by Paul Gilster | Oct 16, 2019 | Culture and Society |
The Russian space agency Roscosmos, as most of you know, has announced the death of cosmonaut Alexei Leonov, who died last Friday at Moscow’s Burdenko Hospital following a long illness. He was 85.
If handling stress under extreme conditions is a prerequisite for someone who is going to the Moon, Leonov had already proven his mettle when the Soviet Union chose him as the man to pilot its lunar lander to the surface. The failure of the N-1 rocket put an end to that plan, but Leonov will always be associated with the 1965 mission aboard Voskhod 2 shared with Pavel Belyayev. This was the spacewalk mission, conducted successfully before NASA could manage the feat 10 weeks later.
Image: A man and his art. Alexei Leonov was as attracted to drawing and painting as he was to flying, creating some work while in orbit. Credit: Roscosmos.
The problems Leonov had with his bulky spacesuit as it ballooned out of shape are widely known, making his re-entry into the capsule a dicey affair, though one he managed with skilful use of a bleed valve in the suit’s lining. But consider everything else that went wrong: The charge fired to remove the airlock caused Voskhod 2 to tumble, while oxygen levels in the cabin began to rise and took several hours to correct.
Add to this the failure of the automated re-entry system, and the tangled separation of the orbital module from the landing capsule, caused by a communications cable that had failed to separate. It was the heat of re-entry itself that finally burned through the cable and allowed the landing module to bring both cosmonauts home. Then they landed so far downrange from their intended target that two days passed before they could be reached in a taiga forest in the Ural Mountains.
Image: Alexei Leonov in 1965. Credit: Associated Press.
This was indeed the kind of man the Soviet Union would have liked to place on the Moon ahead of the Apollo astronauts, but it was not to be. Leonov, who went on to be given the title of Chief Cosmonaut, is also remembered for the Soyuz he piloted and docked with an Apollo capsule in 1975 in the Apollo Soyuz Test Project, which was the first mission conducted jointly between the US and the Soviet Union. A self-taught artist, Leonov created what as far as I know is humanity’s first artwork in space when he did a colored pencil drawing of a sunrise as seen from Voskhod 2.
Stanley Kubrick’s 1968 film 2001: A Space Odyssey included recordings of Leonov’s breathing in space, a great move by a great director, but the later 2010 (directed not by Kubrick but Peter Hyams) would provoke an official response. Twice made Hero of the Soviet Union, but later suspected of disloyalty to the government, Leonov had been brought before the Central Committee of the Communist Party to explain the fact that the spaceship named ‘Leonov’ in the film (nice touch by Clarke) had been filled with Soviet dissidents. Leonov is said to have responded that the committee “was not worth the nail on Arthur C. Clarke’s little finger.”
A quote from Leonov’s Two Sides of the Moon: Our Story of the Cold War Space Race (Thomas Dunne Books, 2004), written with NASA astronaut David Scott, may be the best way to end as we consider how close this man came to being first on the Moon. The time is early 1966, and Soviet Luna probes had completed a series of missions in lunar orbit. Leonov recalls:
I was undergoing intensive training for a lunar mission by this time. In order to focus attention and resources our cosmonaut corps had been divided into two groups. One group, which included Yuri Gagarin and Vladimir Komarov, was training to fly our latest spacecraft — Soyuz — in Earth orbit…
The second group, of which I was commander, was training for circumlunar missions in a modified version of Soyuz known as the L-1, or Zond, and also for lunar-landing missions in another modified Soyuz known as the L-3. Vasily Mishin’s cautious plan called for three circumlunar missions to be carried out with three different two-man crews, one of which would then be chosen to make the first lunar landing.
The initial plan was for me to command the first circumlunar mission, together with Oleg Makarov, in June or July 1967. We then expected to be able to accomplish the first Moon landing — ahead of the Americans — in September 1968.
Alternate histories are fascinating to consider. But no matter which timeline we dwell in, Alexei Leonov was a courageous, generous man who carried the spirit of that insanely adventurous era. It’s a spirit we can strive to recover.
by Paul Gilster | Oct 11, 2019 | Missions |
One of these days we’ll have a spacecraft on a dedicated mission into the interstellar medium, carrying an instrument package explicitly designed to study what lies beyond the heliosphere. For now, of course, we rely on the Voyagers, both of which move through this realm, with Voyager 1 having exited the heliosphere in August of 2012 and Voyager 2, on a much different trajectory, making the crossing in late 2018. Data from both spacecraft are filling in our knowledge of the heliosheath, where the solar wind is roiled by the interstellar medium.
A new study of this transitional region has just appeared, led by Jamie Rankin (Princeton University), using comparative data from the time when Voyager 2 was still in the heliosheath and Voyager 1 had already moved into interstellar space. Leaving the heliosheath, the pressure of the Sun’s solar wind is affected by particles from other stars, and the magnetic influence of our star effectively ends. What the scientists found is that the combined pressure of plasma, magnetic fields, ions, electrons and cosmic rays is greater than expected at the boundary.
“In adding up the pieces known from previous studies, we found our new value is still larger than what’s been measured so far,” said Rankin. “It says that there are some other parts to the pressure that aren’t being considered right now that could contribute.”
Image: This is an illustration depicting the layers of the heliosphere. Credit: NASA/IBEX/Adler Planetarium.
Thus the Voyager data continue to be robust, giving us a look into a dynamic and turbulent region through which future missions will have to pass. The particular area that the study’s authors focused on is called a global merged interaction region, a wave of outrushing plasma produced by bursts of particles from the Sun in events like coronal mass ejections. Such an event is visible in Voyager 2 data from 2012, causing a decrease in the number of galactic cosmic rays, one that Voyager 1 would go on to detect four months later.
Traveling at nearly the speed of light, galactic cosmic rays are atomic nuclei from which all of the surrounding electrons have been stripped away. The difference between how this change in their numbers was detected by the two spacecraft is instructive. Still within the heliosheath at the time, Voyager 2 saw a decrease of galactic cosmic rays in all directions around the spacecraft, whereas at Voyager 1’s vantage beyond the heliosphere, only those galactic cosmic rays traveling perpendicular to the magnetic fields in the region decreased.
This intriguing asymmetry flags the crossing of the heliosheath, though the study’s authors are quick to point out that why this directional change in cosmic rays occurs remains unknown. They are able to calculate the larger than expected total pressure in the heliosheath, and discover that the speed of sound in the heliosheath is roughly 300 kilometers per second (remember that the speed of sound in any medium is simply the speed at which disturbances in pressure propagate, in this case the result of interactions in the solar wind).
Image: The Voyager spacecraft, one in the heliosheath and the other just beyond in interstellar space, took measurements as a solar event known as a global merged interaction region passed by each spacecraft four months apart. These measurements allowed scientists to calculate the total pressure in the heliosheath, as well as the speed of sound in the region. Credit: NASA’s Goddard Space Flight Center/Mary Pat Hrybyk-Keith.
“There was really unique timing for this event because we saw it right after Voyager 1 crossed into the local interstellar space,” Rankin said. “And while this is the first event that Voyager saw, there are more in the data that we can continue to look at to see how things in the heliosheath and interstellar space are changing over time.”
The paper is Rankin et al., “Heliosheath Properties Measured from a Voyager 2 to Voyager 1 Transient,” Astrophysical Journal Vol. 883, No. 1 (25 September 2019). Abstract.
by Paul Gilster | Oct 8, 2019 | Outer Solar System |
While I’m working on the project I discussed the other day, I’m trying to keep my hand in with the occasional article here, looking forward to when I can get back to a more regular schedule. Things are going to remain sporadic for a bit longer this month, and then again in mid-November, but I’ll do my best to follow events and report in when I can. I did want to take the opportunity to use an all too brief break to get to the Enceladus news, which has been receiving attention from the space media and, to an extent, the more general outlets.
We always track Enceladus news with interest given those remarkable geysers associated with its south pole, and now we return to the Cassini data pool, which should be producing robust research papers for many years. In this case, Nozair Khawaja (University of Berlin) and colleagues have tapped data from the spacecraft’s Cosmic Dust Analyzer (CDA) to study the ice grains Enceladus emits into Saturn’s E ring, finding nitrogen- and oxygen-bearing compounds. These are similar to compounds found on Earth that can produce amino acids. Says Khawaja:
“If the conditions are right, these molecules coming from the deep ocean of Enceladus could be on the same reaction pathway as we see here on Earth. We don’t yet know if amino acids are needed for life beyond Earth, but finding the molecules that form amino acids is an important piece of the puzzle.”
Image: This illustration shows how newly discovered organic compounds — the ingredients of amino acids — were detected by NASA’s Cassini spacecraft in the ice grains emitted from Saturn’s moon Enceladus. Powerful hydrothermal vents eject material from Enceladus’ core into the moon’s massive subsurface ocean. After mixing with the water, the material is released into space as water vapor and ice grains. Condensed onto the ice grains are nitrogen- and oxygen-bearing organic compounds. Credit: NASA/JPL-Caltech.
So let’s clarify the process. What the Cosmic Dust Analyzer is looking at appears to be organics that would have been dissolved in the ocean beneath Enceladus’ surface. These would have evaporated from the ocean and then condensed, freezing on ice grains inside fractures in the crust. Rising plumes would have accounted for these materials being blown into space.
We begin to get a window into what might be produced within the ocean, though the view is preliminary. In the excerpt below, note that the scientists classify various types of ice grains on Enceladus according to a taxonomy: Type 1 represents grains of almost pure water ice, Type 2 shows features consistent with grains containing significant amounts of organic material, and Type 3 is indicative of salt-rich water ice grains. The study homes in on Type 2:
It is highly likely that there are many more dissolved organic compounds in the Enceladean ocean than reported here… In this investigation of Type 2 grains, the initial constraints, in particular the choice of salt-poor spectra, favoured the identification of compounds with high vapour pressures. Despite the expected solubility of potential synthesized intermediate- or high-mass compounds, their low vapour pressures mean that they will not efficiently evaporate at the water surface and thus remain undetectable not only in the vapour, but also those Type 2 grains forming from it. Potential soluble biosignatures with higher masses might therefore be found in spectra from Type 3 grains, which are thought to form from oceanic spray (Postberg et al. 2009a, 2011). Finding and identifying such biosignatures will be the main goal of future work.
Image: With Enceladus nearly in front of the Sun from Cassini’s viewpoint, its icy jets become clearly visible against the background. The view here is roughly perpendicular to the direction of the linear “tiger stripe” fractures, or sulci, from which the jets emanate. The jets here provide the extra glow at the bottom of the moon. The general brightness of the sky around the moon is the diffuse glow of Saturn’s E ring, which is an end product of the jets’ material being spread into a torus, or doughnut shape, around Saturn. North on Enceladus (505 kilometers, or 314 miles across) is up and rotated 20 degrees to the left. Credit: NASA/JPL/Space Science Institute.
The researchers believe that similarities between the hydrothermal environment found on Enceladus and what we see on Earth prioritizes the exploration of the Saturnian moon for life. After all, we know of many places on our planet where life develops without sunlight, with the vents supplying the energy that fuels reactions leading to the production of amino acids. Despite the remarkable strides made by Cassini, its Cosmic Dust Analyzer was not, the authors say, designed for deep probing of this question. That makes high-resolution mass spectrometers a key component of any dedicated mission designed to explore the organic chemistry beneath the ice.
The paper is Khawaja et al., “Low-mass nitrogen-, oxygen-bearing, and aromatic compounds in Enceladean ice grains,” Monthly Notices of the Royal Astronomical Society Vol. 489, Issue 4 (November 2019), pp. 5231-5243 (full text).
by Paul Gilster | Oct 2, 2019 | Exoplanetary Science |
The news of a gas giant of half Jupiter’s mass around a small red dwarf, GJ 3512 b, continues to resonate. It goes to what has become a well enshrined controversy among those who follow planet formation models. While core accretion is widely accepted as a way of building planets, gravitational instability has remained an option. We are not talking about replacing one model with another, but rather saying that there may be various roads to planet formation among the gas giants. In any case, GJ 3512 b makes a strong case that we have much to learn.
When I think about gravitational instability, I go back to the work of Alan Boss (Carnegie Institution for Science), as he has long investigated the concept. I learned about it from his papers and his subsequent book The Crowded Universe (Basic Books, 2009). Here’s how Boss describes it there:
Proponents of the top-down mechanism… envision clumps of gas and dust forming directly out of the planet-forming disk as a result of the self-gravity of the disk gas. The clumps would result from the intersections of random waves sloshing around the disk, waves that look much like the arms in spiral galaxies such as the Milky Way. When two spiral arms pass through each other, they momentarily merge to form a wave with their combined heights, just as waves do on the surface of an ocean. Such a rogue wave might rapidly lead to the formation of a clump massive enough to be self-gravitating, and so hold itself together against the forces trying to pull it apart. Once such a self-gravitating clump forms, the dust grains within the clumps settle down to the center of the protoplanet and form a core…
What emerges, then, is a solid core with gaseous envelope. In other words, this ‘disk instability’ model produces a planet that has the same structure as one derived from core accretion. What makes GJ 3512 b so interesting is that its position around a star as small as its host is hard to explain without a truly massive disk, and if that disk were to form, it would be unstable, and the gravitational instability model could come into play. The creator of this model, by the way, is Alastair Cameron (Harvard University), who spawned the notion in 1972. Other key players were Gerard Kuiper and Soviet scientist Victor Safronov, though it was Boss who revived the idea in 1997 and began developing computer models showing how it could occur.
Image: Simulation of the disk of gas and dust surrounding a young star. Credit: Alan Boss.
So what does Boss think of GJ 3512 b? As you might guess, he’s energized by the result:
My new models show that disk instability can form dense clumps at distances similar to those of the Solar System’s giant planets. The exoplanet census is still very much underway, and this work suggests that there are many more gas giants out there waiting to be counted.”
The work he is referring to is a new paper in press at The Astrophysical Journal that suggests there is a likelihood that gas giants in Jupiter-like orbits may be plentiful, with the inherent biases built into our observational techniques making them hard to find. As for how many of these may be formed from disk instability, Boss is computing various protoplanetary disk models to continue the investigation. As he notes in the new paper:
These models are intended to be first steps toward creating a hybrid model for exoplanet population synthesis, where a combination of core accretion and disk instability works in tandem to try to reproduce the exoplanet demographics emerging from numerous large surveys using ground-based Doppler spectroscopy and gravitational microlensing or space-based transit photometry (e.g., Kepler, TESS).
Image: The black box encapsulating Jupiter denotes the approximate region of exoplanet discovery space where Alan Boss’ new models of gas giant planet formation suggest significant numbers of exoplanets remain to be found by direct imaging surveys of nearby stars. NASA’s WFIRST mission, slated for launch in 2025, will test the technology for a coronagraph (CGI) that would be capable of detecting these putative exoplanets. Top Right: This simulation of the disk of gas and dust surrounding a young star shows dense clumps forming in the material. According to the proposed disk instability method of planet formation, they will contract and coalesce into a baby gas giant planet. Credit: Alan Boss.
We’re slowly eking out planets in wider orbits that are tricky for radial velocity, where their signals are more difficult to tease out than large planets close to their star, and also for transit work, because the transits would occur over an orbital period of five years or more. Boss continues to champion the concept that one size may not fit all when it comes to planet formation, with GJ 3512 b a striking case in point. Given a sufficiently massive protoplanetary disk, giant planets form in his models within 20 AU. Another targeted investigation for WFIRST will come out of all this when the mission launches some time in the next decade.
The paper is Boss, “The Effect of the Approach to Gas Disk Gravitational Instability on the Rapid Formation of Gas Giant Planets,” in press at The Astrophysical Journal (preprint).
