Lec 9 Flashcards

(49 cards)

1
Q

rate of energy flow is called

A

power and measured in watts

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2
Q

reflection (mirror)

A

angle of incidence = angle of reflection

A mirror reflects light along
a simple path: The angle at
which the light strikes the
mirror is the same angle at
which it is reflected

Reflection: light can bounce off matter,
leading to what we call reflection when the bouncing is all in the same general direction

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3
Q

scattering

A

when the
bouncing is more random

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4
Q

emission

A

A light bulb emits visible light; the energy of
the light comes from electrical potential energy supplied
to the light bulb

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5
Q

absorption

A

When you place your hand near an incandescent light bulb, your hand absorbs some of the light,
and this absorbed energy warms your hand

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6
Q

transmission

A

Some forms of matter (such as glass or
air) transmit light, allowing it to pass through.

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7
Q

wavelength

A

the distance
from one peak to the next (or one trough to the next)

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8
Q

frequency

A

the number of peaks passing by any point
each second

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9
Q

speed (of waves)

A

tells us how fast their peaks
travel across the pond. Because the waves carry energy, the
speed essentially tells us how fast the energy travels from one place to another

wavelength x freq. = speed

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10
Q

magnetic field

A

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

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11
Q

why do we say light is an electromagnetic wave?

A

Light waves are traveling vibrations of both electric and
magnetic fields, so we say that light is an electromagnetic
wave

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12
Q

relationship between wavelength and
frequency for light:

A

The longer the wavelength, the lower
the frequency, and the shorter the wavelength, the higher
the frequency

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13
Q

photons

A

We say that light comes in individual
“pieces,” called photons, that have properties of both particles and waves.

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14
Q

electromagnetic spectrum

A

In fact, the light that we can
see is only a tiny part of the complete spectrum of light,
usually called the electromagnetic spectrum

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15
Q

electromagnetic radiation

A

light itself is
often called electromagnetic radiation

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16
Q

visible light

A

the light that we can see with our eyes, found in the middle of the spectrum

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17
Q

infrared

A

Light with wavelengths somewhat longer than those of red light is called infrared, because it lies beyond the red end of the rainbow

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18
Q

radio waves

A

Radio waves are the longest-wavelength
light. Light in the region near the border between infrared
and radio waves

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19
Q

microwaves

A

wavelengths range from micrometers
to centimeters, is often called microwaves

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20
Q

ultraviolet

A

On the other side of the spectrum, light with wavelengths somewhat shorter than those of blue light is called
ultraviolet, because it lies beyond the blue (or violet) end of the rainbow.

21
Q

x-rays

A

w. Light with even shorter wavelengths is
called x-rays

22
Q

gamma rays

A

light with the shortest wavelength

23
Q

continuous spectra

A

when the rainbow spans a broad range of wavelengths without interruption

24
Q

emission line spectrum

A

A thin or low-density cloud of gas emits light only at specific wavelengths that depend on its composition and temperature.

The spectrum therefore consists of
bright emission lines against a black background and is called an emission line spectrum

25
absorption line spectrum
If the cloud of gas lies between us and a light bulb (and the cloud is cooler than the light bulb or other light source), we still see most of the continuous spectrum of the light bulb. However, the cloud absorbs light of specific wavelengths, so the spectrum shows dark absorption lines over the background rainbow, making it what we call an absorption line spectrum
26
more on emission line spectra
The atoms in any cloud of gas are continually colliding with one another, exchanging energy in each collision Most of the collisions simply send the atoms flying off in new directions However, a few of the collisions transfer the right amount of energy to bump an electron from a low energy level to a higher energy level. Electrons can’t stay in higher energy levels for long. They always fall back down to the ground state, level 1, usually in a tiny fraction of a second. The energy the electron loses when it falls to a lower energy level must go somewhere, and often it goes into emitting a photon of light. The emitted photon must have the same amount of energy that the electron loses, which means that it has a specific wavelength and frequency
27
more on absorption line spectra
Now, suppose a light bulb illuminates the hydrogen gas from behind The light bulb emits light of all wavelengths, producing a spectrum that looks like a rainbow of color. However, the hydrogen atoms can absorb those photons that have the right amount of energy to raise an electron from a low energy level to a higher one. It is an absorption line spectrum, because the light bulb produces a continuous rainbow of color while the hydrogen atoms absorb light at specific wavelength electrons absorbing photons with this wavelength can rise up from level 2 to level 3 (producing an absorption line at this wavelength
28
molecular bands
A molecule can absorb or emit a photon when it changes its rate of vibration or rotation. The energy changes in molecules are usually smaller than those in atoms and therefore produce lower-energy photons, and the energy levels also tend to be bunched more closely together than in atoms. Molecules therefore produce spectra with many sets of tightly bunched lines, called molecular bands, that are usually found in the infrared portion of the electromagnetic spectrum
29
how does light tell us the temp of planets and stars?
Although continuous spectra can be produced in more than one way, light bulbs, planets, and stars produce a particular kind of continuous spectrum that can help us determine their temperatures Photons tend to bounce around randomly inside such an object, constantly exchanging energy with its atoms or molecules. By the time the photons finally escape the object, their radiative energies have become randomized so that they are spread over a wide range of wavelengths. The wide wavelength range of the photons explains why the spectrum of light from such an object is smooth, or continuous, like a pure rainbow without any absorption or emission lines. Most important, the spectrum from such an object depends on only one thing: the object’s temperature. Remember that temperature represents the average kinetic energy of the atoms or molecules in an object Because the randomly bouncing photons interact so many times with those atoms or molecules, they end up with energies that MATCH the kinetic energies of the object’s atoms or molecules—which means the photon energies depend only on the object’s temperature, regardless of what the object is made of
30
thermal radiation
The temperature dependence of this light explains why we call it thermal radiation (sometimes known as blackbody radiation), and its spectrum is called a thermal radiation spectrum.
31
what objects emit a perfect thermal radiation spectrum?
No real object emits a perfect thermal radiation spectrum, but almost all familiar objects—including the Sun, the planets, rocks, and even you—emit light that approximates thermal radiation.
32
Law 1 (hotter --> brighter)
The curve for a hotter object is everywhere above the curve for a cooler object, showing that hotter objects emit more radiation per unit surface area at every wavelength (the Stefan-Boltzmann law): Each square meter of a hotter object’s surface emits more light at all wavelengths. For example, each square meter on the surface of the 15,000 K star emits a lot more light at every wavelength than each square meter of the 3000 K star, and the hotter star emits light at some ultraviolet wavelengths that the cooler star does not emit at all
33
Law 2 (hotter -->higher energy)
The peak wavelength is farther to the left for hotter objects, showing that hotter objects emit more of their light at shorter wavelength (high energy) (Wien’s law): Hotter objects emit photons with a higher average energy, which means a shorter average wavelength. That is why the peaks of the spectra are at shorter wavelengths for hotter objects. For example, the peak for the 15,000 K star is in ultraviolet light, the peak for the 5800 K Sun is in visible light, and the peak for the 3000 K star is in the infrared
34
doppler effect
The Doppler effect causes similar shifts in the wavelengths of light (FIGURE 5.21c). If an object is moving toward us, the light waves bunch up between us and the object, so its entire spectrum is shifted to shorter wavelengths.
35
blueshift
Because shorter wavelengths of visible light are bluer, the Doppler shift of an object coming toward us is called a blueshift.
36
redshift
If an object is moving away from us, its light is shifted to longer wavelengths. We call this a redshift because longer wavelengths of visible light are redder
37
laboratory spectrum
Object 1 Lines redshifted: -Object moving away from us. Object 2 Greater redshift: -Object moving away faster than Object 1. Object 3 Lines blueshifted: -Object moving toward us. Object 4 Greater blueshift: -Object moving toward us faster than Object 3.
38
continuous spectrum
The visible light we see from Mars is actually reflected sunlight. The Sun produces a nearly continuous spectrum of light, which includes the full rainbow of color
39
scattered/reflected light
Mars is red because it absorbs most of the blue light from the Sun but reflects (scatters) most of the red light. This pattern of absorption and reflection helps us learn the chemical composition of the surface.
40
emission lines
Ultraviolet emission lines in the spectrum of Mars tell us that the atmosphere of Mars contains hot gas at high altitudes.
41
thermal radiation
Objects emit a continuous spectrum of thermal radiation that peaks at a wavelength determined by temperature. Thermal radiation from Mars produces a broad hump in the infrared, with a peak indicating a surface temperature of about 225 K
42
absorption lines
These absorption lines reveal the presence of carbon dioxide in Mars’s atmosphere
43
doppler effect
The wavelengths of the spectral lines from Mars are slightly shifted by an amount that depends on the velocity of Mars toward or away from us as it moves in its orbit around the Sun.
44
what is light?
Light is an electromagnetic wave, but it also comes in individual “pieces” called photons. Each photon has a precise wavelength, frequency, and energy: The shorter the wavelength, the higher the frequency and energy.
45
what is the electromagnetic spectrum?
In order of decreasing wavelength (increasing frequency and energy), the forms of light are radio waves, microwaves, infrared, visible light, ultraviolet, x-rays, and gamma rays.
46
what are the 3 basic types of spectra?
There are three basic types of spectra: a continuous spectrum, which looks like a rainbow of light; an absorption line spectrum, in which specific colors are missing from the rainbow; and an emission line spectrum, in which we see light only with specific colors against a black background.
47
how does light tell us what things are made of?
Emission lines or absorption lines occur only at specific wavelengths that correspond to particular energy level transitions in atoms or molecules. Every kind of atom, ion, and molecule produces a unique set of spectral lines, so we can determine composition by identifying these lines
48
how does light tell us the temp of planets and stars?
Objects such as planets and stars produce thermal radiation spectra, the most common type of continuous spectra. We can determine temperature from these spectra because hotter objects emit more total radiation per unit area and emit photons with a higher average energy.
49
how does light tell us the speed of a distant object?
The Doppler effect tells us how fast an object is moving toward or away from us. Spectral lines are shifted to shorter wavelengths (a blueshift) in objects moving toward us and to longer wavelengths (a redshift) in objects moving away from us.