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UV-Visible spectroscopy 
Dr. V. Krishnakumar 
Professor and Head 
Department of Physics 
Periyar University 
Salem. Tamilnadu 
India
UV Spectroscopy 
I. Introduction 
A. UV radiation and Electronic Excitations 
1. The difference in energy between molecular bonding, non-bonding 
and anti-bonding orbitals ranges from 125-650 kJ/mole 
2. This energy corresponds to EM radiation in the ultraviolet (UV) 
region, 100-350 nm, and visible (VIS) regions 350-700 nm of the 
spectrum 
3. For comparison, recall the EM spectrum: 
g-rays X-rays UV IR Microwave Radio 
4. Using IR we observed vibrational transitions with energies of 8-40 
kJ/mol at wavelengths of 2500-15,000 nm 
5. For purposes of our discussion, we will refer to UV and VIS 
spectroscopy as UV 
Visible
Analysis 
When continuous wave radiation is passed 
through a prism a diffraction pattern is produced 
(called a spectrum) made up of all the 
wavelengths associated with the incident 
radiation. 
When continuous wave radiation passes 
through a transparent material (solid or 
liquid) some of the radiation might be 
absorbed by that material. 
Radiation source 
Diffraction prism 
Spectrum 
Spectrum with ‘gaps’ 
Transparent material 
that absorbs some 
radiation 
in it 
If, having passed through the material, the beam is diffracted by passing through a prism it will produce 
a light spectrum that has gaps in it (caused by the absorption of radiation by the transparent material 
through which is passed). 
The effect of absorption of radiation on the transparent material is to change is from a low energy state 
(called the ground state) to a higher energy state (called the excited state). 
The difference between all the spectroscopic techniques is that they use different wavelength radiation 
that has different associated energy which can cause different modes of excitation in a molecule. 
For instance, with infra red spectroscopy the low energy radiation simply causes bonds to bend and 
stretch when a molecule absorbs the radiation. With high energy UV radiation the absorption of energy 
causes transition of bonding electrons from a low energy orbital to a higher energy orbital. 
The energy of the ‘missing’ parts of the spectrum corresponds exactly to the energy difference between 
the orbitals involved in the transition.
Energy transitions 
s* 
Unoccupied 
Energy 
p* 
n 
p 
s 
Levels 
Occupie 
d Energy 
Levels 
The bonding orbitals with which you are familiar are the s-bonding 
orbitals typified by simple alkanes. These are low energy (that is, 
stable). 
Next (in terms of increasing energy) are the p-bonding orbitals 
present in all functional groups that contain double and triple bonds 
(e.g. carbonyl groups and alkenes). 
Higher energy still are the non-bonding orbitals present on atoms 
that have lone pair(s) of electrons (oxygen, nitrogen, sulfur and 
halogen containing compounds). 
All of the above 3 kinds of orbitals may be occupied in the ground 
state. 
Two other sort of orbitals, called antibonding orbitals, can only be 
occupied by an electron in an excited state (having absorbed UV for 
instance). These are the p* and s* orbitals (the * denotes 
antibonding). Although you are not too familiar with the concept of 
an antibonding orbital just remember the following – whilst electron 
density in a bonding orbital is a stabilising influence it is a 
destabilising influence (bond weakening) in an antibonding orbital. 
Antibonding orbitals are unoccupied in the ground state 
UV 
A transition of an electron from occupied to an unoccupied energy 
level can be caused by UV radiation. Not all transitions are allowed 
but the definition of which are and which are not are beyond the 
scope of this tutorial. For the time being be aware that commonly 
seen transitions are p to p* which correctly implies that UV is useful 
with compounds containing double bonds. 
A schematic of the transition of an electron from p to p* is shown on 
the left. 
Increasing energy
The Spectroscopic Process 
1. In UV spectroscopy, the sample is irradiated with the broad 
spectrum of the UV radiation 
2. If a particular electronic transition matches the energy of a certain 
band of UV, it will be absorbed 
3. The remaining UV light passes through the sample and is 
observed 
4. From this residual radiation a spectrum is obtained with “gaps” at 
these discrete energies – this is called an absorption spectrum 
p* 
p 
p* 
p
Observed electronic transitions 
1. The lowest energy transition (and most often obs. by UV) is 
typically that of an electron in the Highest Occupied Molecular 
Orbital (HOMO) to the Lowest Unoccupied Molecular Orbital 
(LUMO) 
2. For any bond (pair of electrons) in a molecule, the molecular 
orbitals are a mixture of the two contributing atomic orbitals; for 
every bonding orbital “created” from this mixing (s, p), there is a 
corresponding anti-bonding orbital of symmetrically higher 
energy (s*, p*) 
3. The lowest energy occupied orbitals are typically the s; likewise, 
the corresponding anti-bonding s* orbital is of the highest 
energy 
4. p-orbitals are of somewhat higher energy, and their 
complementary anti-bonding orbital somewhat lower in energy 
than s*. 
5. Unshared pairs lie at the energy of the original atomic orbital, 
most often this energy is higher than p or s (since no bond is 
formed, there is no benefit in energy)
Observed electronic transitions 
6. Here is a graphical representation 
Energy 
s* 
p* 
Unoccupied levels 
Atomic orbital Atomic orbital 
n 
p 
s 
Molecular orbitals 
Occupied levels
Observed electronic transitions 
7. From the molecular orbital diagram, there are several possible 
electronic transitions that can occur, each of a different relative 
energy: 
Energy 
s* 
p* 
n 
p 
s 
s 
s 
p 
n 
n 
s* 
p* 
p* 
s* 
p* 
alkanes 
carbonyls 
unsaturated cmpds. 
O, N, S, halogens 
carbonyls
Selection Rules 
1. Not all transitions that are possible are observed 
2. For an electron to transition, certain quantum mechanical 
constraints apply – these are called “selection rules” 
3. For example, an electron cannot change its spin quantum number 
during a transition – these are “forbidden” 
Other examples include: 
• the number of electrons that can be excited at one time 
• symmetry properties of the molecule 
• symmetry of the electronic states 
2. To further complicate matters, “forbidden” transitions are 
sometimes observed (albeit at low intensity) due to other factors
Band Structure 
1. Unlike IR (or later NMR), where there may be upwards of 5 or 
more resolvable peaks from which to elucidate structural 
information, UV tends to give wide, overlapping bands 
2. It would seem that since the electronic energy levels of a pure 
sample of molecules would be quantized, fine, discrete bands 
would be observed – for atomic spectra, this is the case 
3. In molecules, when a bulk sample of molecules is observed, not all 
bonds (read – pairs of electrons) are in the same vibrational or 
rotational energy states 
4. This effect will impact the wavelength at which a transition is 
observed – very similar to the effect of H-bonding on the O-H 
vibrational energy levels in neat samples
Band Structure 
5. When these energy levels are superimposed, the effect can be 
readily explained – any transition has the possibility of being 
observed 
Energy 
E1 Vo 
Vo 
V4 
V3 
V2 
V1 
Disassociation 
R1 - Rn 
R1 - Rn 
R1 - Rn 
R1 - Rn 
E R1 - Rn 0 
V4 
V3 
V2 
V1 
Disassociation 
R1 - Rn 
R1 - Rn 
R1 - Rn 
R1 - Rn 
R1 - Rn
Beer’s Law 
• Based on absorption of light by a sample 
– dPx/Px=dS/S 
• dS/S=ratio of absorbance area to total area 
– Proportional to number of absorbing particles 
• dS=adn 
– a is a constant, dn is number of particles 
– n is total number of particles within a sample 
adn 
S 
P n 
- ò = ò 
an 
an 
dP 
P x 
P 
- = 
P 
o 
P 
S 
P 
S 
P 
o 
x 
o 
2.303 
ln 
log 
0 
=
Beer’s Law 
• Area S can be described by volume and length 
anb 
Po 
– S=V/b (cm2) 
– Substitute for S 
– n/V = concentration 
– Substitute concentration and collect constant into single term e 
• Beer’s law can be applied to mixtures 
– Atot=SAx 
V 
P 
2.303 
log =
The Instrumentation 
The instrumentation used to run a UV is shown below. It involves two lamps (one for visible 
light and one for UV light) and a series of mirrors and prisms as well as an appropriate detector. 
The spectrometer effectively varies the wavelength of the light directed through a sample from 
high wavelength (low energy) to low wavelength (high energy). 
As it does so any chemical dissolved in a sample cell through which the light is passing may 
undergo electronic transitions from the ground state to the excited state when the incident 
radiation energy is exactly the same as the energy difference between these two states. A 
recorder is then used to record, on a suitable scale, the absorption of energy that occurs at each 
of the wavelengths through which the spectrometer scans. 
The recorder 
assembly 
The spectrometer itself – this houses the 
lamps, mirrors, prisms and detector. The 
spectrometer splits the beam of radiation into 
two and passes one through a sample and one 
through a reference solution (that is always 
made up of the solvent in which you have 
dissolved the sample). The detector measures 
the difference between the sample and 
reference readings and communicates this to 
the recorder. 
The samples are dissolved in a solvent which is transparent to UV light and put into sample 
cells called cuvettes. The cells themselves also have to be transparent to UV light and are 
accurately made in all dimensions. They are normally designed to allow the radiation to pass 
through the sample over a distance of 1cm.
Instrumentation 
• Light source 
– Deuterium and hydrogen lamps 
– W filament lamp 
– Xe arc lamps 
• Sample containers 
– Cuvettes 
• Plastic 
• Glass 
• Quartz
Instrumentation 
1. The construction of a traditional UV-VIS spectrometer is very 
similar to an IR, as similar functions – sample handling, 
irradiation, detection and output are required 
2. Here is a simple schematic that covers most modern UV 
spectrometers: 
reference sample 
detector 
I0 
I 
I0 I0 
log(I0/I) = A 
200 700 
l, nm 
UV-VIS sources 
monochromator/ 
beam splitter optics
Instrumentation 
3. Two sources are required to scan the entire UV-VIS band: 
• Deuterium lamp – covers the UV – 200-330 
• Tungsten lamp – covers 330-700 
3. As with the dispersive IR, the lamps illuminate the entire band of 
UV or visible light; the monochromator (grating or prism) 
gradually changes the small bands of radiation sent to the beam 
splitter 
4. The beam splitter sends a separate band to a cell containing the 
sample solution and a reference solution 
5. The detector measures the difference between the transmitted 
light through the sample (I) vs. the incident light (I0) and sends 
this information to the recorder
Instrumentation 
7. As with dispersive IR, time is required to cover the entire UV-VIS 
band due to the mechanism of changing wavelengths 
8. A recent improvement is the diode-array spectrophotometer - 
here a prism (dispersion device) breaks apart the full spectrum 
transmitted through the sample 
9. Each individual band of UV is detected by a individual diodes on a 
silicon wafer simultaneously – the obvious limitation is the size of 
the diode, so some loss of resolution over traditional instruments 
is observed 
sample 
Polychromator 
– entrance slit and dispersion device 
UV-VIS sources 
Diode array
Sample Handling 
1. Virtually all UV spectra are recorded solution-phase 
2. Cells can be made of plastic, glass or quartz 
3. Only quartz is transparent in the full 200-700 nm range; plastic 
and glass are only suitable for visible spectra 
4. Concentration (we will cover shortly) is empirically determined 
A typical sample cell (commonly called a cuvet):
Sample Handling 
5. Solvents must be transparent in the region to be observed; the 
wavelength where a solvent is no longer transparent is referred to 
as the cutoff 
6. Since spectra are only obtained up to 200 nm, solvents typically 
only need to lack conjugated p systems or carbonyls 
Common solvents and cutoff wavelength in nm: 
acetonitrile 190 
chloroform 240 
cyclohexane 195 
1,4-dioxane 215 
95% ethanol 205 
n-hexane 201 
methanol 205 
isooctane 195 
water 190
Sample Handling 
7. Additionally solvents must preserve the fine structure (where it is 
actually observed in UV!) where possible 
8. H-bonding further complicates the effect of vibrational and 
rotational energy levels on electronic transitions, dipole-dipole 
interacts less so 
9. The more non-polar the solvent, the better (this is not always 
possible)
The Spectrum 
1. The x-axis of the spectrum is in wavelength; 200-350 nm for UV, 
200-700 for UV-VIS determinations 
2. Due to the lack of any fine structure, spectra are rarely shown in 
their raw form, rather, the peak maxima are simply reported as a 
numerical list of “lamba max” values or lmax 
lmax = 206 nm 
252 
317 
376 
O 
NH2 
O
The Spectrum 
1. The y-axis of the spectrum is in absorbance, A 
2. From the spectrometers point of view, absorbance is the inverse of 
transmittance: A = log10 (I0/I) 
3. From an experimental point of view, three other considerations 
must be made: 
i. a longer path length, l through the sample will cause 
more UV light to be absorbed – linear effect 
ii. the greater the concentration, c of the sample, the more 
UV light will be absorbed – linear effect 
iii. some electronic transitions are more effective at the 
absorption of photon than others – molar absorptivity, e 
this may vary by orders of magnitude…
The Spectrum 
4. These effects are combined into the Beer-Lambert Law: 
A = e c l 
i. for most UV spectrometers, l would remain constant 
(standard cells are typically 1 cm in path length) 
ii. concentration is typically varied depending on the strength 
of absorption observed or expected – typically dilute – sub . 
001 M 
iii. molar absorptivities vary by orders of magnitude: 
• values of 104-106 are termed high intensity 
absorptions 
• values of 103-104 are termed low intensity 
absorptions 
• values of 0 to 103 are the absorptions of forbidden 
transitions 
A is unitless, so the units for e are cm-1 · M-1 and are rarely 
expressed 
5. Since path length and concentration effects can be easily factored 
out, absorbance simply becomes proportional to e, and the y-axis 
is expressed as e directly or as the logarithm of e
Practical application of UV spectroscopy 
1. UV was the first organic spectral method, however, it is rarely 
used as a primary method for structure determination 
2. It is most useful in combination with NMR and IR data to 
elucidate unique electronic features that may be ambiguous in 
those methods 
3. It can be used to assay (via lmax and molar absorptivity) the proper 
irradiation wavelengths for photochemical experiments, or the 
design of UV resistant paints and coatings 
4. The most ubiquitous use of UV is as a detection device for HPLC; 
since UV is utilized for solution phase samples vs. a reference 
solvent this is easily incorporated into LC design
Visible Spectroscopy 
A. Color 
1. General 
• The portion of the EM spectrum from 400-800 is observable 
to humans- we (and some other mammals) have the 
adaptation of seeing color at the expense of greater detail 
400 500 600 700 800 
l, nm 
Violet 400-420 
Indigo 420-440 
Blue 440-490 
Green 490-570 
Yellow 570-585 
Orange 585-620 
Red 620-780
Visible Spectroscopy 
• When white (continuum of l) light passes through, or is 
reflected by a surface, those ls that are absorbed are 
removed from the transmitted or reflected light respectively 
• What is “seen” is the complimentary colors (those that are 
not absorbed) 
• This is the origin of the “color wheel”
Visible Spectroscopy 
• Organic compounds that are “colored” are typically those 
with extensively conjugated systems (typically more than 
five) 
• Consider b-carotene 
b-carotene, lmax = 455 nm 
lmax is at 455 – in the far blue region of 
the spectrum – this is absorbed 
The remaining light has the 
complementary color of orange
Visible Spectroscopy 
• Likewise: 
lycopene, lmax = 474 nm 
O 
NH 
HN 
O 
indigo 
lmax for lycopene is at 474 nm – in the near blue 
region of the spectrum – this is absorbed, the 
compliment is now red 
lmax for indigo is at 602 nm – in the orange region of 
the spectrum – this is absorbed, the compliment is 
now indigo!
Visible spectroscopy 
• One of the most common class of colored organic molecules 
are the azo dyes: 
N N 
EWGs EDGs 
From our discussion of di-subsituted aromatic 
chromophores, the effect of opposite groups is greater than 
the sum of the individual effects – more so on this heavily 
conjugated system 
Coincidentally, it is necessary for these to be opposite for 
the original synthetic preparation!
OH 
NO2 
N 
N 
Para Red 
N N 
NH2 
H2N 
Fast Brown 
HO 
O3S N N 
SO3 
Sunset Yellow (Food Yellow 3) 
Visible Spectroscopy 
• These materials are some of the more familiar colors of our 
“environment”
Thank you

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UV Visible Spectroscopy

  • 1. UV-Visible spectroscopy Dr. V. Krishnakumar Professor and Head Department of Physics Periyar University Salem. Tamilnadu India
  • 2. UV Spectroscopy I. Introduction A. UV radiation and Electronic Excitations 1. The difference in energy between molecular bonding, non-bonding and anti-bonding orbitals ranges from 125-650 kJ/mole 2. This energy corresponds to EM radiation in the ultraviolet (UV) region, 100-350 nm, and visible (VIS) regions 350-700 nm of the spectrum 3. For comparison, recall the EM spectrum: g-rays X-rays UV IR Microwave Radio 4. Using IR we observed vibrational transitions with energies of 8-40 kJ/mol at wavelengths of 2500-15,000 nm 5. For purposes of our discussion, we will refer to UV and VIS spectroscopy as UV Visible
  • 3. Analysis When continuous wave radiation is passed through a prism a diffraction pattern is produced (called a spectrum) made up of all the wavelengths associated with the incident radiation. When continuous wave radiation passes through a transparent material (solid or liquid) some of the radiation might be absorbed by that material. Radiation source Diffraction prism Spectrum Spectrum with ‘gaps’ Transparent material that absorbs some radiation in it If, having passed through the material, the beam is diffracted by passing through a prism it will produce a light spectrum that has gaps in it (caused by the absorption of radiation by the transparent material through which is passed). The effect of absorption of radiation on the transparent material is to change is from a low energy state (called the ground state) to a higher energy state (called the excited state). The difference between all the spectroscopic techniques is that they use different wavelength radiation that has different associated energy which can cause different modes of excitation in a molecule. For instance, with infra red spectroscopy the low energy radiation simply causes bonds to bend and stretch when a molecule absorbs the radiation. With high energy UV radiation the absorption of energy causes transition of bonding electrons from a low energy orbital to a higher energy orbital. The energy of the ‘missing’ parts of the spectrum corresponds exactly to the energy difference between the orbitals involved in the transition.
  • 4. Energy transitions s* Unoccupied Energy p* n p s Levels Occupie d Energy Levels The bonding orbitals with which you are familiar are the s-bonding orbitals typified by simple alkanes. These are low energy (that is, stable). Next (in terms of increasing energy) are the p-bonding orbitals present in all functional groups that contain double and triple bonds (e.g. carbonyl groups and alkenes). Higher energy still are the non-bonding orbitals present on atoms that have lone pair(s) of electrons (oxygen, nitrogen, sulfur and halogen containing compounds). All of the above 3 kinds of orbitals may be occupied in the ground state. Two other sort of orbitals, called antibonding orbitals, can only be occupied by an electron in an excited state (having absorbed UV for instance). These are the p* and s* orbitals (the * denotes antibonding). Although you are not too familiar with the concept of an antibonding orbital just remember the following – whilst electron density in a bonding orbital is a stabilising influence it is a destabilising influence (bond weakening) in an antibonding orbital. Antibonding orbitals are unoccupied in the ground state UV A transition of an electron from occupied to an unoccupied energy level can be caused by UV radiation. Not all transitions are allowed but the definition of which are and which are not are beyond the scope of this tutorial. For the time being be aware that commonly seen transitions are p to p* which correctly implies that UV is useful with compounds containing double bonds. A schematic of the transition of an electron from p to p* is shown on the left. Increasing energy
  • 5. The Spectroscopic Process 1. In UV spectroscopy, the sample is irradiated with the broad spectrum of the UV radiation 2. If a particular electronic transition matches the energy of a certain band of UV, it will be absorbed 3. The remaining UV light passes through the sample and is observed 4. From this residual radiation a spectrum is obtained with “gaps” at these discrete energies – this is called an absorption spectrum p* p p* p
  • 6. Observed electronic transitions 1. The lowest energy transition (and most often obs. by UV) is typically that of an electron in the Highest Occupied Molecular Orbital (HOMO) to the Lowest Unoccupied Molecular Orbital (LUMO) 2. For any bond (pair of electrons) in a molecule, the molecular orbitals are a mixture of the two contributing atomic orbitals; for every bonding orbital “created” from this mixing (s, p), there is a corresponding anti-bonding orbital of symmetrically higher energy (s*, p*) 3. The lowest energy occupied orbitals are typically the s; likewise, the corresponding anti-bonding s* orbital is of the highest energy 4. p-orbitals are of somewhat higher energy, and their complementary anti-bonding orbital somewhat lower in energy than s*. 5. Unshared pairs lie at the energy of the original atomic orbital, most often this energy is higher than p or s (since no bond is formed, there is no benefit in energy)
  • 7. Observed electronic transitions 6. Here is a graphical representation Energy s* p* Unoccupied levels Atomic orbital Atomic orbital n p s Molecular orbitals Occupied levels
  • 8. Observed electronic transitions 7. From the molecular orbital diagram, there are several possible electronic transitions that can occur, each of a different relative energy: Energy s* p* n p s s s p n n s* p* p* s* p* alkanes carbonyls unsaturated cmpds. O, N, S, halogens carbonyls
  • 9. Selection Rules 1. Not all transitions that are possible are observed 2. For an electron to transition, certain quantum mechanical constraints apply – these are called “selection rules” 3. For example, an electron cannot change its spin quantum number during a transition – these are “forbidden” Other examples include: • the number of electrons that can be excited at one time • symmetry properties of the molecule • symmetry of the electronic states 2. To further complicate matters, “forbidden” transitions are sometimes observed (albeit at low intensity) due to other factors
  • 10. Band Structure 1. Unlike IR (or later NMR), where there may be upwards of 5 or more resolvable peaks from which to elucidate structural information, UV tends to give wide, overlapping bands 2. It would seem that since the electronic energy levels of a pure sample of molecules would be quantized, fine, discrete bands would be observed – for atomic spectra, this is the case 3. In molecules, when a bulk sample of molecules is observed, not all bonds (read – pairs of electrons) are in the same vibrational or rotational energy states 4. This effect will impact the wavelength at which a transition is observed – very similar to the effect of H-bonding on the O-H vibrational energy levels in neat samples
  • 11. Band Structure 5. When these energy levels are superimposed, the effect can be readily explained – any transition has the possibility of being observed Energy E1 Vo Vo V4 V3 V2 V1 Disassociation R1 - Rn R1 - Rn R1 - Rn R1 - Rn E R1 - Rn 0 V4 V3 V2 V1 Disassociation R1 - Rn R1 - Rn R1 - Rn R1 - Rn R1 - Rn
  • 12. Beer’s Law • Based on absorption of light by a sample – dPx/Px=dS/S • dS/S=ratio of absorbance area to total area – Proportional to number of absorbing particles • dS=adn – a is a constant, dn is number of particles – n is total number of particles within a sample adn S P n - ò = ò an an dP P x P - = P o P S P S P o x o 2.303 ln log 0 =
  • 13. Beer’s Law • Area S can be described by volume and length anb Po – S=V/b (cm2) – Substitute for S – n/V = concentration – Substitute concentration and collect constant into single term e • Beer’s law can be applied to mixtures – Atot=SAx V P 2.303 log =
  • 14. The Instrumentation The instrumentation used to run a UV is shown below. It involves two lamps (one for visible light and one for UV light) and a series of mirrors and prisms as well as an appropriate detector. The spectrometer effectively varies the wavelength of the light directed through a sample from high wavelength (low energy) to low wavelength (high energy). As it does so any chemical dissolved in a sample cell through which the light is passing may undergo electronic transitions from the ground state to the excited state when the incident radiation energy is exactly the same as the energy difference between these two states. A recorder is then used to record, on a suitable scale, the absorption of energy that occurs at each of the wavelengths through which the spectrometer scans. The recorder assembly The spectrometer itself – this houses the lamps, mirrors, prisms and detector. The spectrometer splits the beam of radiation into two and passes one through a sample and one through a reference solution (that is always made up of the solvent in which you have dissolved the sample). The detector measures the difference between the sample and reference readings and communicates this to the recorder. The samples are dissolved in a solvent which is transparent to UV light and put into sample cells called cuvettes. The cells themselves also have to be transparent to UV light and are accurately made in all dimensions. They are normally designed to allow the radiation to pass through the sample over a distance of 1cm.
  • 15. Instrumentation • Light source – Deuterium and hydrogen lamps – W filament lamp – Xe arc lamps • Sample containers – Cuvettes • Plastic • Glass • Quartz
  • 16. Instrumentation 1. The construction of a traditional UV-VIS spectrometer is very similar to an IR, as similar functions – sample handling, irradiation, detection and output are required 2. Here is a simple schematic that covers most modern UV spectrometers: reference sample detector I0 I I0 I0 log(I0/I) = A 200 700 l, nm UV-VIS sources monochromator/ beam splitter optics
  • 17. Instrumentation 3. Two sources are required to scan the entire UV-VIS band: • Deuterium lamp – covers the UV – 200-330 • Tungsten lamp – covers 330-700 3. As with the dispersive IR, the lamps illuminate the entire band of UV or visible light; the monochromator (grating or prism) gradually changes the small bands of radiation sent to the beam splitter 4. The beam splitter sends a separate band to a cell containing the sample solution and a reference solution 5. The detector measures the difference between the transmitted light through the sample (I) vs. the incident light (I0) and sends this information to the recorder
  • 18. Instrumentation 7. As with dispersive IR, time is required to cover the entire UV-VIS band due to the mechanism of changing wavelengths 8. A recent improvement is the diode-array spectrophotometer - here a prism (dispersion device) breaks apart the full spectrum transmitted through the sample 9. Each individual band of UV is detected by a individual diodes on a silicon wafer simultaneously – the obvious limitation is the size of the diode, so some loss of resolution over traditional instruments is observed sample Polychromator – entrance slit and dispersion device UV-VIS sources Diode array
  • 19. Sample Handling 1. Virtually all UV spectra are recorded solution-phase 2. Cells can be made of plastic, glass or quartz 3. Only quartz is transparent in the full 200-700 nm range; plastic and glass are only suitable for visible spectra 4. Concentration (we will cover shortly) is empirically determined A typical sample cell (commonly called a cuvet):
  • 20. Sample Handling 5. Solvents must be transparent in the region to be observed; the wavelength where a solvent is no longer transparent is referred to as the cutoff 6. Since spectra are only obtained up to 200 nm, solvents typically only need to lack conjugated p systems or carbonyls Common solvents and cutoff wavelength in nm: acetonitrile 190 chloroform 240 cyclohexane 195 1,4-dioxane 215 95% ethanol 205 n-hexane 201 methanol 205 isooctane 195 water 190
  • 21. Sample Handling 7. Additionally solvents must preserve the fine structure (where it is actually observed in UV!) where possible 8. H-bonding further complicates the effect of vibrational and rotational energy levels on electronic transitions, dipole-dipole interacts less so 9. The more non-polar the solvent, the better (this is not always possible)
  • 22. The Spectrum 1. The x-axis of the spectrum is in wavelength; 200-350 nm for UV, 200-700 for UV-VIS determinations 2. Due to the lack of any fine structure, spectra are rarely shown in their raw form, rather, the peak maxima are simply reported as a numerical list of “lamba max” values or lmax lmax = 206 nm 252 317 376 O NH2 O
  • 23. The Spectrum 1. The y-axis of the spectrum is in absorbance, A 2. From the spectrometers point of view, absorbance is the inverse of transmittance: A = log10 (I0/I) 3. From an experimental point of view, three other considerations must be made: i. a longer path length, l through the sample will cause more UV light to be absorbed – linear effect ii. the greater the concentration, c of the sample, the more UV light will be absorbed – linear effect iii. some electronic transitions are more effective at the absorption of photon than others – molar absorptivity, e this may vary by orders of magnitude…
  • 24. The Spectrum 4. These effects are combined into the Beer-Lambert Law: A = e c l i. for most UV spectrometers, l would remain constant (standard cells are typically 1 cm in path length) ii. concentration is typically varied depending on the strength of absorption observed or expected – typically dilute – sub . 001 M iii. molar absorptivities vary by orders of magnitude: • values of 104-106 are termed high intensity absorptions • values of 103-104 are termed low intensity absorptions • values of 0 to 103 are the absorptions of forbidden transitions A is unitless, so the units for e are cm-1 · M-1 and are rarely expressed 5. Since path length and concentration effects can be easily factored out, absorbance simply becomes proportional to e, and the y-axis is expressed as e directly or as the logarithm of e
  • 25. Practical application of UV spectroscopy 1. UV was the first organic spectral method, however, it is rarely used as a primary method for structure determination 2. It is most useful in combination with NMR and IR data to elucidate unique electronic features that may be ambiguous in those methods 3. It can be used to assay (via lmax and molar absorptivity) the proper irradiation wavelengths for photochemical experiments, or the design of UV resistant paints and coatings 4. The most ubiquitous use of UV is as a detection device for HPLC; since UV is utilized for solution phase samples vs. a reference solvent this is easily incorporated into LC design
  • 26. Visible Spectroscopy A. Color 1. General • The portion of the EM spectrum from 400-800 is observable to humans- we (and some other mammals) have the adaptation of seeing color at the expense of greater detail 400 500 600 700 800 l, nm Violet 400-420 Indigo 420-440 Blue 440-490 Green 490-570 Yellow 570-585 Orange 585-620 Red 620-780
  • 27. Visible Spectroscopy • When white (continuum of l) light passes through, or is reflected by a surface, those ls that are absorbed are removed from the transmitted or reflected light respectively • What is “seen” is the complimentary colors (those that are not absorbed) • This is the origin of the “color wheel”
  • 28. Visible Spectroscopy • Organic compounds that are “colored” are typically those with extensively conjugated systems (typically more than five) • Consider b-carotene b-carotene, lmax = 455 nm lmax is at 455 – in the far blue region of the spectrum – this is absorbed The remaining light has the complementary color of orange
  • 29. Visible Spectroscopy • Likewise: lycopene, lmax = 474 nm O NH HN O indigo lmax for lycopene is at 474 nm – in the near blue region of the spectrum – this is absorbed, the compliment is now red lmax for indigo is at 602 nm – in the orange region of the spectrum – this is absorbed, the compliment is now indigo!
  • 30. Visible spectroscopy • One of the most common class of colored organic molecules are the azo dyes: N N EWGs EDGs From our discussion of di-subsituted aromatic chromophores, the effect of opposite groups is greater than the sum of the individual effects – more so on this heavily conjugated system Coincidentally, it is necessary for these to be opposite for the original synthetic preparation!
  • 31. OH NO2 N N Para Red N N NH2 H2N Fast Brown HO O3S N N SO3 Sunset Yellow (Food Yellow 3) Visible Spectroscopy • These materials are some of the more familiar colors of our “environment”