GRIMM Aerosol Spectrometer and Dust Monitors. Measuring principle
|
|
- Rafe Walton
- 6 years ago
- Views:
Transcription
1 Grimm Aerosol-Technik GRIMM Aerosol Spectrometer and Dust Monitors Measuring principle Eng. Wolfgang Brunnhuber 1 Agenda Part A physical background general principles of optical particle detection Part B Nanoparticles counting and sizing This presentation was brought to you by Mazoon Environmental and Technological Services LLC info@mets-oman.com 2 11 May
2 physical background: Interaction of radiation and aerosol particles a = p d p /l with d p = particle diameter and l = incident wavelength note: p d p = particle circumference, for spherical particles The interaction between incident light and a particle (solid, droplet and or gas molecules!) is strongly dependent on the particles size and the wavelength. To show this dependency, the parameter a is used. [Seinfeld & Pandis, 1998] 4 physical background: dependency of particle size and wavelength on scattering For particle sizes much smaller than the incident wavelength (a << 1) RAYLEIGH-scattering: the oscillating electric field of the light waves induce an oscillating dipole in the particle, causing symmetrical scattering (in forward and backward directions). The Intensity of the scattered light is proportional to the sixth power of particle diameter (I ~ d p 6 ) Example: Sunlight hits gas molecules in the atmosphere, blue sky effect! a = p d p /l with d p = particle diameter; and l incident wavelength note: p d p = particle circumference, for spherical particles [Baron & Willeke, 2001] 5 11 May
3 physical background: dependency of particle size and wavelength on scattering For particle sizes in the size range as the incident wavelengt (depending on the light source! say 0.1µm-1µm) MIE-scattering: strong interaction between the particle and the incident beam, depending although on particle refractive index. No simple relation between scattered intensity and particle diameter (Mie-programs, spherical particles) Gustav Adolf Feodor Wilhelm Ludwig Mie * a = p d p /l with d p = particle diameter; and l incident wavelength note: p d p = particle circumference, for spherical particles [Baron & Willeke, 2001] 6 physical background: dependency of particle size and wavelength on scattering For particle sizes much bigger than the incident wavelength (a >> 1) GEOMETRIC OPTICS: light rays hitting the particle lead to reflection, refraction and absorption, rays passing the particles edge give rise to diffraction. The scattered intensity is proportional to the particle crosssectional area (I ~ d p 2 ) and not strongly dependent on shape or particle composition Example: Sunlight hits water droplets in clouds, they appear white! a = p d p /l with d p = particle diameter; and l incident wavelength note: p d p = particle circumference, for spherical particles [Baron & Willeke, 2001] 7 11 May
4 physical background: scattering intensity vs. particle size Geometric Optic Defines the maximum particle size you are able to detect Mie Rayleigh Defines the minimum particle size you are able to detect. Electronical background noise due to scattered light from gas molecules or particle scattering = particle circumference incident wavelength [Baron & Willeke, 2001] 8 physical background: single particle light scattering, scattering intensity polar diagram BACKWARD SCATTERED Scattered intensity I is a function of a = size parameter = p d p /l with d p = particle diameter, l = incident wavelength m = refractive index = n -i with n = real part (scattering), i = imaginary part (absorption) Q = scattering angle while ~0 = backward scattered, ~180 = forward scattered [Baron & Willeke, 2001, Haller 1999] 9 11 May
5 physical background: single particle light scattering, scattering intensity 3D plot calculation of the scattering intensity for a spherical particle, d p = 2µm, incident light: laser, l = 633nm Figure from: René Michels, ILM Uni-Ulm 10 principles of optical particle detection: components, function and design component Sample air inlet Sample air pump Light source Beam optic Light trap Detection optic Detector Signal processing & data processing function/design reproducibility, rh, isokinetic / various flow rate, concentration, statistic / various signal / laser, diode laser, white light well defined optical volume / various avoiding noise / various known aperture / backward, forward, 90 optical or aerodynamic focusing scattering light / photo diode, multiplier rapid count processing and accurate size classification / various All components together determine the spectrometers counting efficiency (coincidence concentration) and sizing accuracy (particle size resolution) May
6 principles of particle detection Nephelometer aerosol particles y detection volume x Sample in Light source Detector Signal by a group of particles! y 12 principles of particle detection Spectrometer e.g. 90 detection aerosol particles aerosol focusing detection volume 90 y z x Sample in Light source y Detector Light trap GRIMM can do!! Signal by a single particle! May
7 physical background: single particle light scattering, Grimm spectrometer principle 14 principles of particle detection Dual method, spectrometer and gravimetric filter (Grimm) Light scattering in real time for particle number concentration and size distribution Particle sampling on filter for gravimetric use to determine specific particle mass aerosol focusing Dual technology in one device! Grimm patent! (1) filter chamber, open with 49mm PTFE filter (2) May
8 specification: grimm spectrometer Specifications Dust range [µg/m³] Size Range [µm] Size channels [µm] Sample air Particle counting Battery duration Weight / Dimensions Data output via Windows software #1.108 # > > > >32 15 channels counts 31 channels counts 16 channels mass 32 channels mass (0.23)/0.3/0.4/0.5/0.65/ (0.23)/0.25/0.28/0.3/0.35/0.4/0.45/ 0.8/1/1.6/2/3/4/5/7.5/10/ 0.5/0.58/0.65/0.7/0.8/1/1.3/1.6/2/ 15/20 2.5/3/3.5/4/5/6.5/7.5/8.5/10/12.5/ 15/17.5/20/25/30/ l/min up to P/l up to 8h 2.5 kg with battery / 24 x 12 x 6 cm Particle concentration in particles/litre, for all size channels or Particle mass in µg/m³, for all size channels Particle mass fractions in µg/m³, simultaneously according to EN 481 occupational (inhalable, thoracic, respirable) and EPA environmental (PM 10, PM 2.5, PM 1 ) May
The new 11-R (one part of the Mini WRAS) and GRIMM MINI-WRAS Andreas Jaksch. Symposium Stockholm Mai
The new 11-R (one part of the Mini WRAS) and GRIMM MINI-WRAS Andreas Jaksch Symposium Stockholm Mai 2014 1 Outline Optical Particle Detection Method 11-R Main features of the GRIMM 11-R Measurement principle
More informationFundamentals of Particle Counting
Fundamentals of Particle Counting 1 Particle Counting: Remains the most significant technique for determining the cleanliness level of a fluid Useful as a tool for qualification and monitoring cleanroom
More informationWhy is the sky blue?
Why is the sky blue? Volcanic: June 12, 1991: Mt Pinatubo ejected 20 million tons of sulfur dioxide. Aerosols spread globally Haze lowered a drop of global temperature by 1F Size parameter: Rayleigh
More informationThank You for Attending Today s Webinar:
Detect, Measure, Analyze. Thank You for Attending Today s Webinar: Aerosol Monitoring 201 Your Host Jim Behnke Outside Sales RAECO-LIC LLC jim@raeco.com Featured Speaker Achim Edfelder North American Sales
More informationNanophotonics: principle and application. Khai Q. Le Lecture 4 Light scattering by small particles
Nanophotonics: principle and application Khai Q. Le Lecture 4 Light scattering by small particles Previous lecture Drude model, Drude-Sommerfeld model and Drude-Lorentz model for conducting media (metal):
More informationp(θ,φ,θ,φ) = we have: Thus:
1. Scattering RT Calculations We come spinning out of nothingness, scattering stars like dust. - Jalal ad-din Rumi (Persian Poet, 1207-1273) We ve considered solutions to the radiative transfer equation
More informationCONTINUOUS FINE DUST MEASURING SYSTEM
CONTINUOUS FINE DUST MEASURING SYSTEM PM 10 - PM 2,5 - PM 1 Particle count distribution DustMonit ENGINEERING SRL Via Paolo Diacono, 1-20133 Milano (MI) - ITALIA Tel ++39.02.26684830 - E-mail : info@conteng.it
More informationAbsorption and scattering
Absorption and scattering When a beam of radiation goes through the atmosphere, it encounters gas molecules, aerosols, cloud droplets, and ice crystals. These objects perturb the radiation field. Part
More informationThe mathematics of scattering and absorption and emission
The mathematics of scattering and absorption and emission The transmittance of an layer depends on its optical depth, which in turn depends on how much of the substance the radiation has to pass through,
More informationAerosol Optical Properties
ATM 507 Lecture 25 Text reading Chapter 15 Paper Due Dec. 9 Review Session Dec. 9 Final Dec. 12 (10:30 AM-12:30 PM) Today s topic Aerosol Optical Properties 1 Aerosol Optical Properties There are a number
More informationOcean Optics XIV Conference, Kona, Hawaii 1998
INTRODUCTION Ocean Optics XIV Conference, Kona, Hawaii 1998 COASTAL AEROSOL PHASE FUNCTION MEASUREMENTS WITH A CUSTOM POLAR NEPHELOMETER By John N. Porter, Tom F. Cooney, Craig Motell University of Hawaii
More informationNanoparticle Exposure in the Workplace
Nanoparticle Exposure in the Workplace Michele. L. Ostraat, Ph.D. RTI International September 11, 2012 Practical Workplace Issues Related to Setting & Using Engineered Nanomaterial OELs Lack of instrumentation/characterization
More informationDirect reading aerosol monitors
Health and Safety Executive Direct reading aerosol monitors 27 th June 2018 Andrew Thorpe Introduction Direct reading Aerosol Monitors (DRAMs) are often used as a complementary approach to conventional
More informationThe Scattering of Light by Small Particles. Advanced Laboratory, Physics 407 University of Wisconsin Madison, Wisconsin 53706
(4/28/09) The Scattering of Light by Small Particles Advanced Laboratory, Physics 407 University of Wisconsin Madison, Wisconsin 53706 Abstract In this experiment we study the scattering of light from
More informationScattering of EM waves by spherical particles: Overview of Mie Scattering
ATMO 551a Fall 2010 Scattering of EM waves by spherical particles: Overview of Mie Scattering Mie scattering refers to scattering of electromagnetic radiation by spherical particles. Under these conditions
More informationAtmospheric Optics. Lecture 17!! Nature s Light Show. Scattering. Atmospheric Optics. Atmospheric Optics. Scattering Reflection Ahrens Chapter 15
Lecture 17!! Nature s Light Show Atmospheric Optics Nature s Light Show Atmospheric Optics Scattering Reflection Ahrens Chapter 15 1 2 Scattering Reflection Refraction Diffraction Atmospheric Optics The
More informationWhat are Aerosols? Suspension of very small solid particles or liquid droplets Radii typically in the range of 10nm to
What are Aerosols? Suspension of very small solid particles or liquid droplets Radii typically in the range of 10nm to 10µm Concentrations decrease exponentially with height N(z) = N(0)exp(-z/H) Long-lived
More informationRadiation in the atmosphere
Radiation in the atmosphere Flux and intensity Blackbody radiation in a nutshell Solar constant Interaction of radiation with matter Absorption of solar radiation Scattering Radiative transfer Irradiance
More informationLecture 26. Regional radiative effects due to anthropogenic aerosols. Part 2. Haze and visibility.
Lecture 26. Regional radiative effects due to anthropogenic aerosols. Part 2. Haze and visibility. Objectives: 1. Attenuation of atmospheric radiation by particulates. 2. Haze and Visibility. Readings:
More information7. Aerosols and Climate
7. Aerosols and Climate I. Scattering 1. When radiation impinges on a medium of small particles, scattering of some of the radiation occurs in all directions. The portion scattered backward is called the
More informationLecture # 04 January 27, 2010, Wednesday Energy & Radiation
Lecture # 04 January 27, 2010, Wednesday Energy & Radiation Kinds of energy Energy transfer mechanisms Radiation: electromagnetic spectrum, properties & principles Solar constant Atmospheric influence
More informationCharacterisation of atmospheric aerosol sampled from an aircraft using scanning electron microscopy
School of Earth and Environment INSTITUTE FOR CLIMATE & ATMOSPHERIC SCIENCE Characterisation of atmospheric aerosol sampled from an aircraft using scanning electron microscopy Alberto Sánchez-Marroquín,
More informationVisualization of Xe and Sn Atoms Generated from Laser-Produced Plasma for EUV Light Source
3rd International EUVL Symposium NOVEMBER 1-4, 2004 Miyazaki, Japan Visualization of Xe and Sn Atoms Generated from Laser-Produced Plasma for EUV Light Source H. Tanaka, A. Matsumoto, K. Akinaga, A. Takahashi
More informationVISIBLE LIGHT. L 32 Light and Optics [2] Seeing through the window. Windows behaving as mirrors. Seeing through a window
L 32 Light and Optics [2] Measurements of the speed of light The bending of light refraction Total internal reflection Dispersion Dispersion Rainbows Atmospheric scattering Blue sky and red sunsets Mirrors
More information, analogous to an absorption coefficient k a
Light Scattering When light passes through a medium some of it is directed away from its direction of travel. Any photons that are diverted from their direction of propagation are scattered. In the atmosphere
More informationComparison of AERONET inverted size distributions to measured distributions from the Aerodyne Aerosol Mass Spectrometer
Comparison of inverted size distributions to measured distributions from the Aerodyne Aerosol Mass Spectrometer Peter DeCarlo Remote Sensing Project April 28, 23 Introduction The comparison of direct in-situ
More informationCoherent vs. Incoherent light scattering
11. Light Scattering Coherent vs. incoherent scattering Radiation from an accelerated charge Larmor formula Why the sky is blue Rayleigh scattering Reflected and refracted beams from water droplets Rainbows
More informationLecture 6: Continuum Opacity and Stellar Atmospheres
Lecture 6: Continuum Opacity and Stellar Atmospheres To make progress in modeling and understanding stellar atmospheres beyond the gray atmosphere, it is necessary to consider the real interactions between
More informationATM 10. Severe and Unusual Weather. Prof. Richard Grotjahn.
ATM 10 Severe and Unusual Weather Prof. Richard Grotjahn http://atm.ucdavis.edu/~grotjahn/course/atm10/index.html Lecture topics: Optics: Scattering Sky Colors and Rays Optics: refraction Mirages and Refraction
More informationATOC 3500/CHEM 3152 Week 9, March 8, 2016
ATOC 3500/CHEM 3152 Week 9, March 8, 2016 Hand back Midterm Exams (average = 84) Interaction of atmospheric constituents with light Haze and Visibility Aerosol formation processes (more detail) Haze and
More informationDepolarization of Light by Single Particles: Unraveling the Mysteries of Paris Fog
Depolarization of Light by Single Particles: Unraveling the Mysteries of Paris Fog Darrel Baumgardner Centro de Ciencias de la Atmósfera Universidad Nacional Autónoma de México Neda Boyouk Site Instrumental
More informationLight Interaction with Small Structures
Light Interaction with Small Structures Molecules Light scattering due to harmonically driven dipole oscillator Nanoparticles Insulators Rayleigh Scattering (blue sky) Semiconductors...Resonance absorption
More informationCoherent vs. Incoherent light scattering
11. Light Scattering Coherent vs. incoherent scattering Radiation from an accelerated charge Larmor formula Rayleigh scattering Why the sky is blue Reflected and refracted beams from water droplets Rainbows
More informationNTUA. A. Georgakopoulou. A. Papayannis1, A. Aravantinos2 NATIONAL TECHNICAL UNIVERSITY OF ATHENS TECHNOLOGICAL EDUCATIONAL INSTIDUTION OF ATHENS SIENA
High Spectral Resolution LIDAR Receivers, to Measure Aerosol to Molecular Scattering Ratio in Bistatic Mode, for use in Atmospheric Monitoring for EAS Detectors E. Fokitis1, P. Fetfatzis1, 1, S. Maltezos1
More informationScattering. Vog Bank. MET 200 Lecture 14 Nature s Light Show. Atmospheric Optics. Atmospheric Optics. Ahrens Chapter 15
MET 200 Lecture 14 Nature s Light Show Vog Bank Atmospheric Optics Ahrens Chapter 15 1 2 Scattering Reflection Refraction Diffraction Atmospheric Optics The amazing variety of optical phenomena observed
More informationPrinciples of Radiative Transfer Principles of Remote Sensing. Marianne König EUMETSAT
- Principles of Radiative Transfer Principles of Remote Sensing Marianne König EUMETSAT marianne.koenig@eumetsat.int Remote Sensing All measurement processes which perform observations/measurements of
More informationThe Scattering of Light by Small Particles. Advanced Laboratory, Physics 407 University of Wisconsin Madison, Wisconsin 53706
(4/6/10) The Scattering of Light by Small Particles Advanced Laboratory, Physics 407 University of Wisconsin Madison, Wisconsin 53706 Abstract In this experiment we study the scattering of light from various
More informationDetecting high energy photons. Interactions of photons with matter Properties of detectors (with examples)
Detecting high energy photons Interactions of photons with matter Properties of detectors (with examples) Interactions of high energy photons with matter Cross section/attenution length/optical depth Photoelectric
More informationLaser Beam Interactions with Solids In absorbing materials photons deposit energy hc λ. h λ. p =
Laser Beam Interactions with Solids In absorbing materials photons deposit energy E = hv = hc λ where h = Plank's constant = 6.63 x 10-34 J s c = speed of light Also photons also transfer momentum p p
More informationOutline. December 14, Applications Scattering. Chemical components. Forward model Radiometry Data retrieval. Applications in remote sensing
in in December 4, 27 Outline in 2 : RTE Consider plane parallel Propagation of a signal with intensity (radiance) I ν from the top of the to a receiver on Earth Take a layer of thickness dz Layer will
More informationLecture Notes Prepared by Mike Foster Spring 2007
Lecture Notes Prepared by Mike Foster Spring 2007 Solar Radiation Sources: K. N. Liou (2002) An Introduction to Atmospheric Radiation, Chapter 1, 2 S. Q. Kidder & T. H. Vander Haar (1995) Satellite Meteorology:
More informationWhich of the following can be used to calculate the resistive force acting on the brick? D (Total for Question = 1 mark)
1 A brick of mass 5.0 kg falls through water with an acceleration of 0.90 m s 2. Which of the following can be used to calculate the resistive force acting on the brick? A 5.0 (0.90 9.81) B 5.0 (0.90 +
More informationMANIPAL INSTITUTE OF TECHNOLOGY
SCHEME OF EVAUATION MANIPA INSTITUTE OF TECHNOOGY MANIPA UNIVERSITY, MANIPA SECOND SEMESTER B.Tech. END-SEMESTER EXAMINATION - MAY SUBJECT: ENGINEERING PHYSICS (PHY/) Time: 3 Hrs. Max. Marks: 5 Note: Answer
More informationObservation of Smoke and Dust Plume Transport and Impact on the Air Quality Remote Sensing in New York City
Observation of Smoke and Dust Plume Transport and Impact on the Air Quality Remote Sensing in New York City Yonghua Wu*, Chowdhury Nazmi, Cuiya Li, Daniel Hoyos, Barry Gross, Fred Moshary NOAA-CREST and
More informationAtmospheric Lidar The Atmospheric Lidar (ATLID) is a high-spectral resolution lidar and will be the first of its type to be flown in space.
www.esa.int EarthCARE mission instruments ESA s EarthCARE satellite payload comprises four instruments: the Atmospheric Lidar, the Cloud Profiling Radar, the Multi-Spectral Imager and the Broad-Band Radiometer.
More informationINTRODUCTION. Definition:-
INTRODUCTION Definition:- Light scatteringis a form ofscatteringin whichlightis the form of propagating energy which is scattered. Light scattering can be thought of as the deflection of arayfrom a straight
More informationLecture 08. Solutions of Lidar Equations
Lecture 08. Solutions of Lidar Equations HWK Report #1 Solution for scattering form lidar equation Solution for fluorescence form lidar equation Solution for differential absorption lidar equation Solution
More informationAPPLICATION INFORMATION
A-1995A APPLICATION INFORMATION Particle Characterization THE SIZING OF NON-SPHERICAL,SUB-MICRON PARTICLES USING POLARIZATION INTENSITY DIFFERENTIAL SCATTERING (PIDS ) Introduction Nearly all laser-based
More informationMEASURING NANOPARTICLE EXPOSURE
MEASURING NANOPARTICLE EXPOSURE APPLICATION NOTE NSAM-001 The Nanoparticle Surface Area Monitor reports the surface area of inhaled particles deposited in the lung Nanoparticle Exposure There is increasing
More informationImproved Process Measurement & Control. OD 600 vs. AU Measurements in Fermentation Cell Density
Finesse, LLC 3350 Scott Boulevard #1 Santa Clara, CA 95054 9351 Irvine Boulevard Irvine, CA 92618 800-598-9515 www.finesse-inc.com P01 OD 600 vs. AU Measurements in Fermentation Cell Density This technical
More informationLaser heating of noble gas droplet sprays: EUV source efficiency considerations
Laser heating of noble gas droplet sprays: EUV source efficiency considerations S.J. McNaught, J. Fan, E. Parra and H.M. Milchberg Institute for Physical Science and Technology University of Maryland College
More informationCHAPTER 8. AEROSOLS 8.1 SOURCES AND SINKS OF AEROSOLS
1 CHAPTER 8 AEROSOLS Aerosols in the atmosphere have several important environmental effects They are a respiratory health hazard at the high concentrations found in urban environments They scatter and
More information9/12/2011. Training Course Remote Sensing - Basic Theory & Image Processing Methods September 2011
Training Course Remote Sensing - Basic Theory & Image Processing Methods 19 23 September 2011 Introduction to Remote Sensing Michiel Damen (September 2011) damen@itc.nl 1 Overview Electro Magnetic (EM)
More informationOptic Detectors Calibration for Measuring Ultra-High Energy Extensive Air Showers Cherenkov Radiation by 532 nm Laser
Optic Detectors Calibration for Measuring Ultra-High Energy Extensive Air Showers Cherenkov Radiation by 532 nm Laser S. P. Knurenko 1, a, Yu. A. Egorov 1, b, I. S. Petrov 1, c Yu.G. Shafer Institute of
More informationSTUDY ON PHOTOELECTRIC CONFRONTATION OF WATER MIST SCREEN SYSTEM
2013 WJTA-IMCA Conference and Expo September 9-11, 2013 Houston, Texas Paper STUDY ON PHOTOELECTRIC CONFRONTATION OF WATER MIST SCREEN SYSTEM B. Ren, HJ. Zhang, HG. Xu, M. Guan Xi'an Dongfeng Instrument
More informationLecture 6: Radiation Transfer. Global Energy Balance. Reflection and Scattering. Atmospheric Influences on Insolation
Lecture 6: Radiation Transfer Global Energy Balance terrestrial radiation cooling Solar radiation warming Global Temperature atmosphere Vertical and latitudinal energy distributions Absorption, Reflection,
More informationLecture 6: Radiation Transfer
Lecture 6: Radiation Transfer Vertical and latitudinal energy distributions Absorption, Reflection, and Transmission Global Energy Balance terrestrial radiation cooling Solar radiation warming Global Temperature
More informationSPECTRUM. Dispersion. This phenomenon can be observed in a lab environment using a
SPECTRUM Dispersion The phenomenon due to which a polychromatic light, like sunlight, splits into its component colours, when passed through a transparent medium like a glass prism, is called dispersion
More informationNew Instruments from GRIMM
New Instruments from GRIMM Markus Pesch Symposium at Stockholm, 01.11.2016 1 Outline Motivation for new Aerosol measurement devices Objectives for measurements of particle number and sizes GRIMM EDM 665
More informationPortable Instrument for Online Investigations of Optical Properties of Airborne Particles
Portable Instrument for Online Investigations of Optical Properties of Airborne Particles Julian Robertz*, Aleksandar Duric, Martin Allemann Siemens Schweiz AG, Building Technologies Division, Zug, Switzerland
More informationCHEM6416 Theory of Molecular Spectroscopy 2013Jan Spectroscopy frequency dependence of the interaction of light with matter
CHEM6416 Theory of Molecular Spectroscopy 2013Jan22 1 1. Spectroscopy frequency dependence of the interaction of light with matter 1.1. Absorption (excitation), emission, diffraction, scattering, refraction
More informationDetection of X-Rays. Solid state detectors Proportional counters Microcalorimeters Detector characteristics
Detection of X-Rays Solid state detectors Proportional counters Microcalorimeters Detector characteristics Solid State X-ray Detectors X-ray interacts in material to produce photoelectrons which are collected
More informationDetermination of particle size distribution Single particle light interaction methods. Part 4:
Provläsningsexemplar / Preview INTERNATIONAL STANDARD ISO 21501-4 Second edition 2018-05 Determination of particle size distribution Single particle light interaction methods Part 4: Light scattering airborne
More informationNanophysics: Main trends
Nano-opto-electronics Nanophysics: Main trends Nanomechanics Main issues Light interaction with small structures Molecules Nanoparticles (semiconductor and metallic) Microparticles Photonic crystals Nanoplasmonics
More informationPreliminary testing of new approaches to retrieve aerosol properties from joint photometer-lidar inversion
ESA/IDEAS Project- WP 3440-2 Preliminary testing of new approaches to retrieve aerosol properties from joint photometer-lidar inversion Q. Hu, P. Goloub, O. Dubovik, A. Lopatin, T. Povdin, T. Lopyonok,
More informationA new versatile condensation particle counter for research and environmental monitoring
A new versatile condensation particle counter for research and environmental monitoring, Maximilian Weiss Palas GmbH, Greschbachstr. 3b, 76229 Karlsruhe, Germany, http://www.palas.de, spielvogel@palas.de
More informationA Discussion on the Applicable Condition of Rayleigh Scattering
www.ijrsa.org International Journal of Remote Sensing Applications (IJRSA) Volume 5, 015 doi: 10.14355/ijrsa.015.05.007 A Discussion on the Applicable Condition of Rayleigh Scattering Nan Li *1, Yiqing
More informationExploring the Atmosphere with Lidars
Exploring the Atmosphere with Lidars 2. Types of Lidars S Veerabuthiran S Veerabuthiran is working as a research fellow in Space Physics Laboratory, Vikram Sarabhai Space Centre, Trivandrum. His research
More informationTHE MEASUREMENT OF SOLAR ULTRAVIOLET SPECTRAL IRRADIANCE PROBLEMS & SOLUTIONS
THE MEASUREMENT OF SOLAR ULTRAVIOLET SPECTRAL IRRADIANCE PROBLEMS & SOLUTIONS INTRODUCTION In recent years, researchers involved in many unrelated scientific disciplines have acquired an interest in accurately
More informationDifferential Mobility Particle Sizer (Aerosol measurements)
Institute for Atmospheric and Climate Science - IACETH Atmospheric Physics Lab Work Differential Mobility Particle Sizer (Aerosol measurements) Abstract A differential mobility particle sizer (DMPS) is
More informationSurface Sensitivity & Surface Specificity
Surface Sensitivity & Surface Specificity The problems of sensitivity and detection limits are common to all forms of spectroscopy. In its simplest form, the question of sensitivity boils down to whether
More informationEUV Reflectivity measurements on Acktar Sample Magic Black
Report EUV Reflectivity measurements on Acktar Sample Magic Black S. Döring, Dr. K. Mann Laser-Laboratorium Göttingen e.v. October 28, 2011 Contents 1 Introduction 3 2 Setup 3 3 Measurements 4 4 Conclusion
More informationFRITSCH "analysette 22" NanoTec The Result of 30 Years of Experience in Particle Size Measurement. 1 The Inventor of "Reverse Fourier Optics"
FRITSCH "analysette 22" NanoTec The Result of 30 Years of Experience in Particle Size Measurement Wolfgang Mutter FRITSCH GmbH Manufacturers of Laboratory Instruments Industriestrasse 8 55743 Idar-Oberstein
More informationRemote Sensing Systems Overview
Remote Sensing Systems Overview Remote Sensing = Measuring without touching Class objectives: Learn principles for system-level understanding and analysis of electro-magnetic remote sensing instruments
More informationUniverse. Chapter 6. Optics and Telescopes 11/16/2014. By reading this chapter, you will learn. Tenth Edition
Roger Freedman Robert Geller William Kaufmann III Universe Tenth Edition Chapter 6 Optics and Telescopes By reading this chapter, you will learn 6 1 How a refracting telescope uses a lens to form an image
More informationA Novel Optical Instrument for Estimating Size Segregated Aerosol Mass Concentration in Real Time
Aerosol Science and Technology ISSN: 0278-6826 (Print) 1521-7388 (Online) Journal homepage: http://www.tandfonline.com/loi/uast20 A Novel Optical Instrument for Estimating Size Segregated Aerosol Mass
More informationAnalysis of Thermal Diffusivity of Metals using Lock-in Thermography
Analysis of Thermal Diffusivity of Metals using Lock-in Thermography by F. Wagner*, T. Malvisalo*, P. W. Nolte**, and S. Schweizer** * Department of Electrical Engineering, South Westphalia University
More informationMODULE 4.3 Atmospheric analysis of particulates
MODULE 4.3 Atmospheric analysis of particulates Measurement And Characterisation Of The Particulate Content 1 Total particulate concentration 1 Composition of the particulate 1 Determination of particle
More informationObservation of Tropospheric Aerosol Using Mie Scattering LIDAR at Srisamrong, Sukhothai Province
NU Science Journal 27; 4(1): - Observation of Tropospheric Aerosol Using Mie Scattering LIDAR at Srisamrong, Sukhothai Province Siriluk Ruangrungrote 1 *, Arunee Intasorn 1 and Akkaneewut Chabangbon 2
More informationAerosol Optical Extinction Measurements Using a Pulsed Laser Cavity-Ring Down Transmissometer
International Journal of ChemTech Research CODEN( USA): IJCRGG ISSN : 0974-4290 Vol.1, No.3, pp 394-400, July-Sept 2009 Aerosol Optical Extinction Measurements Using a Pulsed Laser Cavity-Ring Down Transmissometer
More informationA simple method for estimating the thickness of the atmosphere by light scattering
A simple method for estimating the thickness of the atmosphere by light scattering Michael Vollmer a) Physikalische Ingenieurwissenschaften, University of Applied Sciences Brandenburg, 14770 Brandenburg,
More informationUniversity of Cyprus. Reflectance and Diffuse Spectroscopy
University of Cyprus Biomedical Imaging and Applied Optics Reflectance and Diffuse Spectroscopy Spectroscopy What is it? from the Greek: spectro = color + scope = look at or observe = measuring/recording
More information2. The spectrum of visible light bounds the region of intensity of light emitted by the Sun. a. maximum b. minimum
CHAPTER 14 LIGHT AND SOUND IN THE ATMOSPHERE MULTIPLE CHOICE QUESTIONS 1. As the Sun s rays travel through the atmosphere, they are by cloud droplets or ice crystals, or by raindrops. a. scattered b. reflected
More informationExtinction. Aerosols
Extinction Extinction is the loss of energy out of a beam of radiation as it propagates. Extinction = absorption + scattering Extinction cross section analogous to the cross-sectional area of absorbers
More informationLecture 06. Fundamentals of Lidar Remote Sensing (4) Physical Processes in Lidar
Lecture 06. Fundamentals of Lidar Remote Sensing (4) Physical Processes in Lidar Physical processes in lidar (continued) Doppler effect (Doppler shift and broadening) Boltzmann distribution Reflection
More informationNature of diffraction. Diffraction
Nature of diffraction Diffraction From Grimaldi to Maxwell Definition of diffraction diffractio, Francesco Grimaldi (1665) The effect is a general characteristics of wave phenomena occurring whenever a
More informationElectromagnetic Waves
ELECTROMAGNETIC RADIATION AND THE ELECTROMAGNETIC SPECTRUM Electromagnetic Radiation (EMR) THE ELECTROMAGNETIC SPECTRUM Electromagnetic Waves A wave is characterized by: Wavelength (λ - lambda) is the
More informationLecture 3: Optical Properties of Insulators, Semiconductors, and Metals. 5 nm
Metals Lecture 3: Optical Properties of Insulators, Semiconductors, and Metals 5 nm Course Info Next Week (Sept. 5 and 7) no classes First H/W is due Sept. 1 The Previous Lecture Origin frequency dependence
More informationLatest Technology and Standardization Trends for Liquid-borne Particle Counters
Latest Technology and Standardization Trends for Liquid-borne Particle Counters Kaoru Kondo Rion Co., Ltd. (Original paper is K.Kondo, Bunseki,Vol.9, p499 (2012)) Abstract Fine particles contaminating
More informationPhysics 214 Course Overview
Physics 214 Course Overview Lecturer: Mike Kagan Course topics Electromagnetic waves Optics Thin lenses Interference Diffraction Relativity Photons Matter waves Black Holes EM waves Intensity Polarization
More informationElectromagnetic spectra
Properties of Light Waves, particles and EM spectrum Interaction with matter Absorption Reflection, refraction and scattering Polarization and diffraction Reading foci: pp 175-185, 191-199 not responsible
More informationReal Time Dust Monitoring Strategies and Tools
Real Time Dust Monitoring Strategies and Tools Indiana H&S Conference Scott Norman, CIH CSP Product Specialist TSI Incorporated Shoreview MN TSI Incorporated Real time measurement instruments + Speedometer
More informationAn Analytical Algorithm for Scattering Type Determination under Different Weather Conditions
Journal of Signal and Information Processing, 2012, 3, 7785 http://dx.doi.org/10.4236/jsip.2012.31010 Published Online February 2012 (http://www.scirp.org/journal/jsip) 77 An Analytical Algorithm for Scattering
More information1 Fundamentals of Lidar
1 Fundamentals of Lidar The lidar profiling technique (Fiocco, 1963) is based on the study of the interaction between a laser radiation sent into the atmosphere and the atmospheric constituents. The interaction
More informationExtrel is widely respected for the quality of mass spectrometer systems that are
Extrel is widely respected for the quality of mass spectrometer systems that are available to the world's top research scientists. In response to increasing requests for complete turn-key systems built
More informationRadiation and the atmosphere
Radiation and the atmosphere Of great importance is the difference between how the atmosphere transmits, absorbs, and scatters solar and terrestrial radiation streams. The most important statement that
More informationTHE OPTICAL SCIENCES COMPANY P.O. Box 446, Placentia, California Phone: (714) Pulsed Laser Backscatter. Glenn A. Tyler.
THE OPTICAL SCIENCES COMPANY P.O. Box 446, Placentia, California 92670 Phone: (714) 524-3622 Report No. TR-400 (v \P Pulsed Laser Backscatter Glenn A. Tyler and David L. Fried November 1980 WBTmiüTIÖlf
More information4.2 CHARACTERISTICS OF ATMOSPHERIC AEROSOLS USING OPTICAL REMOTE SENSING
4.2 CHARACTERISTICS OF ATMOSPHERIC AEROSOLS USING OPTICAL REMOTE SENSING C. Russell Philbrick *, Timothy Wright, Michelle Snyder, Hans Hallen North Carolina State University, Raleigh NC Andrea M. Brown,
More informationLecture 2: Global Energy Cycle
Lecture 2: Global Energy Cycle Planetary energy balance Greenhouse Effect Vertical energy balance Solar Flux and Flux Density Solar Luminosity (L) the constant flux of energy put out by the sun L = 3.9
More informationIntroduction to Radiation Monitoring
Introduction to Radiation Monitoring Iain Darby Honorary Research Fellow, University of Glasgow iain.darby@glasgow.ac.uk https://at.linkedin.com/in/idarby https://www.facebook.com/iain.darby.662 Outline
More information