Fourier Transform Infrared (FTIR) Spectrometer Subhashree Mishra ATMS Grad Student, UNR W. P. Arnott Physics, UNR Introduction to Atmospheric Instrumentation.

Slides:



Advertisements
Similar presentations
Detection of weak optical signals D.R. Selviah, R.C. Coutinho, H.A. French and H.D. Griffiths Department of Electronic and Electrical Engineering, University.
Advertisements

Waves (in general) sine waves are nice
11 Components of Optical Instruments Lecture Spectroscopic methods are based on either: 1. Absorption 2. Emission 3. Scattering.
 PART Absorption Spectrometer Dr. S. M. Condren SourceWavelength SelectorDetector Signal Processor Readout Sample.
FOURIER TRANSFORM INFRARED SPECTROSCOPY
METO 621 Lesson 6. Absorption by gaseous species Particles in the atmosphere are absorbers of radiation. Absorption is inherently a quantum process. A.
OC3522Summer 2001 OC Remote Sensing of the Atmosphere and Ocean - Summer 2001 Review of EMR & Radiative Processes Electromagnetic Radiation - remote.
Principles of Radiation. 1. All object possesses (sensible) heat and emit 1. All object possesses (sensible) heat and emit radiation energy as long as.
Chapter 11: Electromagnetic Waves
Remote sensing in meteorology
Radiative Properties of Clouds ENVI3410 : Lecture 9 Ken Carslaw Lecture 3 of a series of 5 on clouds and climate Properties and distribution of clouds.
MET 61 1 MET 61 Introduction to Meteorology MET 61 Introduction to Meteorology - Lecture 7 “Warming the Earth and Atmosphere” Dr. Eugene Cordero San Jose.
the Natural Greenhouse Effect
Introduction to Infrared Spectrometry Chap 16. Quantum Mechanical Treatment of Vibrations Required to include quantized nature of E From solving the wave.
LESSON 4 METO 621. The extinction law Consider a small element of an absorbing medium, ds, within the total medium s.
Fourier Transform IR Spectroscopy Saptarshi Basu.
Lecture 3 INFRARED SPECTROMETRY
Pat Arnott, ATMS 749 Atmospheric Radiation Transfer Chapter 6: Blackbody Radiation: Thermal Emission "Blackbody radiation" or "cavity radiation" refers.
10/11/ ENGINEERING RESEARCH CENTER FOR S TRUCTURED O RGANIC P ARTICULATE S YSTEMS RUTGERS UNIVERSITY PURDUE UNIVERSITY NEW JERSEY INSTITUTE OF TECHNOLOGY.
Quick Review of Remote Sensing Basic Theory Paolo Antonelli CIMSS University of Wisconsin-Madison Benevento, June 2007.
1 University of Petra Faculty of Science & Arts Department of Chemistry Seminar I.R Spectroscopy By Firas Al-ouzeh Supervisor : Nuha I. Swidan Summer 2007.
INFRA RED ABSORPTION SPECTROSCOPY Kateřina Hynštová.
Fourier Transform Infrared (FTIR) Spectrometer Subhashree Mishra ATMS Grad Student, UNR W. P. Arnott Physics, UNR Introduction to Atmospheric Instrumentation.

National Aeronautics and Space Administration The Energy Budget and the Greenhouse Effect Dr. Lin H. Chambers, NASA Langley Research Center.
Infrared Spectroscopy. Spectroscopy The energy of the interaction of electromagnetic radiaiton (light) with molecules Several different techniques: Infrared.
Lecture 12 ASTR 111 – Section 002.
Spectroscopy Light in chemistry. The Nature of Light Acts as both a particle and a wave Photoelectric effect only explained through waves Interference,
Pat Arnott, ATMS 749, UNR, PRACTICAL CONSEQUENCES OF THE SCHWARZSCHILD EQUATION FOR RADIATION TRANSFER WHEN SCATTERING IS NEGLIGIBLE From Grant Petty’s.
Measurement of Thermal Infrared Radiation Emitted by the Atmosphere Using FTIR Spectroscopy By Narayan Adhikari Charles Woodman 5/11/2010 PHY 360.
 a mathematical procedure developed by a French mathematician by the name of Fourier  converts complex waveforms into a combination of sine waves, which.
Chapter 12 Infrared Spectroscopy Jo Blackburn Richland College, Dallas, TX Dallas County Community College District  2006,  Prentice Hall Organic Chemistry,
5.3 Notes Light & Spectrometry Pg Theory of Light  Color is a visual indication of the fact that objects absorb certain portions of visible.
Radiation Fundamental Concepts EGR 4345 Heat Transfer.
Language of the Energy Cycle: The Electromagnetic Spectrum
The Spectrum of EM Waves According to wavelength or frequency, the EM waves can be distinguished into various types. There is no sharp boundary.
Introduction to Spectrochemical Methods
Pat Arnott, ATMS 749, UNR, 2008 CH 8: ATMOSPHERIC EMISSION: PRACTICAL CONSEQUENCES OF THE SCHWARZSCHILD EQUATION FOR RADIATION TRANSFER WHEN SCATTERING.
Introduction to Thermal Radiation and Radiation Heat Transfer.
Copyright © 2010 Pearson Education, Inc. Lecture Outline Chapter 2 Light and Matter.
Introduction to Thermal Radiation
Optoelectronics.
1.1 What’s electromagnetic radiation
This Week (3) Concepts: Light and Earth’s Energy Balance Electromagnetic Radiation Blackbody Radiation and Temperature Earth’s Energy Balance w/out atmosphere.
For 3 rd year students- Biophysics Department – Faculty of Science – Cairo University Prepared by: Dr. Heba Mohamed Fahmy and Dr. Alaa Mamdouh.
By Madhu Gyawali Narayan Adhikari Yadab Paudel FTIR Measurements on November 06,08 at Reno Nov 18, 08 PHYS 749 UNIVERSITY OF NEVADA, RENO,NV.
Fourier Transform IR Spectroscopy. Absorption peaks in an infrared absorption spectrum arise from molecular vibrations Absorbed energy causes molecular.
Infrared Spectroscopy (IR) Fourier Transform Infrared (FTIR)
Quick Review of Remote Sensing Basic Theory Paolo Antonelli SSEC University of Wisconsin-Madison Monteponi, September 2008.
Blackbody. Kirchhoff’s Radiation  Radiated electromagnetic energy is the source of radiated thermal energy. Depends on wavelengthDepends on wavelength.
Planck’s law  Very early in the twentieth century, Max Karl Ernest Ludwig Planck put forth the idea of the quantum theory of radiation.  It basically.
PRESENTED BY :- ARPIT S. PANDYA I-M.PHARM INDUSTRIAL PHARMACY SRINIVAS COLLEGE OF PHARMACY.
 FT-IR stands for Fourier Transform Infrared, the preferred method of infrared spectroscopy. In infrared spectroscopy, IR radiation is passed through.
Fourier Transform IR (FTIR)
Physical Principles of Remote Sensing: Electromagnetic Radiation
Electromagnetic Radiation Principles
Infrared Spectroscopy of the Atmosphere using the FTIR Spectrometer
Flame Emission Spectrometry
Really Basic Optics Instrument Sample Sample Prep Instrument Out put
Fourier Transform Infrared (FTIR) Spectrometer
Fourier Transform Infrared (FTIR) Spectrometer
Instrument Considerations
Radiation in the Atmosphere
By Narayan Adhikari Charles Woodman
SPECTROPHOTOMETRY Applied Chemistry.
Introduction and Basic Concepts
Light and Energy Electromagnetic Radiation is a form of energy that is created through the interaction of electrical and magnetic fields. It displays wave-like.
Remote sensing in meteorology
Spectrophotometric Analysis
Presentation transcript:

Fourier Transform Infrared (FTIR) Spectrometer Subhashree Mishra ATMS Grad Student, UNR W. P. Arnott Physics, UNR Introduction to Atmospheric Instrumentation (ATMS 360) University of Nevada Reno

Energy Levels: Basic Ideas About 15 micron radiation Basic Global Warming: The C02 dance …

Wavelength and Wavenumber Wavelength = 1 / Wavenumber Wavelength = 1 / Wavenumber For the IR, wavelength is in microns. For the IR, wavelength is in microns. Wavenumber is typically in 1/cm, or cm -1. Wavenumber is typically in 1/cm, or cm microns corresponds to 2000 cm microns corresponds to 2000 cm microns corresponds to 500 cm microns corresponds to 500 cm microns corresponds to 667 cm -1. Much ‘terrestrial’ IR energy at the wavenumber. 15 microns corresponds to 667 cm -1. Much ‘terrestrial’ IR energy at the wavenumber.

Carbon Dioxide Concentration

Example Problem: Instantly Double CO2 Concentration. What is the effect on the infrared spectrum at the surface? Consequence: The Earth’s surface warms because of the additional IR coming to the surface from the Atmosphere.

Example Problem: Instantly Double CO2 Concentration. What is the effect on the infrared spectrum from space? Consequence: The less IR radiation escapes to space when the atmosphere has 800 ppm CO2 because the atmosphere is less transparent to IR emitted by the Earth’s surface. The Earth’s surface temperature must increase to again balance the outgoing IR with the incoming solar radiation.

LEDs As Detectors Each photon with enough energy will normally free exactly one electron, and result in a free hole as well. If this happens close enough to the electric field, or if free electron and free hole happen to wander into its range of influence, the field will send the electron to the N side and the hole to the P side. This causes further disruption of electrical neutrality, and if we provide an external current path, electrons will flow through the path to their original side (the P side) to unite with holes that the electric field sent there, doing work for us along the way. The electron flow provides the current, and the cell's electric field causes a voltage. With both current and voltage, we have power, which is the product of the two. From

LEDs As Detectors: Thermal Noise

FTIRs Often Use MCT Detectors: Mercury Cadmium Telluride HgCdTe or Mercury cadmium telluride (also Cadmium Mercury Telluride, MCT or CMT) is an alloy of CdTe and HgTe and is sometimes claimed to be the third semiconductor of technological importance after Silicon and Gallium(III) arsenide. The amount of cadmium (Cd) in the alloy (the alloy composition) can be chosen so as to tune the optical absorption of the material to the desired infrared wavelength. (from

Outline Introduction Theory Design Applications Measurements Discussions

What is a FTIR Spectrometer? A spectrometer is an optical instrument used to measure properties of light over a specific portion of the electromagnetic spectrum, 5 microns to 20 microns. A spectrometer is an optical instrument used to measure properties of light over a specific portion of the electromagnetic spectrum, 5 microns to 20 microns. FTIR (Fourier Transform InfraRed) spectrometer is a obtains an infrared spectra by first collecting an interferogram of a sample signal using an interferometer, then performs a Fourier Transform on the interferogram to obtain the spectrum. FTIR (Fourier Transform InfraRed) spectrometer is a obtains an infrared spectra by first collecting an interferogram of a sample signal using an interferometer, then performs a Fourier Transform on the interferogram to obtain the spectrum. An interferometer is an instrument that uses the technique of superimposing (interfering) two or more waves, to detect differences between them. The FTIR spectrometer uses a An interferometer is an instrument that uses the technique of superimposing (interfering) two or more waves, to detect differences between them. The FTIR spectrometer uses a Michelson interferometer.

FOURIER TRANSFORMS Fourier transform defines a relationship between a signal in time domain and its representation in frequency domain. Fourier transform defines a relationship between a signal in time domain and its representation in frequency domain. Being a transform, no information is created or lost in the process, so the original signal can be recovered from the Fourier transform and vice versa. Being a transform, no information is created or lost in the process, so the original signal can be recovered from the Fourier transform and vice versa. The Fourier transform of a signal is a continuous complex valued signal capable of representing real valued or complex valued continuous time signals. The Fourier transform of a signal is a continuous complex valued signal capable of representing real valued or complex valued continuous time signals.

Fourier Transforms cont. The Continuous Fourier Transform, for use on continuous signals, is defined as follows: The Continuous Fourier Transform, for use on continuous signals, is defined as follows: And the Inverse Continuous Fourier Transform, which allows you to go from the spectrum back to the signal, is defined as: And the Inverse Continuous Fourier Transform, which allows you to go from the spectrum back to the signal, is defined as: F(w) is the spectrum, where w represents the frequency, and f(x) is the signal in the time where x represents the time. i is sqrt(-1), see complex number theory.

Fourier Transforms cont. A computer can only work with finite discrete signals, not with continuous signals. Thus, we need to define the Discrete Fourier Transform (DFT). A computer can only work with finite discrete signals, not with continuous signals. Thus, we need to define the Discrete Fourier Transform (DFT). In DFT, the infinite borders of the integrals can be replaced by finite ones, and the integral symbol can be replaced by a sum. So the DFT is defined as: In DFT, the infinite borders of the integrals can be replaced by finite ones, and the integral symbol can be replaced by a sum. So the DFT is defined as: And the inverse DFT is defined as:

FTIR Theory

The spectrometer described here is a modified Bomem MB- 100 FTIR. The heart of the FTIR is a Michelson interferometer (figure 2). The mirror moves at a fixed rate. Its position is determined accurately by counting the interference fringes of a collocated Helium-Neon laser. The Michelson interferometer splits a beam of radiation into two paths having different lengths, and then recombines them. A detector measures the intensity variations of the exit beam as a function of path difference. A monochromatic source would show a simple sine wave of intensity at the detector due to constructive and destructive interference as the path length changes (refer figure 3).

In the general case, a superposition of wavelengths enter spectrometer, and the detector indicates the sum of the sine waves added together. Figure 3 shows some idealized light sources, and the interferograms that they would theoretically produce. The difference in path length for the radiation is known as the retardation d (OM = OF + d) in figure 1 and 2. When the retardation is zero, the detector sees a maximum because all wavenumbers of radiation add constructively. When the retardation is l/2, the detector sees a minimum for the wavelength l. An interferogram is the sum of all of the wavenumber intensities.

Figure 1.

Schematic of Michelson Interferometer Source: MS thesis submitted by Carl George Schmitt, UNR, Figure 2.

Wave Interference

Sample interferograms and their theoretical source intensity Source: MS thesis submitted by Carl George Schmitt, UNR, Figure 3.

Calibration of the FTIR spectrometer Source: MS thesis submitted by Carl George Schmitt, UNR, 1998.

The spectrometer produces a complex voltage at each wavenumber. A linear model for the spectrometer response is assumed, where A is an instrument offset, and C is a scaling factor, V= A+CI(1) If the spectrometer views a perfect blackbody, Eq. (1) gives V = A+ CB T (2) where B T is the Planck emission curve for a blackbody of temperature T. The two unknowns (A and C) can be determined from blackbody measurements at two different temperatures, V 1 = A+ CB T1 V 2 = A+ CB T2

Solving for the unknowns yields C = (V 1 -V 2 )/(B T1 -B T2 ) and A = {V 1 (B T1 -B T2 )-B T1 (V 1 -V 2 )}/(B T1 -B T2 ) Returning to Eq (1), The FTIR voltage of another target (V target ) is related to the target radiance (I target ) by I target =[(B T1 -B T2 )V target –B T1 V 2 +B T2 V 1 ]/(V 1 -V 2 ) Thus, with measurements of blackbodies at two temperatures, the calibrated radiance from a target (cloud) can be determined.

APPLICATIONS Identification of inorganic compounds and organic compounds Identification of inorganic compounds and organic compounds Identification of components of an unknown mixture Identification of components of an unknown mixture Analysis of solids, liquids, and gasses Analysis of solids, liquids, and gasses In remote sensing In remote sensing In measurement and analysis of Atmospheric Spectra In measurement and analysis of Atmospheric Spectra - Solar irradiance at any point on earth - Longwave/terrestrial radiation spectra Can also be used on satellites to probe the space Can also be used on satellites to probe the space

Source : UV thoughts from

MODIS Solar Irradiance Source :

Theoretical IR cross sections for absorption in the wavenumber range most relevant to longwave (terrestrial) radiation. Source :

Measurement Example from Reno