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Lecture Objectives Psychrometrics Define Heating and Cooling Loads
Practice for the Quiz Define equation for Sensible and latent heat Define Heating and Cooling Loads
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We will have our first Quiz on Tuesday
First 10 minutes of the class An example is provided in the handout section of the course website At the end of the class we will solve several examples
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enthalpy
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Examples: 1) You heat one pounds of air air A (T=50F, W=0.009 lbW/lbDA) to point T=80F and humidify it to RH 70%. What is the sensible, latent and total heat added to the one pound of air. 2) One pound of air D(T=90F, RH=30%) is humidified by adiabatic humidifier to 90% relative humidity. What is the temperature at the end of humidification process and how much water is added to the air.
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Process in HVAC systems
Heating Cooling Humidification Dehumidification All these processes ca be quantified in Psychrometric Chart Also, all the these quantities can be calculated with and without help of the Psychrometric Chart
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Equations for sensible energy transport by air
Energy per unit of mass Δhsensible = cp × ΔT [Btu/lb] cp - specific heat for air (for air 0.24 Btu/lb°F) Heat transfer (rate) Qs = m × cp × ΔT [Btu/h] m - mass flow rate [lb/min, lb/h], m = V × r V – volume flow rate [ft3/min or CFM] r – air density (0.076lb/ft3) Qs = 1.1 × CFM × ΔT (only for IP unit system)
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Equations for latent energy transport by air
Energy per unit of mass Δhlatent = Δw × hfg [Btu/lbda] hfg - specific energy of water phase change (1000 Btu/lbw) Heat transfer (rate) Ql = m × Δw × hfg [Btu/h] Ql = 1000 × WaterFloowRate (only for IP units)
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Total energy transport calculation using enthalpies from chat
Energy per unit of mass Δh=h1-h2 [Btu/lbda] Heat transfer (rate) Qtotal = m × Δh [Btu/h] Qtotal = Qsensible + Qlatent
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Why do we calculate heating and cooling loads?
10/21/2003 Heating and Cooling Loads Why do we calculate heating and cooling loads? To estimate amount of energy used for heating and cooling by a building Or To size heating and cooling equipment for a building ARE 346N
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Introduction to Heat Transfer
Conduction Components Convection Air flows (sensible and latent) Radiation Solar gains (cooling only) Increased conduction (cooling only) Phase change Water vapor/steam Internal gains (cooling only) Sensible and latent
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1-D Conduction U = k/l Q = UAΔT l k U U-Value [W/(m2 °C)] A
90 °F 70 °F l k A U U-Value [W/(m2 °C)] U = k/l k conductivity [W/(m °C)] l length [m] Q heat transfer rate [W] ΔT temperature difference [°C] A surface area [m2] Q = UAΔT
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Material k Values Material k [W/(m K)] Steel 64 - 41 Soil 0.52 Wood
Fiberglass Polystyrene 0.029 At 300 K Table 2-3 Tao and Janis (k=λ) values in [Btu in/(h ft2 F)]
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Wall assembly l1 l2 R = l/k Q = (A/Rtotal)ΔT Add resistances in series
Add U-values in parallel k1 k2 90 °F 70 °F R1 R2 Tout Tmid Tin
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Rsurface= 1/h Rtotal= ΣRi Surface Air Film Table 2-5 Tao and Janis
h - convection coefficient - surface conductance [W/m2, Btu/(h ft2)] Direction/orientation Air speed Table 2-5 Tao and Janis Tout Tin Rsurface= 1/h Ro R1 R2 Ri Rtotal= ΣRi Tout Tin
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What if more than one surface?
l1 l2 k1, A1 k2, A2 Qtotal = Q1,2 + Q3 Q1,2 A2 = A1 U1,2 = 1/R 1,2=1/(R1+R2) k3, A3 Q1,2 = A1U1,2ΔT Q3 Q3 = A3U3ΔT l3
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Tin Tout Qtotal= Σ(UiAi)·ΔT
Relationship between temperature and heat loss U1A1 U2A2 U3(A3+A5) U4A4 U5A5 A2 A3 A1 A4 Tin Tout A5 A6 Qtotal= Σ(UiAi)·ΔT
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Example Consider a 1 ft × 1 ft × 1 ft box
Two of the sides are 2” thick extruded expanded polystyrene foam The other four sides are 2” thick plywood The inside of the box needs to be maintained at 120 °F The air around the box is still and at 80 °F How much heating do you need?
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The Moral of the Story Calculate R-values for each series path
Convert them to U-values Find the appropriate area for each U-value Multiply U-valuei by Areai Sum UAi Calculate Q = Σ(UAi)ΔT
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Heat transfer in the building Not only conduction and convection !
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Infiltration Q = m × cp × ΔT [BTU/hr, W]
Air transport Sensible energy Previously defined Q = m × cp × ΔT [BTU/hr, W] ΔT= T indoor – T outdoor or Q = 1.1 BTU/(hr CFM °F) × V × ΔT [BTU/hr]
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Latent Infiltration and Ventilation
Can either track enthalpy and temperature and separate latent and sensible later: Q total = m × Δh [BTU/hr, W] Q latent = Q total - Q sensible = m × Δh - m × cp × ΔT Or, track humidity ratio: Q latent = m × Δw × hfg
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Ventilation Example Supply 500 CFM of outside air to our classroom
Outside 90 °F 61% RH Inside 75 °F 40% RH What is the latent load from ventilation? Q latent = m × hfg × Δw Q = ρ × V × hfg × Δw Q = lbair/ft3 × 500 ft3/min × 1076 BTU/lb × ( lbH2O/lbair lbH2O/lbair) × 60 min/hr Q = kBTU/hr
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Where do you get information about amount of ventilation required?
ASHRAE Standard 62 Table 2 Hotly debated – many addenda and changes Tao and Janis Table 2.9A
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Weather Data Table 2-2A (Tao and Janis) or
Chapter 28 of ASHRAE Fundamentals For heating use the 99% design DB value 99% of hours during the winter it will be warmer than this Design Temperature Elevation, latitude, longitude
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Ground Contact Receives less attention:
3-D conduction problem Ground temperature is often much closer to indoor air temperature Use F- value for slab floor [BTU/(hr °F ft)] Note different units from U-value Multiply by slab edge length Add to ΣUA Still need to include basement wall area Tao and Janis Tables 2.10 and 2.11 More details in ASHRAE handbook -Chapter 29
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Ground Contact 3-D conduction problem
Ground temperature is often much closer to indoor air temperature Use F- value for slab floor Multiply by slab edge length and Add to ΣUA
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Summary of Heating Loads
Conduction and convection principles can be used to calculate heat loss for individual components Convection principles used to account for infiltration and ventilation
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