Asteroseismology allows scientists to explore stars with sound. It can help them figure out what a star is burning and even help pin down the age of stars!
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In a sense, stars are the fundamental
building blocks of the universe. I mean, galaxies are made of stars,
planetary systems form around stars, and virtually every atom that isn’t
hydrogen or helium was born inside a star. Given all that, it’s not
surprising that astronomers
00:19:
want to know as much as
possible about these objects. But that is easier said than done. There’s only one star scientists
can study in detail: our Sun. And, even then, we can only
look at it from the outside. Fortunately, astronomers have devised a clever way
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to peek inside stars without actually going there. It’s called asteroseismology, and it takes advantage of the last
sense you might expect: sound. Now we often think of sound
as something that is heard. But audible sound is just a special case
of a more general phenomenon: vibration.
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So, a birdsong isn’t that different
from something like an earthquake. One makes vibrations in the air, the
other in the earth under our feet. But, in both cases, we can get
information about something we cannot see.
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Like, we might know a singing bird is outside
the window, even if the curtains are closed. And, while earthquakes happen deep underground,
we can feel those effects on the surface. Scientists have taken that one step
further with the field of seismology.
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By measuring how earthquake vibrations
bounce around inside the planet, they’ve been able to figure out
the Earth’s internal structure without ever actually seeing it. Which sounds exactly like what astronomers
are looking for in studying stars!
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There’s only one catch, uh, in
space, no one can hear you scream, or, you know, hear anything at all. Because space is a vacuum, and
there’s no medium for sound waves or any other vibrational waves to travel through. Fortunately, stars make it possible
to almost “see” the sound inside them,
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because movement on a star’s surface
reflects what’s going on inside it. A key process here is convection, where pockets of material inside a star
heat up, become less dense, and rise. When they reach the surface, they lose
their heat to space in the form of light.
02:05:
Then, as they cool and get
denser, they sink down again, making way for the next pocket of
rising gas in an endless cycle. This circular motion creates vibrations
that ripple across the surface of the star, or, as we might call it, sound.
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And these sound waves cause tiny
changes in how the surface emits light, creating little flickers
that astronomers can observe. One way researchers have put asteroseismology
to work is figuring out what a star is burning. For most of their life, stars fuse
hydrogen into helium in their core.
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Then, after that hydrogen is exhausted,
they puff up to become red giants. During the red giant phase,
they create energy in two ways. First, they burn hydrogen
in a shell outside the core. Then, they burn the helium
that’s built up inside the core.
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Distinguishing the hydrogen-burning
and helium-burning phases from the outside has generally
been really difficult, because if you just look at the stars,
there’s not much of an obvious difference. But here’s the thing: The helium core is
much denser than the shell of hydrogen
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around it. And density has
a huge effect on vibrations. So, if the red giant hasn’t started
burning its helium core yet, we’ll see different vibrations
on the star’s surface. In a 2011 paper, researchers were able
to use NASA’s Kepler Space Telescope
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to identify those different seismic
waves in around 400 nearby stars, and classify them as either
helium-burning or hydrogen-burning. And so now, being able to separate
these phases of a star’s life will help astronomers understand what other
properties are different in the two groups,
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and what else changes in a red
giant over the course of its life. Beyond that, asteroseismology is also
helping pin down the age of stars in general. Knowing a random, individual star’s
age can answer all kinds of questions,
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like knowing whether it’s been around
long enough to have habitable planets. But traditionally, it’s been
almost impossible to do. You can usually date a cluster of stars by
plotting out their masses and temperatures, and comparing those to other
star clusters and models.
04:01:
But that doesn’t work for a single, lone star. There’s just not enough data, and
although there are some trends, a star looks about the same
for virtually its entire life. Except in 2008, a pair of astronomers proposed a way scientists might one
day be able to overcome that.
04:17:
See, as they age, stars undergo changes in
size, density, temperature, and composition, depending on what elements they’re burning,
fusing together, and also some other stuff. Those changes can affect a
star’s internal structure, which, in turn, affects the way
vibrations travel through the star.
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So, if astronomers could study the seismology
of a group of stars whose ages they do know, such as those in a star cluster, they could calibrate a model
linking seismic activity and age. Then, they could use that model
to study some random star, and calculate its age to within 10-20%;
05:52:
a huge improvement over the
35-40% margin we have now. That would open the door to all kinds of
studies, including how star systems have evolved, how stars change as they age, and of course, whether they could have any
exoplanets that could support life.
05:07:
Asteroseismology illustrates how
clever astronomers have to get when they can’t reach out and
touch what they want to study. It’s a good reminder that, in science, even seemingly-random details like
the bubbling of a star’s surface
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can be the gateway to a deeper
understanding of what’s really going on. Thanks for watching this episode of SciShow Space! If you want to learn more about stars,
we recommend watching this episode about how the first stars changed the universe,
and not just because they were bright.