Primordial dry ice fuels comet jets

Nov 10, 2010
This montage shows the only five comets imaged up close with spacecraft. The comets vary in shape and size. Comet Hartley 2 is by far the smallest and has the most activity in relation to its surface area. This jet activity can be seen extending from the comet's surface and into its outer shell of gas and dust, or coma. This is the first time scientists have been able to link jets to the details of the surface. Credit: NASA/JPL-Caltech/UMD

One of the biggest comet findings coming out of the amazing images and data taken by the University of Maryland-led EPOXI mission as it zipped past comet Hartley 2 last week is that dry ice is the 'jet' fuel for this comet and perhaps many others.

Images from the show spectacular jets of gas and particles bursting from many distinct spots on the surface of the . This is the first time images of a comet have been sharp enough to allow scientists to link jets of dust and gas with specific surface features. Analysis of the spectral signatures of the materials coming from the jets shows primarily CO2 gas (carbon dioxide) and particles of dust and ice.

"Previously it was thought that water vapor from water ice was the propulsive force behind jets of material coming off of the body, or nucleus, of comet," said University of Maryland Astronomy Professor Jessica Sunshine, who is deputy principal investigator for the EPOXI mission. "We now have unambiguous evidence that solar heating of subsurface frozen carbon dioxide (dry ice), directly to a gas, a process known as sublimation, is powering the many jets of material coming from the comet. This is a finding that only could have been made by traveling to a comet, because ground based telescopes can't detect CO2 and current space telescopes aren't tuned to look for this gas," Sunshine said.

Sunshine and other members of the EPOXI science team are meeting all this week at the University of Maryland to analyze the very large amount of data from the closest approach, and new data continues to come down at a rate of some 2000 images a day.

The Deep Impact spacecraft that flew past comet Hartley 2 has three instruments -- two telescopes with digital color cameras and an . The spectrometer measures the absorption, emission and reflection of light (spectroscopic signature) that is unique to each molecular compound. This allows Maryland scientists to determine the composition of the material in the jets, on the comet's surface, etc. They have found that water and carbon dioxide dominate the infrared spectrum of comet Hartley 2's environment and that organics, including methanol, are present at lower levels.

Water and carbon dioxide dominate the infrared spectrum of comet Hartley 2's environment with organics like methanol also present. This is no surprise to scientists. What is surprising is that there is a lot more carbon dioxide escaping this comet than expected. The correlation between the asymmetric distribution of carbon dioxide and dust around the nucleus, which is much different than the isotropic water distribution, informs us that the carbon dioxide rather than water takes dust grains with it into the coma as it leaves the nucleus. For the first time, it is unambiguously shown that the sublimation of subsurface carbon dioxide, a volatile that has been preserved inside the comet since the formation of the solar system, drives the outgassing activity of a comet's nucleus. This spectrum and compositional maps of Hartley 2's coma were derived from data from the Deep Impact spacecraft when it was 44,000 kilometers away from the nucleus, 1 hour before it flew by. The images were taken by EPOXI's High-Resolution Instrument Infrared Spectrometer (HRI-IR) on Nov. 4, 2010. The sun is to the right. Credit: NASA/JPL-Caltech/UMD

This is no surprise to scientists. But what is surprising is that there is a lot more carbon dioxide escaping this comet than expected.

"The distribution of carbon dioxide and dust around the nucleus is much different than the water distribution, and that tells us that the rather than water takes dust grains with it into the coma as it leaves the nucleus, said Assistant Research Scientist Lori Feaga. "The dry ice that is producing the CO2 jets on this comet has probably been frozen inside it since the formation of the solar system."

From Deep Impact to Hartley 2

According to University of Maryland Research Scientist Tony Farnham, findings from the team's 2005 Deep Impact mission to comet Tempel 1, though less conclusive, nonetheless indicate that the Hartley 2 findings that super-volatiles (CO2 ) and not water drive the activity, probably are a common characteristic of comets. "Tempel 1 was most active before perihelion when its southern hemisphere, the hemisphere that appeared to be enhanced in CO2, was exposed to sunlight," said Farnham, a member of both the Deep Impact and EPOXI science teams. "Unlike our Hartley encounter, during the flyby with Tempel 1, we were unable to directly trace the CO2 to the surface, because the pole was in darkness during encounter."

The Maryland scientists devised the plan to reuse the spacecraft and travel to a second comet in order to learn more about the diversity of comets and the processes that govern them. This became the EPOXI mission on which the spacecraft has flown to comet Hartley 2.

The spacecraft's images show that Hartley 2 has an elongated nucleus, 2 kilometers in length and 0.4 kilometers wide at the narrow neck. Hartley 2 is only the 5th cometary nucleus ever seen and exhibits similarities and differences to the bodies or nuclei of other comets. Mission Principal Investigator and science team leader Michael A'Hearn, a University of Maryland professor of astronomy, said the mission has provided, and continues to provide, a tremendous wealth of data about Hartley 2 and the team expects to announce more science findings in the coming weeks.

Explore further: Computer model shows moon's core surrounded by liquid and it's caused by Earth's gravity

More information: See latest images, graphics and movie of comet flyby at EPOXI Website: http://epoxi.umd.edu/

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kevinrtrs
1 / 5 (5) Nov 11, 2010
"The dry ice that is producing the CO2 jets on this comet has probably been frozen inside it since the formation of the solar system."

Interesting statement to make, this. If the solar system is approx. 4.5Ga old, then how could this comet have lasted so long? It should certainly have evaporated long ago - a process that should certainly take far less than 100 000 years. Thus the statement is patently FALSE if one assumes 4.5Ga.
However, if one assumes that the solar system is only about 6k years old, the statement certainly begins to hold water.
I'd like to suggest that evolutionists begin to review carefully what researchers say and not just sop it all up.
Now if the researcher is intimating that the comet only got going long after the formation of the solar system, then he implies that he knows how it formed! And that is a lot of bullocks - no one knows how they formed.
antialias_physorg
5 / 5 (3) Nov 11, 2010
If the solar system is approx. 4.5Ga old, then how could this comet have lasted so long?


a) It need not have been around for all that time. Many comets originate fro mthe Oort cloud - where they reside for long times until a freak accident (swingby of another massive object or a collision) kicks them out and hurtles them towards the sun

b) Even then comets spend most of their time very far away from the sun. It is only hwne they get realtively close that sublimation starts

Start thinking before you declare something as 'patently false'- It might help augment your credibility as a sceptical human.
barakn
5 / 5 (2) Nov 11, 2010
Kevin, your argument can trashed with a simple sentence like "comet orbits can change abruptly due to gravitational interactions with other solar system objects." Take your idiot nonsense somewhere else.
genastropsychicallst
3 / 5 (2) Nov 11, 2010
Granules, to be read on my 'renewed' website.