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Because
stellar lifetimes range from perhaps 40,000 years to longer than 10 billion
years, astronomers never get to watch a particular star go through all of
its life cycle phases. However, there are millions of stars to look
at around the galaxy, each one at a different point in its life cycle.
These images can be sequenced in a logical manner, based on a knowledge
of astrophysics.
People are in much the same
situation. The human life cycle is about eighty years (infant, toddler,
child, adolescent, teenager, adult, mature adult, senior citizen [images]).
Most people can both identify the various stages of the human life cycle
that observable all around us, and put those stages in sequence.
Astronomers have the same task when classifying stars.
By
looking at thousands of pictures and using some basic physics, astronomers
have developed the sequence of a star's birth, life, and death (see
Sequenced Star Life Cycle Page - massive
and sun-like). The picture
begins with a large cloud of interstellar gas and dust, mostly hydrogen.
For reasons that astronomers don't completely understand, these clouds
begin to collapse under their own gravity and heat up. These proto-stars
eventually become dense enough to sustain nuclear reactions (hydrogen
becomes helium) and a star is born.
A
star spends the majority of its life cycle converting lighter elements
into heavier elements (nuclear fusion) in a state of "equilibrium."
The outward force of radiation emitted from the star's core is exactly
balanced by its own gravity pulling inward. This balanced state is
called hydrostatic equilibrium. Usually, astronomers describe stars
in this equilibrium state as being main sequence stars.
Eventually, the interior of
the star can't produce nuclear fusion reactions fast enough, and the star
becomes unstable. It is then called a variable star.
The star contracts and expands and eventually grows enormously large and
cools off. This stage of the star is called a red giant (great
NASA HST image of Betelgeuse).
Most
stars in the red giant phase are in a dramatic disequilibrium. Finally,
the outer atmosphere is cast off leaving a white hot stellar core behind.
The outer atmosphere is called a planetary nebula and eventually
disappears. It's not a planet, but it sometimes looks like one through
a small telescope. The remaining tiny core is called a white dwarf.
The white dwarf cools off very slowly (maybe over 5 billion years or more)
to become a black dwarf, a cold lump of stellar coal made not of carbon,
but mostly helium.
A
few stars, however, have a much more dramatic ending. If they are
sufficiently large, say more than five times the mass of an ordinary star
like our Sun, the red giant phase collapses in an enormous implosion called
a supernova. This results in a scattering of interstellar
matter called a supernova remnant (image)
and an exceedingly small stellar core so densely packed that protons and
electrons are squeezed together to form neutrons. This is a neutron
star. Even more interesting, if the star that collapses is enormous,
say more than eight times the mass of our Sun, the supernova is so intense
that a black hole, a tiny object with a huge
gravity field, is created.
How long a star lives (and
how it dies) depends entirely on how massive it is when it begins.
A small star can sustain basic nuclear fusion for billions of years.
Our sun, for example, probably can sustain reactions for some 10 billion
years. Really big stars have to conduct nuclear fusion at an enormous
rate to keep in hydrostatic equilibrium and quickly falter, sometimes as
fast as 40,000 years.
On-line Resources
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