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This course covers the basics of the solar system, including the study of terrestrial planets and their surface properties. Explore questions about volcanic processes, water presence, and mineral compositions on Mars. Learn about the importance of compositional effects and terrestrial analogs. Discover significant Mars missions such as Viking, Mars Pathfinder, and Mars Global Surveyor. Join the course to gain a deeper understanding of our solar system.
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Astronomy 101The Solar SystemTuesday, ThursdayTom Burbinetomburbine@astro.umass.edu
Course • Course Website: • http://blogs.umass.edu/astron101-tburbine/ • Textbook: • Pathways to Astronomy (2nd Edition) by Stephen Schneider and Thomas Arny. • You also will need a calculator.
There is an Astronomy Help Desk that is open Monday-Thursday evenings from 7-9 pm in Hasbrouck 205. • There is an open house at the Observatory every Thursday when it’s clear. Students should check the observatory website before going since the times may change as the semester progresses and the telescope may be down for repairs at times. The website is http://www.astro.umass.edu/~orchardhill/index.html.
HW #16, #17, #18, and #19 • Due by April 20th at 1 pm
Terrestrial Planets • Have different surface properties • Due to size of the planet • Distance from Sun • Speed of Planetary Rotation
Why Volcanoes are larger on other planets? http://athena.cornell.edu/images/scientists/lava_flow_chart.jpg
Look for evidence for processes that occur on surface of a planet • Geomorphology - scientific study of landforms and the processes that shape them • Important Questions: • Are features on Mars formed by volcanic processes? • Are features on Mars formed by water? • Compositional • Important Questions: • Are the compositions of minerals on Mars consistent with volcanic processes? • Are the compositions of minerals on Mars consistent with forming in the presence on Mars?
Are Features • due to volcanic processes or running water? • Are Rocks • contain minerals formed in volcanic processes (such as olivine or pyroxene) • Or affected by water (precipitates from solution or minerals containing water)
Formed by Lava? http://cdn.physorg.com/newman/gfx/news/hires/lavalikelyma.jpg
Martian basaltic meteorite • Looks like igneous rock
Russell Crater Dunes • Taken by Mars Reconnaissance Orbiter http://blogs.discovermagazine.com/badastronomy/2010/04/12/new-evidence-of-transient-liquid-water-on-mars/
Compositional Effects of Water • Examples: • 2Fe2SiO4 + 4H2O + O2 → 2Fe2O3 + 2H4SiO4 • olivine + water + oxygen → hematite + silicic acid • Form CaSO4·2H2O (Gypsum, a sulfate)
Terrestrial Analogs • You can use terrestrial environments to look for analogs for processes that occur on Mars
Significant Mars Missions • Viking 1 (1976-1982) (NASA) (Lander) • Viking 2 (1976-1980) (NASA) (Lander) • Mars Global Surveyor (1993-2006) (NASA) (Orbiter) • Mars Pathfinder (1997) (NASA) (Lander) • Mars Express (2003-present) (ESA) (Orbiter) • MER Spirit (2004-present) (NASA) (Lander) • MER Opportunity (2004-present) (NASA) (Lander) • Mars Reconnaissance Orbiter (2006-present) (NASA) (Orbiter) • Phoenix (2008) (NASA) (Lander)
Viking Missions • Each spacecraft consisted of an orbiter and a lander • Viking 1 lander landed July 20, 1976 • Viking 2 lander landed September 3, 1976 • Total cost was ~1 billion
Red Color • The red color of the planet comes from the oxidation of iron minerals in the soil. • Fe2+ is becoming Fe3+ • Iron is shiny when it is not oxidized • When it loses two electrons by encountering oxygen, it becomes black or green • When it loses three electrons by encountering oxygen, it becomes red • Rusting
Four Experiments • There were results that were initially positive • But results could all be explained through non-biologic chemistry • For example, Labeled Release Experiment • The nutrients were tagged with radioactive 14C • Looked for emitted 14CO2 gas as evidence for chemical reactions that happen in living organisms to maintain life • Radioactive gases were given off immediately for the first insertion of nutrients • Subsequent insertions did not give off radioactive gases
Four Science Goals of NASA's long-term Mars Exploration Program: • Determine whether Life ever arose on Mars • Characterize the Climate of Mars • Characterize the Geology of Mars • Prepare for Human Exploration
Mars Pathfinder • Landed July 4, 1997 • Weight - 870 kg • Lasted 3 months • Discovery Mission
Objectives of Mars Pathfinder • Discovery Mission - To prove that the development of "faster, better and cheaper" spacecraft is possible (with three years for development and a cost under US $150 million). • To show that it is possible to send a load of scientific instruments to another planet with a simple system and at one fifth the cost of a Viking mission. • To demonstrate NASA's commitment to low-cost planetary exploration finishing the mission with a total expenditure of US$ 280 million, including the launch vehicle and mission operations.
APXS Radioactive Cu-244
AXPS – Alpha Proton X-ray Spectrometer • Radioactive Cu-244 source • Emits alpha particles (helium nuclei), protons, and X-rays • Measures the backscattered alpha particles and protons and emitted X-rays from the rock • Different elements interact with alpha particles, protons, and X-rays differentlyy
Sojourner Rover is investigating Yogi the Rock The rock was the first on Mars found to be made of basalt The smoothness of the surface also suggested the past existence of water in the region.
Yogi Barnacle Bill http://www2.jpl.nasa.gov/snc/a-mgsivsalsi5.gif
Spirit and Opportunity • I used to live in an Orphanage.It was dark and cold and lonely.At night, I looked up at the sparkly sky and felt better.I dreamed I could fly there.In America, I can make all my dreams come true.....Thank-you for the "Spirit" and the "Opportunity"— Sofi Collis, age 9
Spirit landed in Gusev Crater – appeared basaltic (lava flows) • Opportunity landed on Meridiani Planum – appeared to have lots of sedimentary rock