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LECTURE 1




            1
The study of the interaction between
ELECTROMAGNETIC (EM) RADIATION
             and MATTER




                                         2
covers


    ATOMIC                 MOLECULAR
 SPECTROSCOPY             SPECTROSCOPY
(atomic absorption)   (molecular absorption)

                                               3
What is Electromagnetic Radiation?
 is a form of energy that has both Wave and

  Particle Properties.
 For example: Ultraviolet, visible, infrared,

  microwave, radio wave.




                                                 4
5
6
7
   EM radiation is conveniently modeled as waves
    consisting of perpendicularly oscillating
    electric and magnetic fields, as shown below.




                               Direction of
                               propagation



                                                    8
o   At 90° to the direction of propagation is an
    oscillation in the ELECTRIC FIELD.

o   At 90° to the direction of propagation and 90°
    from the electric field oscillation (orthagonal) is
    the MAGNETIC FIELD oscillation.




                                                          9
 Period (p)
           the time required for one cycle to pass a fixed
  point in space.
 Frequency (V @ f )

  the number of cycles which pass a fixed point in space per
  second. Unit in Hz or s-1
 Amplitude (A)

           The maximum length of the electric vector in the
  wave (Maximum height of a wave).
 Wavelength (λ)

  The distance between two identical adjacent points in a
  wave (usually maxima or minima).

                                                               10
 Wavenumber        (ν)
 The number of waves per cm in units of cm-1.
 Radiant   Power ( P )
 The amount of energy reaching a given area per second.
 Unit in watts (W)
 Intensity   (I)
 The radiant power per unit solid angle.




                                                          11
Speed of light = Wavelength x Frequency
   Speed of light = Wavelength x Frequency
                  c = λV
                  c = λV
Where as
Where as
 λ is the wavelength of the waves
  λ is the wavelength of the waves
 V is the frequency of the waves
  V is the frequency of the waves
 c is the speed of light
  c is the speed of light


         c = 3.00 x 1088 m/s = 3.00 x 1010 cm/s
         c = 3.00 x 10 m/s = 3.00 x 1010 cm/s

                                                  12
800 nm




           Infrared radiation      Ultraviolet radiation
            V = 3.75 x 1014 s-1      V = 7.50 x 1014 s-1

Wavelength is inversely proportional to frequency
                         λ ∝ 1/V
   The Higher the Frequency the Shorter the
    Wavelength . The Longer the Wavelength the
    Lower the Frequency.
                                                           13
EMR is viewed as a stream of discrete particles of
energy called photons.
We can relate the energy, E of photon to its
wavelength, frequency and wavenumber by
              hc
     E = hV =    = hcν
              λ
   h = Planck’s constant
   h = 6.63 x 10 -34 J.s

                                                     14
hc
E = hV = hcν =
               λ
Therefore wavenumber, ν

        ν = 1/λ = V/c
Unit of wavenumber is cm-1
What is the energy of a 500 nm photon?

V   = c/λ
    = (3 x 108 m s-1)/(5.0 x 10-7 m)
V   = 6 x 1014 s-1 @ Hz

E   = hV
    = (6.626 x 10-34 J•s)(6 x 1014 s-1)
    = 4 x 10-19 J



                                          16
17
Region     Wavelength
             Range
  UV       180 – 380 nm
Visible    380 – 780 nm
Near-IR    780 – 2500 nm
Mid-IR    2500 – 50000 nm



                            18
Region              Unit         Definition (m)
     X-ray        Angstrom unit, Å      10-10 m
Ultraviolet/visible Nanometer, nm        10-9 m
     Infrared       Micrometer, μm       10-6 m




                                                      19
20
 Atoms are the basic blocks of matter.
 They consist of heavy particles (called protons

  and neutrons) in the nucleus, surrounded by
  lighter particles called electrons.

                                                    21
 An electron will interact with a photon.
 An electron that absorbs a photon will gain
  energy.
 An electron that loses energy must emit a
  photon.
 For absorption to occur, the energy of the
  photon must exactly match an energy level
  in the atom (or molecule) it contacts.
  ◦ Ephoton = Eelectronic transition
 We distinguish two types of absorption
  ◦ Atomic
  ◦ Molecular
                                                22
 Absorption
  EMR energy transferred to absorbing molecule
  (transition from low energy to high energy state).
 Emission

  EMR energy transferred from emitting molecule
  to space (transition from high energy to low
  energy state).
 Scattering

  redirection of light with no energy transfer.
24
 Electrons bound to
  atoms have discrete
  energies (i.e. not all
  energies are allowed).
 Thus, only photons of
  certain energy can
  interact with the
  electrons in a given
  atom.
 Transitions between
  electronic levels of the
  electrons produce line
  spectra.
                             25
 Consider hydrogen, the
  simplest atom.
 Hydrogen has a specific
  line spectrum.
 Each atom has its
  own specific line
  spectrum (atomic
  fingerprint).




                        26
The energy of photon that can promote electrons
to excite/jump to a higher energy level depends
on the energy difference between the electronic
levels.




                                                  27
Each atom has a specific set of energy levels, and
thus a unique set of photon wavelengths with which
it can interact.




                                                     28
 Absorption and emission
     for the sodium atom in the
     gas phase.
    The diagram illustrate the

     transitions (excitation and
     emission) of electrons
     between different energy
     levels in sodium atom.
ΔEtransition = E1 - E0 = hv = hc/λ


                                     29
   The energy, E, associated with the molecular bands:
       Etotal = Eelectronic + Evibrational + Erotational

  In general, a molecule may absorb energy in 3 ways:
1. By raising an electron (or electrons) to a higher
   energy level. (electronic)
2. By increasing the vibration of the constituent nuclei.
   (vibrational)
3. By increasing the rotation of the molecule about the
   axis. (rotational)
hν



En                     En



     hν                     hν


Eo                     Eo



          Absorption             Emission
Rotational
absorption




Vibrational
absorption
33
   Absorption spectrum
    ◦ A plot of the absorbance as a function of
      wavelength or frequency.

   Emission spectrum
    ◦ A plot of the relative power of the emitted
      radiation as a function of wavelength or
      frequency.



                                                    34
Absorption Spectrum of Na




   The two peaks arise from the promotion of
    a 3s electron to the two 3p states


                                                35
Electronic Transition   Vibrational Transition
                        Superimposed on the
                        Electronic Transition




                             Absorption Band –
                             A series of closely
                             shaped peaks




                                                   36
   In solvents the rotational
    and vibrational
    transitions are highly
    restricted resulting in
    broad band
    absorption spectra.




                                 37
   Three types of
    spectra:
    ◦ Lines
    ◦ Bands
    ◦ Continuum
      spectra



                     Emission spectrum of a brine sample
                                                           38
39
Absorption Spectroscopy




Emission Spectroscopy




                          40
1. Source
        A stable source of radiant energy at the
   desired wavelength (or λ range).
2. Sample Holder
        A transparent container used to hold the
   sample (cells, cuvettes, etc.).
3. Wavelength Selector
         A device that isolates a restricted region
   of the EM spectrum used for measurement
                                                      41
   (monochromators, prisms, & filters).
4. Photoelectric Transducer (Detector)
   Converts the radiant energy into a useable
   signal (usually electrical).
5. Signal Processor & Readout
        Amplifies or attenuates the transduced
   signal and sends it to a readout device such as
   a meter, digital readout, chart recorder,
   computer, etc.
                                                     42
Generate a beam of radiation that is stable and has sufficient
power.
A. Continuum Sources
                           emit radiation over a broad
wavelength range and the intensity of the radiation
changes slowly as a function of wavelength.

                            This type of source is commonly
used optical instruments.
                            Deuterium lamp is the most
common UV source.
                            Tungsten lamp is the most       43

common Visible source.
B. Line Sources
Emit a limited number lines or bands of radiation
at specific wavelengths. Used in atomic absorption
spectroscopy.

Types of line sources:
1.Hollow cathode lamps
2.Electrodeless discharge lamps
3.Lasers (Light­amplification by stimulated
emission of radiation)

                                               44
Sample containers usually is called cells or
cuvettes, must have side/windows that are
transparent in the spectral region of interest.

There are few types of cuvettes
1. quartz or fused silica (below 350nm)
    required for UV & VIS region

2. silicate glass (350 – 2000nm)
   cheaper compared to quartz. Used in VIS

3. crystalline sodium chloride
   used in IR                                     45
Wavelength selectors provides a limited, narrow,
continuous group of wavelengths called a band.

Two types of wavelength selectors:
 A) Filters
 B) Monochromators




                                                   46
47
Early detectors in spectroscopic instruments were
the human eye, photographic plates or films.
Modern instruments contain devices that convert
the radiation to an electrical signal.

Two general types of radiation transducers:
    a.    Photon detectors
    b.Thermal detectors




                                                    48
A. Photon Detectors
Commonly useful in ultraviolet, visible and near
infrared instruments.
Several types of photon detectors are available:
    1. Vacuum phototubes
    2.Photomultiplier tubes
    3.Photovoltaic cells
    4.      Silicon photodiodes
    5.Diode array transducers
    6.      Photoconductivity transducers

                                                   49
B. Thermal Detectors
Used for infrared spectroscopy because photons in
   the IR region lack the energy to cause
   photoemission of electrons.

Three types of thermal detectors:
   1. Thermocouples
   2. Bolometers
   3. Pyroelectric transducers




                                                    50
SPECTROMETER
is an instrument that provides information about
   the intensity of radiation as a function of
   wavelength or frequency.

SPECTROPHOTOMETER
is a spectrometer equipped with one or more exit
   slits and photoelectric transducers that permits
   the determination of the ratio of the radiant
   power of two beams as a function of wavelength
   as in absorption spectroscopy.
                                                   51
REGION             SOURCE              SAMPLE           DETECTOR
                                       HOLDER
Ultraviolet     Deuterium lamp       Quartz /fused       Phototube,
                                        silica         Photo Multiplier
                                                         tube, diode
                                                            array
  Visible        Tungsten lamp        Silicate Glass     Phototube,
                                         /Quartz       Photo Multiplier
                                                         tube, diode
                                                            array
 Infrared      Nernst glower (rare      Salt crystals  Thermocouples,
              earth oxides or silicon    (crystalline    bolometers
                 carbide glowers)     sodium chloride)




                                                                          52

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CHM260 - Spectroscopy Method

  • 2. The study of the interaction between ELECTROMAGNETIC (EM) RADIATION and MATTER 2
  • 3. covers ATOMIC MOLECULAR SPECTROSCOPY SPECTROSCOPY (atomic absorption) (molecular absorption) 3
  • 4. What is Electromagnetic Radiation?  is a form of energy that has both Wave and Particle Properties.  For example: Ultraviolet, visible, infrared, microwave, radio wave. 4
  • 5. 5
  • 6. 6
  • 7. 7
  • 8. EM radiation is conveniently modeled as waves consisting of perpendicularly oscillating electric and magnetic fields, as shown below. Direction of propagation 8
  • 9. o At 90° to the direction of propagation is an oscillation in the ELECTRIC FIELD. o At 90° to the direction of propagation and 90° from the electric field oscillation (orthagonal) is the MAGNETIC FIELD oscillation. 9
  • 10.  Period (p) the time required for one cycle to pass a fixed point in space.  Frequency (V @ f ) the number of cycles which pass a fixed point in space per second. Unit in Hz or s-1  Amplitude (A) The maximum length of the electric vector in the wave (Maximum height of a wave).  Wavelength (λ) The distance between two identical adjacent points in a wave (usually maxima or minima). 10
  • 11.  Wavenumber (ν) The number of waves per cm in units of cm-1.  Radiant Power ( P ) The amount of energy reaching a given area per second. Unit in watts (W)  Intensity (I) The radiant power per unit solid angle. 11
  • 12. Speed of light = Wavelength x Frequency Speed of light = Wavelength x Frequency c = λV c = λV Where as Where as λ is the wavelength of the waves λ is the wavelength of the waves V is the frequency of the waves V is the frequency of the waves c is the speed of light c is the speed of light c = 3.00 x 1088 m/s = 3.00 x 1010 cm/s c = 3.00 x 10 m/s = 3.00 x 1010 cm/s 12
  • 13. 800 nm Infrared radiation Ultraviolet radiation V = 3.75 x 1014 s-1 V = 7.50 x 1014 s-1 Wavelength is inversely proportional to frequency λ ∝ 1/V  The Higher the Frequency the Shorter the Wavelength . The Longer the Wavelength the Lower the Frequency. 13
  • 14. EMR is viewed as a stream of discrete particles of energy called photons. We can relate the energy, E of photon to its wavelength, frequency and wavenumber by hc E = hV = = hcν λ h = Planck’s constant h = 6.63 x 10 -34 J.s 14
  • 15. hc E = hV = hcν = λ Therefore wavenumber, ν ν = 1/λ = V/c Unit of wavenumber is cm-1
  • 16. What is the energy of a 500 nm photon? V = c/λ = (3 x 108 m s-1)/(5.0 x 10-7 m) V = 6 x 1014 s-1 @ Hz E = hV = (6.626 x 10-34 J•s)(6 x 1014 s-1) = 4 x 10-19 J 16
  • 17. 17
  • 18. Region Wavelength Range UV 180 – 380 nm Visible 380 – 780 nm Near-IR 780 – 2500 nm Mid-IR 2500 – 50000 nm 18
  • 19. Region Unit Definition (m) X-ray Angstrom unit, Å 10-10 m Ultraviolet/visible Nanometer, nm 10-9 m Infrared Micrometer, μm 10-6 m 19
  • 20. 20
  • 21.  Atoms are the basic blocks of matter.  They consist of heavy particles (called protons and neutrons) in the nucleus, surrounded by lighter particles called electrons. 21
  • 22.  An electron will interact with a photon.  An electron that absorbs a photon will gain energy.  An electron that loses energy must emit a photon.  For absorption to occur, the energy of the photon must exactly match an energy level in the atom (or molecule) it contacts. ◦ Ephoton = Eelectronic transition  We distinguish two types of absorption ◦ Atomic ◦ Molecular 22
  • 23.  Absorption EMR energy transferred to absorbing molecule (transition from low energy to high energy state).  Emission EMR energy transferred from emitting molecule to space (transition from high energy to low energy state).  Scattering redirection of light with no energy transfer.
  • 24. 24
  • 25.  Electrons bound to atoms have discrete energies (i.e. not all energies are allowed).  Thus, only photons of certain energy can interact with the electrons in a given atom.  Transitions between electronic levels of the electrons produce line spectra. 25
  • 26.  Consider hydrogen, the simplest atom.  Hydrogen has a specific line spectrum.  Each atom has its own specific line spectrum (atomic fingerprint). 26
  • 27. The energy of photon that can promote electrons to excite/jump to a higher energy level depends on the energy difference between the electronic levels. 27
  • 28. Each atom has a specific set of energy levels, and thus a unique set of photon wavelengths with which it can interact. 28
  • 29.  Absorption and emission for the sodium atom in the gas phase.  The diagram illustrate the transitions (excitation and emission) of electrons between different energy levels in sodium atom. ΔEtransition = E1 - E0 = hv = hc/λ 29
  • 30. The energy, E, associated with the molecular bands: Etotal = Eelectronic + Evibrational + Erotational  In general, a molecule may absorb energy in 3 ways: 1. By raising an electron (or electrons) to a higher energy level. (electronic) 2. By increasing the vibration of the constituent nuclei. (vibrational) 3. By increasing the rotation of the molecule about the axis. (rotational)
  • 31. hν En En hν hν Eo Eo Absorption Emission
  • 33. 33
  • 34. Absorption spectrum ◦ A plot of the absorbance as a function of wavelength or frequency.  Emission spectrum ◦ A plot of the relative power of the emitted radiation as a function of wavelength or frequency. 34
  • 35. Absorption Spectrum of Na  The two peaks arise from the promotion of a 3s electron to the two 3p states 35
  • 36. Electronic Transition Vibrational Transition Superimposed on the Electronic Transition Absorption Band – A series of closely shaped peaks 36
  • 37. In solvents the rotational and vibrational transitions are highly restricted resulting in broad band absorption spectra. 37
  • 38. Three types of spectra: ◦ Lines ◦ Bands ◦ Continuum spectra Emission spectrum of a brine sample 38
  • 39. 39
  • 41. 1. Source A stable source of radiant energy at the desired wavelength (or λ range). 2. Sample Holder A transparent container used to hold the sample (cells, cuvettes, etc.). 3. Wavelength Selector A device that isolates a restricted region of the EM spectrum used for measurement 41 (monochromators, prisms, & filters).
  • 42. 4. Photoelectric Transducer (Detector) Converts the radiant energy into a useable signal (usually electrical). 5. Signal Processor & Readout Amplifies or attenuates the transduced signal and sends it to a readout device such as a meter, digital readout, chart recorder, computer, etc. 42
  • 43. Generate a beam of radiation that is stable and has sufficient power. A. Continuum Sources emit radiation over a broad wavelength range and the intensity of the radiation changes slowly as a function of wavelength. This type of source is commonly used optical instruments. Deuterium lamp is the most common UV source. Tungsten lamp is the most 43 common Visible source.
  • 44. B. Line Sources Emit a limited number lines or bands of radiation at specific wavelengths. Used in atomic absorption spectroscopy. Types of line sources: 1.Hollow cathode lamps 2.Electrodeless discharge lamps 3.Lasers (Light­amplification by stimulated emission of radiation) 44
  • 45. Sample containers usually is called cells or cuvettes, must have side/windows that are transparent in the spectral region of interest. There are few types of cuvettes 1. quartz or fused silica (below 350nm) required for UV & VIS region 2. silicate glass (350 – 2000nm) cheaper compared to quartz. Used in VIS 3. crystalline sodium chloride used in IR 45
  • 46. Wavelength selectors provides a limited, narrow, continuous group of wavelengths called a band. Two types of wavelength selectors: A) Filters B) Monochromators 46
  • 47. 47
  • 48. Early detectors in spectroscopic instruments were the human eye, photographic plates or films. Modern instruments contain devices that convert the radiation to an electrical signal. Two general types of radiation transducers: a. Photon detectors b.Thermal detectors 48
  • 49. A. Photon Detectors Commonly useful in ultraviolet, visible and near infrared instruments. Several types of photon detectors are available: 1. Vacuum phototubes 2.Photomultiplier tubes 3.Photovoltaic cells 4. Silicon photodiodes 5.Diode array transducers 6. Photoconductivity transducers 49
  • 50. B. Thermal Detectors Used for infrared spectroscopy because photons in the IR region lack the energy to cause photoemission of electrons. Three types of thermal detectors: 1. Thermocouples 2. Bolometers 3. Pyroelectric transducers 50
  • 51. SPECTROMETER is an instrument that provides information about the intensity of radiation as a function of wavelength or frequency. SPECTROPHOTOMETER is a spectrometer equipped with one or more exit slits and photoelectric transducers that permits the determination of the ratio of the radiant power of two beams as a function of wavelength as in absorption spectroscopy. 51
  • 52. REGION SOURCE SAMPLE DETECTOR HOLDER Ultraviolet Deuterium lamp Quartz /fused Phototube, silica Photo Multiplier tube, diode array Visible Tungsten lamp Silicate Glass Phototube, /Quartz Photo Multiplier tube, diode array Infrared Nernst glower (rare Salt crystals Thermocouples, earth oxides or silicon (crystalline bolometers carbide glowers) sodium chloride) 52