Space Sunday: back to Mars with NASA and SpaceX

CuriosityIt’s been a while since there has been any major news from NASA’s Curiosity rover as it explores “Mount Sharp” in Gale Crater.

The last time I covered the rover’s activities, it was investigating a series of sand dunes which are slowly descending down the slopes of “Mount Sharp” as a result of a combination of gravity and wind action.

This work was completed in March, when the rover resumed its progress up the flank of the mound, climbing onto “Naukluft Plateau”, a roughly flat area cut into the side of “Mount Sharp” where aeons of wind erosion has carved the sandstone bedrock into ridges and knobs which were thought could offer a challenge for the rover in terms of wear and tear on the wheels.

The plateau lay between the rover and the next major area of scientific interest for the mission, so the drive team have been edging the rover across the rough terrain in the hope of reaching smoother ground on which it can continue upwards without exposing its six aluminium wheels to risk of severe damage.

 "Naukluft Plateau", which Curiosity has been traversing since March 2016, shown in close-up, revealing how the surface has been shaped and scoured by the wind over the aeons. In the distance can be seen the rim hills of Gale Crater
“Naukluft Plateau”, which Curiosity has been traversing since March 2016, shown in close-up, revealing how the surface has been shaped and scoured by the wind over the aeons. In the distance can be seen the rim hills of Gale Crater. This image was captured om April 4th, 2016, the rover’s1,302nd Sol (Credit: NASA / JPL)

The roughness of the terrain on the plateau had raised concern that driving on it could be especially damaging to Curiosity’s wheels, as it is very similar to terrain the rover crossed in 2013 while en route to “Mount Sharp”, resulting in visible damage to some of Curiosity’s wheels, punching holes and tears into the aluminium, and prompting the mission team to undertake extensive tests on the wheels and their performance following such damage, using a duplicate of the rover here on Earth.

Because of the previous damage caused to the wheels, Curiosity was instructed to periodically image the condition of its wheels during the drive, a process which slowed progress but also revealed any damage being caused was not accelerating beyond what was projected to occur.

“We carefully inspect and trend the condition of the wheels,” said Steve Lee, Curiosity’s deputy project manager. “Cracks and punctures have been gradually accumulating at the pace we anticipated, based on testing we performed at JPL. Given our longevity projections, I am confident these wheels will get us to the destinations on Mount Sharp that have been in our plans since before landing.”

This image taken on April 18th, 2016 (Sol 1,315) by the Mars Hand Lens Imager (MAHLI) camera on the rover's robot arm revels areas of damage on Curiosity's centre left wheel, the result of periodically traversing very rough terrain since the rover arrived on Mars in 2012
This image taken on April 18th, 2016 (Sol 1,315) by the Mars Hand Lens Imager (MAHLI) camera on the rover’s robot arm revels areas of damage on Curiosity’s centre left wheel, the result of periodically traversing very rough terrain since the rover arrived on Mars in 2012 (Credit: NASA / JPL)

In particular, the mission team is watching for breaks or tears which damage the zig-zag treads – called grousers – on the 50cm / 20 in wheels. If three of these grousers are significantly broken, Earth-based tests suggest the damaged wheel will have reached about 60% of its serviceable life.

However, since Curiosity’s current odometry of 12.7 km (7.9 mi) is about 60 percent of the amount needed for reaching all the geological layers planned in advance as the mission’s science destinations, and no grousers have yet broken, the accumulating damage to wheels is not expected to prevent the rover from reaching those destinations on Mount Sharp.

“Naukluft Plateau” is a part of the larger “Stimson formation” which includes a fracture area the rover reached a late April. Dubbed “Lubango”, the area was the target for the rover’s 10th drilling and sample gathering campaign, which was completed on Sol 1320, April 23rd, 2016.

“We have a new drill hole on Mars!” reported Ken Herkenhoff, a MSL science team member, when reporting on the sample gathering in an MSL update on April 28th.

After transferring the cored sample to the CHIMRA instrument for sieving it, a portion of the less than 0.15 mm filtered material was successfully delivered this week to the CheMin miniaturized chemistry lab situated in the rover’s body, which is now analysing the sample and will return mineralogical data back to scientists on earth for interpretation.

“Lubango” was selected for sample gathering after it had been determined following examination using the ChemCam laser and spectrometer,  that it was altered sandstone bedrock and had an unusually high silica content.  To complement the analysis of “Lubango”, the science team has been using the rover’s camera systems to locate a suitable target of unaltered Stimson bedrock as the 11th drill target.

“The colour information provided by Mastcam is really helpful in distinguishing altered versus unaltered bedrock,” MSL science team member Lauren Edgar explained in describing the current work. One possible target, dubbed “Oshikati” has been identified.

A white-balanced telephoto view of Gale Crater's rim, as seen from the flank of "Mount Sharp"
A white-balanced telephoto view of Gale Crater’s rim, as seen from the flank of “Mount Sharp” (Credit: NASA / JPL)

The ChemCam laser has already shot at the “Oshikati” to gather data for an initial analysis of the rock and assess its suitability for drilling operations. If all goes according to plan, Curiosity should make an attempt to gather samples from the rock on Sunday, May 1st.

SpaceX To Launch NASA-Supported Mars Mission in 2018

On April 27th, SpaceX announced it plans to launch an automated mission to Mars in 2018 as a part of a new space act agreement the company has signed with NASA. This will see the US space agency provide technical support to SpaceX with respect to an automated landing of a SpaceX vehicle on Mars, and provide scientific support for the mission.

an artist's impression of Red Dragon arriving on Mars (credit: SpaceX)
An artist’s impression of Red Dragon arriving on Mars (credit: SpaceX)

SpaceX will undertake the mission using Red Dragon, an automated version of the Dragon 2 capsule vehicle which will enter service in 2018 to fly crews two and from the International Space Station.

Red Dragon has been on the drawing boards at SpaceX almost since the inception of the Dragon 2 programme. Designed to be launched atop the upcoming Falcon 9 Heavy launcher, due to enter operations later this year, it is specifically intended to carry science payloads almost anywhere in the solar system, and could potentially deliver as much as 4 tonnes of cargo to the surface of Mars (that’s  the equivalent of delivering 4.5 Curiosity rovers to Mars in one go).

The 2018 mission is primarily intended to look at using a purely propulsive means of achieving a soft landing of a heavy vehicle on Mars. While parachutes could, in theory, be used to help slow a vehicle’s descent through the Martian atmosphere, recent NASA tests of the kind of large-scale “supersonic” parachutes required to slow large space vehicles during their descent haven’t proved overly successful during comparable testing at high altitude on Earth.

The Falcon 9 Heavy, which could lift scientific payloads aboard the Dragon 2 carrier vehicles almost anywhere in the solar system - compared to the current Falcon 9 (Credit: SpaceX)
The Falcon 9 Heavy, which could lift scientific payloads aboard the Dragon 2 carrier vehicles almost anywhere in the solar system – compared to the current Falcon 9 (Credit: SpaceX)

Dragon 2 has been specifically designed so that a series of 8 rocket engines – called Super Draco motors – are embedded in the base of the vehicle. These can be used both as a launch abort system – firing a crew clear of a malfunctioning rocket during lift-off –  and as a means of the vehicle achieving a “soft landing” on land rather than splashing down in the ocean (although the Dragon 2 is capable of this as well).

On Red Dragon, these super Draco motor allow the vehicle to slow itself down through its descent through the tenuous Martian atmosphere, and then act as a final cushioning break as the craft comes into land. Tethered tests here on Earth have already demonstrated Dragon 2 is fully capable of maintaining a hover until the thrust from the engines, and these tests will be expanded upon during the run-up to the mission.

The Red Dragon initiative is a commercial endeavour, funded entirely by SpaceX. NASA will not be contributing to the cost of the mission, but will be providing Earth-side logistical support and a suitable science payload of around 1 tonne. The exact nature of this payload will be defined in the future,  but will likely include a diverse range of instruments which might be used to further characterise the Martian atmosphere, study and Martian weather and soil, and image the surface of Mars. Both SpaceX and NASA will share the data gathered during what is referred to as the EDL phase of the mission – the Entry, Descent and Landing. NASA will also supply a scientific payload for the flight.

Red Dragon marks the first phase of an ambitious programme SpaceX will be announcing in September, but which has been under development for about the last 6 years, for undertaking human missions to Mars in the 2020 / 2030s. I’ll have more on this later in the year.

Space Sunday: China’s ambitions, Dawn’s success and Kepler’s return

China's space station, as it should look in 2022 (credit: China Manned Space Engineering)
China’s space station, as it should look in 2022 (credit: China Manned Space Engineering)

China has confirmed a series of ambitious new goals for its growing space endeavours, starting with the launch later this year of a new orbital facility, and progressing through 2018 with the launch of the core module for a large-scale space station, and which includes further mission to the Moon and to Mars.

The first orbital facility launched by China, Tiangong-1 (“Heavenly Palace-1”), was launched in 2011. Referred to as a “space station”, the unit was more a demonstration test-bed for orbital rendezvous and docking capabilities. While it was visited by two crews in 2012 and 2013, neither stayed longer than 14 days, and sinc 2013,  Tiangong-1 has operated autonomously, although it has suffered a series of telemetry failures in that time.

A model of Tiangong-2, which will be 14.4 metres (47 ft) in length, 4.2 metres (14 ft) in diameter and mass 20 tonnes, seen docked with a crewed Shenzhou ("Divine Craft") orbital vehicle on the left (Credit: unknown originating source)
A model of Tiangong-2, which will be 14.4 metres (47 ft) in length, 4.2 metres (14 ft) in diameter and mass 20 tonnes – almost 3 times the mass of the Tiangong-1 unit, seen docked with a crewed Shenzhou (“Divine Craft”) orbital vehicle on the left (Credit: unknown originating source)

Tiangong-2 will be launched later in 2016, and is designed to build on the experiences gained with the original facility, helping to pave the way for China’s first “genuine” space station. In particular, Tiangong-2 will provide an experiments bay, improved living facilities for longer-during stays, and allow China to verify key technologies such as propellant refuelling while in orbit, and undertake fully automated docking activities using uncrewed vehicles, when the nation’s first automated resupply vehicle, Tianzhou-1 (“Heavenly Vessel-1”) docks with the facility in 2017.

Tiangong-2 will be followed, in 2018 by the launch of the larger Tianhe-1 (“Sky River-1”) unit, which will form the core module for China’s first dedicated space station. Over the four years from 2018, this will grow with the addition of up to three other pressurised modules,  together with a docked “Hubble-class” space telescope. It be supported and maintained by automated re-supply mission from Earth using the Tianzhou, and provide living and working space for up to 6 crew,

A prototype model of the propsed Mars rover China plans to launch in 2020 as part of a 3-phase mission involved an orbiter / carrier vehicle, a static lander and the rover (credit:
A prototype model of the proposed Mars rover China plans to launch in 2020 as part of a 3-phase mission involved an orbiter / carrier vehicle, a static lander and the rover (credit: China National Space Administration)

Nor does it end there. At the end of March, I wrote about China’s aggressive approach to Mars exploration.

As a part of the series of announcements made by the Chinese authorities in the run-up to their first national Space Day on April 24th, 2016 – being the anniversary of the launch of China’s first satellite, Dongfanghong-1 (‘The East is Red’) – it was confirmed that the planned orbiter / rover mission to the red planet will be launched in 2020.

The rover element of the mission will build on experience gained during the deployment and operation of the Yutu vehicle on the Moon in 2013, and will be used to investigate the planet’s soil, atmosphere, environment, and look for traces of water.

As part of the preparations for this mission – although it is also a mission in its own right – China plans to land the its Chang’e-4 (“Moon Goddess”) probe, on the far side of the Moon in 2017, an operation which will be carried out fully autonomously of Earthside intervention.

To ensure all this happens, China is developing two new launch vehicle – the Long March 5 and the Long March 7. The Long March 5 will form the backbone of China’s space activities, offering a family of 6 launch vehicle variants, the largest of which will be capable of placing up to 25 tonnes in low Earth orbit (LEO), 14 tonnes in geosynchronous transfer orbit (GTO) for missions to the Moon, Mars or elsewhere, putting it in the same class of launch vehicles as America’s Atlas V and Delta IV launchers, and the commercial SpaceX Falcon 9 launcher.

Using non-toxic and pollution-free propellant, the 60-metre-long vehicle has a core diameter of 5 metres, and will be equipped with four strap-on booster 3.5 metres in diameter, Long March 5 is the first of China’s launch vehicles to specifically designed for both cargo / satellite launches and crewed mission launches.  The maiden flight of the vehicle is expected to be the Chang’e-4 mission to the far side of the Moon.

China's Long March 5 (l) and Long March 7 (r) next generation launch vehicles
China’s Long March 5 (l) and Long March 7 (r) next generation launch vehicles (credit: Sina Weibo)

The Long March 7 vehicle will be slightly smaller, capable of lifting 13.5 tonnes to LEO, although this will be enhanced over time to allow the vehicle to lift up to 20 tonnes to LEO. It will form the launch vehicle for the  Tianzhou resupply missions to Tiangong-2 and Tianhe-1, and over time will be uprated to crewed launch vehicle status. It is slightly smaller than the Long March 5, with a height of 53 metres, a core diameter of 3.35 metres, and used 4 2.25 metre diameter liquid-fuelled strap-on boosters. The first launch of a Long March 7 vehicle is expected later in 2016, when it lifts Tianzhou-1 for a rendezvous with Tiangong-2.

Continue reading “Space Sunday: China’s ambitions, Dawn’s success and Kepler’s return”

Space Sunday: BEAM and Kepler, Europa and comets

Euorpa's icy, mineral-stained surface as imaged by NASA's Galileo mission - see bwlow (credit: NASA / JPL)
Euorpa’s icy, mineral-stained surface as imaged by NASA’s Galileo mission – see below (credit: NASA / JPL)

In my last Space Sunday article, I covered the arrival of the BEAM inflatable module at the International Space Station, and the concerns for NASA’s Kepler “planet hunter” space observatory. As there’s been further news on both of these, I thought I’d start this Space Sunday with a quick round-up on them, starting with Kepler.

The Kepler observatory, located some 121 million kilometres (75 million miles) “behind” Earth as both orbit the Sun, has been engaged in a 7-year mission to try to locate planets – particularly possible Earth-type planets – orbiting other stars. As I reported last time around, despite one major setback which called a halt to the observatory’s primary mission in 2012, Kepler has been a remarkably successful mission, catalogue some 4,000 potential planets orbiting other suns, with over 1,000 subsequently confirmed as planets.

However, on April 7th, Kepler reported to mission managers that it has entered Emergency Mode – a status indicating a critical problem has occurred, causing the observatory to shut down all science operations and other systems, and was utilising its supplies of valuable propellant to maintain its orientation so it could communicate with Earth, rather than using its electric reaction wheels, powered by sunlight.

Keler 425b - the first Earth-like planet to be found orbiting within its sun's habitable zone
Keler 425b – the first Earth-like planet to be found orbiting within its sun’s habitable zone (credit: NASA)

Over the next several days, mission engineers were able to upload instructions to Kepler so that it could position itself in a “point rest state” where communications could be maintained without eating into further propellant reserves. Following this, a long, slow data download commenced, which allowed engineers to fully understand the extent of the problem – but not the cause. However, this has been enough for a path to recovery to be determined.

Kpler: being nursed back to health from 121 million km away
Kpler: being nursed back to health from 121 million km away (credit: NASA)

Since April 12th, commands have been sent to the observatory instructing it to bring it non-critical systems back on-line one at a time, monitoring responses as it did so. With each system successfully restored, Kepler has been gradually coming to life whilst eliminating potential causes of the original problem. There is still a way to go, but mission managers are now reasonably confident Kepler can be restored to a fully operational status.

“The recovery started slowly and carefully, as we initially merely tried to understand the situation and recover the systems least likely to have been the cause,” said Kepler programme manager Charlie Sobeck on April 14th. “Over the last day and a half, we’ve begun to turn the corner, by powering on more suspect components. With just one more to go, I expect that we will soon be on the home stretch and picking up speed towards returning to normal science operations.”

Meanwhile, BEAM – the Bigelow Expandable Activity Module – an inflatable prototype habitat module which arrived at the International Space Station on April 10th – was extracted from its ferry vehicle, the uncrewed Dragon resupply vehicle, on Saturday April 16th, and successfully secured against the airlock node of one of the station’s modules.

the extraction and relocation were undertaken remotely, using the space station’s robot arm commanded from Earth to lift the BEAM unit, still in its compact “flight” configuration just 2.4 metres (8ft) in length and 2.1 metres (7ft) diameter, from the unpressurised section of the Dragon cargo vehicle and then position it against the US Tranquillity Module of the space station, where it was secured by astronauts Tim Kopra and Jeff Williams.

Space station commander Tim Kopra took this photograph of the BEAM unit, in its compact state, being moved towards the Tranquillity module by the station's robot arm, ready for it to be secured against one of the station's airlocks
Space station commander Tim Kopra took this photograph of the BEAM unit, in its compact state, being moved towards the Tranquillity module (seen on the left, directly under the robot arm) by the station’s robot arm, ready for it to be secured against one of the station’s airlocks (credit: NASA / Tim Kopra)

The module is not due to be inflated until early May, when it will increase in size to some 4m x 3.5m (13ft x 10.5ft) and provide some 16 cubic metres (565 cubic ft) of working space. It will be equipped with monitoring equipment  to investigate how well it protects against solar radiation, space debris and contamination over a 12-18 month period. During this time, ISS crew members will enter the unit 3 or 4 times a year to collect deployment dynamics sensor data, perform microbial surface sampling, conduct periodic change-out of the radiation area monitors, and inspect the general condition of the module.

BEAM-animation
Animation showing the manoeuvre to position BEAM against the Tranquillity module

Continue reading “Space Sunday: BEAM and Kepler, Europa and comets”

Space Sunday: Of Odysseys, rockets, inflatables and exoplanets

Mars Odyssey: 15 years since launch and still going strong
Mars Odyssey: 15 years since launch and still going strong

Fifteen years ago, on April 7th, 2001, NASA launched their Odyssey mission to Mars. Since then, this orbital vehicle, whilst often overlooking in favour of its younger companions, Mars Express from Europe and NASA’s Mars Reconnaissance Orbiter, has done much to revolutionise our understanding of Mars.

Named for 2001: A Space Odyssey, the seminal science-fiction novel by Arthur C. Clarke, Odyssey arrived in orbit around Mars in October 2001. In doing so, not only did it overcome the failures of the 1999 Mars Climate Orbiter and Mars Polar Lander missions, it almost immediately scored its own major success: one suite of instruments found evidence for water ice close to the surface in large areas of Mars – as significant finding which has since gone on to shape much of our thinking about what lies within the Martian crust.

In 2010, Odyssey provided the highest-resolution (at that time) global map of Mars, stitched together from 21,000 images returned by the Thermal Emission Imaging System (THEMIS). Prior to that, in 2008 Odyssey spotted evidence of salt deposits across about 200 places in the south of Mars. NASA considers these areas to be signs of where abundant water used to sit. Scientists theorized the deposits could come from groundwater, which evaporated and left deposits of mineral behind. While in 2007, Odyssey imaged what appeared to be massive cave mouths on the surface of Mars.

THEMIS confirmed the openings – each between 100 to 250 meters (328 to 820 feet) across – were either vertical shafts running into the Martian crust or possibly openings leading to cavernous spaces beneath the surface. Dubbed the “seven Sisters” the openings were discovered on the flank of Arsia Mons, one of the gigantic Tharsis volcanoes, prompting speculation that they might be the collapsed roofs of lava tunnels within the volcano’s slopes.

A 2007 THEMIS image from Mars Odyssey showing entrances to possible Martian caves, dubbed the "seven sisters." Clockwise from upper-left: Dena, Chloe, Wendy, Annie, Abbey, Nikki and Jeanne. Arrows signify direction of solar illumination (I) and direction of North (N) - Credit: GE Cushing, TN Titus, JJ Wynne, USGS, USGS, Northern Arizona University, and PR Christensen of Arizona State University
A 2007 THEMIS image from Mars Odyssey showing entrances to possible Martian caves, dubbed the “seven sisters.” Clockwise from upper-left: Dena, Chloe, Wendy, Annie, Abbey, Nikki and Jeanne. Arrows signify direction of solar illumination (I) and direction of North (N) – Credit: GE Cushing, TN Titus, JJ Wynne, USGS, USGS, Northern Arizona University, and PR Christensen of Arizona State University

The vehicle has also operated in concert with the Mars Reconnaissance Orbiter in support of surface missions, including both the Curiosity and Opportunity rovers. As well as acting as a communications relay for such missions, Odyssey has been able to add context to the rovers’ work by providing thermal and other images which have helped science teams better understand the environments in which the rovers are operating. Nor does it end there. Odyssey has also been a careful observer of the Martian weather.

As each year on Mars lasts around 26 months, Odyssey has observed the planet through more than six Martian years. These observations have revealed some seasonal patterns that repeat each year and other seasonal events, such as large dust storms, which differ significantly from year to year.

A 2001 false colour map of Mars made from data gathered by Odyssey's gamma ray spectrometer reveals the widespread distribution of hydrogen-enriched soil on Mars (in blue), the result of sub-surface ice deposits
A 2001 false colour map of Mars made from data gathered by Odyssey’s gamma ray spectrometer reveals the widespread distribution of hydrogen-enriched soil on Mars (in blue), the result of sub-surface ice deposits

In just this past year, Odyssey’s orbit has put the spacecraft in position to observe Mars in early morning light. Previously, the spacecraft flew over ground that was either in afternoon lighting or pre-dawn darkness. The new orbit enables studies of morning clouds and fogs and comparison of ground temperatures in the morning to temperatures of the same sites in the afternoon and pre-dawn, again helping to increase our understanding of the various atmospheric mechanisms operating on the planet.

With 15 years under its belt, Odyssey continued to work hard around Mars and shows no sign of stopping. So, happy anniversary, Odyssey!

On Land and Sea

Hard on the heels of Blue Origin’s third successful launch and recovery of their sub-orbital New Shephard capsule and propulsion module during a test flight, Elon Musk’s SpaceX has achieved what had been eluding them:  launching a Falcon 9 rocket with a payload bound for the International Space Station and then landing the first stage of the rocket on a platform at sea.

The success comes after four prior attempted to land the first stage of the booster at sea – part of SpaceX’s efforts to develop a semi-reusable system to reduce overall launch costs – all ended with the booster crashing into the floating landing platform, or toppling over post touch-down.

The Falcon 9 1.1 furst stage of CRS-8 stands tall on the the drone ship following its landing on April 8th, 2016
The Falcon 9 1.1 furst stage of CRS-8 stands tall on the drone ship Of Course I Still Love You, following its landing on April 8th, 2016 (credit: SpaceX)

The April 8th launch, officially titled CRS-8, lifted-off from Cape Canaveral Air Force Station, Florida, at 8:53 GMT. After separating from the second stage of the rocket, which carrying the Dragon cargo craft up to orbit, the first stage of the booster performed a series of three burns  to slow it down and boost it back towards the landing platform – referred to as an autonomous drone ship – that was keeping station downrange of the launch site. Eight and a half minutes after the launch, the first stage made a vertical descent over the platform, re-firing its main engines to slow itself as the landing legs deployed from along the side of the rocket’s body, and it eased into a gentle touch-down.

After the landing, crew boarded the platform to weld the rocket’s landing pads to the deck as a precaution against it toppling over while the platform was being towed back to port. Current plans call for the platform to undergo examination and testing at Kennedy Space Centre to ensure no structural damage occurred during the landing, before it is refurbished for a further at-sea landing, possibly in June 2016. The Falcon booster stage will  also undergo post-flight examination prior to being refurbished for a future launch.

Continue reading “Space Sunday: Of Odysseys, rockets, inflatables and exoplanets”

Space Sunday: of rockets, rovers and impacts

Blue Origin's New Shephard lifts-off on Saturday, April 2nd on a successful sub-orbital test flight which saw both capsule and propulsion module successfully recovered
Blue Origin’s New Shephard lifts-off on Saturday, April 2nd on a successful sub-orbital test flight which saw both capsule and propulsion module successfully recovered

Blue Origin, established by  Amazon founder Jeff Bezos, scored a three-for-three with launches and landings of their sub-orbital New Shephard launch vehicle.

Intended to offer passengers the opportunity to experience the microgravity of space, New Shephard is a two stage vehicle comprising the capsule unit which will eventually carry  6 people to the each of space, and a rocket stage simply called the “propulsion module”. Both are designed to be fully re-usable in order to reduce the overall cost of launch operations.

The Blue Origin propulsion module just a couple of seconds from touch down on April 2nd, 2016 (image: Blue Origins)
The Blue Origin propulsion module just a couple of seconds from touch down on April 2nd, 2016 (image: Blue Origins)

Having first flown on November 23rd, 2015, when the capsule unit reached an altitude of 100.5 km (63 mi) before parachuting back to a soft landing and the propulsion module made a powered descent and landing, the April 2nd, 2016, marked the third successful flight for both capsule and propulsion module, the latter now having been used for all three successful flights in November 2015, January 2016 and April 2016.

During the flight, the capsule – which was carrying a small science payload – reached a maximum altitude of 103.4 km (64.4 mi) before making a return to Earth under its parachutes, while the propulsion module steered its way back to the launch site to make a powered landing.

Nor was this a run-of-the-mill return for the propulsion module, as a the ascent / descent engine was re-lit at a much higher altitude that is expected during operational flights, at around 1,107 metres (3,600 ft), in a manoeuvre designed to further test the engine’s reliability and the wear and tear it might suffer during a flight. Understanding both of these factors will help Blue Origin better identify the overall costs involved in refurbishing rocket and engines between flights.

The New Shephard capsule, whilst primarily intended to fly people on sub-orbital flights, can also be used for science research, as demonstrated in this flight, which saw the capsule carry the Box of Rocks experiment from the Southwest Research Institute, designed to explore how rocky debris settles in microgravity, and the University of Central Florida’s Collisions into Dust experiment, which aims to better understand how large bodies interacted with dust in the early Solar System.

The New Shephard capsule being recovered following its parachute landing (image: Blue Origin)
The New Shephard capsule being recovered following its parachute landing (image: Blue Origin)

While Blue Origin appear to be slightly ahead of SpaceX in terms of launching and recovering their rockets, it’s important to remember that the current New Shephard vehicle and the SpaceX Falcon 1.1 are very different beasts. Not only is the latter some 3 times bigger than New Shepard, the first stage of the vehicle flies much higher and faster than the Blue Origin vehicle, both of which make returning the first stage of the booster to a landing site to make a safe touchdown far more of a technical challenge.

That said, the sub-orbital capabilities of New Shephard are only one phase of Blue Origin’s plans. With the vehicle expected to commence crewed test flights in 2017 and offer sub-orbital tourist flights from 2018, the company plan to gradually uprate the vehicle to a point were it will also be able to undertake orbital launches and still be recovered.

Walking with Rovers

NASA is continuing to ramp public interest in Mars, with a new public outreach programme set to begin in summer 2016.

Destination: Mars builds on the ongoing cooperative work between the space agency and Microsoft in developing applications and opportunities for the Miscrosoft HoloLens system. As I’ve previously reported, NASA is already using the HoloLen aboard the International Space Station, and have also developed a means for members of the Curiosity science team put themselves “on” Mars using the HoloLens and data / images returned by the rover.

It is in the latter capacity that Destination: Mars is designed to work, offering the public, using the mixed reality capabilities of the HoloLens to “visit” Mars.

Apollo 11 Lunar Module Pilot and second man on the Moon, Edwin "Buzz" Aldrin, acts as a virtual host for Destination: Mars
Apollo 11 Lunar Module Pilot and second man on the Moon, Edwin “Buzz” Aldrin, acts as a virtual host for Destination: Mars

Continue reading “Space Sunday: of rockets, rovers and impacts”

Space Sunday: of ice and salts, aurorae, and mountains

A true colour image returned by the Dawn space probe of one of the bright "spots" in Occator crater on Ceres, revealing what might be a cryo-volcano
A true colour image returned by the Dawn space probe of one of the bright “spots” in Occator crater on Ceres, revealing what might be a cryovolcano (credit:NASA / JPL-Caltech / UCLA / MPS / DLR / IDA / PSI)

The science team behind the joint NASA / ESA Dawn mission has released the most stunning high-resolution images yet seen of Ceres, one of the solar system’s three “protoplanets” located in the asteroid belt between the orbits of Mars and Jupiter.

The Dawn spacecraft has been mapping Ceres for also a year, operating at its lowest altitude above the tiny world since December 2015. During the course of the year, the images and data it has returned have, alongside information sent to us about Pluto and Charon by the New Horizons mission, caused planetary scientists to start seriously reconsidering all they thought they understood about minor planetary bodies in the solar system.

However, one thing everyone has been waiting for has been to see high-resolution images of Occator crater and the strange bright spots within it which have been the cause of so much interest and speculation, ever since they were first imaged by the Hubble Space Telescope.

A false-colour image showing the main peak in Occator crater with the small bright spots off to the right
A false-colour image showing the main peak in Occator crater with the small bright spots off to the right (credit:NASA / JPL-Caltech / UCLA / MPS / DLR / IDA / PSI)

While the vehicle may have commenced its most detailed mapping orbit of Ceres in December, due to the complexities of Dawn’s orbit around the tiny world, it was not until relatively recently that it was able to overfly the 92 km (57 mi) diameter Occator and capture images of what lay within it, and these images were released on March 22nd, as a part of a science briefing given at the 7th annual Lunar and Planetary Science Conference in Texas.

Taken from an altitude of just 385 kilometres (240 miles) above the crater, the images reveal a huge dome-like structure with a dimpled top forming the brightest of the “spots” in Occator. It looks for all the world like a volcano, prompting speculation that it might be what is called a “cryovolcano”. The theory here being that Ceres may contain significant quantities of volatiles (ices), which are gently heated by the dwarf planet’s interior, causing them to erupt through the surface layer, the deposits they leave behind slowly building up the volcano-like dome.

A false colour elliptical map of Ceres showing that Occator (just right of centre) is not the only bright spot on the tiny planetoid others, mostly associated with young (around 70-150 million years old) craters
A false colour elliptical map of Ceres showing that Occator (just right of centre) is not the only bright spot on the tiny planetoid others, mostly associated with young (around 70-150 million years old) craters (credit:NASA / JPL-Caltech / UCLA / MPS / DLR / IDA / PSI)

However, this is not he only theory on what might be happening. Spectral observations show that the light patches found in Occator and elsewhere are consistent with a magnesium sulphate called hexahydrite, which resembles Epsom salts here on Earth. Thus, an alternative theory is that impacts in places like Occator expose the salt-rich ices trapped in the crust to the vacuum of space. This causes the ice to sublimate (vaporise), leaving the salt behind.

Commenting on the two the two theories, Ralf Jaumann, planetary scientist and Dawn co-investigator at the German Aerospace Center (DLR) said, “Before Dawn began its intensive observations of Ceres last year, Occator Crater looked to be one large bright area. Now, with the latest close views, we can see complex features that provide new mysteries to investigate. The intricate geometry of the crater interior suggests geologic activity in the recent past, but we will need to complete detailed geologic mapping of the crater in order to test hypotheses for its formation.”

In the interim, NASA has released a new video summarising Dawn’s investigations of Ceres.

Cygnus Rendezvous with ISS

March 22nd saw the latest Orbital ATK Cygnus resupply vehicle lifted-off from Space Launch Complex 41 on Cape Canaveral Air Force Station, Florida in a spectacular night-time launch beneath a full Moon.

The automated vehicle, carrying 3.5 tonnes of supplies and equipment up to the International Space Station, made a flawless ascent into the Florida sky, the clear weather and moonlight offer some extraordinary opportunities for photographers, as shown in the image below, taken by Alex Polimeni for Spaceflight Now.

Long exposure photograph shows the trail of the Atlas V launch vehicle as it carries the Cygnus OA6 vehicle "Rick Husband" into orbit on March 22nd, 2016. In the foreground is the world famous Vehicle Assembly Building (VAB) at NASA’s Kennedy Space Centre (credit: Alex Polimeni / Spaceflight Now)
Long exposure photograph shows the trail of the Atlas V launch vehicle as it carries the Cygnus OA6 vehicle “Rick Husband” into orbit on March 22nd, 2016. In the foreground is the world-famous Vehicle Assembly Building (VAB) at NASA’s Kennedy Space Centre (credit: Alex Polimeni / Spaceflight Now)

Continue reading “Space Sunday: of ice and salts, aurorae, and mountains”