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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

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