Jagpal Singh All About Astronomy

Wednesday, 1 May 2013

Where Did The Moon Come From? (eBook)

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The current standard theory of the origin of the Moon is that the Earth was hit by a giant impactor the size of Mars causing ejection of iron poor impactor mantle debris that coalesced to form the Moon. But where did this Mars-sized impactor come from? Isotopic evidence suggests that it came from 1AU radius in the solar nebula and computer simulations are consistent with it approaching Earth on a zero-energy parabolic trajectory. But how could such a large object form in the disk of planetesimals at 1AU without colliding with the Earth early-on before having a chance to grow large or before its or the Earth's iron core had formed? We propose that the giant impactor could have formed in a stable orbit among debris at the Earth's Lagrange point $L_4$ (or $L_5$). We show such a configuration is stable, even for a Mars-sized impactor. It could grow gradually by accretion at $L_4$ (or $L_5$), but eventually gravitational interactions with other growing planetesimals could kick it out into a chaotic creeping orbit which we show would likely cause it to hit the Earth on a zero-energy parabolic trajectory. This paper argues that this scenario is possible and should be further studied.

 Comments: 64 pages, 27 figures, accepted for publication in AJ
 Subjects: Astrophysics





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The Birth And Death Of The Sun (eBook)

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How did our sun come into being? What keeps it hot and luminous, and what will be its ultimate fate? In this fascinating and informative book, George Gamow - renowned physicist and author of the best-seller One Two Three... Infinity - outlines the discoveries and theories that illuminate the evolution of our world. One of the founders of Big Bang theory, Gamow employs language that's both scientifically accurate and simple enough for nonspecialists to trace the development of atomic theory from its earliest articulation in 375 B.C. through studies of nuclear reactions and radioactive decay. Along the way, he discusses the formation of the stars and planets, the nature of red and white dwarfs, the dimensions of our stellar system, and the infinity of space. 1952 ed. 60 figures. 18 halftones.

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Tuesday, 30 April 2013

Asteroids and The Asteroid Belt

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Asteroids are rocky and metallic objects too small to be considered planets. They are sometimes called minor planets. They range in size from Ceres, with a diameter of about 1000 km, down to a few centimeters or less.The name asteroids, meaning "star-like", derives from the fact that, compared with comets, they are star-like in appearance because since they are rocky they do not emit the gases and dust that give comets their fuzzy appearance.


 Asteroids on a collision course with Earth are called meteoroids. If this meteoroid burns up because of frictional heating when it strikes our atmosphere, we term it a meteor (colloquially, a "shooting star"). If the meteoroid doesn't burn up completely and strikes the Earth we call it a meteorite.

The Asteroid Belt 

The highest concentration of asteroids is in a region lying between the orbits of Mars and Jupiter called the asteroid belt that is illustrated schematically in the adjacent figure. Here is a more realistic distribution of semimajor axes for the minor planets. Some 7000 asteroids have been identified so far. Most, but not all, have average orbital radii lying in the region of the asteroid belt. It is likely that the origin of the asteroid belt lies in the gravitational perturbation of Jupiter, which kept these planetisimals from coelescing into larger bodies. 

 


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Monday, 29 April 2013

Einstein’s Theory of General Relativity

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It’s the year 2100. You wake up alone in a small, windowless room. The only other thing in the room is a small ball. Maybe the room is located in your city, but maybe it’s inside that new spaceship everyone’s talking about. How can you tell?

You pick up the ball and drop it. It falls vertically to your feet. You time the fall and calculate that the ball accelerates at 9.8 metres per second per second, exactly the acceleration of gravity at the surface of the Earth.

But a spaceship in the middle of deep space can also accelerate by that much, producing the exact same results. So where are you?

In 1911, Einstein formally proposed that gravitational mass (that which produces a gravitational field) and inertial mass (that which resists acceleration) were one in the same, and this became known as the “equivalence principle”. According to this principle, you can’t tell whether you’re in a gravitational field (such as on the surface of the Earth) or experiencing constant acceleration (a spaceship speeding up, pushing you to the floor, like the g-force of a roller-coaster).
 
Another example is the infamous “Vomit Comet”, officially the Weightless Wonder (see video below), used by NASA for training, and occasionally by Hollywood for filming. Just as with our example with the ball, there’s no way to tell the difference between free fall, and being in the absence of a gravitational field, say in deep space.

This principle led Einstein to consider incorporating gravity into the framework of his special theory of relativity, culminating in his General Theory of Relativity.

At face value, that doesn’t appear such a difficult thing to do. Until this point, the properties of objects in isolation could be described by equations with great accuracy. But what to do about gravity? How does one calculate the properties of a system in which acceleration can be due to either gravity or changes in velocity? It seems to depend on how you are looking at it.

That led to the idea of a “reference frame” – the stage on which the objects you are looking at play out their roles. There may of course be other frames in which the objects appear to behave differently, so we need a description of all the frames, and the way to relate them.

The trick was to consider space and time as a four-dimensional object in itself – not a fixed stage on which the objects are defined, but something that itself can change.


Space-time

 

Let’s say you and I are going to meet for coffee. How do you describe this “event”? One option is to look at a map – “I’ll meet you at the cafe on level two of the building that’s at G5 on the map”. We have described three coordinates: G, 5, and level two. This is another way of saying a set of x, y, and z coordinates. So that we both actually meet for coffee, we’ll also need to add a fourth coordinate: time – say 2:00pm. These four points are what we call a space-time event.

General Relativity says the map can be distorted; and our coordinates will depend on how that happens. If I were to bend the map a little, the distance between two locations changes.

If you measure and add the angles of a triangle on the flat map you would get 180 degrees. If you do this on the curved map, you get a little more or a little less (depending on which way it’s curved). In the same way, the universe itself can have areas of different curvature.

 Now for the mind-bending part …

 You might know that, in the absence of any forces, things like to travel in straight lines (thank you, Newton). What about when the space is curved? We can still talk about straight lines, but now the lines follow the curvature. Think about drawing a small, straight line on a basketball. You can draw a line all the way around the ball and arrive back at the starting point. It’s straight, but also curved.

Odd things happen in “curved space” that contradict what we expect from “flat space”. If you walk north ten kilometres, west ten kilometres then south ten kilometres, you would expect to end up ten kilometres west of where you started. Do that at the South Pole and you end up where you started! Technically this happens everywhere, but on a (non-cylindrical projection) map it’s obvious at the poles.

Now we can expand our definition and say objects not influenced by a force travel along straight lines in curved space. In particular, things with mass (or energy, thanks to E = mc²) follow these straight paths in curved space.

The experimental proof of this occurred during a solar eclipse in 1919 where starlight was observed to be bent by the sun. The amount of bending was predicted by Einstein, and not by the standard “Newtonian” theory.

So matter follows the curvature of space, but we know matter is the source of gravity, so the curvature responds to matter as well. In the words of American theoretical physicist John Archibald Wheeler, “Matter tells space-time how to curve, and curved space tells matter how to move.”

 What if we have lots of matter in one place? Imagine you are driving up a steep hill. There is some steepness that is too much for your car to manage, even at its fastest. In the same way, if we have a very large amount of matter in a very small area, the curvature becomes so strong that not even light (perhaps the fastest thing in the universe) is fast enough to get out. This is a black hole.


Beautiful curves

Starlight and black holes are fun, but what does this have to do with day-to-day life on Earth? Have you ever used the Global Positioning System (GPS)? It’s a common feature of mobile phones today, but it relies entirely on General Relativity to work.

We said our map could be curved so that the points in the space dimensions were closer together. Since space and time behave together as space-time, the same trick happens for time. If we have some large mass, the curvature in the time dimension means that the more curved the space-time is, the slower a clock ticks there (or appears to for someone in a less curved region).

There is a measurable difference between the rate at which your atomic clock ticks on the surface of the Earth, and that at which one in orbit ticks.

Without this correction, GPS satellites would not be able to tell you where you are with such accuracy.
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Saturday, 23 March 2013

Titan, the Largest Moon of Saturn

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Titan has an atmosphere. This can be seen faintly in the image on the left as an outline, and more clearly in the following image
taken by Voyager looking back at Titan and showing sunlight scattering in the atmosphere. The atmosphere of Titan has several layers of haze. It has a pressure at the surface of 1.6 times that of Earth, and is made up primarily of nitrogen, with about a 1% concentration of methane.
The temperature on the surface is very cold, about -180 degrees Celsius. The atmosphere is extremely opaque because of thick smog that appears to result from sunlight interacting with hydrocarbons, much as smog forms on the Earth.

The clouds are probably composed of liquid nitrogen and methane drops, and it is speculated that Titan may be coverered with hydrocarbon lakes or oceans (specifically, methane and ethane). Although many of the organic chemicals thought to have been the precursors to life on Earth are present on Titan, it appears to be too cold for life as we know it to have evolved there. Here is a movie of infra-red images of Titan made with the Hubble Space Telescape. The structure shown in this animation represents heat variations in the atmosphere and surface of Titan.
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