Wednesday, February 22, 2012

Star Formation





Star formation begins when the denser parts of the cloud core collapse under their own weight/gravity. These cores typically have masses around 104 solar masses in the form of gas and dust. The cores are denser than the outer cloud, so they collapse first. As the cores collapse they fragment into clumps around 0.1 parsecs in size and 10 to 50 solar masses in mass. These clumps then form into protostars and the whole process takes about 10 millions years.
There are two common ways this can happen: it can either collide with another dense molecular cloud or it can be near enough to encounter the pressure caused by a giant supernova. Several stars can be born at once with the collision of two galaxies.
Many of the most interesting infrared objects are associated with star formation. Stars form from collapsing clouds of gas and dust. As the cloud collapses, its density and temperature increase. The temperature and density are highest at the center of the cloud, where a new star will eventually form. The object that is formed at the center of the collapsing cloud and which will become a star is called a protostar. Since a protostar is embedded in a cloud of gas and dust, it is difficult to detect in visible light. Any visible light that it does emit is absorbed by the material surrounding it. Only during the later stages, when a protostar is hot enough for its radiation to blow away most of the material surrounding it, can it be seen in visible light. Until then, a protostar can be detected only in the infrared. The light from the protostar is absorbed by the dust surrounding it, causing the dust to warm up and radiate in the infrared. Infrared studies of star forming regions will give us important information about how stars are born and thus on how our own Sun and Solar System were formed.
Websites:
http://www.ipac.caltech.edu/outreach/Edu/sform.html
http://abyss.uoregon.edu/~js/ast122/lectures/lec13.html
http://science.nasa.gov/astrophysics/focus-areas/how-do-stars-form-and-evolve/

Sunday, February 19, 2012

Astronomy Cast: Ice in Space



How much of the Solar System is ice? Well, not a lot by mass. In fact, if you pull together all the mass in the Kuiper Belt, it’s kind of a large rocky planet’s worth of materials — not a lot, and it’s also scattered into what’s called the Scattered Disk, and beyond the Kuiper Belt, beyond the Scattered Disk, the Oort Cloud – not really sure how much mass is tied up out there, haven’t really observed it yet. It’s a lot of stuff though. It’s sort of like when you’re cleaning your house, you don’t realize how many forks you own until you realize that you have forks in every room of your house from those random snacks that have been gathered. the water line is midway through the Asteroid Belt, and then the freeze line is out there pretty much between Jupiter and Saturn, and these are basically the places where you go from completely blasted dry, potato-shaped asteroids to potatoes with water to things of varying mixtures of rock and ice, and then the, in general, pure ice stuff in the outer solar system, and what you’re seeing is, essentially, the thermal gradient of when our Solar System formed. early Solar System was this mix of molecules and atoms. You had all the iron, all of the silica, all of the stuff that we think of as heavy metals. We had all of the carbon molecules, and mixed in all of this was O2 (oxygen); mixed into all this was all kind of carbon gasses, mixed into this was the ammonia and methane, and part of this mixing process…you had different things segregated out into different places due to gravitational attraction pulling things into the center of the Solar System vs. the light pressure forcing things back out. For the most part, the nice, happy, solid icy bodies we see — these are the Centaurs, the Kuiper Belt objects, the Scattered Disk objects — while they have variation in composition, we think, we’re still figuring this out. These suckers are far away and they’re faint. While they may have differences in composition (and we guess at that based on differences in albedo), they all formed in basically the same area and then got scattered around by gravitational interactions. So it’s more like you take the snow bank on the side of the road that has some of it has been attacked by pollution from cars, some of it has random spilled coffee from someone falling on the ice, there’s unfortunately dog pee on the snow bank, and where you grab — or don’t grab — a handful of snow from the snow bank, there’s going to be variations in composition, but in general, it’s all one snow bank. And in this case, it’s all one family of icy objects.

William Huggins Biography

                                    
 
William Huggins was born to a silk mercer and linen draper in London, on February 7, 1824. He attended the City of London School at its opening in 1837, but was later removed and taught by private tutors at home after recovering from smallpox. His predominant interest as a child was in science despite the broadness of his studies, and his first telescope was a cheap one, purchased when he was about eighteen. The combination of family circumstances and the fact that London was too poor of a place for astronomical observations ultimately led him to give up on his studies and take over his father’s business, although he continued his studies in science as a hobby.
In 1854, he joined the Royal Astronomical Society (which he later became president of, in 1900), and moved with his parents out to Tulse Hill, which had better conditions for doing astronomy research. He found himself too sensitive to experiment on animals and decided on astronomy over microscopy for his primary interest, and began to set up an astronomical observatory in his new home. He remained in Tulse Hill for the rest of his life, and once both his parents were deceased he married Margaret Lindsay Murray, who also held a profound interest in astronomy. She contributed to many of his major publications, and seemed to be to him what Caroline Herschel was to her brother.
The earliest astronomical work that Huggins pursued was about conventional lines, and this caused him to form a friendship with W. R. Dawes, who is a well-known amateur observer. Dawes sold him a better telescope and Huggins began to make observations about the planets. However, Huggins is the most well-known for his work in the field of spectroscopy, and in 1859 he heard about Kirschoff’s work on the Fraunhofer lines in the solar spectrum. Immediately Huggins realized that this could be applied to all of the stars, and he convinced a friend and professor of chemistry, W. A. Miller, to collaborate with him. Together, they designed a primitive spectroscope, which was basically two prisms attached to a telescope, and built upon their idea to create a more functional and efficient spectroscope. Huggins compiled maps of twenty-four terrestrial spectra and compared them to stellar spectra using this more efficient telescope, and he and Miller published their results in 1864. Their research concluded that the brightest stars had similar structures to our own sun, and that, although there was a diverse chemical composition, there were just as many similarities as differences.
Continuing on the same notions of his research, Huggins had an epiphany and decided to see what the spectral lines of nebula looked like. He targeted a planetary nebula in Draco, and discovered that the nebula was not composed of a group of stars, but was simply luminous gas. He went on and observed other nebula, and determined that they fell into one of two categories; star cluster, or glowing gas. However, while he could figure out the chemical make-up of the star clusters, he had more trouble with the gas; he could identify the hydrogen, and termed the other lines “nebulium”, which he thought was a new element. It was later discovered by Ira S. Bowen, in 1927, that nebulium was actually ionized oxygen and nitrogen.
Huggins also recognized the possibility of taking photographs of stellar spectra, and attempted to do so with Sirius, but the poor results made him realize that the technology was not yet sufficient. It wasn’t until 1872 that a fellow scientist named Draper was successful, and Huggins immediately followed it up by photographing the spectra of bright stars, and even attempted to do so to detect solar corona in full sunlight, although this was never reached.
However, Huggins was still not satisfied. He observed the radiation of three comets and compared them to the spectral lines of a candle flame, concluding that they were somehow carbon-based, and began to study fainter celestial objects. A younger scientist, Norman Lockyer, indirectly convinced him to study the sunlight when he discovered how to spectroscopically observe solar prominences – Huggins expanded on his idea by widening the slit in the spectroscope, allowing for a full range of observation rather than a narrow spectrum line. Lockyer and Huggins came into conflict later on as Lockyer began to form a hypothesis about celestial evolution based around Huggins’ “nebulium” spectral lines, and Huggins absolutely refused to admit that Lockyer is right. They continued to butt heads, disagreeing on even basic scientific methods, in which Lockyer argued that observation was a means to an end, but Huggins claimed was the end itself. In the end it was a moot point, since both of their scientific observations contributed to one another, and to the greater scientific community.

Friday, February 17, 2012

APOD 3.5-The Rosette Nebula



The Rosette is a cosmic cloud of dust and gas, that also resembles flowers. At the ledge of the large molecular clouds in the constellation Monocerous. The 'petals' of this Nebula are sculpted by the winds and the radiation from its hot, young central stars. These stars are in the NGC 2244 and are only a few million years old. This nebula can be seen first hand with a small telescope toward the constellation Monocerous.

Monday, February 13, 2012

Astronomy Cast: Carina Constellation



This constellation used to actually be part of a much, much larger constellation called Argo Navis, that, if it still existed, would be by far the largest constellation in the sky, and would dwarf absolutely everything else, but because it’s so large, it’s a little bit unwieldy to use for astronomical purposes, so it got broken up into three different constellations. It got broken up into Carina, Puppis, and into Vela, and each of these different parts represents a different part of the ship, where Carina is the keel, and Puppis is the poop deck, and Vela is the sails, so between all three of these you have the ship from Jason and the Argonauts. It just kinda looks like this random shape of stars on the sky. It’s not one of those constellations like, well, this is where Orion does when Orion…you can actually see – it’s a dude in the sky with a sword. Carina, no, it’s just miscellaneous shape of stars.Normally the brightest star in the constellation is Alpha+ the constellation name, so you’d expect “Alpha Carina” to be the brightest star in the constellation and if its not, it’s going to be hard to tell it apart from the star that actually is the brightest star in the constellation by eye. So Carina’s actually a bigger system. They’re very similar in age actually. They both have ongoing star-formation going on. The difference is when you look through Orion, you don’t see as many rich, open clusters as you see with Carina. So there we start to imagine things like the Hyades cluster here in the Northern Hemisphere. This is an open cluster that has had time to spread itself out as it orbits around and around the Milky Way, except this is that system times eight because there are so many open clusters embedded within the Carina Nebula. Now, what’s going to be amazing, though, is the process to get there.

Friday, February 10, 2012

APOD 3.4-Dust of the Orion Nebula



Many people wonder what surrounds a hotbed of star formation. In this picture of Orion is is clear that the Orion Nebula is doing just that. This constellation is 16,000 light years away and contains intricate filaments of dust. The dust seen was made in the outer atmosphere of very large cool stars and is thrown out by a stronger outer wind of particles. A cool star, or carbon star is made up of more carbon than oxygen and is similar to a red giant. Another forming star cluser, Trapezium, is also found in this nebula. In the above image, there are brown filaments of dust surrounded M42 and M43. Much of Orion's dust will be destroyed by the stars being formed there or dispersed into the galaxy!

Tuesday, February 7, 2012

William Huggins Biography Sources

William Huggins Biography Sources:
"William Huggins." NNDB: Tracking the Entire World. Web. 07 Feb. 2012. <http://www.nndb.com/people/389/000103080/>.
"No. 1845: William Huggins." University of Houston. Web. 07 Feb. 2012. http://www.uh.edu/engines/epi1845.htm.
"Sir William Huggins (English Astronomer) -- Britannica Online Encyclopedia." Encyclopedia - Britannica Online Encyclopedia. Web. 07 Feb. 2012. http://www.britannica.com/EBchecked/topic/274848/Sir-William-Huggins.
Huggins, William. The Menagerie of William Huggins 1820-1884: An Exhibition Arranged by Oscar & Peter Johnson Ltd. in Conjunction with the Williamson Art Gallery & Museum, Birkenhead, Metropolitan Borough of Wirral, Department of Leisure Services & Tourism : To Be Held at the Williamson Art Gallery & Museum ... [and] Lowndes Lodge Gallery, London. London] ([27 Lowndes St., SW1X 9HX]): Oscar and Peter Johnson, 1984. Print.

Friday, February 3, 2012

APOD 3.3- Planet Aurora Borealis



There is an eerie green light that eminates from this planet, which is covered in snow and tall pine trees. Of course this is actually Earth and the surrounding stars are above the horizon. The pale greenish illumination you are seeing is from the Northern Lights, also known as Aurora Borealis. The display seen was triggered when a coronal mass ejection lol, produced a strong geomagnetic storm. Recently, increasing solar activity has caused auroral displays to become more widespread. Some of these include Aurora Australis and the Southern Lights.