Chapter 15--Our Sun - Geological Sciences
Chapter 15--Our Sun - Geological Sciences
Chapter 15--Our Sun - Geological Sciences
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Table <strong>15</strong>.1 Basic Properties of the <strong>Sun</strong><br />
Radius (R <strong>Sun</strong><br />
)<br />
Mass (M <strong>Sun</strong><br />
)<br />
Luminosity (L <strong>Sun</strong><br />
)<br />
Composition (by<br />
percentage of mass)<br />
Rotation rate<br />
Surface temperature<br />
Core temperature<br />
696,000 km (about 109 times the<br />
radius of Earth)<br />
2 10 30 kg (about 300,000 times<br />
the mass of Earth)<br />
3.8 10 26 watts<br />
70% hydrogen, 28% helium,<br />
2% heavier elements<br />
25 days (equator) to 30 days (poles)<br />
5,800 K (average); 4,000 K (sunspots)<br />
<strong>15</strong> million K<br />
Figure <strong>15</strong>.3 This photo of the<br />
visible surface of the <strong>Sun</strong> shows<br />
several dark sunspots.<br />
nosity, it would be enough to meet current human energy<br />
demands for roughly the next 500,000 years!<br />
Of course, only a tiny fraction of the <strong>Sun</strong>’s total energy<br />
output reaches Earth, with the rest dispersing in all directions<br />
into space. Most of this energy is radiated in the form<br />
of visible light, but once you leave the protective blanket of<br />
Earth’s atmosphere you’ll encounter significant amounts of<br />
other types of solar radiation, including dangerous ultraviolet<br />
and X rays. Your spaceship will require substantial<br />
shielding to protect you from serious radiation burns caused<br />
by these high-energy forms of light.<br />
Through a telescope, you can see that the <strong>Sun</strong> seethes<br />
with churning gases. At most times you’ll detect at least<br />
a few sunspots blotching its surface (Figure <strong>15</strong>.3). If you<br />
focus your telescope solely on a sunspot, you’ll find that it is<br />
blindingly bright. <strong>Sun</strong>spots appear dark only in contrast to<br />
the even brighter solar surface that surrounds them. A typical<br />
sunspot is large enough to swallow the entire Earth, dramatically<br />
illustrating that the <strong>Sun</strong> is immense by any<br />
earthly standard. The <strong>Sun</strong>’s radius is nearly 700,000 kilometers,<br />
and its mass is 2 10 30 kilograms—about 300,000<br />
times more massive than Earth.<br />
<strong>Sun</strong>spots appear to move from day to day along with<br />
the <strong>Sun</strong>’s rotation. If you watch very carefully, you may<br />
notice that sunspots near the solar equator circle the <strong>Sun</strong><br />
faster than those at higher solar latitudes. This observation<br />
reveals that, unlike a spinning ball, the entire <strong>Sun</strong> does<br />
not rotate at the same rate. Instead, the solar equator completes<br />
one rotation in about 25 days, and the rotation period<br />
increases with latitude to about 30 days near the solar<br />
poles. Table <strong>15</strong>.1 summarizes some of the basic properties<br />
of the <strong>Sun</strong>.<br />
THINK ABOUT IT<br />
VIS<br />
As a brief review, describe how we measure the mass of the<br />
<strong>Sun</strong> using Newton’s version of Kepler’s third law. (Hint: Look<br />
back at <strong>Chapter</strong> 5.)<br />
As you and your spaceship continue to fall toward the<br />
<strong>Sun</strong>, you notice an increasingly powerful headwind exerting<br />
a bit of drag on your descent. This headwind, called the<br />
solar wind, is created by ions and subatomic particles flowing<br />
outward from the solar surface. The solar wind helps<br />
shape the magnetospheres of planets [Sections 11.3, 12.4]<br />
and blows back the material that forms the tails of comets<br />
[Section 13.4].<br />
A few million kilometers above the solar surface, you<br />
enter the solar corona, the tenuous uppermost layer of the<br />
<strong>Sun</strong>’s atmosphere (Figure <strong>15</strong>.4). Here you find the temperature<br />
to be astonishingly high—about 1 million Kelvin. This<br />
region emits most of the <strong>Sun</strong>’s X rays. However, the density<br />
here is so low that your spaceship feels relatively little heat<br />
despite the million-degree temperature [Section 4.2].<br />
Nearer the surface, the temperature suddenly drops to<br />
about 10,000 K in the chromosphere, the primary source<br />
of the <strong>Sun</strong>’s ultraviolet radiation. At last you plunge through<br />
the visible surface of the <strong>Sun</strong>, called the photosphere,where<br />
the temperature averages just under 6,000 K. Although the<br />
photosphere looks like a well-defined surface from Earth,<br />
it consists of gas far less dense than Earth’s atmosphere.<br />
Throughout the solar atmosphere, you notice that<br />
the <strong>Sun</strong> has its own version of weather, in which conditions<br />
at a particular altitude differ from one region to another.<br />
Some regions of the chromosphere and corona are particularly<br />
hot and bright, while other regions are cooler and<br />
less dense. In the photosphere, sunspots are cooler than<br />
the surrounding surface, though they are still quite hot<br />
and bright by earthly standards. In addition, your compass<br />
goes crazy as you descend through the solar atmosphere,<br />
indicating that solar weather is shaped by intense magnetic<br />
fields. Occasionally, huge magnetic storms occur, shooting<br />
hot gases far into space.<br />
Into the <strong>Sun</strong><br />
Up to this point in your journey, you may have seen Earth<br />
and the stars when you looked back, but as you slip beneath<br />
the photosphere, blazing light engulfs you. You are<br />
chapter <strong>15</strong> • <strong>Our</strong> Star 499