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      Astrophysics and Irradiation

     

Stars form by the collapse of gas clouds in interstellar space under their own gravity. As these clouds collapse they break-up into cloudlets that themselves collapse and break-up. Each cloudlet may form a star and thus our Sun is likely to have had many siblings. The formation of the Sun in a cluster of other young stars may have had a significant affect on our Solar System. The image opposite shows the massive Trapezium stars in the Orion Nebula. They are surrounded by young stars with disks.

 
 

     
     

Supernovae Neighbours


A supernova is an exploding star and releases enormous amounts of energy and, perhaps more importantly, new radioactive elements that can quickly decay. If our Sun had a supernova neighbour during its formation then these radioactive elements could have been added to the Solar System and dramatically change the nature of the forming planets.

Supernovae are the death-throws of stars, occurring once a star has too little fuel to support its own mass and collapses in on itself. Different stars can become supernovae at very different times depending on their mass. Large stars, more than 30 times the mass of our Sun, only last a few million years before they explode as supernovae. Massive O and B stars are frequently observed in clusters of young stars and may form supernovae whilst solar mass stars are still surrounded by disks of dust and gas.

The importance of a nearby supernova during our Solar System's formation is two-fold. Firstly the shockwave emanating from the supernova will compress gas clouds and might trigger the collapse that leads to the formation of new stars. Secondly, and just as important, is that supernovae lead to the generation of new radioactive isotopes, since they produce large numbers of neutrons that are captured by atoms to make new heavier atoms. At least some of these radioactive isotopes, in particular 26-aluminium, decay quickly and produce large amounts of heat. If mixed into the Sun's disk of gas and dust, the solar nebula, and incorporated into the bodies forming in the disk, these radioactive materials could cause objects the size of asteroids to melt, and thus to change.

Finding evidence for short-lived radioactive elements provides us with a means of investigating our Sun's astrophysical surroundings during its formation. Certain isotopes, such as 60-iron, that decays relatively quickly, could only have formed within a nearby supernova.

     
     

Irradiation


Supernovae are not the only way of creating short-lived radioactive isotopes. Another major source of these isotopes is irradiation, where radiation splits apart existing atoms to make new nuclides.

Irradiation of solid grains by the early Sun probably occurred at the inner edge of the Solar Nebula generating new isotopes, including 26-aluminium, which could then be scattered across the Solar Nebula by magnetic x-winds. Further new nuclides could also be produced by radiation emanating from other nearby massive stars. Heat producing short-lived isotopes might, therefore, have a much less explosive origin than in a supernova. How much is produced by irradiation and how much by a nearby supernova is thus very important to determine.

An important goal of the Origins-Network is to search for nuclides produced by supernovae and irradiation. 10-Berylium has already been found in calcium-aluminium inclusions , CAIs, in primitive meteorites that are thought to be some of the oldest Solar System materials. This isotope almost certainly forms only by irradiation. 60-iron, however, that is only produced in supernovae is also found within meteorites. The Origins-Network is now searching for 10-berylium, 60-iron, 26-aluminium, 182-hafnium and 41-calcium in a wide range of early Solar System objects to determine what is most important irradiation or supernova in the supply of these nuclides.

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Copyright Origins Network, 2008