Tutorial 2a: Energy flow-paths Q1. Give 3 reasons why two different walls of the same U-value might give rise to substantially different energy requirements.

Slides:



Advertisements
Similar presentations
Common Terminology Emittance Winter U-Factor or U-Value R-Value
Advertisements

1.2 Transfer Processes Conduction Convection
The Three Tiered Philosophy
Atmospheric Stability
Chapter 5: Designing for Heating and Cooling 5.1 Organizing the problem a) Fenestration How much is optimum for the building? What should the form of the.
In the Atmosphere Thermal Energy Transfer. Temperature and Thermal Energy TEMPERATURE - a measure of the average kinetic energy of the individual particles.
Photosynthetically-active radiation (spectral portion, CI) h h h h h h h h.
Atmospheric Analysis Lecture 3.
What happens to solar energy ? 1.Absorption (absorptivity=  ) Results in conduction, convection and long-wave emission 2.Transmission (transmissivity=
Atmospheric Analysis Lecture 2.
MET 10: Chapter 2 Warming the Earth and Atmosphere Dr. Craig Clements San José State University.
Windows. Huge variety of available building components and several important roles Thermally most important they admit solar radiation Advantageous in.
Thermal Energy Chapter 14. Key Ideas  What does temperature have to do with energy?  What makes things feel hot or cold?  What affects the rate that.
PASSIVE SOLAR DESIGN. Design Techniques
Solar Radiation And it’s General Applications Nitin Jayswal.
AOS 100 Lecture 3 Atmospheric Variables Chapter 1 Homework #1 Due September 19, 2014 TYU Ch1: 3,4,5,8,11,13,16,19; TYPSS Ch 1: 1 TYU Ch 2: 1,2,6,9,13,16,20,22,23,25;
Energy and Heat Transfer. Objectives Comprehend Forms of energy Energy conversion Heat transfer processes Principles of operation of various heat exchangers.
Objectives Explain how radiant energy reaches Earth.
Tutorial 4: Response function method Q1. Outline the calculation steps of a time domain response function method. 1. A given heat transfer equation in.
ASRAE Student Branch meeting Speaker: Kenneth Simpson USGBC – LEED rating system Today at 5 pm ECJ
HVACR416 - Design Heat Loss / Heat Gain Part 1. Why? The primary function of Air Conditioning is to maintain conditions that are… o Conductive to human.
1 ISAT Module III: Building Energy Efficiency Topic 7: Transient Heating and Air Conditioning Loads  Thermal Admittance  Intermittent Heating 
Radiation balance Any object in the Universe which has a temperature above the temperature "absolute zero" ( degrees Fahrenheit or degrees.
Heat Transfer Carlos Silva December 9 th Energy transference Energy can be transferred between a system and its surroundings Work Heat Mass flow.
UNIT THREE: Matter, Energy, and Earth  Chapter 8 Matter and Temperature  Chapter 9 Heat  Chapter 10 Properties of Matter  Chapter 11 Earth’s Atmosphere.
GEOGRAPHY 3015A. IT WAS AN INTERESTING SUMMER!
Lecture Objectives: Discuss –solar radiation and heat transfer through windows –Internal heat loads Introduce Homework Assignment 1b –solve 1/3 of the.
Unit 3 Lesson 3 Energy Transfer
Student Chapter Meeting Thursday, Sept. 3 rd 7pm ECJ Interested in HVAC design, MEP, or building environmental systems? Come learn about all of the.
Lecture 8 Evapotranspiration (1) Evaporation Processes General Comments Physical Characteristics Free Water Surface (the simplest case) Approaches to Evaporation.
Unit 10 Lesson 3 Energy Transfer
Investigation 9B  Key Question: How is convection responsible for the movement of air through the atmosphere?? Convection in Earth’s Atmosphere.
Lecture Objectives: Finish with External Boundary Conditions Introduce Internal Surface Energy Balance.
HEAT 11.2.
Lecture Objectives: Summarize heat transfer review
Weather Elements. Summary from Lesson 2 ____________ is the passage of energy, particularly heat and electricity, through an object. An example is a frying.
Active Solar heating Used for space and or water heating
HW/Tutorial # 1 WRF Chapters 14-15; WWWR Chapters ID Chapters 1-2
MECHANISM OF HEAT TRANSFER.  HEAT TRANSFER  Occurs only between regions that are at different temperature and its direction is always from higher to.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 3 The Earth’s Energy Balance Dr. Eugene Cordero San Jose State University Outline.
Modes of Heat Transfer-1 P M V Subbarao Professor Mechanical Engineering Department Various Possibilities of a Natural Happening ….. Change in Class Room.
Earth’s Energy Budget. Modes of Energy Travel Heat Energy can be transferred in three specific ways: Heat Energy can be transferred in three specific.
How much makes it through the atmosphere. Why a seasonal variation? First, why do we have seasons? Earth’s axis is tilted 23.5° to the plane of its orbit.
HW/Tutorial # 1 WRF Chapters 14-15; WWWR Chapters ID Chapters 1-2 Tutorial #1 WRF#14.12, WWWR #15.26, WRF#14.1, WWWR#15.2, WWWR#15.3, WRF#15.1, WWWR.
Composition of the Atmosphere 14 Atmosphere Characteristics  Weather is constantly changing, and it refers to the state of the atmosphere at any given.
Solar Gain The ultimate free lunch!. Some Basics Why do we need to heat our homes? –Living rooms21 o C –Bedrooms18 o C –Staircases & halls16 o C.
Atmosphere-ocean interactions Exchange of energy between oceans & atmosphere affects character of each In oceans –Atmospheric processes alter salinity.
17 Chapter 17 The Atmosphere: Structure and Temperature.
Heat Transfer Su Yongkang School of Mechanical Engineering # 1 HEAT TRANSFER CHAPTER 6 Introduction to convection.
GCSE ENERGY; THERMAL ENERGY TRANSFER 2
Unit 3 Lesson 2 Energy Transfer Copyright © Houghton Mifflin Harcourt Publishing Company.
Atmosphere Notes. The Atmosphere The Earth's atmosphere is a thin layer of gases that surrounds the Earth. It composed of 78% nitrogen 21% oxygen 0.9%
Unit 3 Lesson 2 Energy Transfer
HW/Tutorial # 1 WRF Chapters 14-15; WWWR Chapters ID Chapters 1-2
Surface Energy Budget, Part I
Energy and Heat Transfer
Thermal mass dynamics 1.00 Heat absorption
Heat.
Unit 3 Lesson 2 Energy Transfer
UNIT - 4 HEAT TRANSFER.
ENERGY IN THE BIOSPHERE
Fundamentals of Heat Transfer
Earth’s Energy Budget.
Earth’s Energy Budget.
Energy Budgets Some parts of the earth receive a lot of solar energy (surplus), some receive less (deficit). In order to transfer this energy around, to.
Environmental Controls
Unit 3 Lesson 2 Energy Transfer
Fundamentals of Heat Transfer
HEAT EXCHANGE IN BUILDINGS. TERMINOLOGIES Thermal conductivity: is the rate of heat flow through a unit area of unit thickness of the material for a unit.
Presentation transcript:

Tutorial 2a: Energy flow-paths Q1. Give 3 reasons why two different walls of the same U-value might give rise to substantially different energy requirements. 1.different thermal capacity; 2.different arrangement of layers; and 3.different layer conductivities. Q2. Describe the principal factors affecting each of the following heat transfer processes within buildings: natural convection at internal surfaces; longwave radiation exchange; infiltration and inter-room air flow; and intra-room air movement. 1.Natural convection: surface-to-air temperature difference, surface roughness, direction of heat flow and characteristic dimensions. 2.Longwave radiation: inter-surface temperature difference, surface emissivity, room geometry and content (dictating view factors), and surface reflection (diffuse, specular or mixed). 3.Infiltration: pressure distribution, leakage distribution, buoyancy forces, and occupant interactions. 4.Intra-room air movement: flow regimes (laminar, turbulent or mixed), boundary temperatures and velocities, distribution of heat flux and momentum inputs, and occupant interactions.

Tutorial 2a: Energy flow-paths Q3. Explain the effect on a room's heating load in winter of applying a low emissivity coating to 1) the inside surface of a double glazed window; and 2) the innermost, cavity-facing surface of the same window. 1.The low-ε coating reduces the longwave flux transfer between the room surfaces and the window and so reduces the overall heat loss. The window inside surface is cold. 2.Now the longwave flux transfer can take place with the window inside surface and transfer, via conduction, to the innermost cavity-facing surface. At this point, the heat loss is arrested because the low-ε coating reduces the radiation exchange across the cavity. Thus, the window inside surface is warmer at the expense of a slightly higher heat loss. Q4. Describe two circumstances in which it would be advisable to model wall conduction in three dimensions. 1.At corners, where dissimilar materials may inter-penetrate or where the the material comprising the corner is a significant proportion of the overall construction and therefore its omission may seriously impact on the result. 2.Where thermal bridges are present such as at the junction of the wall and a window frame.

Tutorial 2a: Energy flow-paths Q5. State the advantages and disadvantages of locating insulation on the innermost position of the walls of a room. Advantages: 1.Hides the thermal capacity of the wall that may otherwise give rise to an increased peak plant demand due to the initial rush of energy to capacity at plant start-up in an intermittent scheme. 2.The risk of surface condensation is lower because the inside surface temperature is likely to remain above the dew point temperature of the adjacent air. Disadvantages: 1.Hides the thermal capacity of the wall that may otherwise help to minimise the peaks and maximise the troughs of plant demand and so promote good load levelling. 2.Solar radiation penetrating windows and striking the internal surface cannot be readily stored in the construction since the insulation will act as a barrier. A space experiencing high solar energy penetration is likely to overheat or need cooling. 3.The risk of interstitial condensation is greater in the case of internally located insulation since a substantial portion of the construction may fall below the dew point temperature of moist air permeating through the construction in the absence of an effective vapour barrier.

Tutorial 2a: Energy flow-paths Q6. Differentiate between long- and short-wave radiation. Shortwave radiation comprises visible light and ultraviolet radiation. Longwave radiation is infrared radiation. While the Sun radiates energy mainly in the form of visible light, with small amounts of ultraviolet and infrared radiation; for this reason solar radiation is usually considered shortwave radiation. The radiation emitted from bodies at terrestrial temperatures is longwave. Q7. When modelling external surface longwave radiation exchange, list five influencing factors that must be taken into account. 1. cloud cover/type; 2. effective sky temperature; 3. temperature of surrounding buildings; 4. ground temperature; and 5. view factors between the surface and the sky, ground and surroundings. Q8. What is the purpose of a passive solar element in the context of building design? Identify some typical elements. The purpose is to capture, store and/or transport energy without recourse to mechanical systems. Examples include: solar control devices, sunspaces, phase change materials, desiccant materials, evaporative cooling, induced ventilation and mass walls.