instrumentation in raman spectroscopy-vf

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INSTRUMENTATION IN RAMAN SPECTROSCOPY: ELEMENTARY THEORY AND PRACTICE J.Dubessy, M.C. Caumon, F. Rull, S. Sharma EMU-CNRS International School: Applications of Raman Spectroscopy to Earth Sciences and cultural Heritage : 14-16 th of june 2012

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Page 1: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

INSTRUMENTATION IN RAMAN SPECTROSCOPY:

ELEMENTARY THEORY AND PRACTICE

J.Dubessy, M.C. Caumon,F. Rull, S. Sharma

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 2: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

OUTLINE

• Raman instruments, elementary theory: J.Dubessy

• Calibration: M.C. Caumon

• From the laboratory to the field: F. Rull

• Coupling with other techniques: S. Sharma

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 3: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

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 in Raman microprobes + laser rejection by filters

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 4: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

Where is the information in a Raman spectrum ?

Raman shift: in relative wavenumbers withrespect to the excitation radiation

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

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….

RASMIN (Raman Spectra Database of Minerals and Inorganic Materials)

Raman line shift, width and shape

Musso et al. (2004) Critical line shape behavior of fluidnitrogen. Pure Applied Chem, 76, 147-155

Page 5: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

Raman shift: in relative wavenumberswith respect to the excitation radiation

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

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

jR,ν Raman wavenumber => absolute wavenumber

for a stokes Raman line: jRabs

jR ,0, ννν −=

( )jRabs

jRjR ,0,, 11 νννλ −== wavelength of the Raman line

Raman shift in wavelength: 0,, λλλ −=∆ jRjR

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

Page 6: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

Raman shift: in relative wavenumberswith respect to the excitation radiation

0λ (nm) 0ν (cm-1) abs

jR max,ν (cm-1) max,Rλ (nm) max,Rλ∆ (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:

A precision of 1 cm-1 to 6.3×10-3 nm = 6.2×10-2 Å for the 250 nm excitation

A precision of 1 cm-1 6.1×10-2 nm = 0.61 Å for the 785 nm excitation

The Raman spectrum is scattered over a larger spectral interval range in wavelength for red excitations than for green or UV excitation lines

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 7: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Raman line intensities: orders of magnitude estimated by radiometric calculations

( )( )mNd

d

A

NN

R∆Ω

Ω=−

συυυ

0

0

Number of Raman photons

Number of excitation photons

Differential Raman scattering cross

section

Solid angle of collection

Number of molecules in the excited volume

Excited area of the sample

Page 8: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Raman line intensities: orders of magnitude estimated by radiometric calculations

( )( )mNd

d

A

NN

R∆Ω

Ω=−

συυυ

0

0

( )[ ]0100

)1( λνν photonEWsN =

( ) ( ) ( ) JchE photon187834

001 104105.01031062.6 −−− ×≈×××≈= λλ

-1J.s 0.1 Watt 1.00

==ν

Wphotons 104)1( 17

0×=sNν

1-233-35 .srm 10 to10−≈

Ωd

dσ sr 1=∆Ω ALNm ρ= LANm ρ=

( ) 119228-333517 10 to101010310 to101040

=×××××= −−− R

N νν

( )3-28

23

3

mmolecules. 1031002.602.0

10 ×≈×

=ρ m 01.0=L

Page 9: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Raman line intensities: orders of magnitude estimated by radiometric calculations

Monochromatic luminance of the light of the sun at 0.5 µm wavelength with 1 cm-1

line width

0.02 à 2 Raman photons s -1 !

a narrow band photographic filter to createmonochromatic light (violet), and a filter(yellow-green) to block violet monochromatic light

Page 10: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

First Raman experiment

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Hg excitation lines

Raman lines

Page 11: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

λ λ λ λ = 488 nm

Rayleigh scattering Stokes Raman scattering

Cyclohexane

Rejection filter of the

488 nm

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Raman experiment and eyes !

blog.lib.umn.edu/chaynes/

Page 12: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

117 10 to100

=− RN νν

1312, 10 to10

0=RayleighNν

1715, 10 to10

0=reflectionNν

• excitation source: high power and stable monochromat ic source

• high rejection of the excitation wavelength

• high transmission of the dispersive system and high s pectral resolution

• high efficiency detector

Figures of merit of a Raman spectrometer

Page 13: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

The different elements constitutive of a Raman (micro)-spectrometer

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 14: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

The excitation sources

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

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 Ar + / Kr+ lasers in 2013-2015 ?

Page 15: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

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

hνhνhν

hνhν

Stimulatedemission

Defines the type of laser

+ optical resonator to promote stimulated emission rathe r than spontaneousemission with two mirrors (1 highly reflective at the rear and another partiallyreflective near 99% at the head)

Page 16: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Resonator modes can be divided into two types: longitudinal modes, which differ in frequency from each other; and transverse modes, which may differ in both frequencyand the intensity pattern of the light.

The excitation source: lasers Transverse modes

Only TEM 00 mode is usedin Raman spectroscopy

and microRamanspectroscopy

Gaussian beam profile

Page 17: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

At the Brewster incidence angle, the windows transmit all light polarized parallel to the incident plane (P). Light polarized perpendicular to the incidence plane (S) is reflectedout the cavity.

P

S

S

P

Mirror

( ) ntg Brewster =θ

Polarization of the laser beam

Polarized incident line => access to polarization state of Raman lines

Measurements of depolarization ratio of Raman lines

Consequences of the light transmission of gratings

Page 18: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Perfect Hermite Gaussianlaser beam

θ0

00

,0,02

θθ

××

=w

wM RR

The quality factor, M 2

(called the “M-squared” factor), is defined to describethe deviation of the laser beam from a theoreticalHermite-Gaussian beam.

For CW lasers and helium neon lasers, 1.1<M2<1.3 less than 1.1;

For diode lasers 1.1<M2<1.7

Divergence of the laser beam:Figure of Merit M2

Page 19: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and Cultural Heritage : 14-16th of june 2012

The choice of the excitation source

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;Laser diodes: 405; 635; 660; 785

• luminescence of the usual samples;

• Consequences on optics, gratings, detector

Ar

458 nm

Page 20: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Rejection of λ0

• either by a double or triple spectrometer

• either by a rejection filter with DO = 6

• super-Notch filter: well centred on λλλλ0 30 cm -1

• edge filter: high band pass filters.

6log,0

−=−=

DO

I

I

incident

dtransmitte

Page 21: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Rejection of λ0 and Raman lines separation

1785 1928 1953 1972

Gratings prisms ruled precision holographic

Hairs ! gratings gratings

Refraction based:

n = f(λλλλ)

Diffraction based

Cary: double additive Czerny-Turner spectrometer

Page 22: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATINGS to separate the different radiations

• Gratings work either in transmission or in reflection

• Transmission gratings are made of parallel elongated domains whichtransmit 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 MODELS: ARRANGEMENT OF MANY PARALLEL EQUIDISTANT SLITS WITH THE SAME WIDTH

1 SLIT - 2 SLITS – N SLITS

Page 23: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

GRATING THEORY: 1 single slit: Fraunhoffer slit

2

0

sin

×=β

βII

λθπβ sin××= b

S1

S2

M1

M2

M3

m1

m2

m3

b

P

Sm

Page 24: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING THEORY: 1 single slit

2

0

sin

×=β

βII

λθπβ sin××= b

• Symmetric distribution of maxima and minima

• Secondary maxima for ( ) ( )b

kbk

2

12sin

sin

212 max

λθλ

θππβ +=⇒=+=

• Secondary minima for ( ) ( )b

kbk

λθλ

θππβ 12sin

sin12 min

+=⇒=+=

• Width of central max ≈ 2 (λ/b) θ→ 0 if b is large with respect to λ: point source

• if (λ/b) ≈1, then at k=0, θmin ≈π/2 => large central maxima

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 25: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING THEORY: 2 single slits

γβ

β 22

2

0 cossin

2 ×

×= II

Single slit termenveloppe

( ) θλπγ sind=

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 26: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

( ) θλπγ sind=

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

GRATING THEORY: 2 single slits

When the slits are narrow, the positions of the maxima are determined mainly by cos2γ

Maxima occur for cos 2γγγγ = 1

( )λλλλθ

πππθλπγmd

d

,...3 ,2 , ,0sin

,...3 ,2 , ,0sin

===

γβ

β 22

2

0 cossin

2 ×

×= II

Single slit termenveloppeλ

θπβ sinb= Represents the interferencesresulting from two beams of equal intensity

Page 27: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING THEORY: N single slits

( )( )

λθπγ

γγ

ββ

sin

sin

sinsin2

2

2

2

2

0

××=

×

×=

d

NII

Single slit termenveloppeλ

θπβ sinb=Represents the interferencesresulting from N beams of equalintensity arising from N slits

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 28: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

( )( )

λθπγ

γγ

ββ

sin

sin

sinsin2

2

2

2

2

0

××=

×

×=

d

NII

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

GRATING THEORY: N single slits

( )( ) πγ

γγ

mN

N →±→ when 1sin

sinMaximum value

λλλλλθ mmd ,...3 ,2 , ,0sin =×=×

Page 29: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING THEORY: grating equation

( ) λλλλλθ mmid ,...3 ,2 , ,0sinsin =×=+×

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

2d

,2sinsin as ≤≤+ λθ mi

⇒= 0m Mirror, specularreflection

:m diffraction order

Page 30: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING THEORY: grating equation

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

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

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

Page 31: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING DIFFRACTION

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Monochromaticdiffraction

Polychromaticdiffraction

Superposition of orders

222

111

sin

sin

λθλθ

×=××=×

md

md

221121 λλθθ mm =⇔=2121 2

3 3;2 λλ =⇒== mm

Red: 600 nm

bleu: 400 nm

http://h2physics.org

Page 32: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING DIFFRACTION and Raman spectrum

λlaser = 514.535 nm Raman spectrum; m=1;

No possible overlapwith different orders

m =0

Page 33: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING DIFFRACTION and grooves density

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

( ) λθ ×=+× mid sinsin

6000(VPHG)-3000-150 G

grooves/mm ofnumber 1

:density groove

=

==d

G

λθ ××=+ mGi sinsin

at constant m and wavelength, diffraction angle is pr oportional to groove density

Page 34: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

RULED GRATING and HOLOGRAPHIC GRATING

Page 35: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING DIFFRACTION and Raman spectrumAngular dispersion versus wavelength

Dispersion on the screen of the different wavelengths for a givendiffraction order results in different angular dispersion

( )

( )θθθ

λθθ

θλλθ

coscoscos

and sinsin

Gm

d

mAD

d

dmdd

d

dADmid

==⇒=

≡=+×

AD : proportional to m and G

Page 36: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING DIFFRACTION andChromatic resolving power

mNR =∆

λ

Resolved lines Just resolved line: Rayleigh criterionThe first diffraction minimum of the image

of one source point coincides with the maximum of another.

Unresolved lines

Page 37: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING DIFFRACTION andChromatic resolving power

mNR =∆

λ

d

LN g=

and d

LmR g=⇒ ( ) λθ mid =+× sinsin

2

best λλ

λ gL=

∆The spectral resolution is proportional to the length o f

the grating (perpendiculary to the grooves)

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 38: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

GRATING DIFFRACTION andResolution in wavenumber scale

mNkk =∆=∆λλλπ2=kWave-vector

mNmNkk

λυυυπυπ 1

22 ==∆⇒∆×=∆⇒=

At the first order, if λαλ ×=≈ dd ,gLNd

ααν =×

=∆ min

cm 10

µm 5.0

==

gL

λ1-

min cm 1.010

1 ==∆⇒ νEMU-CNRS International School: Applications of Raman Spectroscopy

to Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 39: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

GRATING DIFFRACTION and line intensity

The incident angle vs the blaze angle The polarization state of the incident radiation

Efficiency curves are function of wavelength: 1) Absolute = Incident(λ)/Diffracted(λ)

2) Relative = Diffracted(λ)/Reflected(λ) by mirror with same coating

Page 40: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

Grating efficiency depends onWavelength , polarization in incident light, incidence angle , diffraction order , groove profile and coating material .

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

GRATING DIFFRACTION and line intensity

Selection of the grating from the exciting radiation wavelength

Blaze angle, maximum efficiency

Page 41: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

CZERNY-TURNER SPECTROMETER:Basic principles

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Sources and detectors are in a fixed position: Dv

= deviation angle

iDv −= θ

λθ ××=+ mGi sinsin

λθθθ ××=

×

+×=

−×

+× mGDiii v

2cos

2sin2

2cos

2sin2

Page 42: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

files.chem.vt.edu

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

CZERNY-TURNER SPECTROMETER:Actual optical design

Page 43: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

opticalea.com

CZERNY-TURNER SPECTROGRAPH:Actual optical design

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 44: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

CZERNY-TURNER SPECTROGRAPH:Actual optical design

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

2vD=ϕ

θϕ −= i2

φωθ −=

ωϕ +=i

( ) ωθ =+ 2i

( ) ϕθ =− 2i

Angular relationships

,

λϕω ××=×× mGcossin2

ϕ

anglerotation =ω

Page 45: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

CZERNY-TURNER SPECTROGRAPH:Sine bar for grating rotation

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 46: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

DETECTORS

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

1928 1940 1950 1964-1967 1978 1986 2012

Eyes, Photomultiplier Image Intensifier Intensified CCD

photographic tube Vidicon Camera Photodiode Array

plate

Page 47: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

CCD DETECTORSInvented in 1969 at AT&T Bell Labs by Willard Boyle and George E. SmithNobel Prize of Physics in 2009

2D Array of individual « detectors » = pixels

1024 x 256 pixels (26 µm x 26 µm)

Formation of an electron/hole pair in p-dopped silico nlayer if E(photon) > Si band gap

200-1100 nm

Electrons are stored in a potential well characterized by is Full Well Capacity and read-out by an electrode

Kodak

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

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

Front or back illuminated: consequences on quantum e fficiency

Page 48: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

CCD Detectors: quantum efficiency curves

Quantum efficiency ( )λEQ = number of electrons generated per incident photon

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Andor Company To choose as a function of the excitation source

CCD detectors: high Q E, lowdark current, low read-out noise => great input in the use of Raman spectroscopy, in Earth sciences.

Page 49: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

CCD : intensity and wavenumber coding

Intensity: vertical binning of pixels

Linear dispersion of the different radiations: deduced from the angular dispersion produced by the grating

BWTEK

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 50: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

CCD : wavenumber coding

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

dx

dRLD

λ≡Average wavelength dispersion or Reciprocal Linear Dispersion

RLD is linked to AD bydx

d

d

d

dx

d ωωλλ ×=

dx

dADRLD

ω×=

Where ωωωω is the rotation angle of the grating

For a spectrometer with a focal distance f ωdfdx ×=

λθθθ ××=

×

+×=

−×

+× mGDiii v

2cos

2sin2

2cos

2sin2

For a Czerny-Turner spectrograph

mfGmf

d

dx

d

×××=××

×= ϕωϕωλ coscos2

coscos2

Page 51: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

CCD : wavenumber coding

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

mfGmf

d

dx

d

×××=××

×= ϕωϕωλ coscos2

coscos2

Numerical application: small ωωωω angle (cos ωωωω =1); f = 800 mm; grooves d = 0.5 µm;

1st order diffraction; φφφφ = 30 °

dx

d

d

d

dx

d λλνν ×=

In wavenumber scale

λν 1=dx

d

dx

d

d

d λνννλλ

ν ×−=⇒−=−=22

2

1As

,

( ) 1-3µm.mm1008.1

800

30cos5.02 −×=°××=dx

CCD of coveragecm 880cm/cm367 11 −− ⇒≈=∆∆

x

ν

At 1000 cm-1 Raman shift / 514.5 nm 111000cm

1 cm18435cm19435 −−

− =⇒= νν laser

Page 52: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

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

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

CCD : wavenumber coding

cm/cm367 1−=∆∆

x

ν 1 pixel 26 µm = 2.6 10 -3 cm

Limiting resolution of the spectrometer including the detector

33 ××

∆∆=×=∆ CCDpixelerspectromet w

xδννδν

Page 53: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

Spectral resolution

( ) ( )22erspectrometslitSR λλλ ∆+∆= ( ) ( )22

erspectrometslitSR ννν ∆+∆=

dx

dlslit

νγν ××=∆ ( )( ) 1 and 1;

cos

cos

spectomer theofpower magnifying :

≈=×= γθ

γ

γ

B

A

B

A

L

L

L

Li

slit width=lThus , for the same numerical application

µm 100 /cm,cm367 1 == − ldx

dν -1cm 67.3=∆ slitν

-1cm 74.4=νSR

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012

Page 54: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012w

Band Shape

( ) ( ) ( ) ( ) ( )000

,, νννννννν ALdALFx

⊗=××= ∫

Source Apparatus function

Modification 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

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EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012w

Coupling sampling system with spectrometer

Optimum coupling conditions: constant flux of photon s transported fromthe sample to the detector without any loss (except thos e resulting fromabsorption): Etendue or throughput is constant

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EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012w

Radiometric calculations

Calculation of number of Raman photons from the source

Calculation of number of Raman photons collected by th e sampling system (lens, microscope objective)

from the value of transmission of each optical element (T= I/I0),

from the value of the QE of the detector, the number of photo-electrons canbe calculated.

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EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012w

Spatial resolution of confocalRaman microspectrometers

( )..46.0 ANxy λδ =Lateral resolution

Axial resolution 2.).(

4.1

ANz

λδ =

Page 58: INSTRUMENTATION IN RAMAN SPECTROSCOPY-Vf

Degradation of spatial resolution by refraction

Use of immersion objective

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012w

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10-15g.(nm 3)

1928 1950 1970 1990 2010

g (cm 3)

10-3g (mm 3)

10-12g (µm 3)

Hg lamp

Conventional laser R.S.

Raman microspectroscopy

Near-field spectroscopy

RAMAN SAMPLING VOLUME

EMU-CNRS International School: Applications of Raman Spectroscopyto Earth Sciences and cultural Heritage : 14-16th of june 2012w

From Delhaye and Dhamelincourt