Energy flows and modelling approaches

Similar documents
AR/IA 241 LN 231 Lecture 4: Fundamental of Energy

Calculating equation coefficients

Chapter 1 INTRODUCTION AND BASIC CONCEPTS

The energy performance of an airflow window

ERT 460 CONTROLLED ENVIRONMENT DESIGN II HEAT TRANSFER. En Mohd Khairul Rabani Bin Hashim

Energy Simulation in Building Design

Applied Thermodynamics HEAT TRANSFER. Introduction What and How?

Energy, Temperature, & Heat. Energy, Temperature, & Heat. Temperature Scales 1/17/11

Radiative Equilibrium Models. Solar radiation reflected by the earth back to space. Solar radiation absorbed by the earth

The inputs and outputs of energy within the earth-atmosphere system that determines the net energy available for surface processes is the Energy

STUDY OF A PASSIVE SOLAR WINTER HEATING SYSTEM BASED ON TROMBE WALL

5. AN INTRODUCTION TO BUILDING PHYSICS

- matter-energy interactions. - global radiation balance. Further Reading: Chapter 04 of the text book. Outline. - shortwave radiation balance

TREES Training for Renovated Energy Efficient Social housing

Cooling of Electronics Lecture 2

Transient Analysis of the Buoyancy Driven Flow in a Passive Solar System for Indoor Heating

5. Thermal Design. Objective: Control heat flow to: Maintain comfortable indoor conditions

Simplified Collector Performance Model

Greenhouse Steady State Energy Balance Model

Autumn 2005 THERMODYNAMICS. Time: 3 Hours

Institut national des sciences appliquées de Strasbourg GENIE CLIMATIQUE ET ENERGETIQUE APPENDICES

Response function method

Earth s Energy Budget: How Is the Temperature of Earth Controlled?

A SIMPLE MODEL FOR THE DYNAMIC COMPUTATION OF BUILDING HEATING AND COOLING DEMAND. Kai Sirén AALTO UNIVERSITY

A) usually less B) dark colored and rough D) light colored with a smooth surface A) transparency of the atmosphere D) rough, black surface

Energy and Radiation. GEOG/ENST 2331 Lecture 3 Ahrens: Chapter 2

ADVANCED ROOF COATINGS: MATERIALS AND THEIR APPLICATIONS

Radiation and the atmosphere

Thermal mass vs. thermal response factors: determining optimal geometrical properties and envelope assemblies of building materials

CAE 331/513 Building Science Fall 2016

ARCH 348 BUILDING AND ENVIRONMENTAL SYSTEMS

Orientation of Building

Glazing selection for solar design

Absorptivity, Reflectivity, and Transmissivity

Calculating equation coefficients

Mechanical Engineering. Postal Correspondence Course HEAT TRANSFER. GATE, IES & PSUs

Energy and Insolation Review 2

Heat and Mass Transfer Unit-1 Conduction

Name(s) Period Date. Earth s Energy Budget: How Is the Temperature of Earth Controlled?

Numerical Analysis of Comfort and Energy Performance of Radiant Heat Emission Systems

Spectrum of Radiation. Importance of Radiation Transfer. Radiation Intensity and Wavelength. Lecture 3: Atmospheric Radiative Transfer and Climate

Lecture # 04 January 27, 2010, Wednesday Energy & Radiation

Lecture 3: Atmospheric Radiative Transfer and Climate

Topic 5 Practice Test

Thermal behavior and Energetic Dispersals of the Human Body under Various Indoor Air Temperatures at 50% Relative Humidity

Chapter 11. Energy in Thermal Processes

Effect of moisture transfer on heat energy storage in simple layer walls

Outline. Stock Flow and temperature. Earth as a black body. Equation models for earth s temperature. Balancing earth s energy flows.

Chapter 3- Energy Balance and Temperature

ApacheLoads Calculation Methodology as used in Revit MEP 2008 <Virtual Environment> 5.7

Chapter 2 Solar and Infrared Radiation

Winter Night. Thermos 6mm Outdoors # #

INTRODUCTION Radiation differs from conduction and convection in that it does not require the presence of a material medium to take place.

Solar Flat Plate Thermal Collector

PAPER 2 THEORY QUESTIONS

CAE 463/524 Building Enclosure Design Fall 2012

1.0 BACKGROUND 1.1 Surface Radiation

INVESTIGATING GLAZING SYSTEM SIMULATED RESULTS WITH REAL MEASUREMENTS

Lecture 4: Heat, and Radiation

2. What does a mercury barometer measure? Describe this device and explain how it physically works.

WUFI Workshop NBI / SINTEF 2008 Radiation Effects On Exterior Surfaces

Chapter 2. Heating Earth's Surface & Atmosphere

Law of Heat Transfer

Chapter Seven. Solar Energy

Double-Skin Facade in Low-Latitude: Study on the Absorptance, Reflectance, and Transmittance of Direct Solar Radiation

HEAT TRANSFER 1 INTRODUCTION AND BASIC CONCEPTS 5 2 CONDUCTION

THE EFFECTS OF CALORIMETER TILT ON THE INWARD-FLOWING FRACTION OF ABSORBED SOLAR RADIATION IN A VENETIAN BLIND

- global radiative energy balance

Chapter 3. Multiple Choice Questions

Lecture 4: Radiation Transfer

Chapter 02 Energy and Matter in the Atmosphere

( 1 d 2 ) (Inverse Square law);

Chapter 3. Basic Principles. Contents

LECTURE NOTES. Heat Transfer. III B. Tech II Semester (JNTUA-R15) CHADALAWADA RAMANAMMA ENGINEERING COLLEGE (AUTONOMOUS)

ATMOSPHERIC ENERGY and GLOBAL TEMPERATURES. Physical Geography (Geog. 300) Prof. Hugh Howard American River College

Prototype Heat Island Application

ME 476 Solar Energy UNIT TWO THERMAL RADIATION

Design of predictive control strategies for active BITES systems using frequency domain models

Lecture 2: Global Energy Cycle

Lecture 4: Global Energy Balance

Lecture 4: Global Energy Balance. Global Energy Balance. Solar Flux and Flux Density. Blackbody Radiation Layer Model.

NUMERICAL ANALYSIS OF HEAT STORAGE AND HEAT CONDUCTIVITY IN THE CONCRETE HOLLOW CORE DECK ELEMENT

Energy Balance and Temperature. Ch. 3: Energy Balance. Ch. 3: Temperature. Controls of Temperature

Energy Balance and Temperature

Chapter 11. Energy in Thermal Processes

Arctice Engineering Module 3a Page 1 of 32

The Atmosphere and Atmospheric Energy Chapter 3 and 4

Simultaneous Conduction and Radiation Energy Transfer

UNIT FOUR SOLAR COLLECTORS

FUNDAMENTALS OF HVAC

Optimization of the Air Gap Spacing In a Solar Water Heater with Double Glass Cover

1. Radiative Transfer. 2. Spectrum of Radiation. 3. Definitions

Table of Contents. Chapter: Atmosphere. Section 1: Earth's Atmosphere. Section 2: Energy Transfer in the Atmosphere. Section 3: Air Movement

Atmospheric Radiation

Global Energy Balance. GEOG/ENST 2331: Lecture 4 Ahrens: Chapter 2

University of New Mexico Mechanical Engineering Spring 2012 PhD qualifying examination Heat Transfer

Fundamentals of WUFI-Plus WUFI Workshop NTNU / SINTEF 2008

EXPERIMENTAL ANALYSIS OF AIR-CONDITIONING IN HOSPITAL ROOMS BY MEANS OF LIGHT RADIANT CEILINGS

Radiation, Sensible Heat Flux and Evapotranspiration

WUFI Workshop at NTNU /SINTEF Fundamentals

Transcription:

Energy flows and modelling approaches

Energy flows in buildings external convection infiltration & ventilation diffuse solar external long-wave radiation to sky and ground local generation fabric heat storage casual gains internal long wave radiation transfer radiative/ convective plant thermal storage Solar on transparent sensible & latent gains internal convection conduction reflection ground exchange Solar on opaque

Energy flows in plant and systems Buildings and systems are strongly coupled and must be handled simultaneously. Plant components can be treated in the same manner as building zones.

New and renewables energy systems Future cities may well have a greater level of new and renewable energy systems deployment. Distributed generation with the grid connection of medium-tolarge scale hydro stations, bio-gas plant and wind farms. Embedded generation with local deployments of combined heat and power plant, district heating schemes, heat pumps, photovoltaic components, hydrogen fuel cells, etc. Such systems can be treated in the same manner as building zones.

Flow-path: transient conduction Lies at the heart of an energy model (q I? ). The process by which a fluctuation of heat flux at one boundary of a solid material finds its way to another boundary, being diminished in magnitude and shifted in time due to the material's thermal inertia. Is a function of the temperature and heat flux excitations at exposed surfaces, the possible generation of heat within the fabric, the temperature- and moisture-dependent (and therefore time-dependent) hygro-thermal properties of the individual materials, and the relative position of these materials. Sometimes important to consider heat flow in more than one direction (e.g. in cases where thermal bridging might be expected to occur). Governed by conductivity, k (W/m.K), density, ρ (kg/m 3 ) and specific heat capacity, C (J/kg.K). Derived properties used to direct material selection, e.g.: materials with high thermal diffusivity transmit a boundary heat flux fluctuation faster; materials with high thermal effusivity absorb a surface heat flux more readily.

3D conduction and thermal bridging

Flow-path: surface convection The process by which heat flux is exchanged between a surface and the adjacent air layer (q I I+1 ). At external surfaces convection is wind induced and considered as forced. At internal surfaces either natural or forced air movement can occur depending on the location of mechanical equipment. The governing parameter is the convection coefficient, h c (W/m 2.K), which depends on surface-to-air temperature difference, surface roughness, direction of heat flow and surface dimensions.

Flow-path: long-wave radiation exchange Function of surface temperature, emissivity, the extent to which surfaces are in visual contact (represented by a view factor), and the nature of the surface reflection (diffuse, specular or mixed). Will tend to establish surface temperature equilibrium by cooling hot surfaces and heating cold ones (q IJ ). Important where temperature asymmetry prevails, as in passive solar buildings where an attempt is made to capture solar energy at some selected surface. A standard energy efficiency measure is to upgrade windows with glazings incorporating a low emissivity coating to increase the reflection of long-wave radiation flux and so act to break inter-surface heat exchange. Long-wave radiation exchange between external surfaces and the sky vault, surrounding buildings and ground can result in a substantial lowering of surface temperatures, especially under clear sky conditions and at night.

Flow-path: short-wave radiation Short-wave energy arrives at a surface directly from the sun and diffusely after atmospheric scatter and terrain reflections. By transient conduction finds its way through the fabric where it will contribute to the inside surface heat flux at some later time via convection and long-wave radiation. With transparent surfaces some flux is transmitted to strike internal surfaces and raise their temperature. Solar irradiation estimation requires the prediction of surface position relative to the solar beam, and the assessment of the changing pattern of internal/external surface insolation The governing thermo-physical properties include shortwave absorptivity, transmissivity and reflectivity.

Flow-path: air flow Three air flow paths: infiltration, zone-coupled flows and mechanical ventilation. Infiltration is the leakage of air from outside (through cracks and the fabric) and via the ingress of air through intentional openings referred to as natural ventilation. Zone-coupled air flow is caused by pressure variations and by buoyancy forces resulting from the density differences associated with the temperatures of the coupled air volumes. Mechanical ventilation is the supply of air to satisfy a fresh air requirement. Random occurrences, such as occupant induced window/door opening, changes in the prevailing wind conditions, and the intermittent use of mechanical ventilation, will influence the magnitude of the air flow.

Flow-path: heat injection The heat gains from lighting installations, occupants, small power equipment, IT devices etc. Modelling requires knowledge of the heat (radiant and convective) and moisture emissions. Sources, such as luminaires and IT equipment, also require knowledge of their electrical behaviour (e.g. in the case of daylight responsive luminaire dimming). Other sources: electrical, chemical, photoelectric effect, etc.

Flow-path: moisture Dampness and mould growth are major problems affecting a significant proportion of houses. High levels of airborne spores may occur due to the growth of fungus on walls and furnishings. Fluctuations in moisture levels within the building's fabric can be problematic, leading to interstitial condensation or causing variations in material thermophysical properties and, thereby, adversely affecting thermodynamic performance.

Control systems Control systems comprise control loops. Control loops comprising: a sensor to measure a simulation parameter or aggregate of parameters; an actuator to receive and act upon the controller output signal; and a regulation law to relate the sensed condition to the actuated state. Control loops are used to regulate HVAC components and manage buildingside entities, such as solar control devices.

Passive solar features a) non-diffusing direct gain b) diffusing direct gain c) earth banking d) attached sunspaces e) thermo-siphon f) double envelope g) mass Trombe-Michel walls h) water Trombe-Michel walls i) induced ventilation j) phase change materials k) transwalls l) roof ponds m) evaporative cooling n) desiccant materials o) movable shading p) movable insulation q) selective thin films

Environmental impact Buildings typically account for around 50% of the total energy consumption in a developed country and a similar portion of the carbon dioxide emissions. Significant additional energy consumption is associated with the production and transportation of construction materials. Associated with energy consumption are gaseous emissions that can contribute to global warming (CO 2 ), acidification (SO x ) and ozone generation (NO x ). The integrated performance modelling approach is able to address all aspects of a building's life cycle and thereby help designers to strike a balance between energy use, indoor comfort and local/global impact.

Uncertainty All design parameters are subject to uncertainty. Programs need to be able to apply uncertainty bands to their input data and use these bands to determine the impact of uncertainty on likely performance. Programs so endowed are able to assess risk, rather than merely presenting performance data to users.

Flow-path: transient conduction Material Conductivit y (W/m.K) Diffusivity (m 2 /s) Effusivity (J/m 2 C 1/2 ) Surface absorptivity (-) Surface emissivity (-) X 0.85 3.2 x 10-7 5.3 x 10 3 0.7 0.8 Y 1.65 0.8 x 10-4 6.7 0.3 0.4 Y transmits a heat flux fluctuation the fastest because the thermal diffusivity is highest. Y absorbs a surface heat flux less readily because the thermal effusivity is lowest. Y conducts heat more readily because the conductivity is highest. Y absorbs less radiation in the short-wave part of the solar spectrum because the surface absorptivity is lowest. Y reflects more radiation in the long-wave part of the electromagnetic spectrum because the surface emissivity is lowest.

Mathematical modelling Underlying flow-paths is the concept of energy, mass and momentum conservation. Models of the heat, air, moisture, light and electricity flows are required. Computer tools have traditionally been constructed by simplifying system equations in order to lessen the computational load and user input burden: aspects of the system may be neglected (e.g. longwave radiation exchange); system parameters may be assumed time invariant (e.g. convection coefficients); or steady state boundary conditions may be imposed. Within a simulation program such assumptions are heresy. A mathematical model is constructed to represent each energy flow-path and all possible interactions; in this sense simulation is an emulation of reality. The aim of integrative modelling is to preserve the integrity of the entire energy system by simultaneously processing all energy transport paths. The energy system is considered to be systemic (there are myriad inter-part interactions), dynamic (the parts evolve at different rates), non-linear (parameter values depend on the thermodynamic state) and stochastic (some events and influences are random).

Modelling methods Steady-state: not dynamic have and have no mechanism for the accurate inclusion of many flow-paths and systems (e.g. solar gain, longwave radiation exchanges, control systems etc.). Simple dynamic: these are mostly based on regression techniques applied to the results of multiple parametric runs of more powerful modelling systems. Useful at the early design stage. Electrical Analogue: exploiting the analogy that exists between electrical flow and heat flow. Has little application in a design context. Response Function: based on an analytical solution of the governing conservation equations under special boundary conditions and assuming that system parameters are linear and time invariant. Numerical: use numerical techniques to solve connected systems of equations that may be non-linear and time varying. Can therefore handle problems of arbitrary complexity.