading to the loss of the stage.

The location of the SaxaVord Spaceport, Scotland

Also commenting on the incident, SaxaVord management indicated that despite the fire and explosion, the launch stand and its supporting infrastructure had not suffered “major” damage. However, all activities at the launch facility are now suspended pending an investigation with will involve the UK’s Civil Aviation Authority (CAA), which has regulatory oversight of UK launch facilities.

The lost of the stage means that RFA’s plans to launch before the end of summer 2024 are at an end; whilst it is too early for a new date to be provided, the company indicated it is now looking towards the first half of 2025 as the period in which they may attempt their maiden flight.

No-one was injured during the incident, and two other launch developers, HyImpulse (also from Germany) and US-based ABL Space Systems, have indicated the incident does not affect their own plans to operate launches out of SaxaVord.

Juice-y Images of the Moon and Earth

In my previous Space Sunday update I wrote about the European Space Agency’s JUpiter ICy moons Explorer (Juice) and its (then) upcoming gravity-assist around Earth and, preceding it, a swing around the Moon in what would be the first Lunar-Earth Gravity Assist (LEGA) manoeuvre ever undertaken by a space probe from Earth.

The Moon imaged by ESA’s JUICE on August 19th, 2024, when it completed a fly-by of the Moon, during which it came to within 700 km of the lunar surface. Credit: ESA/Juice/JMC

The manoeuvre marked the first of a series of complex fly-bys for the probe – launched in April 2023 – all of which are designed to accelerate it to a speed of 2.7 km per second and throw it out towards Jupiter’s orbit, where it will intercept the planet in 2031. As noted in my previous report, the Moon fly-by on August 19th saw Juice pass around the far side of the Moon at just 700 km above the lunar surface, allowing the spacecraft’s course to be precisely adjusted for its passage around the Earth, which it reached on August 20th, passing around the planet at a distance of 6,807 km.

The manoeuvre acted as a slingshot, accelerating the spacecraft and hurling it back around the Sun ready for its next planetary encounter, this one with Venus in August of 2025. After this, JUICE will swing by Earth twice more, in 2026 and 2029 – the latter of which will boost it away from the inner solar system and an 18-month voyage to Jupiter.

An image of Earth captured by ESA’s JUICE during the second part of the LEGA fly-by on August 20th. Credit: ESA/Juice/JMC

The images here show both the Moon and Earth on August 19th and 20th respectively, with the spacecraft visible in both as a result of its orientation during the fly-bys.

Space Sunday: Water in Mars, and a Juice-y flyby

An artist’s illustration of NASA’s INterior Exploration Using Seismic Investigations, Geodesy and Heat Transport (InSight) lander on Mars (active: 2018-2022), which attempted to give the planet its first thorough check up since it formed 4.5 billion years ago. In particular, the mission sought to understand the planet’s interior composition and monitor things like tectonic activity (marsquakes), meteorite impacts, study how much heat is still flowing through the planet, and track Mars’ wobble as it orbits the Sun. Credit: NASA/JPL

The subject of water on Mars has been a topic of scientific debate and speculation for well over 100 years. Since the earliest reliable observations of Mars via telescope, it had been thought that water ice and water vapour existed on the planet and in its atmosphere as a result of the seeing the polar ice caps (although we now know the major stakeholder in these is carbon dioxide) and cloud formations.

However, the idea that Mars was still subject to liquid water flowing across its surface in our modern era became popularised in the late 1800s. In  1877, respective Italian Astronomer  Giovanni  Schiaparelli – already noted for his observations of Mars in which he correctly identified and named multiple visible surface features – used the Great Opposition of 1877 (when Mars and Earth were both on the same side of the Sun relative to one another and Earth was effectively “overtaking” Mars in their respective orbits, thus bringing the two into “close” proximity to one another) to carry out further observations. During these he noted the presence of multiple canali  on Mars.

One of Schiaparelli’s 1877 surface maps of Mars. Note the looping canali (“channels”) he thought he observed in the northern hemisphere of the planet, and which he saw as entirely natural phenomena, although most were later shown to be optical illusions / the misidentification of other features. Credit: Public domain

Canali is an innocent term, meaning “channel”, and Schiaparelli simply used this term to differentiate what he thought is saw from other features he observed. But in English-speaking newspapers it was later translated as canals, evocative of artificial and intelligent construction. This resulted in wealthy Bostonian businessman Percival Lowell, following his return to the United States in the early 1890s to establish an observatory in Flagstaff, Arizona, specifically (initially at least) so he could observe these “canals” for himself.

Over the course of 15 years (1893-1908), Lowell saw his canals, which grew into a globe-spanning network and led to the publication of three books (Mars (1895), Mars and Its Canals (1906), and Mars As the Abode of Life (1908 – an original copy of which I actually own!) in which he expounded his theory that Mars had a network of canals built by an ancient civilisation in a last-ditch effort to carry liquid water from the planet’s poles to their equatorial and temperature cities as the planet increasingly became more desert-like.

A manuscript globe of Mars made by Danish amateur astronomer, Emmy Ingeborg Brun, presenting an image of Lowell’s network of Martian “canals” (together with the names he assigned individual “canals”), and made by combining sketches of his observations and which were published in Mars and Its Canals (1906), and Mars As the Abode of Life (1908). Credit: Royal Greenwich Observatory

Lowell stuck to this belief throughout his observations in spite of increasing scientific evidence that Mars was likely incapable of supporting liquid water on its surface and observations from other observatories with larger telescopes than his which could not find any evidence of “canals”, and that at least some of what he was seeing was actually (as Schiaparelli had believed) lines of demarcation between different elevations / terrains.

As a result of this belief, Lowell has become regarded as a bit of a crackpot  – which is a same, as he led a remarkable life with multiple achievements as a traveller, diplomat, writer and armchair scientist, and did gain recognition in his lifetime for his work – He was elected a Fellow of the American Academy of Arts and Sciences in 1892 and then to the American Philosophical Society in 1897, whilst the volume of work he carried out as an astronomer outside of his theories about Mars saw him receive the Prix Jules Janssen, the highest award of the Société Astronomique de France, in 1904.

Lowell pictured in 1914 seated at the 61-cm (24-in) Alvan Clark & Sons refracting telescope at the Lowell Observatory, Flagstaff, Arizona, as he observes Venus. Credit: Unknown and reconstructed

This volume of work include daytime studies of Venus and the search for “planet X”, a planetary body believed (and still believed by some) to be orbiting the Sun far out beyond the orbit of Neptune. In fact, the Lowell Observatory became a centre for this work, for which it was rewarded in 1930 when Clyde Tombaugh located Pluto using the observatory’s telescopes and equipment.

Of course, whilst liquid water does not exist on the surface of Mars today and hasn’t for billions of years, we have found plenty of evidence for its past presence on the planet’s surface.

In my previous Space Sunday article, for example, I wrote about the Great Lake of Mars, Lake Eridania, whilst both the Mars Science Laboratory Curiosity and Mars 2020 rover Perseverance have literally been following the evidence for free flowing water in both of the locations on Mars they are exploring. Prior to them, the Mars Exploration Rovers Spirit and Opportunity both uncovered evidence of past liquid water on Mars, as have orbital vehicles from NASA, Europe and other nations. But the two big questions have always been – where did it go, and where did it come from?

In terms of where it went, the most common theories are that the water either evaporated and was lost to space along with Mars’ vanishing atmosphere relatively early in the planet’s life or retreated down into the Martian crust where it froze out into icy “reservoirs”. The first is likely for a certain volume of water, whilst subterranean tracts of water ice have been located not too far under the surface of Mars. However, the latter cannot possibly account for the amount of water believed to have existed on the surface of Mars in its early history, not could simple evaporation account for the disappearance of to greater majority of it. So where did the rest go? And where did it come from originally?

Well, in a new report published this month a team of scientists believe they have the answer, and it lay within data obtained by NASA’s InSight (INterior exploration using Seismic Investigations, Geodesy and Heat Transport) lander.

This ambitious craft landed on Mars in 2018, with the mission running from November of that year through until the end of December 2022. In particular, the lander carried with it two unique instruments it deployed onto the Martian surface using a robot arm. One of these was the French-lead Seismic Experiment for Interior Structure (SEIS), designed to measure marsquakes and other internal activity on Mars and things like the response to meteorite impacts, in order to better understand the planet’s internal structure. The data continues to be studied, and has revealed much about the planet’s internal structure and its history.

Most recently, a US team from the Scripps Institution of Oceanography at the University of California, San Diego and the University of California, Berkeley, have been reviewing the SEIS findings specifically to try to answer the question of where the water went. In particular, they have been using mathematical models employed here on Earth to locate aquifers and oil and gas fields deep underground. By adjusting the models so they provided results consistent what is largely known about the Martian crust down to a depth of several kilometres below the surface, they ran a series of passes on data gathered from deeper and deep within the planet’s crust, In particular, the came across two interesting results. The first indicated that while deposits of water ice do exist below the surface of Mars, and less than 5 km from the surface, they are likely to be far less commonplace than had been thought. The second result they took note of was consistent with those indicative of layers of water-saturated igneous rock deep within the Earth’s crust.

Most interestingly, the results of the SEIS data modelled suggest this deep layer of rock and water – laying some 11.5 to 20 km below the surface of Mars could be widespread across the planet to the extent that it could contain more water than would have been required to fill the oceans and seas of ancient Mars.

Taken together, these result indicate that while the theories about water on Mars being lost to space or frozen into subsurface ice are still valid, the vast majority of the water most likely retreated deep down into the planet, possibly returning to the reserves from which it might have originally burst forth to flood parts of Mars during the planet’s late Noachain / early Hesperian period of extreme volcanic activity.

A “core sample” of the Martian interior beneath NASA’s InSight lander from the Scripps / UC Berkeley study. The top 5km of the crust appear to be dry, with limited large-scale deposits of water ice, while a water-saturated zone of fractured rock lies some 11.5 to 20 km below the surface. This is believed to by a widespread layer within the crust, potentially containing more liquid water than the volume believed to have been present in ancient Martian oceans. Credit: J Tuttle; Keane and Aaron Rodriquez, via Scripps Institution of Oceanography

One intriguing question that arises from this work is related to the potential for Mars to have harboured life, and what happened to it as the water vanished. if the modelling in the study is correct, and the water did retreat deep under the surface of Mars and form aquifers and pools with the rocks there, did any ancient microbial life gone with it, and if so – might it have survived? The pressure and temperatures at the depth which the water appears to reside would keep it both liquid and warm and provide energy, as would mineral deposited within the rock; so the question is not without merit.

Establishing that there is a big reservoir of liquid water provides some window into what the climate was like or could be like. And water is necessary for life as we know it. I don’t see why [the underground reservoir] is not a habitable environment. It’s certainly true on Earth — deep, deep mines host life, the bottom of the ocean hosts life. We haven’t found any evidence for life on Mars, but at least we have identified a place that should, in principle, be able to sustain life.

– Michael Manga, Professor of Earth and Planetary Science, UC Berkeley

But the is a question that’s unlikely be to answered any time soon. Determining if the environment is at the very least amenable to life, much less actually finding evidence for life within it – or even simply reaching any of the water deposits –is going to be pretty much impossible for a good while yet. Current deep drilling techniques here on Earth for extracting oil and gas only go down to around 2 km; getting that sort of equipment to Mars and enabling it to dill down at least 11-12 km will pretty much remain the stuff of dreams for a good while to come.

 JUICE to Swing by the Moon and Earth

The European Jupiter Icy Moons Explorer (JUICE) mission will be making a first-of-its kind fly-by of the Moon and Earth this week, the first in more than 5 gravity assist manoeuvres the vehicle will make (excluding those made while orbiting Jupiter) during its mission to study the icy moons on the Jovian system.

An artist’s impression of ESA’s Juice mission approaching the Jovian system in 2031. Credit: ESA

Such manoeuvres are often used with space missions and for a variety of reasons. With JUICE, it means the craft could be flown into space using a medium-lift launch vehicle and make (and albeit relatively sedate) flight to Jupiter, involving a total of three fly-bys of Earth and one of Venus to accelerate it to a peak velocity of 2.7 km per second using the minimum of fuel and then slingshot it out to a point in space where it will intercept the Jovian system, and they use further flybys of the planet and its Moons to both slow itself down into orbit around them and then adjust its course so it can study the icy moons of Jupiter – GanymedeCallisto, and Europa.

This first fly-by comes 16 months since the launch of the vehicle, and will be the very first Earth gravity assist which also employs the Moon as a critical component. On August 19th, Juice will as around the Moon at a distance of just 700 km (reaching the altitude at 21:16 UTC), using the Moon’s gravity to swung it onto a trajectory that will see it pass by Earth just over 24 hours later, passing over north-eastern Asia and the Pacific at an altitude of just 6,807 km on the morning of August 20th (local time) before heading back out to loop around the Sun. After this it will get a further gravity assist from Venus in August 2025 and then two more from Earth (without the Moon helping) in 2026 and 2029, that latter of which will  slingshot the vehicle on it way to rendezvous with Jupiter and its moons.

An animated GIF showing Juice’s flightpath as it loops around the inner solar system (2023-2029 – Yellow= Venus; blue = Earth) prior to gain the velocity required to slingshot out to intercept Jupiter, passing by way of asteroid 223 Rosa (teal). Credit: Phoenix777, using NASA HORIZONS system data, via Wikipedia

On August 15th, Juice briefly caused a stir when it was mistaken as a near-Earth object (NEO) on a potential collision course with Earth. At 27 metres across, most of which is some 85 square metres of solar arrays, Juice is a strong reflector of sunlight, and this briefly confused systems at the ATLAS Sky Survey, Hawai’i, which attempts to locate, identify and track potentially threatening NEOs. However, the system’s confusion was quickly identified as actually being the Juice spacecraft and the alert corrected.

This was actually the second time an ESA deep-space vehicle has been mistaken as a hazardous NEO; in November 2007, and as it approached Earth for a flyby, Europe’s Rosettta mission spacecraft  – also with a large span of solar arrays – was also briefly mis-identified as a NEO on a possible collision course with Earth. On that occasion, it was mis-identified by a human observer, and further manual checking was required before it was confirmed the object being tracked was actually the Rosetta spacecraft and not of any threat to Earth.

Following its arrival at the Jovian system, Juice will spend 1259 days orbiting the system, the majority of which will be in Jupiter-centric orbits that will allow it to study Ganymede, Callisto and Europa, with numerous gravity-assists of both Ganymede and Callisto used to alter its trajectory and velocity, allowing it to study them from different orbital inclinations and also to dip down into the inner Jovian system to study Europa.

However, the final 284 days of the time (from early 2035) will be spent in a dedicated orbit around Ganymede, allowing the spacecraft to complete some 6 months of dedicated studies of the moon once it has settled into a 500 km circular orbit around Ganymede. By the end of 2035, the spacecraft is expected to have expended the last of its 3 tonnes of manoeuvring propellants, bringing the mission to an end. without the ability to manoeuvre, Juice is expected to quickly fall victim to further Jupiter gravitational perturbations and crash into Ganymede within weeks of running out of propellants.

Space Sunday: balloon rides to space and alien lakes

A rendering of the Marine Spaceport (MS) Voyager launching a Space Perspective capsule at the start of a 6-hour journey under a balloon to carry passengers to an altitude of 32 km and then bringing them back to a safe splashdown and recovery. Credit: Space Perspective

Back in 2021 I wrote about Space Perspective, a (then) relatively new entry to the field of sub-orbital space tourism and – if I’m honest – the one I’d really like to try (see: Space Sunday: balloons to space, Mars movies and alien water clouds).

At a time when Blue Origin are lobbing place to the edge of space in ballistic capsules and Virgin Galactic has been (although currently on hiatus) chucking them not-quite-so-high on rocket planes, Space Perspective came up with an altogether more sedate – and longer duration approach to giving people a taste of space: send them up in a  balloon.

Space Perspective’s Neptune capsule test article at their hanger in Titusville, Florida. Credit: Space Perspective

When I first wrote about the endeavour, Space Perspective planned to offer flights for up to 8 passengers and 2 crew starting on land, using a purpose-built balloon with a luxury capsule slung beneath it to carry them up to around 30-32 km altitude (not high enough to qualify for astronaut wings but more than enough to witness the curvature of the Earth and see it passing below as the 6-hour flight heads out to sea) before descending to a splashdown and a return to dry land aboard a luxury boat.

Since then things have changed somewhat. Whilst the overall goal remains the same – and the prototype capsule for the flights, called Neptune, has made a number of demonstration flights, once the system is approved and operational, the entire flight will commence and end at sea, launched and recovered via a purpose-equipped vessel.

MS Voyager undergoing sea trails following her refit and renaming. Credit: Guice Offshore / Space Perspective

The MS (Marine Spaceport) Voyager, as the vessel is known, is a former 3,100 tonne displacement oil platform support vessel (OSV) measuring  90 metres in length, 61 metres of which is a flat working deck which has been specifically outfitted for the launch and recovery of the company’s balloons and capsules. The term “Marine Spaceport” replaces the more usual usage of MS (“Motor Vessel”) to indicate the ship is intended to be a fully ocean-going launch and recovery vessel. Initially it will operate of the United States Space Coast, Florida, but Space Perspective is already eyeing the potential to offer flights out of the Caribbean and other wealthy tourist retreats, thus bringing the thrill of edge-of-space flight to the potential travellers, rather than making them travel to the launch pad.

The name Voyager was chosen in direct reference to NASA’s Voyager mission programme, and specifically Voyager 1. Billed as the “first” in its class and operated by specialist marine and aerospace recovery company Guice Offshore on behalf of Space Perspective, both companies have hinted further vessels (Voyager 2?) might be made available in the future.

A rendering of the inside the Neptune Capsule with an added backdrop of the Earth visible through the windows. The cabin sits 10 – 8 passengers + 2 crew and features a “space spa” (washroom) and drinks and snacks. Credit: Space Perspective
The ship was officially unveiled in January 2024 following a 2-year refit and upgrade. This includes outfitting her for balloon and capsule transport, balloon inflation, capsule launch system, capsule recovery system (following splashdown, rather than trying to recover the capsule directly on the deck) and more. In addition, the vessel has been equipped with luxury staterooms for capsule passengers, a passenger lounge and a fully equipped hospital.  Since its official unveiling in its finished looks (the company did reveal snippets of it during the acquisition and conversion process), Voyager has been undergoing final re-certification and licensing trials prior to moving to ita new berth at Port Canaveral, its base of operations.

The capability to launch and retrieve the Neptune capsule at sea creates worldwide scalability along with an unprecedented closure of the routine operations safety case. We are proud to bring a new spaceflight capability to Port Canaveral and the Space Coast.

– Taber MacCallum, founder and co-CEO of Space Perspective

Whilst no dates have been given, Space Perspective has indicated the next phase of work is to test launch and recovery operations using the Neptune capsule. After these, the company expects to move towards obtaining a commercial license for passenger operations and then to offering flights.

Tickets for the latter have already been offered by the company at US $125,000 per head – far less than either Virgin Galactic or Blue Origin, although both of the latter do offer periods in microgravity, which Space Perspectives cannot provide. The company has not revealed how many tickets it has sold in advance of commencing operations.

The Great Lake of Mars

Mars is a small world when compared to Earth, but it likes to do things big. There’s Olympus Mons, the massive shield volcano , rising almost 22km above the Mars datum (compared to Mauna Loa and Mauna Kea rising some 9-10km above the sea floor on Earth), and covering an area as much as 300,000 sq km in size  (compared to the10,430 sq km of the Island of Hawaii). Or there’s the 4,000+ km length of the Vallis Marineris, in places 7 km deep and more than capable of regarding the 447 km long and 1.6 km deep Grand Canyon as a mere tributary.

Both of these feature are very well known to people even with just a passing interest in Mars. But there is another remarkable – if less obvious – feature on Mars which has been the subject of extended study by Europe’s 20-year Mars orbiting veteran, Mars Express.

Located in the planet’s southern hemisphere, and badly scarred and weathered by impact craters and the passage of time, are the remnants of a vast lake – or perhaps sea might be a better description – that at some point in the ancient Martian past may have been up to 1 km deep, a depth similar to the extent of the southern end of the Caspian Sea, Earth’s largest inland sea. However, where the latter covers an area of some 386,400 sq km, Eridania Lake on Mars once covered an area of some 1.1 million square km – big enough to hold three times the volume of water by volume than the Caspian Sea. And if you’re wondering about how this compares to the Great Lakes in North America, the largest bodies of freshwater on Earth, they “merely” cover an area of some 244,100 sq km with a maximum depth of around 406 metres.

However, like the Great Lakes, Lake Eridana consists of several interconnected basins, all of which likely held water as a common lake between 4.1 and 3 billion years ago. These basins are still visible on the surface of Mars today and, and are now officially called the Ariadnes Colles (“hills”), Coralis Chaos, Atlantis Chaos, Simois Colles, and Gorgonum Chaos.

What is particularly interesting about this region is not the fact it was once a vast lake, but that it is exceptionally mineral and clay rich (the clay deposits being up to 2 km thick), with many of the detected minerals showing clear signs of volcanic origins. This means that the lake bed could once have been home to hydrothermal vents; thus Eridana potentially offered everything life needed to bring itself into being back in the Martian pre-history: the right chemicals and minerals, a source of water, and a source of heat / energy.

An illustration of how volcanic activity may have caused the deposition of minerals on the floor of Lake Eridania and chlorides along the shoreline as a result of evaporation. Credit: J Secosky via wikimedia

The clearest evidence for the region being subject to the effects of volcanism is not so much in the presences of ancient volcanic peaks, but from the presence of significant fault lines collectively called the Sirenum Fossae. Over 2,700 km in length, these fault lines sit either side of a trough of land which dropped below the mean surface level to form a graben as the land either side of the faults was pulled apart. It’s believed this occurred when the crust of the planet was under enormous strain as the massive Tharsis bulge with its three huge volcanoes was forcing itself upwards half a world away, allowing liquid magma to channel its way up to the heat the lake bed, giving rise in turn to the hydrothermal venting.

The hills of Ariadnes and Simois Colles are thought to have been mounds of material deposited within the lake during the early-to-mid Noachain period, when Mars is thought to have been most abundant in liquid water. As the water began to recede in the latter part of the Noachian period (round 3.8 to 3.7 billion years ago), material was exposed to the Martian weather and subject to sculpting into mounds.

An annotated image of four of the principle parts of Eridania Lake, showing the likely water depths during the time the lake was at its greatest. Credit: J Secosky via wikimedia

Then, in the Hesperian period (3.7 to around 3.0 billion years ago), the region of the lake were subject to perhaps multiple periods of flood and clearing  (along with other parts of the planet) as volcanism took more widespread hold on the planet and the likes of Olympus Mons formed, whilst the volcanoes of Tharsis and Elysium added their voices to the choir of eruptions and disruptions. This ebb and flow of water further shaped the vast fields of mounds before they were again exposed to the (much calmer by this time) Martian winds, which have been shaping them ever since.

Such is the wealth of potential science there that the region was proposed as a possible landing zone for NASA’s Mars 2020 rover Perseverance.

Despite the fact that Eridania floor has been mapped as a volcanic ridged plain, several sedimentary mineralogies have been recognised there corroborating i) a low-energy and long-lasting (Late Noachian to Early Hesperian) depositional environment characterised by the presence of ponding water, and ii) a warm Martian paleoclimate with a stable highland water table more than ∼3.5 billion years ago.
For all the above reasons, the Eridania surface provides great potential to search for prebiotic chemistry and past exobiological life: thus we are proposing this region as the Mars 2020 landing site.

– Pajola et al, 2016: Eridania Basin: An ancient paleolake floor as the next landing site for the Mars 2020 rover

Ultimately, and for a variety of reasons, the region was passed over in favour of other locations and, eventually, Jezero Crater was selected as the landing zone for Perseverance. However, the continuing study of Eridania is again awakening calls for a robotic mission there – if a suitable landing zone can be located. Not only does the region offer a fascinating mineralogical history of Mars and the potential for studies into both prebiotic chemistry and potential past biological activity, the richness of the minerals and compounds identified within the clays of the region could potentially preserve the characteristics of the ancient atmosphere and climate. Thus studying them even in the absence of any evidence for organic activities within the clays of the region could do much to further unlock the ancient history of Mars.

Starliner to Remain, Crew-9 Delayed and Embarrassment Rises

So the Starliner saga continues. As noted last time out, the decision on when (and how) to return Boeing’s CST-100 Starliner to Earth was awaiting further review of data on the end-of-July “hot fire” tests of the vehicle’s thrusters systems both on Earth and on the International Space Station (ISS).

At the time of that update, things looked good from both a Boeing and a NASA perspective, but NASA delayed detailed commentary on the results for a week to allow further reviews of the data. These have been carried out, and appear to show there are still issues which may or may not be related to the overheating problem. As the precise cause of the additional issues cannot be determined, NASA announced on August 7th that the Starliner vehicle, comprising the reusable capsule Calypso and its non-reusable service module, will remain at the ISS until mid-August at least.

This announcement came a day after NASA indicated that the Crew 9 mission due to launch to the ISS on August 18th would be delayed until no earlier than September 24th (something I indicated might be the case in my last update).  However, during the August 7thbriefing, NASA did make the admission they are now looking at alternate ways to potentially bring the Starliner’s crew of Barry “Butch” Wilmore and Sunita “Suni” Williams home, if necessary.

“Butch” Wilmore and “Suni” Williams slightly ironically imaged within the ISS airlock and the hatchway of the Crew Dragon vehicle docked at the space station, as engineers at NASA and Boeing continue to seek answers to issues with the Boeing Starliner propulsion systems. Credit: NASA

The most likely scenario for this would launching the Crew 9 mission with only two people on board – most likely Commander Zena Cardman and Pilot Nick Hague, leaving 2 seats free for Williams and Wilmore (although their space suits are different to those used by SpaceX, so this would have to be worked through). Wilmore and Williams would then remain aboard the ISS as a part of the Crew 9 rotation (Expedition 72), returning to Earth with Cardman and Hague in March 2025. As veterans of previous ISS crews (Wilmore as a part of the Expedition 41 rotation in 2014 and Williams as part of both the 2006/7 Expedition 14 and Expedition 32 rotations in 2012), they are more than qualified for such an extended stay.

If the case, this would not be the first time a crew has faced an extended stay on the ISS – as many commentators seem to have forgotten.

In September 2022 cosmonauts Sergey Prokopyev, Dmitry Petelin and NASA astronaut Frank Rubio arrived aboard the ISS for a 6-month rotation. Three months into their stay, their space vehicle, Soyuz MS-22 suffered a major coolant leak, rendering it unfit for crewed flight. Instead, in February 2023, Russia launched Soyuz MS-23 to the space station without its crew of three. Rubio, Petelin and Prokopyev then remained on the ISS through the end of September 2023, carrying the work planned for the original MS-23 crew.

However, this would then require the Starliner to make an automated return to Earth. In theory, Starliner is fully capable of doing this (unlike SpaceX Dragon), having a fully automated flight control software suite. This was demonstrated in May 2022 with the unscrewed Orbital flight Test 2 in May 2022. The problem here being that Calypso was launched without some (or all) of the necessary software (notably, the software required for the vehicle to automated undock and move away from the ISS).

Starliner capsule S2 with the hatch for its docking adaptor open, approaches the ISS in May 2022 using its automated flight software to conduct a fully automatic rendezvous and docking with the station. However, some (or all) of this software is not currently available to the Calypso, and would have to be uploaded to the vehicle and configured if the craft is to make an uncrewed return to Earth. Credit: NASA

While this is partially understandable – this flight was, after all, intended to test the vehicle under human control –  it is nevertheless highly embarrassing that neither Boeing nor NASA sought to ensure the automated flight software was available on Calypso just in case it was needed. Instead, the software would have to be uploaded, configured and tested – a process that could take up to 4 weeks to complete.

This lead to something of a public tiff between company and agency, Boeing aggressively stating the craft is fully capable of a crewed return to Earth. NASA, however, isn’t (rightly) open to taking chances with its personnel – so for now the saga will continue.

Space Sunday: Mars rocks and space taxis

NASA’s Perseverance Mars rover took this selfie on July 23rd, 2024 (sol 1,218 of the mission). The “arrowhead” rock dubbed “Cheyava Falls” is centred in the image. The white spot on surface of “Cheyava Falls” is one of two points “cleaned” of surface dust so the rover could examine the composition of the rock’s surface directly. The second spot was used by the rover’s drilling mechanism to obtain a core sample of the rock, the hole for which as be seen just below the abrasion patch. Credit: NASA/JPL / MSSS

On July 25th, NASA released a statement on a recent find made by the Mars 2020 rover Perseverance as it continues to explore an ancient river outflow delta within Jezero Crater on Mars.

The statement relates to a rather unusual arrowhead-like rock NASA has dubbed “Cheyava Falls” which attracted interest both due to its general shape and the fact its surface has white veins of calcium sulphate—minerals that precipitate out of water – running across it. More particularly, between the veins, Perseverance imaged tiny mineral “leopard spots”, whitish splotches ringed by black material.

On Earth, such spotting can form when organic molecules react with hematite, or rusted iron. These reactions, in turn, can fuel microbial life. “Cheyava Falls” is the first time they’ve been seen on Mars, and so it is understandably a cause for interest and some excitement, and marked the rock – measuring around a metre in length and half a metre across at its widest, – and a target for more detailed study.

Captured on June 12th, 2024 (sol 1,178) this 360-degree view of the region dubbed “Bright Angel”, the outflow plain on the edge of Jezero Crater in which “Cheyava Falls,” is located. The 346 images making up this view were captured using the MastCam-Z instrument on the rover’s mast and stitched together after being sent back to Earth. The colour of the completed mosaic has been enhanced to bring out subtle details. Credit: NASA/JPL / MSSS

This commenced with analyses of various parts of the rock using instruments mounted on the turret at the end of the rover’s robotic arm, notably SHERLOC, PIXL and WATSON.

SHERLOC – the Scanning Habitable Environments with Raman & Luminescence for Organics & Chemicals  – revealed the compounds both within the white veins and on the surface of the rock as a whole, are consistent with those known to be involved in the advent of life. Meanwhile, WATSON, the Wide Angle Topographic Sensor for Operations and eNgineering imager associated with SHERLOC was able to provide detailed images of the “leopard spots” and the calcium sulphate veins, revealing multiple other minerals to be present, some of which contain elements which might assist in the formation of life; whilst the Planetary Instrument for X-Ray Lithochemistry (PIXL) instrument confirmed the “leopard spots” themselves contain both iron and phosphate, and so might possibly have once powered organic processes.

Captured on July 18th, 2024 (sol 1212 of the mission) using the WATSON imager aboard the NASA rover Perseverance, this image of the rock dubbed “Cheyava Falls” show to of the large white calcium sulphate veins running across the rock, and between them bands of material whose reddish colour indicates the presence of hematite, covered in millimetre-sized light patches surrounded by a thin ring of dark material, and referred to as “leopard spots”. Similar spots can form on sedimentary terrestrial rocks and are frequently an energy source for microbes. Also annotated is one of a number of nodules of pale green olivine. Credit: NASA/JPL / MSSS

This is the first time that a combination of all three of these types of deposit have been found in a single location on Mars, thus raising even more interest in “Cheyava Falls” and potentially making  it the strongest contender yet for indicating basic microbial life may have at one time existed on the planet. However, as the science team has noted, the situation is far from clear.

On Earth, whilst they are noted for their association with microbial life, “leopard spots” are initially the result of an abiotic chemical reaction. So even if the same processes were at work on Mars and may have eventually gone on to feed Martian microbe which may have come about courtesy of the other processes at work in the rock, it is also possible other factors intervened which halted any microbes getting a kick-start with life. In this, matters are complicated by the presence of olivine mineral fragments in the rock.

Olivine is a product of magma – and magma is not friend to organics, as such, their presence in the rock suggest they and the phosphates may have been deposited at temperatures too great to allow organic material to survive, but the phosphates were deposited into veins and pits in the rock after it had been initially laid down as sedimentary mud and compressed into rock, thus giving rise to the veins and spots.

To understand how the rock may have formed, the rover was instructed to take a core sample of “Cheyava Falls” on July 21st, and only the 22nd rock sample to be taken by the rover since it arrived on Mars in February 2021 – the being due to drilling operations having been cut back as a result of a series of issues with the drill mechanism and a desire to avoid it failing prematurely as a result of wear and tear.

Some of this sample will be analysed by the rover itself using its on-board lab. Unfortunately, while this may reveal more of the rock’s history, its unlikely to definitive answer the question of whether microbes might have once nommed on the minerals in the rock; there are simply too many variables involved for the rover’s limited capabilities to reach such a definitive conclusion on its own.

Captured using the front right Hazard Avoidance Camera A on the the rover’s chassis, this image shows Perseverance with the turret of its robot arm positioned over “Cheyava Falls”, ready to drill a core sample. This image was captured at the local mean solar time of 15:16:29 on July 21st, 2024 (sol 1215 of the mission. The image is unprocessed and show natural daytime lighting on Mars. Credit: NASA/JPL / MSSS.

As such, the material gathered in the sample would need to be returned to Earth. For this to happen NASA need to sort out how it is going to managed getting the sample – and others Perseverance has gathered (and in some cases already cached on the Martian surface). The problem here being that, as I’ve noted in previous Space Sunday updates, is that NASA has no clear idea as to how such a sample return mission might be completed; its original planes for far too complicated and way too costly – estimates by the agency’s own Office of Inspector General (OIG) pushing the mission upwards of US $9 billion – making it impractical and prompted NASA to re-think the whole thing.

Given this, the mystery of “Cheyava Falls” is liable to remain long after Perseverance has moved on in its exploration.

Boeing Starliner: “Hot Fire” Test Success, But No Return Date

In my previous Space Sunday update, I provided an update on the Boeing CST-100 Starliner Crew Flight Test (CFT) mission to the International Space Station (ISS), but things were hanging in the balance, as there were tests taking place at the time which could determine the vehicle’s readiness to make a return to Earth.

At the risk of repeating myself, Starliner vehicles use two propulsion systems: four larger orbital manoeuvring and attitude control (OMAC) system, used for making significant manoeuvres, and 28 smaller reaction control system (RCS) thrusters used to carry out precise manoeuvring and also to help stabilise and fine tune the vehicle’s pitch, yaw and roll during and after use of the OMACs. Four sets of thrusters, each comprising an OMAC unit and seven RCS units, are equidistantly places around the Starliner’s service module in external units called “doghouses”. During the flight up to the ISS, the RCS thrusters in particular suffered a series of issues and helium purge line leaks.

Since then, NASA and Boeing has been working through matters, delaying the return to Earth for both the vehicle and its crew of Barry “Butch” Wilmore and Sunita “Suni” Williams. Most recently, comparative testing between “doghouse” units on Earth and those on the Starliner in orbit revealed large temperature spikes occurring within latter’s doghouses when pulse-firing the RCS thrusters immediately after the used of the OMACs – and these spikes are believed to be the cause of leaks detected in the RCS helium purge lines and cause the failure of one of the RCS thrusters.

To combat this, Boeing and NASA have been developing an alternate procedure for the use of the RCS systems in an attempt to eliminate the noted temperature spikes in the “doghouses”, and the tests carried out on July 27th aboard Calypso were designed to test these new procedures. Following an initial review of the test data, NASA issued a statement noting:

The test involved firing 27 of the spacecraft’s 28 jets for short bursts, moving through them one at a time to check thruster performance and helium leak rates. Preliminary results show all the tested thrusters are back to preflight levels based on thrust and chamber pressure.
As part of the test configuration, all helium manifolds, which control and direct the flow of helium, were opened allowing engineers to continue evaluation of Starliner’s helium supply and leak rates. The teams verified Starliner continues to show the margin needed to support a return trip from the station.

– NASA Hot Fire Test statement, July 30th, 2024

Boeing CST-100 Starliner major vehicle elements. Credit: Boeing

In other words, there is currently a high confidence within NASA and Boeing that Starliner is fit for purpose in being able to bring Wilmore and Williams back to Earth.

However, prior to a final decision being made in this regards, a formal return readiness review meeting must be held. This is a necessary step to certifying a vehicle which has experienced issues is believed to be fit for a return to Earth, and which usually sees a target date for its return is identified.

Prior to the hot-fire test, NASA indicated this meeting might take place during the week immediately after the test; but on August 2nd, NASA indicated it would not occur any earlier than the week commence August 5th, so as to allow further review and vetting of the test results. This resulted (again) in a lot of social media driven speculation NASA were about to “abandon” Starliner.

This speculation appears based on unlinking a number of suppositions: that: a) NASA’s delay with the readiness review meeting shows “something is wrong”; b) as NASA is still prepping the four-person Crew 9 for launch to the ISS on August 18th, but doesn’t have room for it to dock (there are only two docking ports on the ISS which can be used by Crew Dragon, one of which is occupied by the vehicle used by the 4-person Crew 8, and the other by Starliner); ergo, c) NASA “must” be considering sending Starliner back to Earth uncrewed, in order to make way for the Crew 9 flight.

While it is true that that data may yet surface that warrants NASA to consider returning Calypso to Earth uncrewed and looking to other means to bring Wilmore and Williams home, there is absolutely no evidence for this being the case at this point in time. Further, it’s actually not the only contingency NASA has at its disposal.

If the confidence in Starliner remains high, but the return cannot be completed until after August 18th (and assuming Crew 9’s launch is not itself delayed), the agency could opt to bring Crew 8 back to earth ahead of the launch of Crew 9. Doing things in this order would not be optimal – but it is possible. However, as it stands, and as Steve Stich, NASA’s Commercial Crew Programme Manager, has made it clear where NASA’s focus for Starliner lies.

I think we’re starting to close in on those final pieces of the flight rationale to make sure that we can come home safely, and that’s our primary focus right now. We have contingency options; NASA always has contingency options … But right now we’re really focused on bringing Butch and Suni home on Starliner.

– NASA Commercial Crew Programme Manager Steve Stich

Outside of this, and following the July 27th tests, Boeing issued its own statement noting that return preparations are underway, and has held an “integrated simulation”  – essentially a full dress rehearsal of Starliner and Calypso’s departure from the ISS and return to Earth, involving ground controllers and Wilmore and Williams in readiness for readying for “potential returns throughout August”.

In addition the ISS crew used the station’s CanadArm 2 robotic arm to complete a visual inspection of Starliner’s exterior – both the Calypso capsule and the service module. Such inspections are a normal part of preparing for a vehicle’s departure from the ISS. All of which seems to underline Boeing and NASA are fully expecting Williams and Wilmore to return to Earth aboard the vehicle.

In the meantime, and in news unlikely to sit well with Boeing shareholders, the continuing issues with the Crew Flight Test have resulted in Boeing taking a further US $125 million charge from NASA. This brings the total amount charged to Boeing as a result of the delays across the entire Starliner programme to US $1.6 billion against NASA payments to Boeing for Starliner development totalling US $5.1 billion.

Space Sunday: observatories, rockets and capsules

An artist’s impression of the Chandra X-Ray Observatory orbiting Earth. Credit: NASA

Twenty-five years ago, on July 23rd, 1999, the Chandra X-Ray Observatory was launched aboard the Space Shuttle Columbia as a part of STS-93. At the time of its launch, it was the third of NASA’s four Great Observatories, the other three being the Hubble space Telescope (HST), launched in 1990; the Compton Gamma Ray Observatory (1991–2000) and the Spitzer Space Telescope launched after Chandra, in 2003 and operating through until 2020.

Originally called the Advanced X-ray Astrophysics Facility (AXAF), Chandra can trace its history back to the mid-1970s. Originally intended for operations in an orbit similar to that of Hubble, thus making its servicing and upgrade possible using the space shuttle, the observatory went through various design changes during the 1980s and 1990s, with its overall mission being redefined in 1992. This saw Chandra have four of it planned 12 mirrors eliminated from the telescope, together with two of the six planned science payloads. To compensate for this, the telescope’s mission was revised so that it could be placed in an orbit well above Earth and well clear of the planet’s radiation belts, allowing it to have a clearer view of deep space.

The Chandra X-ray observatory, wrapped it its thermal protection blanket, attached to its IUS space launcher, images from the space shuttle Columbia shortly after the latter had deployed them from its payload bay, July 23rd, 1999. Credit: NASA

Renamed in 1998 in honour of Nobel Prize-winning astrophysicist Subrahmanyan Chandrasekhar, Chandra was deployed from Columbia’s payload the same day as it launched, attached to a 2-stage Boeing  Inertial upper Stage (IUS) space launch system. Together, they represented the heaviest payload ever carried to orbit by the shuttle system, massing 22.75 tonnes.

Once the shuttle had moved to a safe distance, the IUS first stage fired for 125 seconds, boosting Chandra away from Earth (and beyond any capacity for it to be upgraded or serviced), followed by a 117-second burn of the IUS upper stage motor. The later placed Chandra into a geocentric orbit with a perigee some 14,307.9 km from Earth and an apogee of 134,527.6 km, roughly one-third of the way to the Moon.

Following a short period of commissioning, Chandra started returning data to Earth within a month of launch, and has continued to do so almost without interruption through to 2024 – although its primary mission period was placed at a conservative 5 years. Through this time, only one system on board has suffered significant damage, but it is still operational alongside the other science instruments, and only one significant glitch – lasting three days in October 2018 – when the observatory entered a safe mode as a result of a short-term issue with one of the gyroscopes used for pointing it at targets and holding it steady during observations. All science functions were fully restored once the issue had been resolved.

Chandra X-Ray Observatory diagram. Credit: NASA Chandra Space Centre

Over the years, Chandra’s import and discoveries have tended to be overshadowed by Hubble and, more recently, the James Webb Space Telescope (JWST). These have included the first observations of a “mid-sized” black hole, claimed to be the “missing link” between stellar-sized black holes and the super massive black holes found at the centres of galaxies; making one of the most accurate measurements of the Hubble constant; observing the most massive X-ray flare yet recorded from the super massive black hole Sagittarius A* (pronounced “Sagittarius A star”) at the centre of our galaxy; and making possibly the first observation of an object (possibly an asteroid) crossing the black hole’s event horizon; and also making potentially the first indirect observations of an exoplanet in another galaxy.

In additional to all of this, Chandra has supported Hubble in making significant observations of the planet and dwarf planets and moons in our own solar system, and also like Hubble, has benefitted the work of early career researchers, helping them to become established in the fields of astronomy, astrophysics and space science.

To mark Chandra’s 25th anniversary, NASA has issued a wallpaper featuring 25 of Chandra’s most stunning images captured in the X-ray wavelengths. The official announcement of the images can be found on the Chandra website, and the images are previewed in the video below, as well as being available for download as a wallpaper mosaic for computers.

Sadly, the celebration is a potentially bitter-sweet affair. Currently, Chandra has the ability to remain operational for at least another decade – possibly long enough to see the European Space Agency launch what might be seen as its successor, the Advanced Telescope for High-ENergy Astrophysics (Athena), which is due to be launched sometime in the early-to-mid 2030s. Unfortunately, this is may not now be the case; Chandra could cease operations within the next 12 months.

The reason for this is that NASA’s space science budget is being tightly squeezed, largely as a result of the rising costs associated with Project Artemis and returning humans to the surface of the Moon. In 2024, the space science budget had been due to get a US $500 million boost. Instead, Congress actually cut it by that amount. For 2025, Congress is looking to cut NASA’s space science directorate’s budget by almost US $1 billion.

Cassiopeia A, a supernova remnant 11,000 light-years away, imaged in X-ray & Infrared light, with the x-ray image produced by Chandra. Credit: NASA / ESA / CXC

As a result NASA has been looking at programmes to cut – and Chandra has been one to top the lists, with NASA management suggesting its US $67 million budget could be cut by 40%. The reaction to this was swift, with those managing Chandra both from within and without NASA pointing out that a cut that large would effectively end Chandra’s science mission forthwith. Thus, in an attempt to find some middle ground that would allow both Chandra and Hubble to continued to be operated, various ideas were put forward as to how Chandra’s costs could be reduced and / or how both the Chandra and Hubble science missions could be redefined, in order to allow both to continue for the next few years.

In response to this efforts, NASA authorised an Operations Paradigm Change Review (OPCR) to look at all of the suggested options and make a determination on their viability to reduce costs. The findings of this review were presented on the very day of the 25th anniversary of Chandra’s launch, during a meeting of the Astrophysics Advisory Committee, or APAC, the body, chartered to provide advice to NASA’s astrophysics programme. And the news was not good.

Having reviewed all the options weighted the costs and saving, the OPCR has essentially concluded that while they believe Chandra could be operated a a budget smaller than its present allocation, it would still require funding beyond what the new science directorate budget can afford – at least not without putting programmes and missions outside of it and Hubble at risk. Therefore, it may not be feasible for Chandra to continue from 2025 onwards.

When a massive star exploded in the Large Magellanic Cloud LMC), a satellite galaxy to the Milky Way, it left behind an expanding shell of debris called SNR 0519-69.0. This image shows a composite of the debris gas field using Chandra to reveal the multimillion degree gas cloud (blue) and Hubble to reveal the expanding edge of the explosion (red) and the stars of the The outer edge of the explosion (red) and stars of the LMC. Credit: NASA / STScl / CXC

The OPCR findings drew some frustration from APAC members, in part because APAC was itself excluded from any involvement in the OPCR process and was not given the opportunity to review the report ahead of the announcement. In response, OPCR members stated the review had to be handled on a short-term turn-around so that if a way forward could be identified and which offered a reasonable compromise on costs, it had to be published rapidly, so as to allow NASA and the agencies responsible for both Chandra and Hubble (the Chandra X-Ray Centre and Space Telescope Science Institute) to assess the overall feasibility ahead of staff layoffs across both programmes that are due to commence in September 2024.

The report does not automatically seal Shandra’s fate, options may yet arise where it is allowed to continue – such as through the support of one or both of the houses in Congress – but right now, it does make Chandra’s future appear to be grim.

SpaceX Resumes Starlink Flights with Falcon 9; Announces Dragon Splashdowns to Move back to US West Coast

In my previous Space Sunday article, I noted that SpaceX Falcon 9 flights were suspended pending the results of a Federal Aviation Administration (FAA) Mishap Investigation relating to the loss of a Falcon 9 upper stage and its Starlink payload during a July 11th/12th launch.

On July 25th, SpaceX announced the root cause of the loss had been traced to fatigue causing a a crack in a redundant “sense line” in the upper stage, resulting in “excessive cooling” of engine components, causing the rocket motor to fail. A near-term fix – removing the redundant line – has been identified pending a more in-depth fix, and this has been enough for the FAA to clear Falcon 9 to resume commercial launches. As a result, on July 27th, a Falcon 9 lifted-off from Kennedy Space Centre’s Launch Complex 39A, carrying 23 of the company’s own Starlink satellites.

One Falcon 9 stands on the pad at Space Launch Complex 40 while another lifts off from nearly by Launch Complex 39A early July 27th, 2024, marking the resumption of non-NASA related Falcon 9 launches. Credit: SpaceX

Whilst successful, the flight does not mean Falcon 9 flights to the International Space Station will necessarily immediately resume. NASA still plans for a “rigorous certification” of Falcon 9 and the software associated with the sensor to which the sense line had been connected, once SpaceX has completed all modifications to the upper stage of the vehicle. As such, the agency is not committing to going ahead with the launch of the 4-person Crew 9 mission to the ISS, due to lift-off on August 18th, 2024. However, whether this also means the planned launch of an automated Cygnus resupply vehicle to the station due on August 3rd remains on hold, is unclear; NASA’s had previously indicated all Falcon 9 flights to the ISS would be suspended pending re-certification, but following the July 27th launch, the agency specifically only mentioned the Crew 9 flight.

In a separate press release, SpaceX has indicated it will be switching Dragon splashdowns to off the west coast of the United States from 2025 onwards, rather than bringing them down off the Florida coast.

The decision is in the wake of significant pieces of debris from the Dragon vehicle’s trunk (effectively the power and propulsion “service module”) surviving re-entry into the denser atmosphere to fall to ground in places as wide apart as Australia, North Carolina and Saskatchewan. The change means that from 2025, instead of being used in the initial de-orbit burn and and then jettisoned from the Dragon capsule, which then performs its own final de-orbit burn, leaving the trunk to decay in its orbit and later re-enter the atmosphere a burn up, dragon vehicles will remain attached to the trunk throughout both de-orbit burns, with the trunk being jettisoned just before both reach the re-enter interface.

This means the the capsule and trunk will come down over the Pacific Ocean, rather than passing over the North American continent, with any trunk debris surviving its re-entry hitting the water somewhat up-range from where the capsule will splash down under parachutes.

Boeing Starliner Remains at ISS Amidst More Media Alarmism

The past week saw NASA provide an update on the Boeing Starliner situation, in which the CST-100 Calypso remains docked at the International Space Station, where it has been for some 50 days, despite the first planned crewed flight of the vehicle only being intended to last some 6 days in total following its launch in early June 2024.

As noted previously in these pages, issues occurred during the vehicle flight to the ISS, when it suffered a series of thruster failures – an issue that has been dogging the Starliner programme for some time. While the vehicle, carrying astronauts Barry “Butch” Wilmore and Sunita “Suni” Williams managed to safely docked with the ISS, its return has been repeatedly delayed leading to highly inaccurate references in the media and on social media to the idea that Wilmore and Williams are somehow “stranded” in space.

A time-lapse photograph of the CST-100 Starliner Calypso docked at the International Space Station as both orbit the Earth. Credit: NASA

This is far from the case, again as I noted as recently as June 30th (see: Space Sunday: of samples and sheltering); the delays have been purely to allow Boeing and NASA to conduct further comparative tests between systems on the ground and those aboard the Starliner docked at the ISS to better understand precisely where the issue lies. These tests are necessary inasmuch as the service module of the vehicle – which is home to the problematic thruster systems –will not be returning to Earth, but will burn-up in the atmosphere when Calypso does eventually make its return. Ergo, keeping it in space and carrying out these tests is the only means of verifying the findings of on-going Earthside investigations.

With further tests taking place over the weekend of July 27th/28th, both NASA and Boeing believe they are honing into on the root cause. Starliner has four clusters of thrusters gathered around the outside of the service module. These clusters, comprising a mix of four larger orbital manoeuvring and attitude control (OMAC) thrusters and smaller reaction control system (RCS) thrusters (28 in total, of which only one has completely failed) are housed in protective units call “doghouses”. Both the OMACs and RCS units are required during flight operations, often firing in sequence.

What appears to be happening is that under orbital conditions, pulse-firing the RCS thrusters (a rapid series of short, sharp burst of firing) immediately following the use of the OMACs thrusters in a doghouse can cause the temperatures inside the unit to rise well above anticipated levels. This causes the helium purge valves to leak, causing problems.

Boeing’s Starliner capsule is seen docked to the International Space Station in this zoomed-in and slightly pixelated view of an image captured by Maxar Technologies’ WorldView-3 satellite on June 7th, 2024. Credit: Maxar Technologies

Because of this, engineers, together with Wilmore and Williams, have been looking to make operational changes to how the OMCS and RCS system are used – such as by reducing the number of pulses the RCS makes when fired, or by reducing the number of times OMACs and RCS need to be fired either individually or in sequence, thus preventing the temperature spikes within the doghouse units.

During the update, NASA clearly stated that if the July 27th/28th tests yield good results, then an agency-level review on clearing Starliner for a return to Earth could take place within a week of the test results being confirmed. However, this still didn’t stop some media continuing to report Wilmore and Williams as continuing to be “stuck” or “stranded” in orbit, because drama maketh the headline.

Space Sunday: of “planet” and planets

Celestial bodies from our solar system and beyond – although technically, only two meet the current IAU definition of the term “planet”. Credit: NASA

What is a “Planet”? This might sound like a catch question, but in fact it has been the cause for debate for almost two decades at least, and its roots go back as far as – wait for it – 1801.

Up until the start of the 21st century, everyone was reasonably comfortable with the idea of what a planet was: we’d discovered a total of nine making their way around our star over the previous centuries, including the somewhat oddball Pluto. The general (and informal) agreement was that a “planet” was that of a large, roundly spheroid / round object moving in an orbit around the Sun.

Then, in 1801 Ceres was discovered. Whilst tiny by comparison to the like of our Moon, it was nevertheless almost circular in shape and bumbling around the Sun in its own orbit. Hence, many argued, it was a planet – that in fact it was the so-called “missing planet” believed to exist between Mars and Jupiter. However, by 1851 the discovery of yet more bodies within this region of space had pushed the total number of “planets” in the solar system to 23; the eight large planets of Mercury through Neptune, and all these “little” planets, many of which weren’t entirely circular in shape (but others, like Juno, Vesta and Pallas) came pretty close. It was also clear the number was liable to keep on growing.

Thus, astronomers started cataloguing these smaller bodies in their own right and, effectively, the idea of the asteroid belt was born, with Ceres becoming the first asteroid within the belt to be discovered. Problem solved; not even Clyde Tombaugh’s discovery of Pluto in 1930 didn’t upset this approach too much, nor the definition of “satellite / moon”. But then in 1978, someone had to go and find Pluto’s Moon Charon, a body so large, it broke the traditional view of a “moon”, coming close to being a twin planet to Pluto. Then, in 2005, Eris was discovered, and the wheels really started coming off the wagon.

Whilst two other relatively large, “planet-like” Kuiper Belt bodies had been discovered orbiting the Sun – Quaoar (2002) and Sedna (2004) – prior to Eris, they were comparatively small and easy to lump into the “asteroid” container alongside Ceres. But Eris turned out to be around the size of Pluto, and more massive; so, either it was a planet (and was actually referenced the “tenth planet” of the solar system immediately following its discovery) – or Pluto wasn’t a planet. Cue astronomical bun fight.

Planets, dwarf planets, satellites, oh my! Credit: M. Özgür Nevres

The fight between classifying Eris as a planet or downgrading Pluto to “not a planet” became quite heated relatively quickly, prompting much debate within the International Astronomical Union (IAU) which wrestled mightily with the question of how all the various celestial bodies in the solar system should be formally classified – starting with was should be meant by “planet”.   In the end, and possibly fearful of the sudden blossoming of planetary bodies within the Kuiper Belt following the discovery of Eris, as had been seen 200 years ago with the asteroid belt following the discovery of Ceres, in 2006 the IAU settled on the side of downgrading Pluto’s status from “planet” to “dwarf” planet.

In doing so, the organisation also sought to ratify the term “planet”, eventually settling on three criteria, published under what id now referred to as Resolution 5B, as found within GA26-5-6. Clause 1 of which holds:

Is it a dwarf planet? A TNO? A Plutoid? An Euler Diagram showing the IAU Executive Committee conception of the types of bodies in the Solar System during the 2006 General Assembly. Credit: Holf Weiher

A planet is a celestial body that:

  • is in orbit around the Sun;
  • has sufficient mass so as to assume hydrostatic equilibrium (aka “a round shape”);
  • has “cleared the neighbourhood” around its orbit.

The decision caused (and still causes) a lot of emotional upset where Pluto is concerned, and this masked a potentially bigger issue with Resolution 5B-1: be defining a planet and a “celestial body orbiting the Sun”, it immediately excluded the term being formally used with regards to planets orbiting other stars.

Oops.

In fairness, while astronomers have been locating exoplanets since 1992, by the time the IAU arrived at their definition in 2006 the number discovered was measured in the handful, so considering them didn’t really factor into the IAU’s thinking. Since then, of course, things have changed dramatically: we’re fast approaching 6,000 planets known to be orbiting other stars.

Again, being fair to the IAU, they did try to address the issue of exoplanets (the term simply means planet outside the solar system, rather than having any meaningful definition) in 2018. However, the effort never got beyond the “working” phase. In fact, the 2018 discussions revealed that even when applied to just the solar system, Resolution 5B-1 was pretty woolly and unquantifiable; something better was needed. Things weren’t much better by the time of the next IAU General Assembly in 2021.

Potentially, the best way to offer a properly unquantifiable definition for planets wherever they might be found, do this is via mathematical modelling, removing any subjectivity from how both the term and planets are defined.

This is precisely what a team from the USA and Canada has attempted to do. AS they note in their study, published in The Planetary Science Journal, they sought to break down the the potential taxonomy of planetary bodies – both solar and extra-solar – in terms of critical physical characteristics: mass, density, etc., local dynamical dominance within their orbits, the bodies they orbit (single stars, brown dwarfs, binary systems, etc.). Using mathematical models to quantify these measures, they have been able to show that celestial bodies tend to fall in to distinct clusters, and this has enabled them to develop a far more quantifiable definition of the term “planet”, thus:

A planet is a celestial body that:
a.       Orbits one or more stars, brown dwarfs or stellar remnants and
b.       Is more massive than 1023 kg and
c.       Is less massive than 13 Jupiter masses (2.5 x 1026 kg)

This definition is due to be presented at the 32nd IAU General Assembly being held in Cape Town, South Africa in August. If adopted, it will establish a meaningful framework by which planets, dwarf planets and natural satellites – wherever they might be found – can be quantitatively defined in  manner that could objectively, rather than subjectively, help shape our understanding of the universe and our place in it.

VIPER Cancelled

On July 17th, NASA announced it has cancelled its Volatiles Investigating Polar Exploration Rover (VIPER) mission due to cost increases and schedule delays.

Roughly the size of a golf cart (1.4m x 1.4m x 2m), VIPER was a relatively lost-cost (in the overall scheme of things) rover charged with an ambitious mission: to carry out extensive prospecting the permanently shadowed areas of the Moon’s South Polar Region, seeking resources and mapping the distribution and concentration of water ice. However, the project has been repeatedly hit by delays and increasing costs, both with the rover (built by NASA) and its Griffin lander vehicle, supplied by commercial space company Astrobotic Technology Inc., and which was due to fly with additional payloads to the rover.

VIPER (Volatiles Investigating Polar Exploration Rover) was to be robotic lunar rover tasked to prospect for natural lunar resources within a permanently shadowed region near the lunar south pole. Rendering credit: NASA

In 2022, these delays resulted in the mission being pushed back to a late 2024 launch date from a planned 2023 date. This was then further pushed back to September 2025. At the time this decision was made, the overall cost for the rover had risen from US $250 million to US $433.5 million and would likely exceed US $450 million by the 2025 launch date. More recently, a review found that whilst the rover is largely completely, it has yet to undergo environmental testing and still lacked proper ground support systems, noting that delays with either of these could quickly eliminate any chance of meeting the 2025 launch date and push the costs up even further.

At the same time, the cost to NASA for the development of the Griffin lander has risen by over 30% (from some US $200 million to US $323 million). These are likely to rise even further as a result of NASA’s requested additional testing of the lander in the wake of the January failure with Astrobiotic’s smaller Peregrine One lunar lander, test which could have also impacted the lander’s readiness for a 2025 launch.

VIPER being assembled in a clean room at NASA’s Johnson Space Centre, Texas. Credit: NASA

The problem here is that the VIPER mission can only be launched at certain times in order to capitalise on favourable lighting conditions in its proposed landing zone; any delay beyond November 2025 for mission launch would therefore mean the mission could not take place until the second half of 2026. As a result, overall costs for the mission could be nudging US $1 billion by the time it is launched. Given NASA’s overall science budget for 2025 has already been tightly constrained by Congress, this was seen as unacceptable by the review board, as it potentially meant putting other missions at risk. Ergo, the decision was made to cancel VIPER.

That said, the Griffin lander flight to the Moon will still go ahead with NASA support, allowing it to fly its planned commercial payloads, together with a payload simulator replacing the rover. In addition, NASA is also seeking to get the rover to the Moon by offering it to any USA company and / or any of NASA’s international partners willing to fly it to the Moon at their own cost. If no such offers are received by August 1st, 2024, then the rover will be dissembled and its science instruments and other components put aside for use with other missions.

NASA Confirms Use of SpaceX for ISS Deorbit Whilst Suspending  Falcon 9 Station  Launches

On July 17th, 2024, NASA supplied further information on the planned use of SpaceX hardware to de-orbit the International Space Station (ISS) when it reached its end of life in 2030, whilst simultaneously effectively suspending SpaceX launches to the space station pending its own review of Falcon 9 following the recent loss of a Falcon 9 upper stage and its payload.

NASA originally awarded the contract for the United States Deorbit Vehicle (USDV) – the vehicle that will physically de-orbit the ISS – was awarded to SpaceX on June 26th, 2024 with little in the way of specifics, other than NASA aimed to obtain the vehicle for no more than US $843 million. In the more recent statement, NASA confirmed that SpaceX will provide NASA with an “enhanced” version of their Dragon vehicle, comprising a standard capsule with a lengthened “trunk” (the service module providing propulsion and power) equipped with a total of 46 Draco motors and 16 tonnes of propellants.

An artist’s impression of the enhanced SpaceX Dragon docked with the Harmony module on the International Space Station and using its Draco engines to de-orbit the station. Credit: SpaceX

Under NASA’s plans, the USDV will be launched prior to the final crew departing. At this point, the station’s orbit will be allowed to naturally decay to around 330 km, at which point the last crew will depart. The station’s orbit will then be allowed to decay for a further six months prior to the USDV being used to orient the ISS for re-entry in a manner that will see much of the station burn-up in the atmosphere, and what survives falling into the south Pacific.

The contract awarded to SpaceX is for the Dragon vehicle only, not for its launch or operation; on completion, the vehicle will be handed over to NASA to operate. However, given the 30-tonne mass of the USDV and the fact it is a Dragon vehicle makes the SpaceX Falcon Heavy a strong contender as a potential launch vehicle (unless superseded by the company’s Starship / Super Heavy combination by the time USDV is ready for launch).

In the meantime, NASA has suspended all Falcon 9 launches to the ISS pending their own reauthorisation review in the wake of the July 11th loss of a Falcon 9 upper stage and its payload of Starlink satellites.

That loss is already under investigation on behalf of the US Federal Aviation Administration, however, on July 17th, NASA confirmed it will carry out its own review once the FAA’s work in concluded, although preparations for upcoming flights – notably a launch of a Cygnus resupply vehicle via Falcon 9 due on August 3rd and the launch of the Crew 9 rotation due later in August – will continue.

Screenshot from the webcast of a SpaceX Starlink launch on July 11th, 2024, showing a build-up of white material on the upper stage of a Falcon 9 rocket. This is thought to be ice from a liquid oxygen propellant leak, and may have led to the loss of the vehicle. Credit: SpaceX

The suspension of operations is normal when a launch vehicle utilised by the space agency is involved, and NASA made it clear that none of the crew currently on the ISS are in danger or at risk of running out of supplies.

SpaceX has sought to limit the impact of the FAA investigation citing that given the fault occurred in the vehicle’s upper stage and when it was entering orbit, it posed no threat to public safety and so other launches should not be discriminated against as a result. However, NASA has indicated that even if the FAA agreed with SpaceX and allowed Falcon 9 launches to continue during the mishap investigation, the NASA suspension of operations would remain in place until such time as its own review has been completed.

Crew safety and mission assurance are top priorities for NASA. SpaceX has kept the agency informed as it works closely with the Federal Aviation Administration throughout the investigation, including the implementation of any corrective actions necessary ahead of future agency missions. NASA and its partners also will implement the standard flight readiness review process to ensure we fly our crew missions as safely as possible.

NASA statement on ISS-related Falcon 9 launches in the wake of the July 11 loss of a Falcon 9 upper stage