Page 2 of 12: Survey of elementary geobiochemistry > the Lithosphere > Origin of the chemical elements
			Structure of the Earth			Formation and evolution of the Earth

The Earth is composed of 90 chemical elements, of which 81 have at least one stable isotope. Most of these elements have also been detected in stars. Where did these elements come from? The accepted scenario is that the first major element to condense out of the primordial soup was helium , which still comprises about one-quarter of the mass of the known universe.

				Hydrogen is the least thermodynamically stable of the elements, and at very high temperatures will combine with itself in a reaction known as nuclear fusion to form the next element, 2He4. "Heavier" nuclei (that is , those having high atomic numbers, indicated here by the subscript preceding the element symbol), are more stable than "lighter" ones, so this fusion process can continue up to 56Fe, which is the most energetically stable of all the nuclides. Beyond this point, heavier nuclei slowly become less stable, so fission becomes more likely. FIssion, however, is not considered an important mechanism of primordial nucleosynthesis, so other processes are invoked, as discussed farther below.
		Click on the above image to see a more detailied plot of nuclear binding energy as a function of atomic number.

Primordial Chemistry

According to the “big bang” theory for which there is now overwhelming evidence, the universe as we know it (that is, all space, time, and matter) had its origin in a point source or singularity  that began an explosive expansion about 12-15 billion years ago, and which is still continuing.

Following a brief period of extremely rapid expansion called inflation, protons and neutrons condensed out of the initial quantum soup after about 10^–32 s. Helium and hydrogen became stable during the first few minutes, along with some of the very lightest nuclides up to ₇Li, which were formed through various fusion and neutron-absorption processes. Formation of most heavier elements was delayed for about 10⁶ years until nucleosynthesis commenced in the first stars. Hydrogen still accounts for about 93% of the atoms in the universe.

Stellar nucleosynthesis

All elements beyond hydrogen were formed in regions where the concentration of matter was large, and the temperature was high; in other words, in stars. The formation of a star begins when the gravitational forces due to a large local concentration of hydrogen bring about a contraction and compression to densities of around 10⁵ g cm^–3. This is a highly exothermic process in which the gravitational potential energy is released as heat, about 1200 kJ per gram, raising the temperature to about 10⁷ K. Under these conditions, hydrogen nuclei possess sufficient kinetic energy to overcome their electrostatic repulsion and undergo nuclear fusion:

Hydrogen burning

There will be a net mass loss in above process, which will therefore be highly exothermic and is known as “hydrogen burning”. As hydrogen burning proceeds, the helium collects in the core of the star, raising the density to 10⁸ g cm^–3 and the temperature to 10⁸ K. This temperature is high enough to initiate helium burning, which proceeds in several steps:

The size of a star depends on the balance between the kinetic energy of its matter and the gravitational attraction of its mass. As the helium burning runs its course, the temperature drops and the star begins to contract. The course of further nucleosynthesis and the subsequent fate of the star itself depends on the star’s mass.

Small stars

If the mass of the star is no greater than 1.4 times the mass of our sun, the star collapses to a white dwarf, and eventually cools to a dark, dense dead star.

Big stars

In larger stars, the gravitational forces are sufficiently strong to overcome the normal repulsion between atoms, and so gravitational collapse continues. The gravitational energy released in this process produces temperatures of 6 10⁸ K, which are sufficient to initiate a complex series of nuclear reactions known as the carbon-nitrogen cycle. The net reaction of this cycle is the further fusion of hydrogen to helium, in which C¹² acts as a catalyst, and various nuclides of nitrogen and oxygen are intermediates. The temperature is sufficiently high, however, to initiate fusion reactions of some of these intermediates:

Supernovas

The intense gamma radiation that is produced in some of these reactions breaks some of the product nuclei into smaller fragments, which can then fuse into a variety of heavier species, up to the limit of ₂₆Fe⁵⁶, beyond which fusion is no longer exothermic. The greater relative abundance of elements such as ₆C¹², ₈O¹⁶, and ₁₀Ne²⁰ which differ by a ₂He⁴ nucleus, reflects the participation of the latter species in these processes. These exothermic reactions eventually produce temperatures of 8 10⁹ K, while contraction continues until the central core is essentially a ball of neutrons having a radius of about 10 km and a density of 10¹⁴ g cm^–3. At the same time the outer shell of the star is blasted away in an explosion known as a supernova.

Elements heavier than iron

Since ₂₆Fe⁵⁶ has the highest binding energy per nucleon of any nuclide, there are no exothermic processes which can lead to the formation of heavier elements. Fusion into heavier species is also precluded by the electrostatic repulsion of the highly charged nuclei. However, the process of neutron capture can still take place (this is the same process that is used to make synthetic elements). The neutrons are by-products of a large variety of stellar processes, and are present in a wide range of energies. Two general types of neutron capture processes are recognized. In an “s” (slow) process, only a single neutron is absorbed and the product usually decomposes by b-decay into a more proton-rich species:

This process occurs at rates of about 10⁵ yr^–1 , and accounts for the lighter isotopes of many elements. The other process (the “r”, or rapid process) occurs in regions of high neutron density and involves multiple captures at rates of 0.1-10 sec^–1:

This mechanism favors the heavier, neutron-rich isotopes and the heaviest elements.

Other elements

A few nuclei are not accounted for by any of the processes mentioned. These are all low-abundance species, and they probably result from processes having low rates. Examples are Sn¹¹² and Sn¹¹⁴ which may be produced through proton-capture, and H², Li⁶, Li⁷, Be, B¹⁰ and B¹¹, which may come from spallation processes resulting from collisions of cosmic ray particles with heavier elements.

References

 Page last modified: 21.01.2008