Measurement of Thermal Radiation of Properties of Solids PDF Download
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Author: Joseph C. Richmond
Publisher:
ISBN:
Category : Materials
Languages : en
Pages : 608
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Book Description
Author: Joseph C. Richmond
Publisher:
ISBN:
Category : Materials
Languages : en
Pages : 608
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Book Description
Author: A. L. Greig
Publisher:
ISBN:
Category : Nevada National Security Site (Nev.)
Languages : en
Pages : 36
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Book Description
Author: David P. DeWitt
Publisher: John Wiley & Sons
ISBN: 9780471610182
Category : Technology & Engineering
Languages : en
Pages : 1156
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Book Description
Here is the most comprehensive treatment available on practical temperature measurement methods using radiation thermometry. All aspects of measurement technology are covered: basic principles, types of radiation thermometers, calibration methods, and applications. Covers the latest instruments and discusses the central problem of radiation thermometry--how to infer the true temperature from the indicated temperature. Generously illustrated.
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 97
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Book Description
Basic thermal-radiation measurements, comprising total and broad-band spectral distribution of radiant energy, radiant energy function of field of view of the measuring instrument, and total radiant power versus time, are reported for the second thermal pulse of Shots 1, 2, 3, 5, 6, 9, and 10. All data were taken from ground stations at ranges as close as feasible to the detonations. The data are reported and analyzed to obtain the total thermal energy, the total thermal emission per unit of time, fireball sizes and geometries, and color and power temperatures, all as a function of time. New methods of analysis are used that show promise of correlating the thermal characteristics of the fireball with burst parameters. The new methods result in significantly higher thermal yields in all cases. Significant differences are shown in the thermal properties of tower and air bursts. The air bursts have higher thermal yields, higher peak temperatures, and different pulse shapes than tower bursts. The thermal properties of an air burst are shown to vary with altitude. The higher the altitude, the shorter the time scale, the larger the fireball, and the lower the total thermal energy. The peak temperature is little changed.
Author: Joseph C. Richmond
Publisher:
ISBN:
Category : Materials
Languages : en
Pages : 616
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Book Description
Author: Lawrence Davis
Publisher:
ISBN:
Category : Physics
Languages : en
Pages : 590
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Book Description
"Body Physics was designed to meet the objectives of a one-term high school or freshman level course in physical science, typically designed to provide non-science majors and undeclared students with exposure to the most basic principles in physics while fulfilling a science-with-lab core requirement. The content level is aimed at students taking their first college science course, whether or not they are planning to major in science. However, with minor supplementation by other resources, such as OpenStax College Physics, this textbook could easily be used as the primary resource in 200-level introductory courses. Chapters that may be more appropriate for physics courses than for general science courses are noted with an asterisk symbol (*). Of course this textbook could be used to supplement other primary resources in any physics course covering mechanics and thermodynamics"--Textbook Web page.
Author: Douglas M. Burch
Publisher:
ISBN:
Category : Heat
Languages : en
Pages : 60
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Book Description
Author: Joseph C. Richmond
Publisher:
ISBN:
Category : Materials
Languages : en
Pages : 624
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Book Description
Author: United States. Air Force. Systems Command
Publisher:
ISBN:
Category : Heat
Languages : en
Pages : 587
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Book Description
Author: William R. Bandeen
Publisher:
ISBN:
Category : Infrared radiation
Languages : en
Pages : 40
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Book Description
In the TIROS II, the satellite's spin provides the scan line of the medium resolution radiometer which is then advanced by the orbital motion. The spatial resolution is about 40 miles square when the earth directly beneath the satellite is viewed. The five channels employ bolometer detectors and filters to limit the spectral responses to five bands: 6 to 6.5 microns, 8 to 12 microns, 0.2 to 6 microns, 8 to 30 microns, and 0.55 to 0.75 microns. These five bands study, respectively: radiation in the water vapor absorption band; day and nighttime cloud cover; albedo thermal radiation; and visual maps for comparison with satellite vidicon pictures. The low resolution non-scanning radiometer measures the earth's blackbody temperature and albedo. This radiometer consists of two thermistors, each in the apex of a reflective cone which provides optical gain. One thermistor is black and responds to both ther al and reflected solar radiation. The second responds to thermal but reflects solar radiation. (Author).
