Lecture 2 Flashcards

1
Q

human contribution to global warming

A

global warming by approximately 1 degree is caused by human made carbon dioxide

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2
Q

lag in GHG emission

A

if GHG emissions were ceased, there would still be an increase in global warming bc there’s a lag between the GHG levels and the eventual temperature

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3
Q

albedo effect

A

warming due to more dark soil, rocks, etc. exposed when ice is melting (there is less sunlight reflected)

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4
Q

permafrost deposits of methane

A

warming due to the release of methane from clathrates when ice is melting (methane is trapped in ice lattices)

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5
Q

carbon dioxide in oceans

A

warming due to the release of trapped GHG when oceans are warmed up

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6
Q

inorganic chemistry’s affect on GHG

A

promote reactions that will use up carbon dioxide

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7
Q

solar fuels

A
  • produced when carbon dioxide is reacted with water, catalyzed by energy (sunlight)
  • burning solar fuels does not add new carbon dioxide to the environment
  • must be stored
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8
Q

electron duality

A

behaves as both a particle and wave

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9
Q

de Broglie wavelength

A

wavelength calculated by Planck’s constant over momentum

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10
Q

photoelectron effect

A
  • no electrons were emitted unless the threshold was reached

- intensity of light did not emit electrons below energy threshold, only when the light energy was above threshold level

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11
Q

Heisenberg’s Uncertainty Principle

A
  • the more precise a position is known, the less precise a momentum is known and vice versa
  • uncertainty in position x uncertainty in momentum > Planck’s constant / 4*pi
  • cannot know the precise position and momentum of a particle at the same time
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12
Q

Schrodinger Equation

A
  • described the energy of electrons as waves, denoted as wavefunction (psi)
  • Hamiltonian operator (eigenfunction) x psi = energy of the electron x psi
  • eigenfunction gives the energy of an electron in a H atom
  • E is the energy
  • psi can be treated mathematically to give shapes, phases, and nodes of an electron wave in an atom
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13
Q

theories that formed the Schrodinger Equation

A
  • took 3 months to formulate
  • light was a solid beam; and
  • light was a wave
  • led to the equation
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14
Q

integral of psi^2

A
  • probability of finding the electron in a certain region of space defined by the integral limits
  • integral of the overall space should equal 1
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15
Q

shape of an orbital

A
  • defined by the probability over space (integral of psi^2)
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16
Q

orbital

A
  • shape of region with highest probability of finding the elecron wave
  • shape of stable wavefunction for an electron atom
  • if an electron has a wavelength, the shape of the orbital represents a whole number of wavelengths, like a standing wave
17
Q

wavefunction

A
  • a whole number of wavelengths
  • a standing wave without destructive interference
  • electrons of a given wavelength will have one stable shape
18
Q

Schrodinger Equation drawbacks

A
  • only gives precise solutions for single electron systems
19
Q

polyelectron system

A
  • polyelectron systems have electrons that are attracted to the nucleus, while also exhibiting repulsion against other electrons
  • both electrons are moving, therefore there is no precise mathematical equation
  • can be approximated because they behave like hydrogen atoms; approximations are good
  • precise solution for helium DNE but it does for He+
20
Q

polar coordinates

A
  • most convenient way to represent wavefunction
  • r is the radius, the distance from the nucleus
  • depends on the principal quantum number, n
  • n = 0, 1, 2, 3…
  • theta is the angle from perpendicular axis
  • depends on the angular momentum quantum number, l
  • l = n-1
  • phi is the angle from one axis
  • depends on the magnetic quantum number, ml
  • ml = -l, …, 0, …, +l
21
Q

angular momentum quantum number of s orbitals

A
  • n = 1

- l = 0

22
Q

angular momentum quantum number of p orbitals

A
  • n = 2

- l = 1

23
Q

angular momentum quantum number of d orbitals

A
  • n = 3

- l = 2