cavity ring down spectroscopy aysenur bicer. outline what is crd spectroscopy a simple crds...
TRANSCRIPT
Outline
• What is CRD spectroscopy • A simple CRDS experiment• Pulsed laser CRDS versus CW-CRDS• CW- CRDS experimental schema• Experimental results • Knife edge method
What is CRD spectroscopy• CRDS is a sensitive absorption technique in which the rate of
absorption in an optical cavity is measured• It has significantly high sensitivity
1. The effective absorption path length is very long2. The sensitivity is independent of intensity fluctuations of the light
source• Small fractional absorptions sub- ppm levels CO2 400 ppm
(open air)A Simple CRDS Experiment
A laser pulse coupled into an optical cavity The decay time is determined by measuring the time dependence of the light
leaking out of the cavityBy measuring the decay time the rate of absorption is determined directly
providing the losses on an absolute scale
• After one pass-through the cavity the intensity of the first optical pulse (Beer-Lambert’s law)
• The intensity of the second pulse
• After n complete round trip the pulse intensity behind the cavity will be
)exp(20 LTII laser
)2exp(201 LRII
)2exp(2 LnRII non
Pulsed laser CRD spectroscopy
• Pulsed lasers promise Fourier transform limited line widths of the order of 100 MHz, in practice it is difficult to archive
• The length of the cavity, L, and the radius of the mirrors curvature of the mirrors should be chosen such that cavity is optically stable
• They are rather bulky, require massive amounts of electricity to run, and cost several hundred thousand dollars
• The pulsed lasers have the advantage of broad wavelength coverage
Continuous Wave CRD spectroscopy
• The main advantage of using CW laser radiation sources in any spectroscopic system is the increased resolution in the frequency domain
• (Trigger event ) In order to observe a ring down transits CW have to be switched of
• The bandwidth of these lasers is very small so can be only scanned over small wavelength regions
• each mode can have various allowed longitudinal modes associated with it
• The frequency spacing between two successive transverse modes is usually much smaller than the spacing between two successive longitudinal modes and depends on the characteristics of the cavity (length, mirror radii)
CRD spectroscopy Using Continuous Wave Laser
• Because of narrow line width of the laser and high finesse of the cavity, spectral overlap between the laser frequency and the frequency of the cavity modes are no longer obvious • 1605.74nm- 1602.31nm infrared light region to solution He- Ne laser can be used The helium-neon laser (He-Ne) was the first gas laser. The most
widely used laser wavelength is the red wavelength (632.8 nm) with a CW power output ranging from 1mW to 100mW and laser lengths varying from 10 to 100 cm.
Diode laser controller
Wavemeter or OSA
Scope
DFB diode laser
1.6~1.61µ m
He-Ne laser
PD preamp
AOM
AOM Driver
PZT driver
L
First step
• The DFB laser has a stable wavelength that is set during manufacturing by the pitch of the grating, and can only be tuned slightly with temperature.
• It has elliptical beam shape• The beam pass through wave plates
Second step• AOM uses the acousto-optic effect to diffract and shift the frequency of light using
sound waves so we can use it in CRD spectroscopy for frequency control• The laser light that passes through AOM will be diffracted into multiple orders • The first order diffracted beam is directed through the optical cavity• Frequency of radiation from CW laser is coincident with cavity mode, power is
likely build up within the optical cavity• Trigger pulse is sent to AOM to switch it off• The first order beam is quickly extinguish 150ns/mm
1600 1601 1602 1603
6.5
7.0
7.5
8.0
8.5
Experimental Data
12CO2 98.42% of 400ppm
H2O 1.5%
13CO2
1.11% of 400ppm
at atmospheric pressure and room temperature
Wavelength (nm)
CR
D D
ecay
Tim
e (
s)
0.5
0.4
0.3
0.2
0.1
0.0
Calculated H
itran Absorbance
C0Temperature (Celsius) 13 - 30.30 increasing by 0.10Wavelength between 1600.566nm – 1602.534nm
C0 C0
1590 1595 1600 1605 1610 1615 1620
0.0
0.1
0.2
0.3
0.4
0.5
12CO2 98.42%
13CO2
1.11%
at atmospheric pressure and room temperature
Wavelength (nm)
12C
O2 ~
400ppm
abso
rban
ce
0.000
0.001
0.002
0.003
0.004
0.005
0.006
13C
O2 ~
4ppm
abso
rbance
1600 1602 1604 1606 1608 1610
0.0
0.1
0.2
0.3
0.4
0.5
12CO2 98.42%
13CO2
1.11%
at atmospheric pressure and room temperature
Wavelength (nm)
12C
O2 ~
400pp
m a
bsor
banc
e
0.0
0.1
0.2
0.3
0.4
0.513C
O2 ~
4ppm
absorbance
1605.0 1605.2 1605.4 1605.6 1605.8 1606.0
0.00
0.02
0.04
0.06
0.08
0.10
0.12
0.14
12CO2 98.42%
13CO2
1.11%
at atmospheric pressure and room temperature
Wavelength (nm)
12C
O2 ~
400pp
m a
bsor
banc
e
0.00
0.02
0.04
0.06
0.08
0.10
0.12
0.1413C
O2 ~
4.4 ppm absorbance
1604 1605 1606 16076
7
8
9
10
Wavelength (nm)
Dec
ay T
ime
(s)
-0.6
-0.5
-0.4
-0.3
-0.2
-0.1
0.0
8/13/2012 Measured with CRD, Yokogawa OSA
(0.1nm accuracy) Calculated from Hitran(400ppm CO
2 atmosphere
room temperature)
Absorbance(ln(I/I0 ))
1604 1605 1606 16073
4
5
6
7
8
9
8/14/2012 Measured with CRD, Yokogawa OSA
(0.1nm accuracy) Calculated from Hitran(400ppm CO
2 atmosphere
room temperature)
Wavelength (nm)
Dec
ay T
ime
(s)
-0.6
-0.5
-0.4
-0.3
-0.2
-0.1
0.0
Absorbance(ln(I/I0 ))
1604.5 1605.0 1605.5 1606.0 1606.5 1607.07
8
9
10
Experimental Data(wavelength measured with Yokogawa, +/- 0.2nm)
12CO2 98.42% of 400ppm
H2O 1.5%
13CO2
1.11% of 400ppm
at atmospheric pressure and room temperature
Wavelength (nm)
CR
D D
eca
y Tim
e (
s)
0.3
0.2
0.1
0.0
Calcu
late
d H
itran A
bsorb
ance
Knife edge method
84.0
),(
),(
16.0
),(
),(
)(
2
2
)(22
22
yxdxIdy
yxdxIdy
yxdxIdy
yxdxIdy
exI
w
w
w
yx
• First order diffracted beam 10.42mW 10.42×0.84=8.752mW
9.9775mm 10.42×0.16=10.7950mW 10.7950mm10.7950-9.9775=0.817mm
• First order diffracted beam 10.54mW
10.54×0.84=8.8636mW 16.690mm 10.54×0.16=1.6864mW 17.350mm 17.350-16.690=0.660mm