AST201 week 4

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gravitational contraction

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1

gravitational contraction

the sun generates energy by slowly contracting in size, a gradually shrinking sun would always have some gas moving inward converting gravitation potential energy into thermal energy

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sun has 2 kinds of balance that keep its size and energy output stable

gravitational equilibrium and energy balance

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gravitational equilibrium

between outward push of internal gas pressure and the inward pull of gravity

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energy balance

between the rate of which fusion releases energy in the sun’s core and the rate at which the sun’s surface radiates this energy into space

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in about 5 billion years…

the sun will finally exhaust its nuclear fuel and gravitational contraction will begin once again

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sunspots

visible splotches that appear darker than the surrounding surface (larger in life than earth)

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power

the rate at which energy is used or released

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luminosity

a stars total power output

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solar wind

stream of charged particles continually blown outward in all directions from the sun

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corona

outermost layer of the atmosphere, temp is astonishingly high, density is very low

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cromosphere

middle layer of the solar atmosphere and the region that radiates most of the sun’s UV light

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photosphere

lowest layer of the atmosphere, visible surface of the earth

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convection zone

where energy generated in the solar core travels upward, transported by the rising of hot gas and falling of cool gas called convection

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radiation zone

where energy moves outward primarily in the form of photons of light, turbulence of convection zone gives way to the calmer plasma

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core

source of suns energy, density is more than 100 times that of water, extreme pressure

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radiative energy

the energy that light carries

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joules

the unit we measure energy in

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power

the rate of energy flow, measured in units called watts

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spectrum

a prism split light into the rainbows of light

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white light

a mix of all these colours in roughly equal proportions

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black light

when we perceive no light and hence no colour

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primary colours of vision

red, green, blue (RGB)

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how do light and matter interact

emission, absorption, reflection

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transparent

materials which transmit light

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opaque

materials that absorb light

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particle

can sit still or move from one place to another

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waves

consist of peaks

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wavelength

distance from one peak to the next

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frequency

number of peaks passing by any point each second

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hertz

another name for cycles per second

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field

describe the strength of force that a particle would experience at any point in space

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electromagnetic waves

light waves are traveling vibrations of both electric and magnetic fields

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photons

light comes in individual “pieces” that have properties of both particles and waves

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electromagnetic spectrum

light that we can see

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electromagnetic radiation

light itself

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visible light

light that we can see with the naked eye

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infared

light with wavelengths somewhat longer than those of red light

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Ultraviolet

lies between blue and end of the rainbow in wavelengths

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atoms

all ordinary matter is composed of atoms

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element

atoms come in different types and each type corresponds to a different chemical element

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atoms are made up off:

  • protons

  • neutrons

  • electrons

  • nucleus

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attraction and repulsion

oppositely charged particles attract and similarly charged particles repel

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molecules

number of different material substances is far greater than the number of chemical elements because atoms can combine to form molecules

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chemical bond

interactions between electrons that hold the atoms in a molecule together

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molecular dissociation

high enough temp, the collisions become so violent they break chemical bonds

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pressure

force per unit area pushing on an objects surface

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energy levels

the possible energy of an atom

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energy level transitions

an electron can rise from a low energy level to a higher one, or fall from a high level to a lower level

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spectroscopy

the process of obtaining a spectrum and reading the info it contains

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three basic types of spectra

  1. continuous spectrum

  2. emission line spectrum

  3. absorption line spectrum

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continuous spectrum

the spectrum of a traditional, or incandescent, light bulb is a rainbow of colour, because the rainbow spans a brand range of wavelengths without interruption

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emission line spectrum

a thin or low density cloud of gas emits light only at a specific wavelengths that depend on its composition and temp, the spectrum consists of bright emission lines against a black background

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absorption line spectrum

cloud of gas lies between us and a lightbulb, still see most of the continuous spectrum of the light bulb, but the cloud absorbs light of specific wavelengths, so the spectrum shows dark absorption lines over the background rainbow

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two laws of thermal radiation

  1. each square metre of a hotters object surface emits more light at all wavelengths

  2. hotter objects emit photons with a higher average energy

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doppler effect

if an object is moving toward us the light waves bunch up and its entire spectrum is shifted shorter wavelengths

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sun’s size

diameter is 100 times Earth’s diameter

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sun’s distance

8 light minutes from Earth

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Cecilia Payne-Gaposchkin

showed that the sun was made mostly of hydrogen, a little helium, and tiny amounts of other elements

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colour and wavelength

the wavelength of light determines its colour and energy

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short wavelengths

bluer (and more energetic)

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red light

low energy (700 nm)

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blue light

high energy (400 nm)

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the sun appears to have

a continuous spectrum: it has some of every colour of light

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opaque objects

emit a special kind of continuous spectrum

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<p>blackbody spectrum</p>

blackbody spectrum

the amount of light given off by a blackbody and the wavelength where it emits the most light set by the temp of the blackbody

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as you heat an opaque object

it emits more light

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as you heat a blackbody

the wavelength at which it emits the most light shifts to shorter wavelengths

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spectral lines

tell us what the sun and other stars are made of

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electrons can be forced to jump to a higher-energy orbital by

absorbing light

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different chemical elements have

different sets of orbitals

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electrons can spontaneously drop to a lower-energy orbital by

emitting light

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orbitals do not have colours but

transitions between orbitals do

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stars are

blackbodies or “thermal emitters”

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sun is not

on fire, it is mainly made of hydrogen

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plasma

a gas that is so hot, the electrons break free from the atoms

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hydrostatic equilibrium

the sun is in this, the pressure pushing outwards and the gravity pulling inwards is balanced

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sun’s surface temperature

5800 K

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sun's core temperature

15 million K

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E = mc^2

the reaction between energy and mass

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nuclear reactions can

convert matter to energy (or the reverse)

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in the centre of the sun,

hydrogen is being converted into helium via nuclear fusion

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nuclear fusion

providing enough outward pressure necessary to support stars against collapse

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neutrinos

only interact with other matter via the weak nuclear force and gravity, can pass through objects that are very large and dense

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neutrinos dont

respond to the electromagnetic force, so they dont interact with most matter

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