INSTRUMENTATION IN RAMAN SPECTROSCOPY: …georaman2016.igm.nsc.ru/images/Dubessy1.pdfcompany. •...

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INSTRUMENTATION IN RAMAN SPECTROSCOPY: ELEMENTARY THEORY J.Dubessy, M.C. Caumon GeoRessources (Nancy, France) l = 488 nm Rayleigh scattering Stokes Raman scattering Cyclohexane Rejection filter of the 488 nm GEORAMAN-XXII-2016 School joint to the VIII th International Siberian Early Career GeoScientists Conference

Transcript of INSTRUMENTATION IN RAMAN SPECTROSCOPY: …georaman2016.igm.nsc.ru/images/Dubessy1.pdfcompany. •...

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INSTRUMENTATION IN RAMAN SPECTROSCOPY:

ELEMENTARY THEORY

J.Dubessy, M.C. Caumon

GeoRessources (Nancy, France)

l = 488 nm

Rayleigh scattering Stokes Raman

scattering

Cyclohexane

Rejection filter

of the 488 nm

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

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Raman instruments, elementary theory

• Initially, Raman a physics « curiosity »: low intensity signals

• The lasers and electronic detection (PM): crystals, gases, liquid studies in physical-chemistry-crystallography laboratories

• Raman microprobes: 1975-1978: Rosasco (USGS) and Delhaye-Dhamelincourt (LASIR, Lille, France) + instrument company.

• CCD detectors + Raman microprobes + laser rejection by filters: highly luminous systems

• Highly simplified « portable » systems: Earth surface, Mars surface (EXOMARS mission, Supercam system)

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

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Raman shift: in relative wavenumbers with

respect to the excitation radiation

RASMIN (Raman Spectra Database of Minerals and

Inorganic Materials) Raman line intensities, function of:

• Intrinsic polarisation of the line

• Polarisation conditions of the

excitation and signal collection

• Concentration

• Raman scattering cross-section

• Molecular interactions….

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

Where is the information in a Raman spectrum ?

Raman line shift, width and shape

Musso et al. (2004) Critical line shape behavior of

fluid nitrogen. Pure Applied Chem, 76, 147-155

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Raman shift: in relative wavenumbers

with respect to the excitation radiation

00 1 l wavelength of the excitation radiation => absolute wavenumber:

jR, Raman wavenumber => absolute wavenumber

for a Stokes Raman line: jR

abs

jR ,0,

0l

jR

abs

jRjR ,0,, 11 l wavelength of the Raman line

Raman shift in wavelength: 0,, lll jRjR

1 µm 10000 cm-1; 0.5 µm = 500 nm 20000 cm-1

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Raman shift: in relative wavenumbers

with respect to the excitation radiation

0l (nm) 0 (cm

-1) abs

jR max, (cm-1

) max,Rl (nm) max,Rl (nm)

250 40000 36000 277.7 27.7

400 25000 21000 476.2 76.2

500 20000 16000 625.0 125.0

660 15151 11151 896.7 236.7

785 12739 8739 1144.3 359.3

1064 9398 5398 1852.5 788.5

Stokes Raman shift (4000 cm-1) in wavelength:

Precision of 1 cm-1 to 6.310-3 nm = 6.310-2 Å precision in l for l0 = 250 nm

Precision of 1 cm-1 6.110-2 nm = 0.61 Å precision in l for l0 = 785 nm

The Raman spectrum is scattered over a larger spectral interval range in

wavelength for red excitations than for green or UV excitation lines

Consequences on the variation of the efficiency of components

GEORAMAN-XXII-2016 School joint to the

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Raman line intensities: orders of magnitude

estimated by radiometric calculations

mNd

d

A

NN

R

0

0

Number of Raman

photons

Number of

excitation photons

Differential Raman

scattering cross

section

Solid angle of

collectionNumber of molecules in

the excited volume

Excited area of the

sample

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

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Raman line intensities: orders of magnitude

estimated by radiometric calculations

mNd

d

A

NN

R

0

0

0100

)1( l photonEWsN

JchE photon

196834

001 104)105.0(1031062.6 ll

-1J.s 0.01 Watt 01.00

W

photons 102)1( 16

0

sN

1-233-35 .srm 10 to10

d

dsr 1 ALNm LANm

97228-333516 10 to1061010310 to101020

R

N

3-28

23

3

mmolecules. 1031002.602.0

10

m 01.0L

GEORAMAN-XXII-2016 School joint to the

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107 10 to100

R

N

• excitation source: high power and stable monochromatic source

• high rejection of the excitation wavelength

• high transmission of the dispersive system and high spectral resolution

• high efficiency detector: high sensitivity, high dynamics

Figures of merit of a Raman spectrometer

1512

,10 to10

0

reflection

N

6-9 orders of

magnitude

1311

,10 to10

0

Rayleigh

N

3-5 orders of

magnitude

GEORAMAN-XXII-2016 School joint to the

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The different elements of a Raman

(micro)-spectrometer

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The excitation sources

Sun, Townes suggests First laser use Ar+, Kr+ Nd-Yag Laser diodes

Hg lamp the use of lasers (Porto-Weber) 532 nm

1964 (He-Ne) on

Cary spectrometer

1928 1960 1963 1969 2000 2005

End of high power (1W-10W) Ar+ / Kr+ lasers soon ?

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The excitation source: lasersLaser = Light amplification by stimulated emission of radiation: 1957-1960

Charles Hard Townes, Arthur Leonard Schawlaw (Bell labs); Gordon Gould (Columbia

University); Theodore H. Maiman (Hugue Research lab)

Ground level

Excited level E2

E1

Light absorption Spontaneous

emission

Pumping:

population

inversion

hh

h

hh

Stimulated

emission

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Different materials: Gases, solids (crystals, glasses, semi-conductors), liquids

Different pumping systems.

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Wavelength of lasers and laser choice

Ar+: 351.1; 364; 457.9; 488; 514.5 Kr+: 350.7; 406.7; 413.1; 530.9; 647.1; 676.4

Nd-YAG+: 256; 365; 532; 1064;

The choice of the excitation source• Luminescence of the usual samples;

• Consequences on optics, gratings, detector

OPSL(InGaAS): 458; 488; 514; 532; 552; 561; 568; 588; 594 nm

FIBER LASERS: 488; 515 nm

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solid: 660; diode laser : 785

UV NIRV I S I B L E

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Figures of merit of laser beam

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1.Frequency stability

2.Spectral width (kHZ to Ghz (8 Ghz for 488 nm Ar+ without etalon). 3 GHz

= 0.1 cm-1.

3. Output polarization: linear > 100/1

4. Power stability: <0.2 %

5. The quality factor, M2:describe the deviation of the laser beam from a

theoretical Hermite-Gaussian beam. M2<1.1

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• either by a double (50 cm-1/l0) or triple spectrometer (5 cm-1 /l0)

• either by a rejection filter with DO = 6

• super-Notch filter: well centred on l0 (30-100 cm-1) /l0

• edge filter: high band pass filters (30-100 cm-1) /l0

6log,0

DO

I

I

incident

dtransmitte

GEORAMAN-XXII-2016 School joint to the

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Two types of Raman spectrometers

1) FFT spectrometer: excitation in the NIR

2) Dispersive spectrometer: excitation in the UV or visible

Rejection of l0 and Raman lines separation

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1785 1928 1953 1972

Gratings prisms ruled precision holographic

Hairs ! gratings gratings

Refraction based:

n = f(l)

Diffraction based

Cary: double additive

Czerny-Turner

spectrometer

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

Rejection of l0 and Raman lines separation

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GRATINGS : geometrical lines separation

• Gratings work either in transmission or in reflection

• Transmission gratings are made of parallel elongated domains which

transmit the light and opaque domains: thus they can be considered as

arrangement of parallel slits corresponding to the transmission zones

• Reflection gratings are an assembly of elongated mirrors acting as slits;

the grooves are the opaque parts.

PHYSICS MODEL: ARRANGEMENT OF MANY PARALLEL

EQUIDISTANT SLITS WITH THE SAME WIDTH

1 SLIT – N SLITS

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GRATING THEORY: 1 single slit (Fraunhoffer slit)

2

0

sin

II

l

sin

b

S1

S2

M1

M2

M3

m1

m2

m3

b

P

Sm

GEORAMAN-XXII-2016 School joint to the

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l

sin

sin

sinsin2

2

2

2

2

0

d

NII

Single slit term

enveloppel

sinb

Represents the interferences

resulting from N beams of equal

intensity arising from N slits

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

GRATING THEORY: N slits

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GRATING THEORY: grating equation

http://hyperphysics.phy-astr.gsu.edu/

m = -2 m = -1 m = 0 m = +1 m = +2

lllll mmd ,...3 ,2 , ,0sin GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

GRATING THEORY: grating equation

l

sinfor maximum

sin

sin2

2

d

mN

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Monochromatic diffraction

Polychromatic diffraction

http://h2physics.org

llaser = 514.535 nm Raman

spectrum; m=1; m =0

Mirror, specular reflection

GEORAMAN-XXII-2016 School joint to the

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GRATING THEORY: monochromatic/polychromatic

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lllll mmid ,...3 ,2 , ,0sinsin

m: diffraction order

m = 1 for Czerny-Turner

spectrometers

l mGi sinsinat constant m and wavelength, diffraction angle is proportional to groove density

at constant m and G, diffraction angle increases with wavelength.

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GRATING THEORY: grating equation

Groove density /mm

G = 1/d = 150-3000

to 6000 (VPHG)

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l

l

l

coscoscos

and sinsin

Gm

l

mADdmdl

d

dADmil

AD : proportional to m and G

AD increases for higher Stokes wavenumber

m = -2 m = -1 m = 0 m = +1 m = +2

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VIIIth International Siberian Early Career GeoScientists Conference

GRATING THEORY: angular dispersion

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Efficiency curves are function of wavelength

Relative = Diffracted(l)/Reflected(l)

by mirror with same coating

Grating efficiency depends on

Wavelength, polarization in incident light, incidence angle,

diffraction order, groove profile and coating material.

Selection of the grating from the exciting radiation wavelength

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

GRATING THEORY: line intensity

The polarization state

of the incident radiation

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CZERNY-TURNER SPECTROMETER:basic principles

Sources and detectors

are in a fixed position: Dv

= deviation angle

iDv

l mGi sinsin

l

mG

Diii v

2cos

2sin2

2cos

2sin2

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

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2vD

i2

i

2i

2i

Angular relationships

,

l mGcossin2

anglerotation

GEORAMAN-XXII-2016 School joint to the

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CZERNY-TURNER SPECTROMETER:rotating grating

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l mGcossin2

GEORAMAN-XXII-2016 School joint to the

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CZERNY-TURNER SPECTROMETER: sine bar

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DETECTORS

1928 1940 1950 1964-1967 1978 1986 2016

Eyes, Photomultiplier Image Intensifier Intensified CCD / EMCCD

photographic tube Vidicon Camera Photodiode Array CMOS-SPAD

plate

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

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Invented in 1969 at AT&T Bell Labs by Willard Boyle and George E. Smith

Nobel Prize of Physics in 2009

2D Array of individual « detectors » = pixels

1024 x 256 pixels (26 µm x 26 µm) or smaller in size

Formation of an electron/hole pair in p-dopped silicon

layer if E(photon) > Si band gap

200-1100 nmKodak

Cooled at -90 °C (Pelletier effect) or -130°C (liquid N2) to eliminate thermal noise

Front or back illuminated: consequences on quantum efficiency.

UV or non-UV coated

GEORAMAN-XXII-2016 School joint to the

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EMCCD: Electron Multiplying CCD. No read-out noise limitation. Used for very

weak signals from spectra with quasi neal background (no fluorescence). Rare in

Earth sciences materials ! Raman imaging with short integration time.

DETECTORS

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Quantum efficiency lEQ = number of electrons generated per

incident photon

Andor Company

Criterion choice as a function

of the excitation source:

visible, UV, red

highest QE,

low dark current,

low read-out

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

CCD: figures of merit

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Intensity: vertical

binning of pixels

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

BWTEK

BWTEK

CCD: intensity and wavenumber coding

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Resolved lines

1 pixel 26 µm corresponds to 0.95 cm-1 /pixel = pixel size resolution

Limiting resolution of the

spectrometer including the detector

33

CCDpixelerspectromet w

x

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

CCD: pixel limiting resolution

Unresolved

lines

Just resolved line:

Rayleigh criterion:

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Spectral resolution of a Raman spectromer

22

erspectrometslitSR lll 22

erspectrometslitSR

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Procedure:

1. Spectrum of atomic

emission line

2. Profile fitting

3. Measurement of FWHM

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Band Shape

00

0

,, ALdALFx

Source Apparatus

functionModification of the band

profile by the instrument.

Lorentzian => Gaussian,

mixtures

Condition of no modification

of the band profile and no

enlargement:

Instrumental resolution < 1/5

FWHM of natural profile

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

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Coupling sampling system with spectrometer

Optimum coupling conditions: constant flux of photons

transported from the sample to the detector without any loss

(except those resulting from absorption).

Etendue or throughput should be constant

GEORAMAN-XXII-2016 School joint to the

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Spatial resolution of confocal Raman spectrometers

..46.0 ANxy l Lateral resolution

Axial resolution 2.).(

4.1

ANz

l

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Degradation of spatial resolution by refraction

Use of immersion objective

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VIIIth International Siberian Early Career GeoScientists Conference

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10-15g.(nm3)

1928 1950 1970 1990 2010

g (cm3)

10-3g (mm3)

10-12g (µm3)

Hg lamp

Conventional laser R.S.

Raman microspectroscopy

Near-field spectroscopy

RAMAN SAMPLING VOLUME

From Delhaye and Dhamelincourt

GEORAMAN-XXII-2016 School joint to the

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1928: First Raman experiment

Hg excitation lines

Raman lines

GEORAMAN-XXII-2016 School joint to the

VIIIth International Siberian Early Career GeoScientists Conference

2016 :Highly simplified « portable » systems: Earth surface, Art objects,

Mars surface (EXOMARS mission, Supercam system)