INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most...

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Transcript of INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most...

Page 1: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.
Page 2: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

INTRODUCTION

• Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural elucidation.

• The ultraviolet and visible Spectrophotometry is mainly used for quantitative analysis and used as a auxiliary tool for structural elucidation.

Page 3: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Useful Terminology

Photometer is an instrument which measuring the ratio, or some function of the two of radiant power of two electromagnetic beams.

Colorimetry is the use of the human eyeto determine the concentration of colored species.

Spectrophotometry is the use of instruments to make the same measurements. It extends the range of possible measurements beyond those that can be determined by the eye alone. it use more sensitive detectors.

Page 4: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Visual Observations – Because colorimetry is based on inspection of materials with the human eye, it is necessary to review aspects of visible light.

Visible light is the narrow range of electromagnetic waves with the wavelength of 400-700 nm.

= the mnemonic used to remember the colors of the visible spectrum.

Colorimetry

ROY G. BIV

Page 5: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Visible light is only a very small portion of the electromagnetic spectrum.

Note: Frequency (υ) and Energy (E) are directly proportional whereas Frequency (υ) and Wavelength (λ) are inversely proportional.

Page 6: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Type of Radiation

Frequency Range (Hz)

Wavelength Range

Type of Transition

gamma-rays 1020-1024 <1 pm nuclear

X-rays 1017-1020 1 nm-1 pm inner electron

ultraviolet 1015-1017 400 nm-1 nm outer electron

visible 4-7.5x1014 750 nm-400 nm

outer electron

near-infrared 1x1014-4x1014 2.5 µm-750 nmouter electron molecular vibrations

infrared 1013-1014 25 µm-2.5 µm molecular vibrations

microwaves 3x1011-1013 1 mm-25 µmmolecular rotations, electron spin flips*

radio waves <3x1011 >1 mm nuclear spin flips*

Electromagnetic Spectrum

Page 7: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

(a) longer wavelength, lower energy; (b) shorter wavelength, higher energy.

Electromagnetic radiation is characterized by its wavelength, , Frequency, and energy, E:

E = h= hc / c =

Where h = Planck’s constant & c = speed of light in a vacuum.

Page 8: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Theory of spectrophotometry

• When a beam monochromatic light passes through a transparent medium, part of the light is absorbed and the transmitted beam has a lower intensity than the intensity of the incident beam.

Page 9: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

• The TRANSMITTANCE, T of the solution is defined as the ratio of the intensities of the transmitted beam, P to the intensity, Po of the incident beam:

T = P/Po

• The ABSORBANCE, A of a solution is defined as• Absorbance

A = log10 P0 / PA = log10 1 / T A = log10 100 / %TA = 2 - log10 %T

A = -log10TSince A is a logarithmic function, it is dimensionless.

Page 10: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Equation Summary

T= (I/Io) = 10-A %T = (I/Io) x 100 A = -logT = log(1/T)

Note the scale for Absorbance: 9/10th of the scale is from 0-1 and 1/10th is from 1-2.For this reason, the spectrometers have been calibrated in % Transmittance andall readings will be taken in %Transmittance.

Sample Calculation

If %T = 95%, then A = log(100/95) = log(1/.95) = -log(.95)

A = 0.02227

Page 11: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Lambert’s Law

• “When a beam of light is allowed to pass through a transparent medium, the rate of decrease of intensity with the thickness of medium is directly proportional to the intensity of the light”

- dI / dt α IOr

- dI / dt = kI

Page 12: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

• Integrating on both sides putting I=I0 When t=0, we getIn I0 / It = kt

or It = I0 e-kt

Where k is the constant which depends on wavelength and absorbing medium used.

• Converting to natural log

It = I0 10 -0.4343kt = I0 10 -Kt

Where K=k/2.3026 which is absorption coefficient, which is defined as “the reciprocal of the thickness which is required to reduce the light to 1/10 of its intensity”

I0 / It = 0.1=10-kt or Kt =1 or K α 1 / t

Page 13: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Beer’s Law• Lambert’s law shows that there exists a

logarithmic relationship between the transmittance and the length of the optical path through the sample.

Page 14: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

• Beers observed that a similar relationship between the transmittance and the conc of a solution. i.e “ the intensity of a beam of monochromatic light decrease exponentially with the increase in conc if the absorbing substance arithmetically”

It = I0 e-k’c

It = I0 10 -0.4343k’t = I0 10 –K’t

Where k’ and K’ are constants and c is the concentration of the absorbing substance.

Page 15: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

It = I0 10 -act

or log I0 / It = act

• This is mathematical statement of Beer-Lambert law. • This is the fundamental for colorimetry and

Spectrophotometry.• Where c is the conc expressed in mole dm-3

• t is the path length which is expressed in cm.• a is replaced with Є and is termed as the Molar

absorption coefficient or molar absorptivity (molar extinction coefficient)

Beer’s Law

Page 16: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Beer-Lambert law

log I0 / It = act

A = act

A= ЄctЄ=A/ct

Where A is absorbance (no units, since A = log10 P0 / P )

Є is the molar absorbtivity with units of L mol-1 cm-1

b is the path length of the sample - that is, the path length of the cuvette in which the sample is contained. We will express this measurement in centimetres.c is the concentration of the compound in solution, expressed in mol L-1

Page 17: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Deviations from Beer’s Law

• Beer’s law states that a plot of absorbance versus concentration should give a straight line passing through the origin with a slope equal to ab. However, deviations from direct proportionality between absorbance and concentration are sometimes encountered.

• These deviations are a result of one or more of the following three things ; real limitations, instrumental factors or chemical factors.

Page 18: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Real Limitations

• Beer’s law is successful in describing the absorption behavior of dilute solutions only ; in this sense it is a limiting law. At high concentrations ( > 0.01M ),the average distance between the species responsible for absorption is diminished to the point where each affects the charge distribution of its neighbors.

• This interaction, in turn, can alter the species’ ability to absorb at a given wavelength of radiation thus leading to a deviation from Beer’s law.

Page 19: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Limitations (cont)

• Deviations also arise because e is dependent upon the refractive index of the solution. Thus, if concentration changes cause significant alterations in the refractive index h of a solution, departures from Beer’s law are observed.

Page 20: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Chemical Deviations

• Chemical deviations from Beer’s law are caused by shifts in the position of a chemical or physical equilibrium involving the absorbing species.

• A common example of this behavior is found with acid/base indicators.

• Deviations arising from chemical factors can only be observed when concentrations are changed. eg:dichromate ions on dilution.

Cr2O72- + H2O -- 2HCrO4

- - 2H+ + 2CrO4 2-

(orange color) (yellow color)

Page 21: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Instrumental Factors

• Unsatisfactory performance of an instrument may be caused by fluctuations in the power-supply voltage, an unstable light source, or a non-linear response of the detector-amplifier system.

Page 22: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

• There are at least six conditions that need to be fulfilled in order for Beer’s law to be valid. These are:– The absorbers must act independently of each other;– The absorbing medium must be homogeneous in the interaction

volume– The absorbing medium must not scatter the radiation - no turbidity;– The incident radiation must consist of parallel rays, each traversing

the same length in the absorbing medium;– The incident radiation should preferably be monochromatic, or have

at least a width that is narrower than that of the absorbing transition; and

– The incident flux must not influence the atoms or molecules; it should only act as a non-invasive probe of the species under study. In particular, this implies that the light should not cause optical saturation or optical pumping, since such effects will deplete the lower level and possibly give rise to stimulated emission.

Page 23: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Instrumentation

• Source: A continuous source of radiant energy covering the region of spectrum in which the instrument is designed to work.

• Filter or Monochromator: Both filter and monochromator allow the light of the required wavelength to pass through but absorb the light of other wavelengths.

• Sample cells: All instrument must contain a container for the sample.

• Detector: It is used for measuring the radiant energy transmitted through the sample.

Page 24: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Radiation sources

• Requirements of a radiation sources– It must be stable.– It must be of sufficient intensity for the

transmitted energy to be detected at the end if the optical path.

– It must supply continuous radiation over the entire wavelength region in which it is used.

Page 25: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Tungsten filament lamp

• It is most common source of visible radiation.• Its construction is similar to the household

lamp. But the tungsten wire is heated at controlled atm.

• Constant power supply is needed to achieve constant radiant energy.

Page 26: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Drawback of tungsten lamp

• Major portion of its radiant energy in the near IR region of the spectrum, i.e only 15% at the operating temp of about 2725o c and only 1 % at 1725o c.

• If the temp is increased to 2850o c and above will increase the total energy output and shift the wavelength of maximum intensity to shorter wavelength but the life of the lamp will be reduced.

Page 27: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

• Tungsten lamp is the most satisfactory for lamp filaments but the carbon arc is used when a more intense source is required.

• The energy from a tungsten lamp can be used above 375 nm.

Page 28: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Filters and Monochromators

• A Source is generally emits the continuous spectra.

• We need a device to select the narrow bands from wavelengths of the continuous spectra.

• For that selection we have– Filters and– Monochromators.

Page 29: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

FILTERS

• A light filter is device that allow light of the required wavelength to pass but absorbs light of other wavelengths wholly or partially.

• Filter are two type– 1) absorption filters and– 2) interference filters

Page 30: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Absorption filter

• It is a solid sheet of glass on which the color pigments are dispersed.

• Absorption filters are classed as either cut off or band pass filters.

Page 31: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Color Wheel(ROYGBIV)

Complementary colors lie across the diameter on the color wheel and combine to form “white light”, so the color of a compound seen by the eye is the complement of thecolor of light absorbed by a colored compound; thus it completes the color.

Page 32: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

 Observed Color of

Compound

 Color of Light

Absorbed

 Approximate

Wavelength of Light Absorbed

 Green

   700 nm

 Blue-green

   600 nm

 Violet

   550 nm

 Red-violet

   530 nm

 Red

   500 nm

 Orange

   450 nm

 Yellow

   400 nm

Page 33: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

 Observed Color of

Compound

 Color of Light

Absorbed

 Approximate

Wavelength of Light Absorbed

 Green

 Red

 700 nm

 Blue-green

 Orange-red

 600 nm

 Violet

 Yellow

 550 nm

 Red-violet

 Yellow-green

 530 nm

 Red

 Green

 500 nm

 Orange

 Blue

 450 nm

 Yellow

 Violet

 400 nm

Page 34: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Interference filters

• These filters works on the phenomena of interference.

• It has a semi-transparent metal film is deposited on the glass plate.

• Then the metal film is coated with thin layer of dielectric material like MgF2.

• Followed by another metal film and then glass plate for support.

Page 35: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Interference filters

Page 36: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Monochromators

• It is separate the narrow wavelength more specifically then filters.

• Monochromators have the following parts– An Entrance slit– A dispersing element (Prism or grating) and– An Exit slit

Page 37: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.
Page 38: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

• Replica grating are cheaper than prisms.• Main disadvantage of the gratings is that they

produce more then one order of diffraction.• For instance, the second order of 400 mμ may

interfere with the first order of 800 mμ.• This can be removed my employing filters in

front of the entrance slit to absorb interfering radiation.

Page 39: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Grating• A Grating consist of large number if parallel

lines ruled on a highly polished surface such as alumina.( 15,000 – 30,000 lines per square inch)

• Grating are very difficult to prepared. Therefore replica gratings are prepared from an original grating using an epoxy resin.

Page 40: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

• The main advantage of prisms is that they undergo dispersion giving wavelengths which do not overlap.

• But the main disadvantage is that they give Non-linear dispersion.

• On the other hand gratings give linear dispersion but they suffer from an overlap of spectral orders.

• For this reason, filters are employed to reduce the radiation of different orders and stray radiation.

Page 41: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Cells

Page 42: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

DETECTORS

• PHOTOVOLTANIC CELL• PHOTOTUBES• PHOTOMULTIPLIER

Page 43: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

PHOTOVOLTANIC CELL

Page 44: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Photocell or Phototubes

Page 45: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Photoemissive cell

Page 46: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Photomultiplier tube

Page 47: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Power supply

• The power supply serve a triple function– It decrease the line voltage to the instrument’s

operating level with a transformer.– It convert alternating current to direct current

with a rectifier if direct current is required by the instrument.

– It smooths out any ripple which may occur in the line voltage in order to deliver a constant voltage to the source lamp and instrument.

Page 48: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Visual comparators

• There are four techniques for color comparison in quantitative visual colorimetry.– Multiple standard method,– Duplication method,– Dilution methods, and– Balancing method-uses Klett Bio colorimeter or

Dubosque colorimeter

Intensity: For light shining through a colored solution, the observed intensity of the color is found to be dependent on both the thickness of the absorbing layer (pathlength) and the concentration of the colored species.

Page 49: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Multiple standard method

• The unknown solution is taken in a 50/100 ml Nessler tube and made up to the mark.

• The color of the unknown solution is compared with the series of known amount of the known substance.

• The conc of the unknown will be equal to the conc of known if the color matches exactly.

Page 50: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

For One Color: A series of solutions of a single color demonstrates the effect of either concentration or pathlength, depending on how it is viewed.

←Side view

←Top view(a.k.a. Bird’s eye view)

Page 51: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

For more than one color: the ratio of an unknown mixture can also be determined by matching the shade of the color to those produced from known ratios.

In this example, the ratio of a mixture of red and blue can be determined visibly by comparing the mixture to purples produced from known ratios of red and blue.

←Ratio used

←Purple produced

Visual Colorimetry

Page 52: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Duplication method

• The unknown solution is taken in one Nessler tube followed by the development of color with appropriate reagent, and made up to the mark.

• In another tube the solution of developing reagent is taken and made up a little lower than the mark on the Nessler tube.

• From the burette the std solution is added to this tube until the color matches the unknown solution.

Page 53: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Dilution methods

• Two Nessler tubes of equal diameter, height and made out same quality of glass are used.

• To the first tube we add a standard solution and to the second with the unknown conc solution.

• Light from the same source is allowed to pass through each cell and the emergent beams are the compared.

Page 54: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

• The more concentrated solution is progressively diluted until the intensity of the emerging light from the both the cells become equal.

• At this point the concentrations per unit volume of solution in both the tubes (std and the unknown) should also be the same.

Page 55: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

• As the two beams are equal in intensity, the absorbance A is equal in each case.

A=εc1t1

A=εc2t2

from the above equations, we getεc1t1 = εc2t2

But t1 = t2

Therefore c1 = c2

Page 56: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

• As the total quantity of material in the sample remains equal to the original concentration x original volume of sample.

c1 V2 = c(original) V1 ------------- original

• but the final conc of the sample C1 is equal to the conc of the std, therefore

c(original) =c1 V2 / V1 or

Conc of std x volume of solution after dilution

Original volume of solution

Page 57: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Balancing method

• Dubosque colorimeter is used.• By varying the length of the light oath in two

solutions the color of the unknown is matched with the std.

Page 58: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Intensity: When the product of the concentration and the pathlength of any two solutions of a colored compound are the same, the same intensity or darkness of color is observed.

Duboscq visual

colorimeterAdjustable

Path Lengths

Page 59: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

problems

• 40 ml of the 0.5 M Fe3+ std is diluted with 25 ml of water in order to match the intensity of the unknown. Calculate the Fe3+ conc of the unknown solution.

• 50 ml of the unknown sample is diluted to a total volume of 60 ml in order to match the intensity of the original std. the final conc of the unknown is 0.04 M. find out the original conc of the unknown.

Page 60: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Single beam instrument

Page 61: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Double beam instrument

Page 62: INTRODUCTION Absorption Spectrophotometry in the ultraviolet and visible region is one of the most oldest methods used for quantitative analysis and structural.

Advantage of double beam

• It is not necessary to continually replace the blank with the sample or to zero adjust at each wavelength as in the single beam units.

• The ration of the power of the sample and reference beams is constantly obtained and used.

• B’cos if the previous two factor the double beam system leads itself to rapid scanning over a wide wavelength region.