RULES CERTIFICATE Department of Commerce
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Thermal Conductivity 1 Thermal Conductivity
Thermal conductivity 1 Thermal conductivity In physics, thermal conductivity, , is the property of a material's ability to conduct heat. It appears primarily in Fourier's Law for heat conduction. Thermal conductivity is measured in watts per kelvin-meter (W·K−1·m−1, i.e. W/(K·m) or in IP units (Btu·hr−1·ft−1·F−1, i.e. Btu/(hr·ft⋅F). Multiplied by a temperature difference (in kelvins, K) and an area (in square meters, m2), and divided by a thickness (in meters, m), the thermal conductivity predicts the rate of energy loss (in watts, W) through a piece of material. In the window building industry "thermal conductivity" is expressed as the U-Factor [1], which measures the rate of heat transfer and tells you how well the window insulates. U-factor values are generally recorded in IP units (Btu/(hr·ft⋅F)) and usually range from 0.15 to 1.25. The lower the U-factor, the better the window insulates. The reciprocal of thermal conductivity is thermal resistivity. Measurement There are a number of ways to measure thermal conductivity. Each of these is suitable for a limited range of materials, depending on the thermal properties and the medium temperature. There is a distinction between steady-state and transient techniques. In general, steady-state techniques are useful when the temperature of the material does not change with time. This makes the signal analysis straightforward (steady state implies constant signals). The disadvantage is that a well-engineered experimental setup is usually needed. The Divided Bar (various types) is the most common device used for consolidated rock samples. -
Thermal Metrics for High Performance Enclosure Walls: the Limitations of R-Value
building science.com © 2009 Building Science Press All rights of reproduction in any form reserved. Thermal Metrics for High Performance Enclosure Walls: The Limitations of R-Value Research Report - 0901 2007 John Straube Abstract: This document summarizes the theory behind thermal insulation and building system heat flow control metrics and presents a literature review of selected research into this area. RR-0901: Thermal Metrics for High Performance Enclosure Walls: The Limitations of R-Value Review of the R-value as a Metric for High Thermal Performance Building Enclosures. 1 Introduction The R-value was developed over 50 years ago to provide users and specifiers of insulation with an easy-to-compare, repeatable measure of insulation performance. Everett Schuman, an early director of Penn State’s housing research institute, is often credited with first proposing (in 1945) and popularizing standardized measures of resistance to heat transfer. R-values were later widely applied to industrial and residential insulating materials and helped consumers make more energy-efficient choices. The strength of the R-value is that it is simple to measure, easy to communicate, and widely accepted. Over recent decades a much broader range of insulation types, and application methods of insulation have been developed and deployed than were available when the R-value was conceived. As the building industry strives to reduce energy consumption for environmental and economic reasons, building enclosures with high thermal performance, reliably and affordably installed in the field are demanded. The R-value of the insulation products in many of the new building enclosure systems is increasingly unable to measure their actual thermal performance because system effects, sensitivity to construction defects, and airflow can play such a significant role in overall performance. -
Thermal Properties of Rocks
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY THERMAL PROPERTIES OF ROCKS by Eugene C. Robertson 1 Open-File Report 88-441 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. 1 Reston, Virginia 1988 CONTENTS Page Abstract- 1 Introduction 1 Units------------------- 3 Symbols 4 Thermal conductivity 5 Introduction 5 Solidity 5 Thermal impedance 5 Calculation of composite models - 6 Porefluid - - 8 Quartz, olivine, pyroxene, amphibole, and clay content 8 Rock conductivity at 300 K 10 Introduction 10 Mafic igneous rocks, air in pores 11 Mafic igneous rocks, water in pores 13 Felsic igneous rocks, air or water in pores 14 Limestone, air or water in pores - 16 Dolostone, air or water in pores - 18 Sandstone, air in pores 20 Sandstone, water in pores - 22 Shale, water in pores 24 Shale, air in pores 26 Soils, air in pores - - ~ 28 Anhydrite, gypsum, air in pores 30 Selected rocks 31 Conductivity anisotropy of metamorphic rocks 32 Rock conductivity change with temperature 34 Introduction 34 Basalt and other mafic rocks - 34 Felsic igneous rocks 35 Carbonate rocks 36 Quartz-bearing rocks - 37 Ultramafic rocks - 39 Rock glasses - 40 Mineral conductivity change with temperature 41 Introduction - - 41 Quartz - - - 41 Feldspar - - 42 Plagioclase 43 Mafic silicate minerals 44 Olivine - 46 Calcite and aragonite 47 Halite 48 Mineral conduction mechanisms 49 Phonon and imperfection conductivity 49 Radiative conductivity 49 Analysis of mechanisms - - - . - 50 Miscellaneous thermalconductivities 58 Pressure effect on thermal conductivity 59 Thermal conductivity under vacuum - 62 Thermal expansion and density of minerals - - 65 11 Specific heat of rock 71 Introduction 71 Calculation of specificheat-- -- - - - - - 85 Diffusivity and thermal inertia 88 Calculation ofparameters 88 Heat transfer coefficients 91 Radioactive heat generation in rocks - 96 Appendix I. -
Heat Transfer
CHAPTER 9 Heat Transfer 9.1. INTRODUCTION In the majority of chemical processes heat is either given out or absorbed, and fluids must often be either heated or cooled in a wide range of plant, such as furnaces, evaporators, distillation units, dryers, and reaction vessels where one of the major problems is that of transferring heat at the desired rate. In addition, it may be necessary to prevent the loss of heat from a hot vessel or pipe system. The control of the flow of heat at the desired rate forms one of the most important areas of chemical engineering. Provided that a temperature difference exists between two parts of a system, heat transfer will take place in one or more of three different ways. Conduction. In a solid, the flow of heat by conduction is the result of the transfer of vibrational energy from one molecule to another, and in fluids it occurs in addition as a result of the transfer of kinetic energy. Heat transfer by conduction may also arise from the movement of free electrons, a process which is particularly important with metals and accounts for their high thermal conductivities. Convection. Heat transfer by convection arises from the mixing of elements of fluid. If this mixing occurs as a result of density differences as, for example, when a pool of liquid is heated from below, the process is known as natural convection. If the mixing results from eddy movement in the fluid, for example when a fluid flows through a pipe heated on the outside, it is called forced convection. -
Heat Loss Calculations and Principles
Heat Loss Calculations and Principles Course No: M05-003 Credit: 5 PDH A. Bhatia Continuing Education and Development, Inc. 22 Stonewall Court Woodcliff Lake, NJ 07677 P: (877) 322-5800 [email protected] HVAC HEATING LOSS CALCULATIONS & PRINCIPLES Introduction There are two different but related calculated values of interest to the heating system designer. The first is to estimate the maximum rate of heat loss to properly size the heating equipment (furnace). The second calculated value that must be determined is the annual heating bill. This is determined by calculating the annual energy requirement based from the design heat loss rate. In this course, we will learn to determine the rate at which heat is lost through building elements using a process called heat loss calculation. You will learn how to extrapolate your calculation of a maximum hourly rate into an annual energy usage rate. You will also learn some useful tips on saving heating energy. The section-3 of the course includes one sample example. Factors Affecting Comfort in winter 1. TEMPERATURE difference between the inside and outside of the building is the primary cause of heat loss in the winter months. The greater this difference, the higher the rate of heat loss. Since most buildings are controlled to a constant inside temperature by the occupants, higher heat loss occurs when it is colder outside. This also means that the annual heating bill can be reduced by lowering the setting on the thermostat …. (but only if the occupants agree to it!) 2. WIND is the second greatest source of heat loss during the winter.