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Atomic Spectroscopy

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Reviewer for Atomic Spectroscopy

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Page 1: Atomic Spectroscopy

Atomic Spectroscopy

Page 2: Atomic Spectroscopy

An Introduction of Spectrometric Methods

Page 3: Atomic Spectroscopy

Properties of Electromagnetic Radiation

Electromagnetic Radiation– energy radiated in the form of a WAVE caused

by an electric field interacting with a magnetic field

– result of the acceleration of a charged particle– does not require a material medium and can

travel through a vacuum

Page 4: Atomic Spectroscopy

Properties of Electromagnetic Radiation

vi = i

where vi => velocity => frequency i => wavelength

Page 5: Atomic Spectroscopy

Properties of Electromagnetic Radiation

in vacuum, velocity is independent of frequency,

maximum value

c =

= 2.998 X 108 m/s

Page 6: Atomic Spectroscopy

Properties of Electromagnetic Radiation

"Representation of a beam of monochromatic, plane polarized radiation. The arrows represent the electrical vectors."

Page 7: Atomic Spectroscopy

Properties of Electromagnetic Radiation

"Effect of change of medium on a monochromatic beam of radiation."

Page 8: Atomic Spectroscopy

Properties of Electromagnetic Radiation

"Regions of the electromagnetic spectrum"

Page 9: Atomic Spectroscopy

Properties of Electromagnetic Radiation

"Common Spectroscopic Methods Based on electromagnetic Radiation"

Page 10: Atomic Spectroscopy

Properties of Electromagnetic Radiation

Wave Equationfor a single wave

y = A sin (2t + )

Page 11: Atomic Spectroscopy

Properties of Electromagnetic Radiation

for n waves of same frequency superimposed of phase angle y = A1 sin (2t + 1 )

+ A2 sin (2t + 2 )+ A3 sin (2t + 3 )+ + An sin (2t + n )

Page 12: Atomic Spectroscopy

Properties of Electromagnetic Radiation

"Superposition of sinusoidal waves: (a) same frequency, small difference in phase (b) same frequency, large difference in phase (c) difference frequencies, starting in phase.

Page 13: Atomic Spectroscopy

Properties of Electromagnetic Radiation

for n waves of different frequencies superimposed of phase angle y = A1 sin (2

t + 1 )+ A2 sin (2

t + 2 )+ A3 sin (2

t + 3 )+ + An sin (n t + n )

Page 14: Atomic Spectroscopy

Properties of Electromagnetic Radiation

"Superposition of sine waves to form a square wave: (a) combination of three sine waves, and (b) combination of three, as in (a), and nine sine waves."

Page 15: Atomic Spectroscopy

Diffraction

"Propagation of waves through a slit: (a) xy >(b) xy ."

Page 16: Atomic Spectroscopy

Diffraction

"Diffraction of monochromatic radiation by slits."

Page 17: Atomic Spectroscopy

Diffraction

= CF = BC sin

n

= CF = BC sin

DE = OD sin

Page 18: Atomic Spectroscopy

DiffractionBC DE BC DE

n = ---------- = ------------OD OE

where OE => distance from screen to plane of slitsBC => slit spacingDE => band spacing

Page 19: Atomic Spectroscopy

EXAMPLE: Suppose that the screen in the figure shown is 2.00 m from the plane of the slits and that the slit spacing is 0.300 mm. What is the wavelength of radiation if the fourth band is located 15.4 mm from the central band?

Page 20: Atomic Spectroscopy

EXAMPLE: Suppose that the screen in the figure shown is 2.00 m from the plane of the slits and that the slit spacing is 0.300 mm. What is the wavelength of radiation if the fourth band is located 15.4 mm from the central band?

BC DE BC DEn

= ------------ = ------------

OD OEn = 4

___OE = 2.00 m___BC = 0.300 mm___DE = 15.4 mm

Page 21: Atomic Spectroscopy

EXAMPLE: Suppose that the screen in the figure is 2.00 m from the plane of the slits and that the slit spacing is 0.300 mm. What is the wavelength of radiation if the fourth band is located 15.4 mm from the central band?

n = 4 OE = 2.00 m___ ___BC = 0.300 mm DE = 15.4 mm

(0.300 mm)(15.4 mm) = ----------------------------

4 (2 * 1000)mm= 5.78 X 10-4 mm or 578 nm

Page 22: Atomic Spectroscopy

Transmission of RadiationTransmission

– rate at which radiation passes through a transparent material is less than through a vacuum

– depends upon the kinds and concentrations of atoms, ions, and molecules in the medium

– radiation must interact with material– interaction must not undergo permanent energy

transfer

Page 23: Atomic Spectroscopy

Transmission of Radiation

Transmissionni = c/vi

where ni => refractive index, measure of interactionc => speed of light in vacuumvi => speed of light in medium

Page 24: Atomic Spectroscopy

Transmission of Radiation

Dispersion– variation in refractive index of a substance with

wavelength or frequencyRefraction of Radiation

– Snell’s Law

sin

n2 v1

sin

n1 v2

Page 25: Atomic Spectroscopy

Reflection of Radiation

• reflection always occurs when radiation passes from one medium to another

• reflection greatest when two materials have the greatest difference on their refractive indices

Page 26: Atomic Spectroscopy

Scattering of Radiation

Types of Scattering– Rayleigh Scattering

• scattering involving molecules which are considerably smaller than the wavelength of radiation

• blue sky results from greater scattering of shorter wavelength visible light

Page 27: Atomic Spectroscopy

Scattering of Radiation

Types of Scattering– Scattering by Large Molecules

• can be measured• a function of the size and shape of molecule

Page 28: Atomic Spectroscopy

Scattering of Radiation

Types of Scattering– Raman Scattering

• part of the radiation undergoes quantized frequency changes

Page 29: Atomic Spectroscopy

Quantum-Mechanical Properties of Radiation

E = h

= hc/

Page 30: Atomic Spectroscopy

Emission of Radiation

• Line spectra• Band spectra• Continuum spectra

Page 31: Atomic Spectroscopy

Line spectra

“Emission spectrum of a brine obtained with an oxy-hydrogen flame”

Page 32: Atomic Spectroscopy

Line spectra

“X-ray emission spectrum of Molybdenum metal”

Page 33: Atomic Spectroscopy

Band spectra

“Energy-level diagram for (a) a sodium atom showing the source of a line spectrum and (b) a simple molecule showing the source of a band spectrum.”

Page 34: Atomic Spectroscopy

Continuum spectra“Blackbody radiation curves”

Page 35: Atomic Spectroscopy

Absorption of Radiation

energy of exciting photon must equal energy difference between ground state and 1 excited state for absorption to occur

Page 36: Atomic Spectroscopy

Absorption of Radiation

"Some typical ultraviolet absorption spectra."

Page 37: Atomic Spectroscopy

Atomic Absorption

• absorption occurs with only a few well- defined frequencies

• electronic excitation

Page 38: Atomic Spectroscopy

Molecular Absorption

E = Eelectronic + Evibrational + Erotational

Page 39: Atomic Spectroscopy

Molecular Absorption

"Partial energy level diagram for a fluorescent organic molecule."

Page 40: Atomic Spectroscopy

Emission of Radiation

• radiation resulting from the relaxation to lower energy states of excited particles

Page 41: Atomic Spectroscopy

Absorption Methods, Transmittance

T = P/Po

where T => transmittanceP => power of transmitted radiationPo => power of incident

radiation%T = (P/Po )*100

where %T => percent transmittance

Page 42: Atomic Spectroscopy

Absorption Methods, Absorbance

A = - log10 T = - log10 (P/Po )

where A => absorbance

Page 43: Atomic Spectroscopy

Absorption Methods, Beer’s Law

A = abc = bcwhere a => absorptivity

b => path lengthc => concentration

=> molar absorptivity

Page 44: Atomic Spectroscopy

Spectroscopic Methods

“Major classes of spectroscopic methods”

Page 45: Atomic Spectroscopy

Absorption Methods

“Attenuation of a beam of radiation by an absorbing species”

Page 46: Atomic Spectroscopy

Absorption Methods“Single-beam photometer for absorption measurements in the visible region.”

Page 47: Atomic Spectroscopy

Absorption Methods“Readout for an inexpensive photometer.”

transmittance scale is linearabsorbance scale is exponentialthus, read transmittance, then calculate absorbance