Introduction to Forms of Energy
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A Novel and Cost Effective Radiant Heat Flux Gauge This Paper Presents a Patent-Pending Methodology of Measuring Radiation Emiss
A Novel and Cost Effective Radiant Heat Flux Gauge S. Safaei and A. S. Rangwala Department of Fire Protection Engineering, Worcester Polytechnic Institution, Worcester, MA, 01609, USA V. Raghavan Department of Mechanical Engineering Indian Institute of Technology Madras, Chennai, India T.M. Muruganandam, Department of Aerospace Engineering, National Center for Combustion Research and Development, Indian Institute of Technology Madras, Chennai, India This paper presents a patent-pending methodology of measuring radiation emissions from fires, for the purposes of more practical optical flame detection and analysis. Flame radiation comprises of three phenomena: chemiluminescence, photoluminescence, and thermal radiation. The first two types are caused by elementary breakdown reactions of the reactants and the molecular excitations of products such as H2O and CO2, respectively. These emissions are within narrow bands of electromagnetic radiation wavelengths, and due to their specific molecular physics, are largely fuel dependant. The third type, thermal radiation emissions come from high temperature soot, which is a blanket term for any carbonaceous intermittent species of the combustion reaction. The amount and temperature of soot is case-specific, as it is influenced by fuel type, geometries, fuel-oxidizer premixing and the resulting level of combustion efficiency. However since naturally occurring fire hazards are diffusion flames, soot is present in high quantities and the majority of the radiation can be attributed to soot alone [1 – 2]. These soot emissions are over large ranges of the electromagnetic spectrum, from ultraviolet all the way to Long wave Infrared (LWIR), following the classic Planck Law for Blackbody emitters. This distribution of radiant energy, E, is highly dependent on the temperature of the emitter, T, due to its exponential relation E=T4. -
Low Cost Solar Thermoelectric Water Floating Device to Supply Measurement Platform
78 IAPGOŚ 4/2019 p-ISSN 2083-0157, e-ISSN 2391-6761 DOI: 10.35784/IAPGOS.734 LOW COST SOLAR THERMOELECTRIC WATER FLOATING DEVICE TO SUPPLY MEASUREMENT PLATFORM Andrzej Nowrot1, Monika Mikołajczyk2, Anna Manowska1, Joachim Pielot1, Antoni Wojaczek1 1Silesian University of Technology, Department of Electrical Engineering and Automation in Industry, Gliwice, Poland, 2Famur Institute Ltd, Katowice, Poland Abstract. This work presents the prototype of the solar – thermoelectric device, which can float on water surface. It produces electrical energy as a result of the Seebeck effect in a commercial, low-cost Peltier module. The main application of the device will be an autonomous and a floating measurement platform. An important advantage of the presented solution is the possibility to work alike at day, when a solar light heats the surface of the absorber, and at night, when the different of temperatures between air and water causes the heat flux and in an effect the electricity. The device is capable of working for many cloudy days and also in winter on very short days. The presented device is based on low-cost and widely available components. Keywords: thermoelectric devices, solar power generation, energy conversion TERMOELEKTRYCZNE URZĄDZENIE SOLARNE DO ZASILANIA PLATFORMY POMIAROWEJ Streszczenie. W pracy zaprezentowano prototypowe solarne urządzenie termoelektryczne pływające po powierzchni wody. Wytwarza ono w niedrogim, komercyjnym module Peltiera energię elektryczną w wyniku zachodzącego w nim zjawiska Seebecka. Docelowo głównym obszarem aplikacyjnym urządzenia będzie zasilanie autonomicznej, pływającej platformy pomiarowa do monitorowania parametrów środowiskowych. Istotną zaletą przedstawionego rozwiązania jest możliwość pracy zarówno w dzień, gdy światło słoneczne ogrzewa powierzchnię absorbera, jak również w nocy, gdy różnica temperatur między powietrzem a wodą powoduje powstawanie strumienia ciepła w module Peltiera. -
United States Patent [191 4,2313J97 Sher
United States Patent [191 4,2313J97 Sher [54] RADIANT ENERGY TO ELECTRIC ENERGY 4,084,101 4/1978 Sher ..................................... 290/1 R CONVERTER 4,096,393 6/1978 Sher ..................................... 290A R [76] Inventor: Arden Sher, 108 Charles River OTHER PUBLICATIONS Landing Rd., Williamsburg, Va. R. Solomon et al., “Polarization in LaF,”, J. Appl. Phys., 23185 VO~.37, pp. 3427-3432, (1966). [ * 3 Notice: The portion of the term of this patent A. Sher et al., “Transport Properties of LaF3”, Phys. subsequent to Apr. 11,1995, has been Rev., vol. 144, pp. 593-604, (1966). disclaimed. J. E. Drummond, “Electrical Power Conversion”, IECEC Record ’75, pp. 569-575. [21] Appl. No.: 889,514 S. B. Skinner, “Thermodielectric Energy Conversion [22] Filed: Mar. 23,1978 by Thin Films: Experiment & Theory”, Intersociety Energy Conv. Eng. Con$, (1967), pp. 865-873. Related U.S. Application Data A. Sher et al., “LaF3 Infrared Detector”, Appl. Phys. Lett., vol. 28, pp. 676-678, (1976). [63] Continuation-in-part of Ser. No. 631,689, Nov. 13, 1975, Pat. No. 4,084,101. Primary Examiner-Aaron Weisstuch Attorney, Agent, or Firm-Lowe, King, Price and [51] Int. Cl.2 ............................................. HQlL31/Q4 Becker [52] U.S. Cl. ............................... 136/89 SP; 290/1 R 361/280; 361/282; 310/308; 310/309; 250/211 1571 ABSTRACT 250/212; 250/336 R; Radiant energy is converted into electric energy by [58] Field of Search ............ 136/89 R, 89 NB, 89 SP; irradiating a capacitor including an ionic dielectric. The 250/211 R, 212, 336; 290/1 R 361/280,282; 310/308, 309 dielectric is a sintered crystal superionic conductor, e.g., lanthanum trifluoride, lanthanum trichloride, or [561 References Cited silver bromide, so that a multiplicity of crystallites exist U.S. -
Energy Literacy Essential Principles and Fundamental Concepts for Energy Education
Energy Literacy Essential Principles and Fundamental Concepts for Energy Education A Framework for Energy Education for Learners of All Ages About This Guide Energy Literacy: Essential Principles and Intended use of this document as a guide includes, Fundamental Concepts for Energy Education but is not limited to, formal and informal energy presents energy concepts that, if understood and education, standards development, curriculum applied, will help individuals and communities design, assessment development, make informed energy decisions. and educator trainings. Energy is an inherently interdisciplinary topic. Development of this guide began at a workshop Concepts fundamental to understanding energy sponsored by the Department of Energy (DOE) arise in nearly all, if not all, academic disciplines. and the American Association for the Advancement This guide is intended to be used across of Science (AAAS) in the fall of 2010. Multiple disciplines. Both an integrated and systems-based federal agencies, non-governmental organizations, approach to understanding energy are strongly and numerous individuals contributed to the encouraged. development through an extensive review and comment process. Discussion and information Energy Literacy: Essential Principles and gathered at AAAS, WestEd, and DOE-sponsored Fundamental Concepts for Energy Education Energy Literacy workshops in the spring of 2011 identifies seven Essential Principles and a set of contributed substantially to the refinement of Fundamental Concepts to support each principle. the guide. This guide does not seek to identify all areas of energy understanding, but rather to focus on those To download this guide and related documents, that are essential for all citizens. The Fundamental visit www.globalchange.gov. Concepts have been drawn, in part, from existing education standards and benchmarks. -
LESSON 1 What Is Energy?
LESSON 1 What is Energy? Overview In this lesson students review what they know about energy in everyday life, define it, learn the different energy forms through play, and differentiate between potential and kinetic energy. Student • I can use my own words to show I understand “energy.” Learning • I can describe the main forms of energy and give examples. Targets • I can show potential and kinetic energy with my body and I can give examples of each. • I can give examples of how I use energy every day. NGSS MS-PS3-5. Construct, use, and present arguments to support the claim that when the kinetic energy of an object changes, energy is transferred to or from the object. [Clarification Statement: Examples of empirical evidence used in arguments could include an inventory or other representation of the energy before and after the transfer in the form of temperature changes or motion of object.] [Assessment Boundary: Assessment does not include calculations of energy.] Background Energy is part of everything that happens in the world and everything we do. Energy can be in the form of heat, light, gravity, sound, motion, chemical reactions, or electricity. Energy is the ability to do work or make a change. Nine forms of energy: (see Overhead 1 “Forms of Energy”) • Chemical: Chemical energy is the energy stored in the bonds of atoms and molecules. Biomass, petroleum, natural gas, propane and coal are examples of stored chemical energy. • Nuclear: Nuclear energy is the energy stored in the nucleus of an atom. It is the energy that holds the nucleus together. -
Estimation of the Dissipation Rate of Turbulent Kinetic Energy: a Review
Chemical Engineering Science 229 (2021) 116133 Contents lists available at ScienceDirect Chemical Engineering Science journal homepage: www.elsevier.com/locate/ces Review Estimation of the dissipation rate of turbulent kinetic energy: A review ⇑ Guichao Wang a, , Fan Yang a,KeWua, Yongfeng Ma b, Cheng Peng c, Tianshu Liu d, ⇑ Lian-Ping Wang b,c, a SUSTech Academy for Advanced Interdisciplinary Studies, Southern University of Science and Technology, Shenzhen 518055, PR China b Guangdong Provincial Key Laboratory of Turbulence Research and Applications, Center for Complex Flows and Soft Matter Research and Department of Mechanics and Aerospace Engineering, Southern University of Science and Technology, Shenzhen 518055, Guangdong, China c Department of Mechanical Engineering, 126 Spencer Laboratory, University of Delaware, Newark, DE 19716-3140, USA d Department of Mechanical and Aeronautical Engineering, Western Michigan University, Kalamazoo, MI 49008, USA highlights Estimate of turbulent dissipation rate is reviewed. Experimental works are summarized in highlight of spatial/temporal resolution. Data processing methods are compared. Future directions in estimating turbulent dissipation rate are discussed. article info abstract Article history: A comprehensive literature review on the estimation of the dissipation rate of turbulent kinetic energy is Received 8 July 2020 presented to assess the current state of knowledge available in this area. Experimental techniques (hot Received in revised form 27 August 2020 wires, LDV, PIV and PTV) reported on the measurements of turbulent dissipation rate have been critically Accepted 8 September 2020 analyzed with respect to the velocity processing methods. Traditional hot wires and LDV are both a point- Available online 12 September 2020 based measurement technique with high temporal resolution and Taylor’s frozen hypothesis is generally required to transfer temporal velocity fluctuations into spatial velocity fluctuations in turbulent flows. -
Turbulence Kinetic Energy Budgets and Dissipation Rates in Disturbed Stable Boundary Layers
4.9 TURBULENCE KINETIC ENERGY BUDGETS AND DISSIPATION RATES IN DISTURBED STABLE BOUNDARY LAYERS Julie K. Lundquist*1, Mark Piper2, and Branko Kosovi1 1Atmospheric Science Division Lawrence Livermore National Laboratory, Livermore, CA, 94550 2Program in Atmospheric and Oceanic Science, University of Colorado at Boulder 1. INTRODUCTION situated in gently rolling farmland in eastern Kansas, with a homogeneous fetch to the An important parameter in the numerical northwest. The ASTER facility, operated by the simulation of atmospheric boundary layers is the National Center for Atmospheric Research (NCAR) dissipation length scale, lε. It is especially Atmospheric Technology Division, was deployed to important in weakly to moderately stable collect turbulence data. The ASTER sonic conditions, in which a tenuous balance between anemometers were used to compute turbulence shear production of turbulence, buoyant statistics for the three velocity components and destruction of turbulence, and turbulent dissipation used to estimate dissipation rate. is maintained. In large-scale models, the A dry Arctic cold front passed the dissipation rate is often parameterized using a MICROFRONTS site at approximately 0237 UTC diagnostic equation based on the production of (2037 LST) 20 March 1995, two hours after local turbulent kinetic energy (TKE) and an estimate of sunset at 1839 LST. Time series spanning the the dissipation length scale. Proper period 0000-0600 UTC are shown in Figure 1.The parameterization of the dissipation length scale 6-hr time period was chosen because it allows from experimental data requires accurate time for the front to completely pass the estimation of the rate of dissipation of TKE from instrumented tower, with time on either side to experimental data. -
STARS in HYDROSTATIC EQUILIBRIUM Gravitational Energy
STARS IN HYDROSTATIC EQUILIBRIUM Gravitational energy and hydrostatic equilibrium We shall consider stars in a hydrostatic equilibrium, but not necessarily in a thermal equilibrium. Let us define some terms: U = kinetic, or in general internal energy density [ erg cm −3], (eql.1a) U u ≡ erg g −1 , (eql.1b) ρ R M 2 Eth ≡ U4πr dr = u dMr = thermal energy of a star, [erg], (eql.1c) Z Z 0 0 M GM dM Ω= − r r = gravitational energy of a star, [erg], (eql.1d) Z r 0 Etot = Eth +Ω = total energy of a star , [erg] . (eql.1e) We shall use the equation of hydrostatic equilibrium dP GM = − r ρ, (eql.2) dr r and the relation between the mass and radius dM r =4πr2ρ, (eql.3) dr to find a relations between thermal and gravitational energy of a star. As we shall be changing variables many times we shall adopt a convention of using ”c” as a symbol of a stellar center and the lower limit of an integral, and ”s” as a symbol of a stellar surface and the upper limit of an integral. We shall be transforming an integral formula (eql.1d) so, as to relate it to (eql.1c) : s s s GM dM GM GM ρ Ω= − r r = − r 4πr2ρdr = − r 4πr3dr = (eql.4) Z r Z r Z r2 c c c s s s dP s 4πr3dr = 4πr3dP =4πr3P − 12πr2P dr = Z dr Z c Z c c c s −3 P 4πr2dr =Ω. Z c Our final result: gravitational energy of a star in a hydrostatic equilibrium is equal to three times the integral of pressure within the star over its entire volume. -
Energy Conservation in a Spring
Part II: Energy Conservation in a Spring Activity 4 Title: Forces and Energy in a Spring Summary: Students will use the “Masses and Springs” simulation from PhET to investigate the relationship between gravitational potential energy, spring potential energy, and mass. Standard: PS2 (Ext) - 5 Students demonstrate an understanding of energy by… 5aa Identifying, measuring, calculating and analyzing qualitative and quantitative relationships associated with energy transfer or energy transformation. Specific Learning Goals: 1. Understand how to calculate the force constant of a spring using the formula F = -k ∆x 2. Understand that even though energy is transformed during the oscillation of a spring among gravitational potential energy, elastic potential energy, and kinetic energy, the total energy in the system remains constant. 3. Understand how to calculate the gravitational potential energy for a mass which is lifted to a height above a table. 4. Understand how to calculate the elastic potential energy for a spring which has been displaced by a certain distance. Prior Knowledge: 1. The restoring force that a spring exerts on a mass is proportional to the displacement of the spring and the spring constant and is in a direction opposite the displacement: F = -k ∆x 2. Gravitational potential energy is calculated by the formula: PEg = mgΔh 2 3. Elastic potential energy is calculated by the formula: PEs = ½ k ∆x 4. In a mass and spring system at equilibrium, the restoring force is equal to the gravitational force on the suspended mass (Fg = mg) Schedule: 40-50 minutes Materials: “Masses and Springs 2.02 PhET” Engage: Three different masses are suspended from a spring. -
Work and Energy Summary Sheet Chapter 6
Work and Energy Summary Sheet Chapter 6 Work: work is done when a force is applied to a mass through a displacement or W=Fd. The force and the displacement must be parallel to one another in order for work to be done. F (N) W =(Fcosθ)d F If the force is not parallel to The area of a force vs. the displacement, then the displacement graph + W component of the force that represents the work θ d (m) is parallel must be found. done by the varying - W d force. Signs and Units for Work Work is a scalar but it can be positive or negative. Units of Work F d W = + (Ex: pitcher throwing ball) 1 N•m = 1 J (Joule) F d W = - (Ex. catcher catching ball) Note: N = kg m/s2 • Work – Energy Principle Hooke’s Law x The work done on an object is equal to its change F = kx in kinetic energy. F F is the applied force. 2 2 x W = ΔEk = ½ mvf – ½ mvi x is the change in length. k is the spring constant. F Energy Defined Units Energy is the ability to do work. Same as work: 1 N•m = 1 J (Joule) Kinetic Energy Potential Energy Potential energy is stored energy due to a system’s shape, position, or Kinetic energy is the energy of state. motion. If a mass has velocity, Gravitational PE Elastic (Spring) PE then it has KE 2 Mass with height Stretch/compress elastic material Ek = ½ mv 2 EG = mgh EE = ½ kx To measure the change in KE Change in E use: G Change in ES 2 2 2 2 ΔEk = ½ mvf – ½ mvi ΔEG = mghf – mghi ΔEE = ½ kxf – ½ kxi Conservation of Energy “The total energy is neither increased nor decreased in any process. -
Potential Energy
Potential Energy • So far: Considered all forces equal, calculate work done by net force only => Change in kinetic energy. – Analogy: Pure Cash Economy • But: Some forces seem to be able to “store” the work for you (when they do negative work) and “give back” the same amount (when they do positive work). – Analogy: Bank Account. You pay money in (ending up with less cash) - the money is stored for you - you can withdraw it again (get cash back) • These forces are called “conservative” (they conserve your work/money for you) Potential Energy - Example • Car moving up ramp: Weight does negative work ΔW(grav) = -mgΔh • Depends only on initial and final position • Can be retrieved as positive work on the way back down • Two ways to describe it: 1) No net work done on car on way up F Pull 2) Pulling force does positive F Normal y work that is stored as gravitational x potential energy ΔU = -ΔW(grav) α F Weight Total Mechanical Energy • Dimension: Same as Work Unit: Nm = J (Joule) Symbol: E = K.E. + U 1) Specify all external *) forces acting on a system 2) Multiply displacement in the direction of the net external force with that force: ΔWext = F Δs cosφ 3) Set equal to change in total energy: m 2 m 2 ΔE = /2vf - /2vi + ΔU = ΔWext ΔU = -Wint *) We consider all non-conservative forces as external, plus all forces that we don’t want to include in the system. Example: Gravitational Potential Energy *) • I. Motion in vertical (y-) direction only: "U = #Wgrav = mg"y • External force: Lift mass m from height y i to height y f (without increasing velocity) => Work gets stored as gravitational potential energy ΔU = mg (yf -yi)= mg Δy ! • Free fall (no external force): Total energy conserved, change in kinetic energy compensated by change in m 2 potential energy ΔK.E. -
How Long Would the Sun Shine? Fuel = Gravitational Energy? Fuel
How long would the Sun shine? Fuel = Gravitational Energy? • The mass of the Sun is M = 2 x 1030 kg. • The Sun needs fuel to shine. – The amount of the fuel should be related to the amount of – The Sun shines by consuming the fuel -- it generates energy mass. from the fuel. • Gravity can generate energy. • The lifetime of the Sun is determined by – A falling body acquires velocity from gravity. – How fast the Sun consumes the fuel, and – Gravitational energy = (3/5)GM2/R – How much fuel the Sun contains. – The radius of the Sun: R = 700 million m • How fast does the Sun consume the fuel? – Gravitational energy of the Sun = 2.3 x 1041 Joules. – Energy radiated per second is called the “luminosity”, which • How long could the Sun shine on gravitational energy? is in units of watts. – Lifetime = (Amount of Fuel)/(How Fast the Fuel is – The solar luminosity is about 3.8 x 1026 Watts. Consumed) 41 26 • Watts = Joules per second – Lifetime = (2.3 x 10 Joules)/(3.8 x 10 Joules per second) = 0.6 x 1015 seconds. • Compare it with a light bulb! – Therefore, the Sun lasts for 20 million years (Helmholtz in • What is the fuel?? 1854; Kelvin in 1887), if gravity is the fuel. Fuel = Nuclear Energy Burning Hydrogen: p-p chain • Einstein’s Energy Formula: E=Mc2 1 1 2 + – The mass itself can be the source of energy. • H + H -> H + e + !e 2 1 3 • If the Sun could convert all of its mass into energy by • H + H -> He + " E=Mc2… • 3He + 3He -> 4He + 1H + 1H – Mass energy = 1.8 x 1047 Joules.