Update # 65 of December 6th, 1997, at 19:45 UTC Sagan Memorial Station Special edition:
Now we know what Mars is like
That's what we've learnt from Pathfinder !
Although science hadn't been the primary task of the
Mars
Pathfinder Mission (that had been engineering experiments) the
dramatic yet short-lived enterprise has advanced our
knowledge about the red planet in several areas quite
considerably.
While some results were mere confirmations of
established facts about Mars - e.g. that Ares Vallis has seen a
major flood 3 billion years ago - or almost mirrored the respective
data from the
Viking missions (such as the weather
observations), other findings have raised intriguing questions:
Did the camera really spot rounded pebbles and conglomerate
rocks that would point to an era even before the flood, when Mars
must have had a warmer climate with stable liquid water on the
surface? Does the existence of magnetized dust support this
view? Are some of the rocks - e.g. Scooby Doo - actually sediments
from that wet era?
The instrumentation of Pathfinder and Sojourner was too limited
to yield clear answers to these fundamental questions - but here
is what we do know, as reported in 7 papers in the
Dec. 5th
issue of Science magazine
(also discussed
here and
here)
and at a major Dec. 4th news
conference at the Max Planck Institute for Chemistry in Mainz,
Germany, by leading German researchers of the APXS and IMP
instruments (also summarized
here and mentioned
here):
The
Alpha Proton X-ray Spectrometer
from German, U.S. and Russian researchers (which got onto the
Sojourner rover merely by chance - as a spin-off from a similar
instrument built for the later ill-fated Mars'96 mission) told us
the following:
The dust on Mars is virtually the same all over the planet:
The chemical composition measured in Ares Vallis and at the two
Viking landing sites is virtually identical. This means that global
air transport, esp. the famous dust storms, mix and distribute
the dust very efficiently.
All the rocks are more or less dusty, and since the
very lightweight and technically simple APXS (with a mass of only
540 grams!) didn't carry a brush, the dust has to be subtracted
mathematically from the rock spectra; this is indeed possible and
quite reliable.
Having done that correction all measured rocks are
alike, i.e. some media reports about two distinct chemical
classes were premature and plain wrong. The chemical
composition of all the rocks that Sojourner visited in Ares Vallis
differed significantly both from the dust and from the 12
Martian meteorites found on Earth.
The Ares Vallis rocks are unexpectedly rich in silica (Si) and
potassium (K), but low in Magnesium (Mg) - they seem to
resemble in composition terrestrial andesites and are "close to
the mean composition of Earth's crust," as R. Rieder et al.
write in Science: "However, we cannot be certain that these
rocks are igneous." There is also a possibility that they are
sediments or metamorphic or even impact melts. Pathfinder
didn't carry instrumentation to check for the necessary details.
In any case the APXS results demonstrate that Mars has
different "geological provinces": There must be other regions
on the planet where the rocks are much more primitive than
those found in Ares Vallis and do actually resemble the Martian
meteorites. The reasoning is simple: To make the ubiquitous dust
with its composition in between the Ares Vallis rocks and the
Martian meteorites, you have to mix material of both types.
The story of the APXS isn't over yet, by the way: Because the
reseachers had underestimated the influence of the Martian
carbon dioxide atmosphere on the measurements of the lighter
elements in the rocks, reliable data so far are available only for Mg,
Al, K and Fe etc. But the data for lighter elements such as carbon
will be recovered: Right now the lab version of the APXS is being
re-calibrated in Mainz, with simulated Martian atmospheric
conditions at the time the original rock data were taken. Results
could be available by next spring.
The IMP camera
on the lander has revealed "a
complex surface of ridges and troughs covered by rocks that have
been transported by fluvial, aeolian and impact processes," say P.
Smith et al., but mineralogical information from the
images, despite the use of 24 color filters, was limited. An
additional problem (and an itriguing scientific result of its own)
was the significant change of Mars' sky color during the day.
Nonetheless it seems that
There are 3 basic kinds of rocks and 4 kinds of soils
in Ares Vallis, apparently representing different stages of
weathering and other physical changes. Dark rocks like Barnacle
Bill and Bamm-Bamm are more original and were probably placed
on the surface by the meteorite impact that formed Big Crater 2.2
km away. Bright rocks are more weathered and dusted, pink
rocks are actually compacted soils.
IMP has confirmed the minute amounts of water
vapor in the atmosphere, but it is now becoming clear that
the water is not completely mixed with the carbon dioxide: It has a
different height structure. This indicates that there is a reservoir
in the Martian surface that exchanges water vapor with the
atmosphere in a daily cycle.
And there is also dust in the atmosphere, more than
expected actually: The height profile could be measured when
Mars' moon Phobos underwent a lunar eclipse and a detailled
light curve could be measured - which is more complex than would
have been expected from a simple model.
Other key results from the Pathfinder mission, as
summarized
by its lead scientist M. Golombek et al. include
the presence in IMP images of "rounded pebbles and cobbles and a
possible conglometerate" which "suggest fluvial processes that
imply liquid water in equilibrium with the atmosphere and thus a
warmer and wetter past. The moment of inertia indicates a central
metallic core of 1300 to 2000 kilometers in radius.
Composite airborne dust particles appear magnetized by freeze-dried
maghemite stain or cement that may have been leached from
crustal materials by an active hydrological cycle." And Golombek
is particularly proud that he predicted the conditions at the
landing site, down to the size distribution and number of small
rocks, quite well - just from remote sensing data.
Coming attractions:
More flight opportunities for MPF-proven instruments
This raises the confidence of NASA and ESA planners for
upcoming missions to Mars - the next landing will be already
on Dec. 3rd, 1999. On two upcoming NASA missions in 1999 and
2001 and a - not yet confirmed - ESA mission in 2003, German
scientists will again be present with key instruments, among
then:
Another IMP and a camera on a robot arm of the
MVACSMars Surveyor 1998/1999
lander: This robot arm camera will look at the samples a shovel on the arm
collects, with 20 micrometer per pixel resolution and three colors. This is
the only Mars mission ever to target the South polar region of
Mars, with an emphasis on Mars' volatiles and climate processes.
On the Mars
Surveyor 2001 there will be another
rover with a far greater range than Sojourner - again equipped
with an APXS and this time also some other instruments. This
rover will also start collecting rocks for a possible sample return in
2005.
Only next June will ESA decide whether it can afford its
Mars Express mission in 2003 (there are contradictory
reports in Nature of Nov. 27 and Science of Nov. 28,
p. 325 and1553, regarding the chances). If it does, there will be an
orbiter (with key instruments that also were on Mars'96) - and
one or more landers. One of them could carry a tiny rover called
Nanokhod, developped in Russia and Mainz, and also carrying an
APXS and up to 5 other instruments.
Two more APXS', by the way, are booked for the
RoLand lander of
the Rosetta
comet mission (under construction; launch in 2003)
and the semi-commercial Euromoon
mission to the lunar South pole (under consideration by ESA and private
companies in Europe for a launch in 2001 the earliest).
Martian "bacteria" questioned:
Objects in ALH84001 just crystals?
16 months after the first publication about possible evidence for
ancient microbial life on Mars in the old
Martian meteorite
ALH84001 by a team of NASA scientists, the
debate
is continuing without the pro or con side
on a clear winning track (see also The Planetary ReportXVII#6 Nov. 1997, pp. 10-13) - but now the most "visible"
argument could be gone. ALH84001, contains no biological life
forms, according
to a Case Western Reserve University researcher and colleagues,
who report their analysis of ALH 84001 in the December 4 issue of
Nature. The geochemical evidence for ancient traces of life were
not challenged in this study, however.
R. Harvey et al., who used the same methods as the NASA researchers,
report that most of the purported nanofossils or
"worm-like images" are nothing more than lamellae, or fractured surfaces of
pyroxene and carbonate crystals. "We have now found two different types
of mineral forms in ALH84001 that look just like nanofossils, but they
are strictly non-biological origins. Sometimes even nature has a perverse
sense of humor," he added. The worm-like mineral lamellae are commonly
found at the fractured surfaces of planar crystals. Harvey noted that
lunar rocks -- in which there has been no evidence of life found -- contain
these same formations.
Update # 64 of December 3rd, 1997, at 16:45 UTC
Plasma satellite EQUATOR-S launched on Ariane
The first German scientific small Satellite
EQUATOR-S was launched this morning as a secondary customer on
Ariane flight V103 - by now the
German Space Operations
Center (GSOC) is controlling the 250 kg satellite. This was one of the
visually more impressive Ariane launches, with colorful flow phenomena
in the liquid and solid rocket plumes of the Ariane 44P model.
EQUATOR-S will fill a gap in the 3D coverage of Earth's magnetosphere,
namely in the equatorial region; the mission had been approved by the
(now-defunct) German space agency DARA only 3 years ago. That there is
still room for innovative missions into the Earth's magnetosphere 40 years
after its discovery with Explorer 1 and 3 in 1958 is proof that near-Earth
plasma physics remains a 'hot topic'. (MPG PRI SP 3/1995)
More launches: Astra 1G on Proton, TRMM, ETS-7 on H-II
Another successful launch in same night was performed by a Proton in Baikonur,
carrying Astra 1G. The launch was
broadcast live on a transponder on an earlier Astra that is normally used
for promotion purposes. It was amazing to listen to "Proton launch control"
in plain American - the launch was
managed by Lockheed-Martin
for the Luxemburg-based satellite operator.
And the weather in Kazhakstan was so clear that the Proton could be
followed optically for 8 minutes and a few seconds; the separations of the
1st and of the 2nd stage were clearly visible! This is the 7th
satellite of the series of European direct-broadcast TV satellites - check
here for the view the other 6 present in the sky over Germany!
Already on Nov. 27, a
Japanese H-II had launched NASA's
Tropical Rainfall Measurement Mission (TRMM) and NASDA's
ETS-7
experimental satellite that will try out in-orbit
rendezvous
and docking maneuvers. In an unusual move, NASDA had partially
insured ETS-7 against a mission failure (normally only commercial
spacecraft are insured), but there would have been reimbursement only for
a fraction of the $260 million cost. (AW&ST Nov. 24, 1997, p. 18)
More NASA cooperation with European countries?
During a recent trip to France and Germany NASA's Dan Goldin has proposed
that individual European countries team up with NASA for mainly
bilateral missions - apparently his trust in the European Space Agency
with its troubled budget is fading. On the other hand NASA acknowledges
the technological and scientific expertise of Europe, which could play a
role in
the Mars Sample Return mission NASA plans for about 2005.
France has proposed to launch it on an Ariane 5, which could allow to
bring back samples from two different sites;
the Crew Rescue Vehicle for the International Space Station.
NASA wants one anyway, and there has been a lot of work in this field in
Europe in the last 10 years, but France isn't interested anymore right
now.
Goldin has also expressed interest in the vague European plans for
Mars Express, which could actually replace one of the NASA Mars
missions on 2003, but the dire financial situation of ESA's science
programme had made the future of Mars Express very uncertain. (AW&ST
Nov. 24, 1997, p. 30)
Briefly noted:
A dust storm has started on Mars and has been detected both by
the Mars Global Surveyor TES instrument and camera, according to
news flashes from
MarsWatch in the last few days. The MGS mission with the slow
aerobraking is progressing smoothly so far - and on Dec. 4th a special
issue of Science magazine will report on the scientific
results of the Mars Pathfinder in 7 papers in the Dec. 5th issue.
Columbia's astronauts had little trouble to
capture the SPARTAN
satellite - but there was not enough fuel left in the orbiter to risk
another deployment and possible 2nd chase. Bringing back the reusable
satellite and another
EVA today had priority. Columbia is
due back at KSC at
12:19 UTC on December 5th.
The current constellation of many of the bright planets close together
has caused quite a stir
in the news media - several U.S. TV networks covered the "Heavenly Bodies"
(CBS) in their main news programs, although not always with the
most convincing of graphics...
In a Nutshell: The timetable for Cassini has
changed
slightly due to the launch delay; the arrival at Saturn stays on
July 1st, 2004, however. / Prices for Martian meteorites
are still high: Ads in the NYT recently offered 0.02 grams of the
Zagami for $ 98.- ... (New Scientist Nov. 22, 1997, p. 14) /
Someone has proposed to project corporate logos onto the Moon with big
mirrors - the latest weird idea in space advertising. (ibid p. 116)
Update # 63 of November 24th, 1997, at 19:20 UTC
Spacewalk to catch SPARTAN tonight!
A supposedly uneventful shuttle mission has suddenly turned dramatic:
Immediately after the free-flying solar observatory
SPARTAN 201 was released,
it lost its attitude control - and when the astronaut operating the robot
arm tried to capture it again, it was touched and got into a slow tumble.
Tonight (starting on Tuesday at 0:16 UTC) two astronauts are
supposed to catch SPARTAN with
their hands in a maneuver only tried once before, during the rescue
of an Intelsat satellite on STS-49 in May, 1992. For the current mission,
STS-87, the astronauts have trained
retrieving
SPARTAN by hand - but not in a spinning state. Retrieving the satellite
is a priority now because it is expensive and reusable (this is already
SPARTAN 201's 4th flight). And if the malfunction with the attitude
control can be fixed right away, the 2 day free-flight of SPARTAN 201-4
might even take place later in the current 16-day mission that began
on November 19th.
"Dial up the Sky":
New surveys will revolutionize astronomy
A new generation of sky surveys promises to change the ways astronomical
research is being done forever: Terabytes of data showing much of the
sky in up to 14 wavelengths from the UV to radio will be produced in the
next few years - and then be available to everybody via the WWW!
Already the question of how to deal with the trillions of bytes of
information and how to connect the individual sky surveys into the
ultimate hypercube of data has become more important than the technical
challenges of the involved telescopes and detectors.
Among the largest of the mega-sky surveys in the works are the
Digitized Palomar Sky
Survey (DSS), which promises a catalog of up to 2 billion
stars and other objects, the
Two-Degree Field Survey
(2dF) with the Anglo-Australian Telescope, the huge
Sloan Digital Sky Survey with an
expected 100 million galaxy images and spectra, the UV survey
from the just authorized GALEX satellite (one of the Small Explorers from
Update #61), the
Two Micron All
Sky Survey (2MASS) and FIRST,
a radio survey of hundreds of thousands of galaxies with the VLT.
The amount of raw data expected from these surveys is staggering and
ranges from "only" 120 Gigabytes to the 40 Terabytes expected from
Sloan (which will fortunately shrink to 1.2 Terabytes in reduced form).
Few people would want to have complete copies of these data sets at home,
and so central servers - accessible via the Internet - are the natural
solution. But astronomers want even more: the merger of the
surveys. And a system called sky tesselation is a likely answer: The
objects catalogued in the vast data bases can be selected by e.g. proximity
to a certain place, or color, or spectrum, or combination of all the above.
Not only professional astronomers but also amateurs will be able to access
this data superstructure - and the latter can still make contributions, too:
e.g. with The Amateur
Sky Survey that has already 23 volunteer participants! (Finkbeiner,
Science Nov. 7, 1997, p. 1010-12)
ESA's space science plans in deep trouble
The well-organized long-term
planning of the European Space Agency, the Horizon 2000
program could soon disintegrate if the European governments cannot
committ themselves to stopping and reversing the annual decline in ESA's
science budget. This unhealthy trend started in 1995 when the science
missions had to suffer for the cost overruns in the Space Station
program: The budget was frozen, which means that the actual purchasing
power has already dropped by 9%.
Now it seems inevitable that at least
some of the smaller science missions might have to be sacrificed in
order to save the major 'cornerstones'. Whether (or when) Europe could
then afford e.g. its own Mars mission
("Mars
Express") is uncertain. With no cash infusion from the larger ESA
nations (like Germany) in sight, the only steps ESA can take is to increase
the efficiency of its science program even further, i.e. to do more
missions for less money. (Abott, Nature Nov. 6, 1997, p. 8)
ESA's science program may be in disarray (see above), but then there is
the Euromoon proposal: Can
engineers, scientists and private industry come up with the money
(some 300 million ECU) for a semi-commercial mission to near the lunar South
Pole? The lander could go down on a mountain that's always in sunlight
(Peak of Eternal Light) and then set free some tiny rovers - for a rallye
to the South Pole. A mission in 2001 is still deemed possible.
(Nature Nov. 6, 1997, p. 8)
One more argument against the 'small comets' (see Update #61)
has been made by Frank's critics - and it's both simple and strong. If
the 10 m comets would exist, they would form an expanding cloud of water
ice crystals when they break up close to the Earth - and these clouds
would shine as bright in the sunlight as Venus or even the Moon! Every few
minutes such a brilliant object would appear in the sky: Good out and look...
(Rizk & Dessler, Preprint -> Geophys. Res. Lett. Dec. 15, 1997.
More on the UVI-vs.-VIS debate can also be found in Kerr, Science Nov. 14, 1997,
p. 1217-18)
Heavily armed gangsters in late October tried to steal 60 tons of
ultrapure gallium from the
Baksan Neutrino Observatory in Russia but failed: The scientists had
recently installed high-security defenses! The reason: For the past
year the government had tried to sell off the valuable material -
a scientific scandal which has so far been avoided thanks to protests from
the American collaborators in this solar neutrino observatory.
(Allakhverdov & Pokrovsky, Science Nov. 14, 1997, p. 1220-21)
As expected the mission of the Mars Pathfinder
has come to an end,
although there will still be attempts once in a while to reestablish
contact. The spacecraft had returned 2.6 billion bits of information,
including more than 16,000 images from the lander and 550 images from the
rover, as well as more than 15 chemical analyses of rocks and extensive
data on winds and other weather factors. Now the mission will be
honored with
a stamp!
Finally, there are now more detailled models of the
past
Martian climate: A blanket of dry ice clouds may have kept ancient
Mars
warm enough to let water flow on its surface, and may have
encouraged life in its caves and oceans.
The Earth's inner core us turning independently,
but more
slowly than previously thought: The inner core's independent rotation
is thought to be caused by a process called convection in the molten iron
outer core that surrounds the inner core and that produces the Earth's
magnetic field.
Space station Mir is in fine shape after a number of internal and
external spacewalks which have
restored power
to nearly full levels. It now seems that the station will be used until
at least 1999 and possibly beyond 2000.
Update # 61 of November 3rd, 1997, at 18:50 UTC
The "mini-comets" - case closed?
5 months after the excitement about the sudden reappearance of Lou Frank's
"Small Comet Hypothesis"
(Update #48) severe doubts have been raised about the reality of the very
phenomenon itself that the claim was based upon in 1986 and again in 1997 - it
seems that the "atmospheric holes" just don't exist. These dark spots in
the UV dayglow of the Earth's upper atmosphere appear both in Frank's and
other scientists' images from instruments on the Polar satellite, discussed
at length in the Geophysical Research Letters24 #19 [Oct. 1,
1997] pp. 2423-2438, and it had seemed that the geophysical origin of this
phenomenon (as opposed to an instrumental effect) was by now established.
Not so, say G. Parks et al. (preprint, to appear in GRL): They
operate the UVI
instrument on Polar that had shown the same dark spots as
Frank's VIS instrument.
But a detailed analysis of the UVI images and especially a comparision with
calibration images taken before launch has now shown that the
dark spots must be instrumental: "there is no scientific evidence from
UVI shat snowballs pelt Earth." Will the non-detection of the "atmospheric
holes" by UVI drag the VIS "detections" down as well, and will the bizarre
affair of the "mini-comets" be over? Stay tuned...
Ariane 5 - success with the 2nd launch!
A big sigh of relief all over Europe: On its 2nd attempt ("flight 502")
the big Ariane 5 rocket
made
it to orbit on Oct. 30th - even though
the
Vulcain engine shut down too soon (and the whole launch was delayed by
43 minutes because of a minor electrical problem on the ground). This launch
success was crucial
for ESA and got its high-flying plans
back on track.
Besides two dummy satellites (MAQSAT) to study the effects of the launch on
future payloads, a small real satellite was also on board:
TEAMSAT, built by Dutch and
Spanish students. It succeded in taking pictures (!) of crucial steps
during Ariane's 502 flight - stay tuned!
NASA close to giving up Mars Pathfinder
No communication has been received from the Sagan Memorial Station since Oct.
7th and no data since Sept. 26th. It is possible that the Mars lander has
become so cold
that the transmitter frequency has drifted a lot - or the spacecraft has
stopped operating. E.g. the computer might have been damaged and doesn't boot
properly anymore. Since the project has funding well into 1998,
attempts
to reestablish contact continue, but if nothing has been heard from the MPF
until tomorrow, these
attempts will become ever
rarer. Despite this unglamorous end of the mission, it has been an
overwhelming success, and the project stays busy analyzing the data from
nearly 3 months of operation.
Meanwhile the Mars Global Surveyor will resume its aerobraking very
carefully on Nov. 7th, in order not to endanger the solar panel that started
behaving strangely in October and was probably damaged. This
decision
means, however, that the final mapping orbit will be reached only several
months after the initial target date of mid-March, 1998 - and what this
orbit will look like is still unclear. Even now, however, the MGS is
delivering exciting data, including this fine
view of Olympus Mons, the big Martian volcano.
The first Brazilian attempt to launch a rocket was a failure on
Nov. 2nd: The
VLS
had to be destroyed when one of its 4 first stage engines failed to
ignite. Meanwhile yet another small U.S. satellite named
STEP 4
is in deep trouble and could be a loss.