When Phoenix Lands.. |
When Phoenix Lands.. |
Jan 24 2006, 06:05 PM
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Interplanetary Dumpster Diver Group: Admin Posts: 4404 Joined: 17-February 04 From: Powell, TN Member No.: 33 |
I have been wondering about something....given the performance of the MERs, if one or both survive this winter, is it not conceivable that they could be operational when Phoenix lands? It would, I believe, be the first landing on anything but the moon with other landers (other than parts of the same mission) still operational.
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Apr 15 2008, 06:21 PM
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The Poet Dude Group: Moderator Posts: 5551 Joined: 15-March 04 From: Kendal, Cumbria, UK Member No.: 60 |
For those people who haven't yet taken a look (shame on you! ) at Rui's excellent Q&A from yesterday with Peter Smith over on the spacEurope blog, here are some snippets... some real gold nuggets of info in here...
The robotic arm is 2.35 m long and powerful enough to scrape into hard materials. It is true that if the spacecraft footpad perches on a rock or is otherwise unstable, then the RA has the strength to move the lander. We often joke that landing on ice in low gravity will allow us to pull ourselves along the surface using the RA from rock to rock. If the ice is exceptionally hard we will not dig through it, but instead, will use our RASP to scrape up samples to be delivered to instruments on our deck. The MARDI instrument was found to interfere with the guidance system under rare circumstances forcing the difficult decision to turn it off during the descent. The microphone does work and may be used later in the mission to hear the sounds of the RA scraping on the Martian ice. Discovering Martian life is beyond the goal of this mission. We are looking first to see if the Martian arctic is habitable: periodic liquid water, organic material (it could be from meteors), and energy sources available for power an organism. On May 25, the lander "feels" the Martian gravity and begins to accelerate toward the planet. Its speed increases from 6000 to 12,500 mph. Fifteen minutes before entry, the lander separates from the cruise stage that have been its life support system for the last 10 months since launch. Seven minutes before landing, we enter the upper atmosphere and the aeroshell experiences the heat of friction with the thin atmosphere. We must enter within a degree of our proper angle or else we can skip off into space or heat too rapidly and overwhelm our protection systems. After the aeroshell has slowed us to 900 mph, the parachute is deployed and we start a leisurely descent to about 1 km above the surface. At a speed of 150 mph, the spacecraft is released from the backshell and drops toward the surface. Twelve thruster ignite and using radar for guidance bring us to our landing site at a speed of 5 mph. the specially designed landing legs take up the shock of landing. Fifteen minutes later the solar arrays deploy and the camera starts taking images. Our mission begins. The first week of the mission consists of taking images and preparing for gathering samples. At the end of the first week we expect to have delivered a surface sample to our TEGA instrument. The summer is our prime science opportunity and we expect to meet all our mission goals by September. As you might expect, the mission will continue longer than this up until solar conjunction in mid-November. Recovering operations after that in late December will be very difficult as the Sun is setting in this high arctic region. By February we expect that carbon dioxide ice is forming a thick layer around the lander and without heat Phoenix will not survive. No 4 year mission for us. The landing site has been well imaged from space by the HiRISE camera, a 0.5 m telescope with resolution of rocks 1 - 1.5 m or greater. We have found a safe site with few boulders to insure a safe landing. However, it will not be free of cobbles and smaller pebbles. I am curious to see how these stones have weathered over time and whether they are aligned with the polygonal boundaries. There are few slopes in the neighborhood and the horizon should look extremely flat, no hills. However, the site is far from boring. We are near a 10 km crater and should be on the ejecta blanket containing material brought to the surface from depth. We are also on the slope of a large volcano, Alba Patera and may encounter ash blown from the interior. Finally, the site is a shallow valley and has undergone erosion which may leave signatures. We land just before summer solstice and the first few months of the mission have plenty of sunlight altho our power generation depends on the tilt of the lander which we cannot control. Our science team has many arguments about how ice might react when the overburden of soil is removed. We will try to force some of the ice to melt by putting it in the warmest place we can find--the lander deck, then imaging it as solar heating tries to melt it. The question is will it sublimate before melting? We are flying an atomic force microscope built in Switzerland by Urs Staufer for the first time ever. This is a difficult instrument to fly because it is sensitive to vibration even the tiny vibes caused by temperature change and wind. It has worked well in the lab and during environmental tests giving a resolution of an amazing 100 nm per pixel. Our TEGA instrument which has 8 ovens is used to determine the minerals in the soil and to drive off vapors which are measured in a mass spectrometer. The ovens can only be used once so we must allocate them intelligently. Our basic goal is a surface measurement, an ice sample, and a sample half way between. Then will try to verify that what we have seen is real if the signal are near the noise level. Our thruster use hydrazine as fuel, its formula is N2H4 and our ultra-pure mixture has no detectable organics. The combustion products are ammonia and water. The more difficult question is what about the 1% that doesn't combust, it is highly reactive and may alter the chemistry of the surface layers that it contacts. We are vigilant and will try to avoid contaminated areas. Another major part of our science is the study of polar climate. Not only is Phoenix a traditional weather station, but we use LIDAR, built by our Canadian partners, to measure cloud properties and heights. The camera has special lenses for determining dust opacity and we do look for atmospheric phenomena like dust devils and solar haloes. The end of the mission has not been carefully studied and there are no guarantees after we complete our primary mission. As much as anything, the NASA budget limits our longevity. We will do everything in our power to last until the last rays of sunlight energize the spacecraft. All good things come to an end and we will leave important questions for future mission to unravel--Phoenix is a stepping stone on the path to discovering the Truth about Mars. Good bye all and thank you for your interest! -------------------- |
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