SUN:Unlimited Source of Energy
Sun,star around which Earth and the other components of the solar
system revolve. It is the dominant body of the
system, constituting more than 99 percent of
its entire mass. The Sun is the source of an enormous amount of energy and
the basis of all power , a portion of which provides Earth with the light and heat necessary to support life. The Sun is personified in many mythologies: the Greeks
called it Helios and the Romans called
it Sol.
The Sun is classified as a G2 V star,
with G2 standing for the second hottest stars of the yellow G class—of
surface temperature about 5,800 kelvins (K)—and the V representing a main sequence, or dwarf, star, the typical star for this temperature class. The Sun exists in the outer part of the Milky
Way Galaxy and was formed from
material that had been processed inside a Supernova.
Index:
- Our Sun
- Profile
- Sun as a star
- Atmosphere
- Photo sphere
- Chromo sphere
- Corona
- Internal Structure
- Core
- Radioactive Zone
- Convective Zone
- Magnetic activities
- Sun: Nuclear Powerhouse
Physical Characteristics:
Parameter | Value |
Mean Diameter | 1.392 x 106 km |
Equatorial Radius | 6.955 x 105 km |
Mass | 1.989 x 1030 kg |
Average Density | 1.408 x 103 kg/m3 |
Equatorial Surface Gravity | 274 m/s2 |
Temperature | 5778 K |
Luminosity | 3.846 x 1026 w/m2 |
Escape Velocity | 617.7 m/s2 |
- Sun is 13,00,000 times larger than Earth. 109 Earth requires to cover Sun.
- Light takes 8.24 min. to reach Earth.
- It emits EM.
Rotation:
At equator: 25.05 day
At pole: 34.3 day
Rotation velocity: 7.189x103 km/h
Rotation of sun in its different part varies.
It is not similar to Earth.
Atmospheric Layer:
Sun has also an atmosphere with different layer like Earth.
#Sun has 3 layers:
·
Photosphere
·
Chromosphere
·
Corona
Photosphere:
The photosphere is
the deepest layer of the Sun that we can observe directly. It reaches from the
surface visible at the centre of the solar disk to about 250 miles (400 km)
above that. The temperature in the photosphere varies between about 6500 K and
4000 K. Most of the photosphere is covered by granulation.
Granulation: the rice-grain-like structure of the
solar photosphere; granulation is produced by upwelling currents of gas that
are slightly hotter, and therefore brighter, than the surrounding regions,
which are flowing downward into the Sun.
Sun’s
outer atmosphere is transparent, allowing us to look a short distance through
it. But when we try to look through the atmosphere deeper into the Sun, our
view is blocked.The photosphere is
the layer where the Sun becomes opaque and marks the boundary past which we
cannot see. The energy that emerges from the photosphere was originally
generated deep inside the Sun. This energy is in the form of photons, which
make their way slowly toward the solar surface.Outside the Sun, we can
observe only those photons that are emitted into the solar photosphere, where the density of atoms is sufficiently low and the photons can
finally escape from the Sun without colliding with another atom or ion.
So,
photons making their way through the Sun are constantly bumping into atoms,
changing direction, working their way slowly outward, and becoming visible only
when they reach the atmosphere of the Sun where the density of atoms is too low
to block their outward progress.
Astronomers
have found that the solar atmosphere changes from almost perfectly transparent to almost completely opaque in a distance of just over 400 km; it is this thin
region that we call the photosphere, a word
that comes from the Greek for “light sphere”.
Observations with telescopes show that the photosphere has a mottled
appearance, resembling grains of rice spilled on a dark tablecloth or a pot of
boiling oatmeal. This structure of the photosphere
is called granulation. Granules, which
are typically 700 to 1000 km in diameter, appear as bright areas surrounded by
narrow, darker (cooler) regions.The lifetime of an individual granule is only
5 to 10 minutes. Even larger are super granules,which are about 35,000 km
across (about the size of two Earths) and last about 24 hours.
Chromosphere:
Until
this century, the chromosphere was visible only when the photosphere was
concealed by the Moon during a total solar eclipse. In the seventeenth
century, several observers described what appeared to them as a narrow red
“streak” or “fringe” around the edge of the Moon during a brief instant after
the Sun’s photosphere had been covered. The name chromosphere,
from the Greek for “colored sphere,” was given to this red
streak.
Observations
made during eclipses show that the chromosphere is about 2000 to 3000 km thick,
and its spectrum consists of bright emission lines, indicating that this layer
is composed of hot gases emitting light at discrete wavelengths. The reddish
colour of the chromosphere arises from one of the strongest emission lines in
the visible part of its spectrum—the bright red line caused by hydrogen, the
element that, as we have already seen, dominates the composition of the Sun.
#There is
another region called Transition Region is found, where temperature of
sun increases rapidly.
Corona:
The corona is the
outermost layer of the Sun, starting at about 1300 miles (2100 km) above the
solar surface (the photosphere). The temperature in the corona is 500,000 K up
to a few million K. The corona cannot be seen with the naked eye except during
a total solar eclipse, or with the use of a coronagraph. The corona does
not have an upper limit.
The corona extends millions of km above the photosphere and emits about half as much light as the full moon. The reason we don’t see this light until an eclipse occurs is the overpowering brilliance of the photosphere. Just as bright city lights make it difficult to see faint starlight, so too does the intense light from the photosphere hide the faint light from the corona. While the best time to see the corona from Earth is during a total solar eclipse.
Studies of its spectrum show the corona to be very low in
density. At the bottom of the corona, there are only about 109 atoms/cm3, compared with about 1016 atoms/cm3 in the upper photosphere. The corona thins
out very rapidly at greater heights, where it corresponds to a high vacuum by
Earth laboratory standards. The corona extends so far into space—far past
Earth—that here on our planet, we are technically living in the Sun’s
atmosphere.
#Fact: Surprisingly the name of the virus which locked down the whole world this
year is similar to name of the outermost layer of sun’s atmosphere.
Internal Structure:
Core:
The core of the Sun is considered to extend
from the centre to about 0.2 to 0.25 of solar radius.It is
the hottest part of the Sun and
of the Solar System. It has
a density of 150 g/cm3 at the centre, and a temperature of 15 million
kelvins. The core inside 0.20 of the solar radii
contains 34% of the Sun's mass,but only 0.8% of the Sun's volume. Inside the
0.24 solar radius is the core which generates 99% of the fusion power of the Sun.
Radioactive Zone:
The Sun's
radiative zone is the section of the solar interior between the
innermost core and the outer convective zone. In the radiative
zone, energy generated by nuclear fusion in the core moves
outward as electromagnetic radiation. In other
words, the energy is conveyed by photons. When the energy reaches the top of the
radiative zone, it begins to move in a different fashion in the convective
zone. In the convective zone, heat and energy are carried outward along with
matter in swirling flows called convection cells.
The inner parts of the Sun (core and radiative zone) spin differently than the outer
layers (convective zone). The boundary between these two types of rotation,
which lies between the radiative and convective zones, is called the tachocline.
Convective Zone:
It is made out of plasma. The convective zone, like the rest of the
Sun, is made up entirely of plasma. A
plasma is a 'gas' that conducts electrical currents, just like a wire does. The
'gas' contained in neon light bulbs is a plasma for example. The plasma in the
convective zone is mainly made up of hydrogen (70% by mass), helium (27.7% by
mass) plus small quantities of carbon, nitrogen and oxygen.
It is convecting (boiling). As
we have seen above,
the bottom of the convection zone is heated by the radiations coming out of
the radiative
zone, a bit like a room is heated by a radiator. The temperature at the
bottom of the convection zone is 200,000° C. At the same time the top of the
convection zone is being cooled by the creation of light.
The temperature at the surface is only about 5700° C. Thus, there exist a large
temperature difference between the base and the surface of the convection zone.
SUN:
Nuclear Powerhouse:
The Sun puts out an incomprehensible amount of energy—so much that its
ultraviolet radiation can cause sunburns from 93 million miles away. Evidence
shows that the Sun formed about 4.5 billion years ago and has been shining ever
since. How can the Sun produce so much
energy for so long?
The Sun’s energy output is about 4 × 1026 watts. This
is unimaginably bright: brighter than a trillion cities together each with a
trillion 100-watt light bulbs. The total amount of energy produced over the
entire life of the Sun is staggering, since the Sun has been shining for billions
of years. Scientists were unable to explain the seemingly unlimited energy
of stars like the Sun prior to the twentieth century.
When
striving to understand how the Sun can put out so much
energy for so long, scientists considered many different types of energy.
Nineteenth-century scientists knew of two possible sources for the Sun’s
energy: chemical and gravitational energy. The source of chemical
energy most familiar to them was the burning (oxidation) of wood,
coal, gasoline, or other fuel. We know exactly how much energy the burning of
these materials can produce. However, we know from geologic evidence that water
was present on Earth’s surface nearly 4 billion years ago, so the Sun must have
been shining brightly (and making Earth warm) at least as long as that.
Conservation
of Energy:
Other
nineteenth-century attempts to determine what makes the Sun shine used
the law of conservation of energy. Simply stated, this
law says that “Energy cannot be created or
destroyed, but can be transformed from one type to another, such as from heat
to mechanical energy”. The steam engine, which was key to the Industrial
Revolution, provides a good example. In this type of engine, the hot steam from
a boiler drives the movement of a piston, converting heat energy into motion
energy.
Gravitational
Contraction as a Source of Energy
If we
assume that the Sun began its life as a large, diffuse cloud of gas, then we
can calculate how much energy has been radiated by the Sun during its entire
lifetime as it has contracted from a very large diameter to its present size.
The amount of energy is on the order of 1042 joules. Since the solar
luminosity is 4 × 1026 watts (joules/second) or about 1034 joules per year,
contraction could keep the Sun shining at its present rate for roughly 100
million years.
It was
only in the twentieth century that the true source of the Sun’s energy was
identified. The two key pieces of information required to solve the puzzle were
the structure of the nucleus of the atom and the fact that mass can be
converted into energy.
To
imagine what would happen if this hypothesis were true, picture the outer layer
of the Sun starting to fall inward. This outer layer is a gas made up of
individual atoms, all moving about in random directions. If a layer falls
inward, the atoms acquire an additional speed because of falling motion. As the
outer layer falls inward, it also contracts, moving the atoms closer together.
The temperature of a gas is a measure of the kinetic energy (motion) of the
atoms within it; hence, the temperature of this layer of the Sun increases. Collisions also excite electrons within the atoms to higher-energy orbits. When
these electrons return to their normal orbits, they emit photons, which can
then escape from the Sun Kelvin and Helmholtz calculated that a contraction of the Sun at a rate of only about 40 meters per year would be
enough to produce the amount of energy that it is now radiating. Over the span
of human history,the decrease in the Sun’s size from such a slow contraction
would be undetectable.
# Thanks,
see you soon. 🌞🌞🌞🌞🌞🌞🌞🌞🌞🌞🌞🌞🌞🌞🌞