Instrumentation
•Flameemissionspectrometers(flamephotometers)areprobablythesimplesttype
ofatomicspectrometers.Theyarenormallydesignedtomakemeasurementson
upto10differentelements,usuallythosefromgroupIandIIoftheperiodictable.
Thisisachievedusinginterchangeablecolouredfiltersordiffractiongratings,
whichisolateanareaofthespectrumcontainingthechosenemissionline.
•The sequence of events occurring is as follows:
1.Solution is introduced into the flame as a fine spray. This is normally achieved
using an aspirator. Solution is drawn out of the sample holder using a pump and
fed into the gas stream through a thin nozzle creating an aerosol spray .
2.Solvent evaporate leaving the dehydrated salt.
3.Salt dissociate into free gaseous atoms in the ground state.
4.A certain fraction of atoms absorbs energy and are raised into excited state.
5.These excited atoms on returning to ground state emits photons of characteristic
wavelength.
6.The emission from the flame passes through a conventional monochromator
which filters out all emitted light except the wavelength of our interest.
7.A photoelectric detector measures the intensity of the filtered light.
b.AtomiserBurnersFlamePhotometry
Thesampleisintroducedintheformofafinesprayatacontrolledrate
intotheflameofburnerwiththehelpofnebuliser.Intheburner,the
analyteundergoesanumberofprocessesasmentionedearlier.
•The following processes occur in the flame.
i) Desolvation: The sample containing metal particles is dehydrated by the
heat of
the flame and the solvent is evaporated.
ii) Vapourisation: The heat of the flame vapourises the sample constituents.
No chemical change takes place at this stage.
iii) Atomisation: At this stage the metal ions that were in the solvent are
reduced to
metal atoms. For example,
Mg
2+
(aq)+ 2e
-
Mg
(g)
By heat of the flame and action of the reducing gas (fuel), molecules and
ions of the sample species are decomposed and reduced to give atoms.
Types of flame used
Themostcommoninstrumentsuseairastheoxidant.Thetemperature
oftheflamesproducedisrelativelylowsothetechniqueisonlysuitable
forelementsthatareeasilyexcitedsuchasalkaliandalkaliearth
elements.Whenoxygenornitrousoxideisusedamuchhigher
temperaturecanbeobtained.
Flame Temp/°C
Gas/Air 1700–1900
Gas/O
2 2700–2800
H
2/Air 2000–2100
H
2/O
2 2550–2700
C
2H
2/Air 2100–2400
C
2H
2/O
2 3050–3150
C
2H
2/N
2O 2600–2800
A higher temperature will tend to increase the number of atoms in the
excited state and hence the signal.
Some detection limits for flame emission methods.
Element Spectral Detection
line Limits
/nm Flame /ppm
Al 396 C
2H
2/ N
2O 0.01
Ba 553 C
2H
2/ N
2O 0.001
K 766 C
2H
2/ O
2 0.001
Li 671 C
2H
2/ N
2O 0.0001
Structure of Flames
•Flamesarenotuniformincomposition,lengthorcross
section.Thestructureofapremixedflame,supportedasa
laminarflowisshowninFig.7.7.
•As seen in the figure, the flame may be divided into the
following regions or zones.
i) Preheating zones
ii) Primary reaction zone or inner zone
iii) Internal zone
iv) Secondary reaction zone
Limitation of Flame Emission Photometry
•Asnaturalgasandairflameisemployedforexcitationthetemperatureisnothigh
enoughtoexcitetransitionmetals,thereforethemethodisselectivetowards
detectionofalkaliandalkalineearthmetals.
•Thelowtemperaturemakesthismethodsusceptibletocertaindisadvantages,
mostofthemrelatedtointerferenceandthestabilityoftheflameandaspiration
conditions.Fuelandoxidantflowratesandpurity,aspirationrates,solution
viscosity,affectthese.Itisthereforeveryimportanttomeasuretheemissionofthe
standardandunknownsolutionsunderidenticalconditions.
•Therelativelylowenergyavailablefromtheflameleadstorelativelylowintensity
oftheradiationfromthemetalatoms,particularlythosethatrequirelargeamount
ofenergytobecomeexcited.
•Flame photometry is a means of determining the total metal concentration of a
sample; it tells us nothing about the molecular form of the metal in the original
sample.
•Only liquid samples can be used. In some cases, lengthy steps are necessary to
prepare liquid samples.