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2 edition of The determination of radiative properties of surfaces using reflectance technquies found in the catalog.

The determination of radiative properties of surfaces using reflectance technquies

G. J. Dorman

The determination of radiative properties of surfaces using reflectance technquies

computer programs for use on theHP 9845.

by G. J. Dorman

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Published by Commission of the European Communities in Luxembourg .
Written in English


Edition Notes

SeriesEnergy
ContributionsCommission of the European Communities. Directorate-General for Science, Research and Development.
ID Numbers
Open LibraryOL22715852M
ISBN 100119399032

Physical surfaces such as metal, plastic, and paper possess difierent optical qualities that lead to difierent character-istics in images. We have found that humans can efiectively estimate certain surface re°ectance properties from a single image without knowledge of illumination. We develop a machine vision system to perform similar re. reflectance reliably across real-world illuminations • Subjects should be poor at estimating surface reflectance properties when their assumptions about the statistics of the illumination are infringed, i.e. under illuminations with atypical statistics, surface reflectance estimation should be poor.

The radiative properties that will be reported are the solar reflectance (SR) and the infrared emittance (e) and calculated SRI Radiative properties are determined and verified through testing by ECRC approved test laboratories and a process of random testing of rated products The ECRC product rating program does not specify minimum or target. Reflectance and emittance spectroscopy are increasingly important tools in remote sensing and have been employed in most recent planetary spacecraft missions. They are primarily used to measure properties of disordered materials, especially in the interpretation of remote observations of the surfaces of the Earth and other terrestrial s: 2.

4 Factors affecting spectral reflectance measurements Introduction is required to correct for its non-ideal reflectance properties (including non-ideal reflectivity and non-Lambertial behaviour), and K r = measured reflectance of standard reflectance in band pass rS. Abstract: Based on the theory of Goos-Hänchen shift and its continuity near the critical angle, we introduce the concept of penetration depth below the critical angle, and obtain the general formula of reflectance using the gradient complex refractive index multilayered model. Compared with the fitting curve with Fresnel's Formula, our calculated results are more consistent with experimental.


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The determination of radiative properties of surfaces using reflectance technquies by G. J. Dorman Download PDF EPUB FB2

Determination of Solar Reflectance Index of Ceramic Coatings for Use in outside Surfaces Article (PDF Available) in Materials Science Forum November with 3, Reads. Reflectance behaviour of soils under different field conditions was analysed and the spectral reflectance curves for different soil types were obtained.

Soil samples pertaining to each test site were analysed for mechanical composition, physioco-chemical properties to identify their relationship with soil by: surface reflectance properties.

We also discuss a number of cues that appear to underlie this aptitude. Surface Reflectance Estimation Estimating surface reflectance is difficult because the image presented by a material depends not only on the reflectance properties but also on the conditions of illumination.

The image of a chrome sphere, forCited by: Moisture Effects on Soil Reflectance. less attention has been paid to predict soil hydraulic properties using soil spectral data.

Roughness of surfaces was measured using a laser scanner. The Effect of Non-Lambertian Surface Reflectance on Aerosol Radiative Forcing P. Ricchiazzi, W. O’Hirok, and C. Gautier Institute for Computational Earth System Science University of California Santa Barbara, California Introduction Surface reflectance is an important factor in determining the strength of aerosol radiative forcing.

This test method does not supplant Test Method E which measures solar reflectance over the wavelength range to nm using integrating spheres. The portable solar reflectometer is calibrated using specimens of known solar reflectance to determine solar reflectance from measurements at four wavelengths in the solar spectrum: nm, nm, nm, and nm.

In this study, thermal and optical properties (emittance and reflectance of solar radiation) of different colors ceramic tiles for use in outside surfaces were measured. Although widely used in the brazilian residential market, these materials are not properly characterized with respect to these properties.

The thermal emittance measures were performed using an emissometer (D&S pattern SA1. Radiative flux is often referred to as irradiance. The units of radiative flux are Wm 2 mm 1. The broad-bandalbedo,orsimplythealbedo,islikewisegivenby the ratio of the total radiative fluxes, a ¼ Fþ F ½2 where the integration over wavelength is performed separately for the incident and reflected radiative.

and aerosols as it is implemented in the 6SV radiative transfer code (Vermote et al. b, Kotchenova et al. ): [1a] where TOA is the reflectance at the top of the atmosphere, atm is the atmosphere intrinsic reflectance, Tratm is the total atmosphere transmission (downward and upward), Satm is the.

Reflectance of the surface of a material is its effectiveness in reflecting radiant is the fraction of incident electromagnetic power that is reflected at an interface. The reflectance spectrum or spectral reflectance curve is the plot of the reflectance as a function of wavelength.

A methodology to measure the infrared reflectance of specular materials. • A thermographic camera and an infrared radiation source were used. • The analysis of errors and how to select the temperature of the source were described. • Specular surfaces of glass and metals were measured at varying angles.

• Methodology proved to be adequate. [8] Radiative forcing by LAI in snow and the ability to quantify it with optical remote sensing come from two physical properties: (i) larger particles (greater than ∼ μm) tend to accumulate near the snow surface as ablation advances [Conway et al., ], and (ii) transported LAI arrive and concentrate during late winter and spring when.

Here the depth argument of "in air" indicates that is evaluated using the water-leaving radiance and in the air, just above the water surface. The remote-sensing reflectance is a measure of how much of the downwelling radiance that is incident onto the water surface in any direction is eventually returned through the surface into a small solid angle centered on a particular direction, as.

The measured spectra are rather typical for terrestrial silicates.All samples have low reflectance in the infrared range 7–50 μm. In this region the features associated with the Si–O stretching and O–Si–O bending vibration bands (the reststrahlen bands) are observed (Fig.

11, Fig. 12, Fig. 13).These fundamental bands are dominated by surface scattering, which is why the. Abstract. The present paper describes the detailed analysis of the spectral reflection properties of skin surface with make-up foundation, based on two approaches of a physical model using the Cook-Torrance model and a statistical approach using the PCA.

Cihlaret al., ; Gutman et al., ]. Most land surfaces reflect incident radiation anisotropically. Anisotropic prop-erties are described by the surface bidirectional reflectance distribution function (BRDF) [Nicodemus et al., ]. An accurate determination of surface BRDF properties is essential because they are directly related to the.

1 Spectral reflectance: When the solar radiation is incident upon the earth’s surface, it is either reflected by the surface, transmitted into the surface or absorbed and emitted by the surface.

Remote sensing is based on the measurement of reflected or emitted radiations. •Reflectance peaks occur at about μmand μm, between the absorption bands •Throughout the range beyond μm, leaf reflectance is approximately inversely related to the total water present in a leaf which is a function of both the moisture content and the thickness of a leaf.

Thomas H. Painter, Felix C. Seidel, Ann C. Bryant, S. McKenzie Skiles and Karl Rittger, Imaging spectroscopy of albedo and radiative forcing by light‐absorbing impurities in mountain snow, Journal of Geophysical Research: Atmospheres,17, (), ().

The surface reflectance may then be viewed as a combi- nation of two different components representative of these two different bidirectional signatures.

First is a component of diffuse reflection by matedhal surfaces, of reflectance Pgeom, which takes into account the geometrical structure of opaque reflectors and shadowing effects. Attenuated Total Reflectance Spectroscopy of Polymers: Theory and Practice (Polymer Surfaces and Interfaces Series) [Urban, Marek W.] on *FREE* shipping on qualifying offers.

Attenuated Total Reflectance Spectroscopy of Polymers: Theory and Author: Marek W. Urban.MEASUREMENT OF THE SPECIFIC SURFACE AREA OF CLAYS BY INTERNAL REFLECTANCE SPECTROSCOPY 1 D.

J. MULLA, 2 P. F. LOw, AND C. B. ROTH Department of Agronomy, Purdue University West Lafayette, Indiana Abstract--The specific surface area, S, of a clay is commonly measured by the adsorption of ethylene.A GUIDE TO REFLECTANCE COATINGS AND MATERIALS 5 Duraflect Reflectance Coating Duraflect is a proprietary white reflectance coating for use where hostile environments, weathering and wear may affect a coating, yet high lambertian reflectance is required.

Duraflect is generally used in applications in the visible to the very near.