Mars Water hypothesis

Mars Water hypothesis. On March 2, 2004, NASA announced that “Opportunity has landed in an area of Mars where liquid water once drenched the surface”. Associate administrator Ed Weiler told reporters that the area “would have been good habitable environment”, although no traces of life have yet been found.

Larger Grains Suggest Presence of Fluid

This statement was made during a press conference, where mission scientists listed a number of observations that strongly support this view:
Distributions of spherules
Hypothesis: Spherules are concretions created in water as a solvent.
Competing hypothesis: Spherules are rehardened molten rock droplets, created by volcanoes or meteor strikes.

Supporting data: Location of spherules in the rock matrix is random and evenly spread.
Quote from Steve Squyres: “The little spherules like blueberries in a muffin are embedded in this rock and weathering out of it. Three ideas, lapilli, little volcanic hailstones, one possibility. Two, droplets of volcanic glass or impact. We’ve looked at these things very carefully. Probably concretions. If so, it’s pointing towards water.”

Detailed analysis of environmental, chemical, and mineralogical data taken from the Opportunity rover led to the elimination of the competing hypotheses, and the confirmation of the conclusion that the spherules were formed in place as post-depositional sedimentary concretions from an aqueous source.

In the lower left, a spherule can be seen penetrating the interior of a vug
Vugs
Hypothesis: Rock was formed in water, for instance by precipitation.
Competing hypothesis: Rock were formed by ash deposits.
Supporting data: Voids found in bedrock resemble “vugs” which are left by eroded away disk-shaped crystals, possible dissolved in a watery environment.
Quote from Steve Squyres: Second piece of evidence is that when we looked at it close-up, it was shot through with tabular holes. Familiar forms. When crystals grow within rocks, precipitated from water. If they’re tabular, as they grow you can get tabular crystals and water chem changes and they go away or they weather away.”
Sulfates and jarosite
Hypothesis: Water created tell-tale salt chemicals in the rock.
Competing hypothesis: Chemistry of rocks is determined by volcanic processes.
Supporting data: Sulfate salts and jarosite mineral were found in the rock. On Earth they are made in standing water (possibly during evaporation).
Quote from Steve Squyres: “Next piece of evidence comes from APXS. We found it looked like a lot of sulfur. That was the outside of the rock. We brought with us a grinding tool, the RAT and we ground away 2-4 mm and found even more sulfur. Too much to explain by other than that this rock is full of sulfate salts. That’s a telltale sign of liquid water. Mini-TES also found evidence of sulfate salts. Most compelling of all, the Mossbauer spectrometer in the RATted space showed compelling evidence of Jarosite, an iron sulfate hydrate. Fairly rare, found on earth and had been predicted that it might be found on Mars some day. This is a mineral that you got to have water around to make.”

Crossbedding features in rock “Last Chance”

On March 23, 2004, NASA announced that they believe that Opportunity had not landed in a location merely “drenched in water”, but on what was once a coastal area. “We think Opportunity is parked on what was once the shoreline of a salty sea on Mars,” said Dr. Steve Squyres of Cornell University.

The announcement was based on evidence of sedimentary rocks that are consistent with those formed by water and not wind. “Bedding patterns in some finely layered rocks indicate the sand-sized grains of sediment that eventually bonded together were shaped into ripples by water at least five centimeters (two inches) deep, possibly much deeper, and flowing at a speed of 10 to 50 centimeters (four to 20 inches) per second,” said Dr. John Grotzinger, from MIT. The landing site was likely a salt flat on the edge of a large body of water that was covered by shallow water.

Other evidence includes findings of chlorine and bromine in the rocks which indicates the rocks had at least soaked in mineral-rich water, possibly from underground sources, after they formed. Increased assurance of the bromine findings strengthens the case that rock-forming particles precipitated from surface water as salt concentrations climbed past saturation while water was evaporating.

The evidence for water was published in a series of scientific papers, with the initial results appearing in the journal Science [2] and then with a detailed discussion of the sedimentary geology of the landing site appearing in a special issue of the journal Earth and Planetary Science Letters [3]

Spherules and Hematite

Early in the mission, mission scientists were able to prove that the abundant spherules at Eagle crater were the source of hematite in the area discovered from orbit.

Hematite

The distribution of hematite in Sinus Meridiani, where Meridiani Planum is located

Geologists were eager to reach a hematite-rich area (in the center of the picture at right) to closely examine the soil, which may reveal secrets about how the hematite got to this location. Knowing how the hematite on Mars was formed may help scientists characterize the past environment and determine whether that environment provided favorable conditions for life.

“Grey hematite is a mineral indicator of past water,” said Dr. Joy Crisp, JPL project scientist. “It is not always associated with water, but it often is.”

Scientists have wanted to find out which of these processes created grey hematite on Mars since 1998, when Mars Global Surveyor spotted large concentrations of the mineral near the planet’s equator (seen in the left picture). This discovery provided the first mineral evidence that Mars’ history may have included water.

“We want to know if the grains of hematite appear to be rounded and cemented together by the action of liquid water or if they’re crystals that grew from a volcanic melt,” said Crisp. “Is the hematite in layers, which would suggest that it was laid down by water, or in veins in the rock, which would be more characteristic of water having flowed through the rocks.”

The next picture shows a mineral map, the first ever made on the surface of another planet, which was generated from a section of the panorama picture overlaid with data taken from the rover’s Mini-TES. The Mini-TES spectral data was analyzed in a way that the concentration of the mineral hematite was deduced and its level coded in color. Red and orange mean high concentration, green and blue low concentration.

This spectral map of Eagle crater shows hematite.

The next picture shows a hematite abundance “index map” that helps geologists choose hematite-rich locations to visit around Opportunity’s landing site. Blue dots equal areas low in hematite and red dots equal areas high in hematite. The colored dots represent data collected by the miniature thermal emission spectrometer on Sol 11, after Opportunity had rolled off of the lander and the rover was located at the center of the blue semi-circle. (The spectrometer is located on the panoramic camera mast.)

A hematite abundance index map of Eagle crater.

The area to the left (with high concentration of hematite) was selected by mission members for further investigation, and called Hematite Slope.

During Sol 23 (February 16) Opportunity successfully trenched the soil at Hematite Slope and started to investigate the details of the layering.

Spherical Granules (Spherules)
Main article: Martian spherules

This color-enhanced image shows spherical granules.

Microscopic images of the soil taken by Opportunity revealed small spherically shaped granules. They were first seen on pictures taken on Sol 10, right after the rover drove from the lander onto martian soil.

When Opportunity dug her first trench (Sol 23), pictures of the lower layers showed similar round spherules. But this time they had a very shiny surface that created strong glints and glares. “They appear shiny or polished,” said Albert Yen, science team member, during a press conference on February 19. He said: “Data will hopefully help us figure out what’s altering them.” At the same press briefing, Dr. Squyres noted this as one of the main question: “Where did those spherules come from, dropped from above or grown in place?”

Mission scientists reported on March 2 that they concluded a survey of the distribution of spherules in the bedrock. They found that they spread out evenly and randomly inside the rocks, and not in layers. This supports the notion that they grew in place, since if their origin was related to volcanic or meteoric episodes one would expect layers of spherules as a “record in time” for each event. This observation was added to the list of evidence for liquid water being present at this rock site, where it is thought the spherules formed.

Berry Bowl

The rock “Berry Bowl”

On March 18 the results of the investigation of the area called “Berry Bowl” was announced. This site is a large rock with a small, bowl-shaped depression, in which a large number of spherules had accumulated. The Moessbauer spectrometer was used to analyze the depression and then the area of the rock right beside it. Any difference in the measured data was then attributed to the material in the spherules. A large difference in the obtained “spectra” was found. “This is the fingerprint of hematite, so we conclude that the major iron-bearing mineral in the berries is hematite,” said Daniel Rodionov, a rover science team collaborator from the University of Mainz, Germany. This discovery seems to strengthen the conclusion, that spherules are concretions, grown in wet condition with dissolved iron.

First atmospheric temperature profile

Temperature profile taken by MGS over the MER-B site.

During a press conference on March 11, 2004, mission scientists presented the first temperature profile of the martian atmosphere ever measured. It was obtained by combining data taken from the Opportunity Mini-TES infrared spectrometer with data from the TES instrument onboard the Mars Global Surveyor (MGS) orbiter. This was necessary because Opportunity can only see up to 6 km high, and the MGS camera could not measure data all the way down to the ground. The data was acquired on February 15 (Sol 22) and is split into two data sets: Since the orbiter is in motion, some data was taken while it was approaching the Opportunity site, other when it was moving away. In the graph, these sets are marked “inbound” (black color) and “outbound” (red color). The dots represent Mini-TES (= rover) data and the straight lines are TES (=orbiter) data.

Atmospheric science from the MER rovers has been published in a series of scientific papers in Science [4][5] and Journal of Geophysical Research[6]

Astronomical observations

Opportunity observed the eclipse, or transits of Phobos and transits of Deimos across the Sun,[7] and photographed the Earth, which appeared as a bright star in the Martian sky.

A transit of Mercury from Mars took place on January 12, 2005 from about 14:45 UTC to 23:05 UTC, but camera resolution did not permit seeing Mercury’s 6.1″ angular diameter.

Transits of Deimos across the Sun were seen, but at 2′ angular diameter, Deimos is about 20 times larger than Mercury’s 6.1″ angular diameter.

~ by labsinfo on January 9, 2010.

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