Determination and Validation of the Spectral Power Distribution (SPD) of Artificial Weathering (Lightfastness) Instruments
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1 LIGHT PHYSICS Light and Lighting Francesco Anselmo Light Intro Light Animates and Reveals Architecture
1 LIGHT PHYSICS Light and Lighting Francesco Anselmo Light intro Light animates and reveals architecture. Architecture cannot fully exist without light, since without light there would be nothing to see. Yet in architectural design light is usually either expected from nature or developed as an add-on attachment very late in the design process. The course explores the symbiotic relationship between architecture and light. As much as light can reveal architecture, architecture can animate light, making it bounce, scatter, refract, altering its spectrum and colour perception, absorbing it or reflecting it, modulating its path and strength in both space and time. It aims at developing a sensibility and intuition to the qualities of light, whilst giving the physical and computational tools to explore and validate design ideas. 4 7 1 2 5 3 6 1 LIGHT PHYSICS 4 LIGHT ELECTRIC 7 LIGHT CONNECTED 2 LIGHT BIOLOGY 5 LIGHT ARCHITECTURE 3 LIGHT NATURAL 6 LIGHT VIRTUAL Reading list Books Free online resources Bachelard, Gaston. The poetics of space, Beacon Press 1992 • http://hyperphysics.phy-astr.gsu.edu/hbase/ligcon.html Banham, Reyner. The architecture of the well-tempered Environment, Chicago University Press 1984 • http://thedaylightsite.com/ Bazerman, Charles. The languages of Edison’s light, MIT Press 2002 Berger, John. Ways of seeing, Pearson Education, Limited, 2002 • http://issuu.com/lightonline/docs/handbook-of-lighting-design Berger, John. About looking, Bloomsbury Publishing 2009 • http://www.radiance-online.org/ Bluhm, Andreas. Light! The industrial age 1750-1900, Carnegie Museum of Art 2000 Boyce, Peter R. Human Factors in Lighting, Taylor & Francis 2003 Calvino, Italo. -
Download the DIA Color Chart
DEMI-PERMANENT HAIRCOLOR 2 COMPLIMENTARY LINES OF HAIRCOLOR Each with its own benefit & expertise both provide maximum creativity & freedom ADVANCED ALKALINE TECHNOLOGY GENTLE ACID TECHNOLOGY HIGH PERFORMANCE HIGH PERFORMANCE • Demi-permanent crème • Luminous demi-permanent gel-crème • Rich tones, exceptional softness • Zero lift • Covers up to 70% grey • Intense care for the hair THE PROCESS THE PROCESS • Lifts (up to 1.5 Levels with 15-vol), then deposits • Zero lift, deposit only BEFORE COLOR DURING COLOR AFTER COLOR BEFORE COLOR DURING COLOR AFTER COLOR On natural hair, the cuticle The alkaline agents slightly open DIA Richesse has the ability to lighten up On color-treated & DIA Light has an acid The cationic polymers in scales are closed. the hair fiber allowing colorants to 1.5 levels, cover up to 70% white hair sensitized hair, the cuticle pH close to the natural pH of the hair. DIA Light have a resurfacing to penetrate the cuticle. & create rich, profound tones. scales are already open. effect on the cuticle, leaving There is no lift with gentle penetration the hair with amazing shine. of colorants for long lasting color. ADVANCED ALKALINE TECHNOLOGY ADVANCED ALKALINE TECHNOLOGY HIGH PERFORMANCE • Demi-permanent crème • Rich tones, exceptional softness • Covers up to 70% grey THE PROCESS • Lifts (up to 1.5 Levels with 15-vol), then deposits BEFORE COLOR DURING COLOR AFTER COLOR On natural hair, the cuticle The alkaline agents slightly open DIA Richesse has the ability to lighten scales are closed. the hair fiber allowing colorants up to 1.5 levels, cover up to 70% white to penetrate the cuticle. -
TIE-35: Transmittance of Optical Glass
DATE October 2005 . PAGE 1/12 TIE-35: Transmittance of optical glass 0. Introduction Optical glasses are optimized to provide excellent transmittance throughout the total visible range from 400 to 800 nm. Usually the transmittance range spreads also into the near UV and IR regions. As a general trend lowest refractive index glasses show high transmittance far down to short wavelengths in the UV. Going to higher index glasses the UV absorption edge moves closer to the visible range. For highest index glass and larger thickness the absorption edge already reaches into the visible range. This UV-edge shift with increasing refractive index is explained by the general theory of absorbing dielectric media. So it may not be overcome in general. However, due to improved melting technology high refractive index glasses are offered nowadays with better blue-violet transmittance than in the past. And for special applications where best transmittance is required SCHOTT offers improved quality grades like for SF57 the grade SF57 HHT. The aim of this technical information is to give the optical designer a deeper understanding on the transmittance properties of optical glass. 1. Theoretical background A light beam with the intensity I0 falls onto a glass plate having a thickness d (figure 1-1). At the entrance surface part of the beam is reflected. Therefore after that the intensity of the beam is Ii0=I0(1-r) with r being the reflectivity. Inside the glass the light beam is attenuated according to the exponential function. At the exit surface the beam intensity is I i = I i0 exp(-kd) [1.1] where k is the absorption constant. -
Reflectance and Transmittance Sphere
Reflectance and Transmittance Sphere Spectral Evolution four inch portable reflectance/ transmittance sphere is ideal for measuring vegetation physiological states SPECTRAL EVOLUTION offers a portable, compact four inch reflectance/transmittance (R/T) integrating sphere for measuring the reflectance and transmittance of vegetation. The 4 inch R/T sphere is lightweight and portable so you can take it into the field for in situ meas- urements, delivered with a stand as well as a ¼-20 mount for use with tripods. When used with a SPECTRAL EVOLUTION spectrometer or spectroradiometer such as the PSR+, RS-3500, RS- 5400, SR-6500 or RS-8800, it delivers detailed information for measurements of transmittance and reflectance modes. Two varying light intensity levels (High and Low) allow for a broader range of samples to be measured. Light reflected or transmitted from a sample in a sphere is integrated over a full hemisphere, with measurements insensitive to sample anisotropic directional reflectance (transmittance). This provides repeatable measurements of a variety of samples. The 4 inch portable R/T sphere can be used in vegetation studies such as, deriving absorbance characteristics, and estimating the leaf area index (LAI) from radiation reflected from a canopy surface. The sphere allows researchers to limit destructive sampling and provides timely data acquisition of key material samples. The R/T sphere allows you to collect all diffuse light reflected from a sample – measuring total hemispherical reflectance. You can measure reflectance and transmittance, and calculate absorption. You can select the bulb inten- sity level that suits your sample. A white reference is provided for both reflectance and transmittance measurements. -
WHITE LIGHT and COLORED LIGHT Grades K–5
WHITE LIGHT AND COLORED LIGHT grades K–5 Objective This activity offers two simple ways to demonstrate that white light is made of different colors of light mixed together. The first uses special glasses to reveal the colors that make up white light. The second involves spinning a colorful top to blend different colors into white. Together, these activities can be thought of as taking white light apart and putting it back together again. Introduction The Sun, the stars, and a light bulb are all sources of “white” light. But what is white light? What we see as white light is actually a combination of all visible colors of light mixed together. Astronomers spread starlight into a rainbow or spectrum to study the specific colors of light it contains. The colors hidden in white starlight can reveal what the star is made of and how hot it is. The tool astronomers use to spread light into a spectrum is called a spectroscope. But many things, such as glass prisms and water droplets, can also separate white light into a rainbow of colors. After it rains, there are often lots of water droplets in the air. White sunlight passing through these droplets is spread apart into its component colors, creating a rainbow. In this activity, you will view the rainbow of colors contained in white light by using a pair of “Rainbow Glasses” that separate white light into a spectrum. ! SAFETY NOTE These glasses do NOT protect your eyes from the Sun. NEVER LOOK AT THE SUN! Background Reading for Educators Light: Its Secrets Revealed, available at http://www.amnh.org/education/resources/rfl/pdf/du_x01_light.pdf Developed with the generous support of The Charles Hayden Foundation WHITE LIGHT AND COLORED LIGHT Materials Rainbow Glasses Possible white light sources: (paper glasses containing a Incandescent light bulb diffraction grating). -
Light, Color, and Atmospheric Optics
Light, Color, and Atmospheric Optics GEOL 1350: Introduction To Meteorology 1 2 • During the scattering process, no energy is gained or lost, and therefore, no temperature changes occur. • Scattering depends on the size of objects, in particular on the ratio of object’s diameter vs wavelength: 1. Rayleigh scattering (D/ < 0.03) 2. Mie scattering (0.03 ≤ D/ < 32) 3. Geometric scattering (D/ ≥ 32) 3 4 • Gas scattering: redirection of radiation by a gas molecule without a net transfer of energy of the molecules • Rayleigh scattering: absorption extinction 4 coefficient s depends on 1/ . • Molecules scatter short (blue) wavelengths preferentially over long (red) wavelengths. • The longer pathway of light through the atmosphere the more shorter wavelengths are scattered. 5 • As sunlight enters the atmosphere, the shorter visible wavelengths of violet, blue and green are scattered more by atmospheric gases than are the longer wavelengths of yellow, orange, and especially red. • The scattered waves of violet, blue, and green strike the eye from all directions. • Because our eyes are more sensitive to blue light, these waves, viewed together, produce the sensation of blue coming from all around us. 6 • Rayleigh Scattering • The selective scattering of blue light by air molecules and very small particles can make distant mountains appear blue. The blue ridge mountains in Virginia. 7 • When small particles, such as fine dust and salt, become suspended in the atmosphere, the color of the sky begins to change from blue to milky white. • These particles are large enough to scatter all wavelengths of visible light fairly evenly in all directions. -
The Electromagnetic Spectrum
The Electromagnetic Spectrum Wavelength/frequency/energy MAP TAP 2003-2004 The Electromagnetic Spectrum 1 Teacher Page • Content: Physical Science—The Electromagnetic Spectrum • Grade Level: High School • Creator: Dorothy Walk • Curriculum Objectives: SC 1; Intro Phys/Chem IV.A (waves) MAP TAP 2003-2004 The Electromagnetic Spectrum 2 MAP TAP 2003-2004 The Electromagnetic Spectrum 3 What is it? • The electromagnetic spectrum is the complete spectrum or continuum of light including radio waves, infrared, visible light, ultraviolet light, X- rays and gamma rays • An electromagnetic wave consists of electric and magnetic fields which vibrates thus making waves. MAP TAP 2003-2004 The Electromagnetic Spectrum 4 Waves • Properties of waves include speed, frequency and wavelength • Speed (s), frequency (f) and wavelength (l) are related in the formula l x f = s • All light travels at a speed of 3 s 108 m/s in a vacuum MAP TAP 2003-2004 The Electromagnetic Spectrum 5 Wavelength, Frequency and Energy • Since all light travels at the same speed, wavelength and frequency have an indirect relationship. • Light with a short wavelength will have a high frequency and light with a long wavelength will have a low frequency. • Light with short wavelengths has high energy and long wavelength has low energy MAP TAP 2003-2004 The Electromagnetic Spectrum 6 MAP TAP 2003-2004 The Electromagnetic Spectrum 7 Radio waves • Low energy waves with long wavelengths • Includes FM, AM, radar and TV waves • Wavelengths of 10-1m and longer • Low frequency • Used in many -
Guide for the Use of the International System of Units (SI)
Guide for the Use of the International System of Units (SI) m kg s cd SI mol K A NIST Special Publication 811 2008 Edition Ambler Thompson and Barry N. Taylor NIST Special Publication 811 2008 Edition Guide for the Use of the International System of Units (SI) Ambler Thompson Technology Services and Barry N. Taylor Physics Laboratory National Institute of Standards and Technology Gaithersburg, MD 20899 (Supersedes NIST Special Publication 811, 1995 Edition, April 1995) March 2008 U.S. Department of Commerce Carlos M. Gutierrez, Secretary National Institute of Standards and Technology James M. Turner, Acting Director National Institute of Standards and Technology Special Publication 811, 2008 Edition (Supersedes NIST Special Publication 811, April 1995 Edition) Natl. Inst. Stand. Technol. Spec. Publ. 811, 2008 Ed., 85 pages (March 2008; 2nd printing November 2008) CODEN: NSPUE3 Note on 2nd printing: This 2nd printing dated November 2008 of NIST SP811 corrects a number of minor typographical errors present in the 1st printing dated March 2008. Guide for the Use of the International System of Units (SI) Preface The International System of Units, universally abbreviated SI (from the French Le Système International d’Unités), is the modern metric system of measurement. Long the dominant measurement system used in science, the SI is becoming the dominant measurement system used in international commerce. The Omnibus Trade and Competitiveness Act of August 1988 [Public Law (PL) 100-418] changed the name of the National Bureau of Standards (NBS) to the National Institute of Standards and Technology (NIST) and gave to NIST the added task of helping U.S. -
Physics, Chapter 40: Light As a Wave Motion
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Robert Katz Publications Research Papers in Physics and Astronomy 1-1958 Physics, Chapter 40: Light as a Wave Motion Henry Semat City College of New York Robert Katz University of Nebraska-Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/physicskatz Part of the Physics Commons Semat, Henry and Katz, Robert, "Physics, Chapter 40: Light as a Wave Motion" (1958). Robert Katz Publications. 177. https://digitalcommons.unl.edu/physicskatz/177 This Article is brought to you for free and open access by the Research Papers in Physics and Astronomy at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Robert Katz Publications by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. 40 Light as a Wave Motion 40-1 Wave Versus Particle Let us recount some of the characteristics of the motion of particles and the propagation of waves, with a view toward analyzing the behavior of light. In accordance with Newton's first law, a particle moves in a straight-line path in the absence of external forces. Thus we might infer, as Newton suggested, that light is composed of particles, and that, in a continuous medium, there is no deflecting force on the light particles. At the interface between two media, light may be propagated in a straight line parallel to the interface. Thus even at an interface there is no force on the particles of light unless the light passes through the interface, and in that event the force acting must be perpendicular to the interface. -
Extraction of Incident Irradiance from LWIR Hyperspectral Imagery Pierre Lahaie, DRDC Valcartier 2459 De La Bravoure Road, Quebec, Qc, Canada
DRDC-RDDC-2015-P140 Extraction of incident irradiance from LWIR hyperspectral imagery Pierre Lahaie, DRDC Valcartier 2459 De la Bravoure Road, Quebec, Qc, Canada ABSTRACT The atmospheric correction of thermal hyperspectral imagery can be separated in two distinct processes: Atmospheric Compensation (AC) and Temperature and Emissivity separation (TES). TES requires for input at each pixel, the ground leaving radiance and the atmospheric downwelling irradiance, which are the outputs of the AC process. The extraction from imagery of the downwelling irradiance requires assumptions about some of the pixels’ nature, the sensor and the atmosphere. Another difficulty is that, often the sensor’s spectral response is not well characterized. To deal with this unknown, we defined a spectral mean operator that is used to filter the ground leaving radiance and a computation of the downwelling irradiance from MODTRAN. A user will select a number of pixels in the image for which the emissivity is assumed to be known. The emissivity of these pixels is assumed to be smooth and that the only spectrally fast varying variable in the downwelling irradiance. Using these assumptions we built an algorithm to estimate the downwelling irradiance. The algorithm is used on all the selected pixels. The estimated irradiance is the average on the spectral channels of the resulting computation. The algorithm performs well in simulation and results are shown for errors in the assumed emissivity and for errors in the atmospheric profiles. The sensor noise influences mainly the required number of pixels. Keywords: Hyperspectral imagery, atmospheric correction, temperature emissivity separation 1. INTRODUCTION The atmospheric correction of thermal hyperspectral imagery aims at extracting the temperature and the emissivity of the material imaged by a sensor in the long wave infrared (LWIR) spectral band. -
Including Far Red in an LED Lighting Spectrum
technically speaking BY ERIK RUNKLE Including Far Red in an LED Lighting Spectrum Far red (FR) is a one of the radiation (or light) wavebands larger leaves can be desired for other crops. that regulates plant growth and development. Many people We have learned that blue light (and to a smaller extent, consider FR as radiation with wavelengths between 700 and total light intensity) can influence the effects of FR. When the 800 nm, although 700 to 750 nm is, by far, the most active. intensity of blue light is high, adding FR only slightly increases By definition, FR is just outside the photosynthetically active extension growth. Therefore, the utility of including FR in an radiation (PAR) waveband, but it can directly and indirectly indoor lighting spectrum is greater under lower intensities increase growth. In addition, it can accelerate of blue light. One compelling reason to deliver at least some flowering of some crops, especially long-day plants, FR light indoors is to induce early flowering of young plants, which are those that flower when the nights are short. especially long-day plants. As we learn more about the effects of FR on plants, growers sometimes wonder, is it beneficial to include FR in a light-emitting diode (LED) spectrum? "As the DLI increases, Not surprisingly, the answer is, it depends on the application and crop. In the May 2016 issue of GPN, I wrote about the the utility of FR in effects of FR on plant growth and flowering (https:// bit.ly/2YkxHCO). Briefly, leaf size and stem length photoperiodic lighting increase as the intensity of FR increases, although the magnitude depends on the crop and other characteristics of the light environment. -
Electromagnetic Spectrum
Electromagnetic Spectrum Why do some things have colors? What makes color? Why do fast food restaurants use red lights to keep food warm? Why don’t they use green or blue light? Why do X-rays pass through the body and let us see through the body? What has the radio to do with radiation? What are the night vision devices that the army uses in night time fighting? To find the answers to these questions we have to examine the electromagnetic spectrum. FASTER THAN A SPEEDING BULLET MORE POWERFUL THAN A LOCOMOTIVE These words were used to introduce a fictional superhero named Superman. These same words can be used to help describe Electromagnetic Radiation. Electromagnetic Radiation is like a two member team racing together at incredible speeds across the vast regions of space or flying from the clutches of a tiny atom. They travel together in packages called photons. Moving along as a wave with frequency and wavelength they travel at the velocity of 186,000 miles per second (300,000,000 meters per second) in a vacuum. The photons are so tiny they cannot be seen even with powerful microscopes. If the photon encounters any charged particles along its journey it pushes and pulls them at the same frequency that the wave had when it started. The waves can circle the earth more than seven times in one second! If the waves are arranged in order of their wavelength and frequency the waves form the Electromagnetic Spectrum. They are described as electromagnetic because they are both electric and magnetic in nature.