HVAC Equations, Concepts, and Definitions Presented By: David Sellers Senior Engineer; Facility Dynamics Engineering A Few Acronyms and Definitions Acronyms • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • AFD – Adjustable Frequency Drive AHU – Air Handling Unit ASHRAE – American Society of Heating Ventilating and Air Conditioning Engineers CV - Constant Volume HVAC – Heating Ventilating and Air Conditioning MOA – Minimum Outdoor Air Psych Chart – Psychrometric Chart VAV – Variable Air Volume VFD – Variable Frequency Drive VFD – (Adjustable Frequency Drive) VSD – Variable Speed Drive VFD – (Adjustable Frequency Drive) AFD Acronym Definition AFD A Few Days AFD Abbreviated Functional Description AFD Accelerated Freeze-Drying (food processing) AFD Accident Free Discount (insurance) AFD Acid Fractionator Distillate AFD Acoustic Flat Diaphragm (electronics) AFD Acrofacial Dysostosis AFD Acrofacial Dysostosis, Catania Type AFD Active Format Descriptor AFD Adaptive Flexible Defense AFD Adaptive Flight Display AFD Adjustable Frequency Drive AFD Advanced Full-screen Debugger AFD African Development Foundation AFD African Development Fund AFD Aft Flight Deck AFD Agence Française de Développement (French Development Agency) AFD Air Force Depot AFD Airfield Database AFD Airport Facilities Directory AFD Alarm Format Definition AFD Albany Fire Department AFD Alcohol Free Day AFD Alexandria Fire Department AFD All Friggin' Day AFD Alt.fan.dragons (Usenet newsgroup) AFD Alternative Forms of Delivery (Canada) AFD Amarillo Fire Department (Amarillo, TX) AFD American Funds Distributors, Inc. AFD Amsterdam Fire Department AFD Ancillary Function Driver • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • AFD Angwin Fire Department (Angwin, CA) AFD Anticipatory Failure Determination AFD Apical Fibrobullous Disease AFD Approved for Design AFD Approximately Finite Dimensional AFD April Fool's Day AFD April Fools Day AFD Arc Fault Detection AFD Arc-Fault Detection AFD Architecture Flow Diagrams AFD Area Forecast Discussion (US National Weather Service) AFD Armed Forces Division AFD Arming & Fusing Device AFD Arming-Firing Device AfD Articles for Deletion (Wikipedia) AFD Ask for Details AFD assign fixed directory (US DoD) AFD Assistant Flight Director AFD Association Franèaise des Diabétiques AFD Athletic Field Design AFD Atlanta Fire Department AFD Austin Fire Department (Texas) AFD Autómata Finito Determinista AFD Automated File Designator AFD Automated Forging Design AFD Automatic Fault Detection AFD Automatic File Distribution AFD Automatic Fire Detection AFD Average Fade Duration AFD Away from Desk AFD Axial Flux Density AFD Axial Flux Difference AFD Active Format Description AFD Adaptive Forward Differencing AFD Adjustable Frequency Drives AFD Asus Foundation Drivers DEFINITIONS AND USEFUL EQUATIONS 2 AFA2D Acronyms • • • • • • • • • • AFD – Adjustable Frequency Drive AHU – Air Handling Unit ASHRAE – American Society of Heating Ventilating and Air Conditioning Engineers CV - Constant Volume HVAC – Heating Ventilating and Air Conditioning MOA – Minimum Outdoor Air Psych Chart – Psychrometric Chart VAV – Variable Air Volume VFD – Variable Frequency Drive (Adjustable Frequency Drive) VSD – Variable Speed Drive (Adjustable Frequency Drive) DEFINITIONS AND USEFUL EQUATIONS 3 AFA2D Definitions • Sensible energy, QS (Btu’s, Btu’s/lb) Energy that causes a temperature change we can feel • Dry bulb temperature, Tdb (°F) An indication of sensible energy measured by a standard thermometer exposed to air; increasing dry bulb temperature = increasing sensible energy DEFINITIONS AND USEFUL EQUATIONS 4 AFA2D Definitions • Latent energy, QL (Btu’s, Btu’s/lb) Energy that is used to keep water in a vapor state • Wet bulb temperature, Twb (°F) An indication of latent energy measured by a standard thermometer with its bulb covered by a wick that is saturated with water and exposed to moving air; increasing wet bulb temperature = increasing latent energy DEFINITIONS AND USEFUL EQUATIONS 5 AFA2D Definitions • Dew point temperature, Tdp (°F) The temperature at which water will begin to condense out of a given sample of air. Also an indication of moisture content; increasing dew point = increasing latent energy. At saturation Tdp = Twb = Tdb DEFINITIONS AND USEFUL EQUATIONS 6 AFA2D Definitions • Enthalpy, h (Btu/lbdry air) A measure of the total energy content of air including both sensible and latent energy; increasing enthalpy = increasing energy content DEFINITIONS AND USEFUL EQUATIONS 7 AFA2D Definitions • Relative humidity, RH (%) The amount of water vapor in the air at a given temperature relative to what it could hold at that temperature; 100% = saturation; increasing specific humidity = increasing moisture content, increasing dew point, and increasing wet bulb temperature. In Antarctica, the relative humidity approaches 100% much of the time, just like in Florida after a thunderstorm DEFINITIONS AND USEFUL EQUATIONS 8 AFA2D Definitions • Specific humidity, w (lbwater/lbdryair, grainswater/lbdryair) The ratio of the mass of water to the mass of dry air in a given sample of air; increasing specific humidity = increasing moisture content, increasing dew point, and increasing wet bulb temperature. In Antarctica, the specific humidity at a relative humidity of 100% is very low. In Florida, the specific humidity at a relative humidity of 100% is quite high relative to Antarctica. DEFINITIONS AND USEFUL EQUATIONS 9 AFA2D Definitions • Psychrometrics The field of engineering concerned with the determination of physical and thermodynamic properties of gas-vapor mixtures. DEFINITIONS AND USEFUL EQUATIONS 10 ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0 0.8 SENSIBLE HEAT TOTAL HEAT 0 300 0.4 Qs Qt 50 55 .025 45 - .024 2.0 -2000 -100 0 4.0 -8.0 -8 .0 20 0 .0 -4 .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1 0.5 0.3 5000 0.6 0.2 0.1 AFA2D 0 .02355 80 40 0 85 .022 0 .021 500 h W .020 35 75 UN D PE R PO 70 0 5 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com DEFINITIONS AND USEFUL EQUATIONS 15 90 85 80 75 70 65 55 50 40 45 10 DRY BULB TEMPERATURE - °F Y IDIT HUM 110 20 VE ATI REL 8% 6% 4% 2% 105 35 10 35 30 15 25 10 30 25 20 20 15 15 5 10 0 5 0 0 -5 -5 10 30 40 25 % 15 100 45 0 550 40 95 35 20 55 60 40 30 60 70 50 25 % 80 55 45 5 65 90 15 60 EN TH AL PY -B TU 60 HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR 65 .016 .015 .01445 .013 .012 .011 .010 .009 40 .008 .007 .006 .00535 .004 .003 .002 115 DR Y AI R 75 25 20 5 50 .017 70 10 0 .018 30 O F • Psychrometric Chart Scary, complicated looking graph. .019 80 .001 120 1000 150 0 Definitions ENTHALPY HUMIDITY RATIO 30 20 25 ENTHALPY - BTU PER POUND OF DRY AIR 11 AFA2D Definitions • Psychrometric Equations The alternative to using the psych chart. DEFINITIONS AND USEFUL EQUATIONS 12 ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0 0.8 SENSIBLE HEAT TOTAL HEAT 0 300 0.4 Qs Qt 50 55 .025 45 - .024 2.0 -2000 -100 0 4.0 -8.0 -8 .0 20 0 .0 -4 .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1 0.5 0.3 5000 0.6 0.2 0.1 AFA2D 0 .02355 80 40 0 85 .022 0 .021 500 1000 150 0 Definitions ENTHALPY HUMIDITY RATIO h W .020 35 75 .019 80 .018 • Psychrometric Chart Graphical tool that allows the informed user to determine multiple parameters like enthalpy, dew point, relative humidity, specific humidity, dry bulb temperature and wet bulb temperature for a sample of air if any two of them are know. 30 0 5 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com DEFINITIONS AND USEFUL EQUATIONS 15 90 85 80 75 70 65 55 50 40 45 10 DRY BULB TEMPERATURE - °F 20 Y IDIT HUM 110 35 10 35 30 15 25 10 25 20 20 15 15 5 10 0 5 0 0 -5 -5 10 30 VE ATI REL 8% 6% 4% 2% 105 25 5 30 40 20 % 15 100 45 0 550 40 95 35 30 55 60 40 5 60 70 50 25 % 80 55 45 0 65 90 15 60 EN TH AL PY -B TU 60 .016 .015 .01445 .013 .012 .011 .010 .009 40 .008 .007 .006 .00535 .004 .003 .002 .001 120 70 20 PE R PO UN D O F 65 115 DR Y AI R 75 25 HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR .017 70 10 50 30 20 25 ENTHALPY - BTU PER POUND OF DRY AIR 13 ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0 SENSIBLE HEAT TOTAL HEAT 0 300 20 00 0.2 0.1 5000 0.4 .025 45 - .024 Qs Qt 2.0 4. -8.0 0 -8 .0 -2000 -100 0 0 -4. .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1 0 .5 0.3 0.6 55 0 0 .02355 80 40 85 .022 .021 500 1000 150 0 ENTHALPY HUMIDITY RATIO h W .020 35 75 .019 80 .018 30 PO UN D O F 65 70 PE R 20 55 0 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com 5 DEFINITIONS AND USEFUL EQUATIONS 90 85 80 75 70 65 55 50 45 40 35 30 Dry Bulb Temperature Axis and Lines 5 1 1 2 8% 6% 4% 2% .016 .015 .01445 .013 .012 .011 .010 .009 40 .008 .007 .006 .00535 .004 .003 .002 115 10 0 DRY BULB TEMPERATURE - °F 20 110 20 25 15 20 10 15 5 10 0 5 0 0 -5 -5 5 30 25 35 Y IDIT HUM E ATIV REL 105 25 15 30 40 20 % 15 100 45 0 550 40 95 35 30 25 % 80 5 55 60 40 10 Increasing temperature 60 and energy content 70 50 45 0 65 90 15 60 EN TH AL PY -B TU 60 HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR 75 25 DR Y AI R 70 10 50 .017 .001 120 0.8 50 30 25 0 ENTHALPY - BTU PER POUND OF DRY AIR 14 ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0 0 300 20 00 0.2 0.1 5000 0.4 .024 Qs Qt 2.0 4. -8.0 0 -8 .0 -2000 -100 0 0 -4. .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1 0 .5 .025 45 - 0 0 .02355 80 40 85 .022 .021 500 1000 150 0 ENTHALPY HUMIDITY RATIO h W .020 35 75 .019 80 .018 30 PE R 0 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com 5 15 DEFINITIONS AND USEFUL EQUATIONS 90 85 80 75 70 65 55 50 45 40 10 DRY BULB TEMPERATURE - °F 8% 6% 4% 2% 110 20 Y IDIT HUM E ATIV REL 105 35 10 35 30 15 25 10 30 25 20 20 5 15 15 0 10 0 5 5 0 -5 -5 10 30 40 25 % 15 100 45 0 550 40 95 35 20 55 60 40 30 60 70 50 25 % 80 55 45 0 65 90 15 60 EN TH AL PY -B TU 60 HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR PO UN D O F 65 Increasing moisture and 70 energy content .016 .015 .01445 .013 .012 .011 .010 .009 40 .008 .007 .006 .00535 .004 .003 .002 115 DR Y AI R 75 25 20 5 50 .017 70 10 Specific Humidity Axis and Lines SENSIBLE HEAT TOTAL HEAT 0.3 0.6 55 .001 120 0.8 50 30 20 25 ENTHALPY - BTU PER POUND OF DRY AIR 15 ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0 0.8 SENSIBLE HEAT TOTAL HEAT 0 300 20 00 0.2 0.1 5000 0.4 2.0 4. -8.0 0 -8 .0 0 55 .025 45 - .024 Qs Qt 0 -4. .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1 0 .5 0.3 0.6 50 -2000 -100 0 0 .02355 80 40 85 .022 .021 500 1000 150 0 ENTHALPY HUMIDITY RATIO h W .020 35 Increasing.019 relative 50 .018 energy humidity and .017 content 75 PO UN D O F 65 70 20 PE R Relative Humidity Lines and Saturation Curve 15 (100% RH) 90 0 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com 5 25 % 20 15 DEFINITIONS AND USEFUL EQUATIONS 90 85 80 75 70 65 60 55 50 45 40 10 DRY BULB TEMPERATURE - °F 35 10 35 30 15 25 10 30 25 20 20 5 15 15 0 10 0 5 5 0 -5 -5 10 20 8% 6% 4% 2% Y IDIT HUM E ATIV REL 110 40 25 0 30 105 45 % 15 95 35 0 550 40 100 40 30 55 60 45 5 60 70 50 10 65 55 80 EN TH AL PY -B TU 60 .016 .015 .01445 .013 .012 .011 .010 .009 40 .008 .007 .006 .00535 .004 .003 .002 .001 120 75 25 DR Y AI R 70 115 30 HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR 80 30 20 25 ENTHALPY - BTU PER POUND OF DRY AIR 16 ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0 SENSIBLE HEAT TOTAL HEAT 0 300 20 00 0.2 0.1 5000 0.4 2.0 4. -8.0 0 -8 .0 0 .025 45 - .024 Qs Qt 0 -4. .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1 0 .5 0.3 0.6 55 -2000 -100 0 0 .02355 80 40 85 .022 .021 500 1000 150 0 ENTHALPY HUMIDITY RATIO h W .020 35 75 .019 80 .018 30 PO UN D 70 20 PE R Wet Bulb temperature Axis15 and Lines 90 0 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com 5 15 DEFINITIONS AND USEFUL EQUATIONS 8 6% 4% 2% ID HUM 110 90 85 80 75 70 65 60 55 50 45 40 10 DRY BULB TEMPERATURE - °F 25 % 20 10 35 30 15 25 10 30 25 20 20 5 15 15 0 10 0 5 5 0 -5 -5 10 35 105 25 20 E TIV ELA R % 30 40 100 45 .016 .015 .01445 .013 .012 .011 .010 .009 40 .008 .007 .006 Increasing temperature % 5 .00535 1and energy content ITY 0 550 40 95 35 30 55 60 40 5 60 70 50 45 0 65 55 80 EN TH AL PY -B TU 60 .004 .003 .002 115 O F 65 HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR 75 25 DR Y AI R 70 10 50 .017 .001 120 0.8 50 30 20 25 ENTHALPY - BTU PER POUND OF DRY AIR 17 50 Note that constant enthalpy and constant wet bulb temperature lines are almost but not quite parallel SENSIBLE HEAT TOTAL HEAT 2.0 4. -8.0 0 -8 .0 .024 -2000 -100 0 0 0 .02355 80 40 85 .022 .021 500 1000 150 0 ENTHALPY HUMIDITY RATIO h W .020 35 75 Increasing enthalpy or 80 energy content 30 .019 .018 75 DR Y AI R 70 25 PO UN D O F 65 70 PE R 20 90 0 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com 5 15 DEFINITIONS AND USEFUL EQUATIONS 90 85 80 75 70 65 55 50 45 40 10 DRY BULB TEMPERATURE - °F 8% 6% 4% 2% 110 20 10 35 30 25 15 30 25 20 20 10 15 5 10 0 5 0 0 -5 -5 5 15 35 Y IDIT HUM E ATIV REL 105 25 10 30 40 20 % 15 100 45 0 550 40 95 35 25 % 80 40 30 55 60 45 5 60 70 50 10 0 65 55 60 EN TH AL PY -B TU 60 15 50 .017 HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR 0 300 20 00 0.2 0.1 5000 0.4 Qs Qt 0 -4. .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1 0 .5 0.3 0.6 .025 45 - .016 .015 .01445 .013 .012 .011 .010 .009 40 .008 .007 .006 .00535 .004 .003 .002 115 0.8 55 .001 120 ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0 30 20 25 ENTHALPY - BTU PER POUND OF DRY AIR 18 ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0 0.8 SENSIBLE HEAT TOTAL HEAT 0 300 0.4 Qs Qt 50 55 .025 45 - .024 2.0 -2000 -100 0 4.0 -8.0 -8 .0 20 0 .0 -4 .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1 0.5 0.3 5000 0.6 0.2 0.1 AFA2D 0 .02355 80 40 0 85 .022 0 .021 500 1000 150 0 Definitions ENTHALPY HUMIDITY RATIO h W .020 35 75 .019 80 .018 • Psychrometric Chart If you know the dry bulb temperature and relative humidity entering and leaving a cooling coil, you can plot those points on the chart and determine: • The entering and leaving enthalpy (energy content) • The load (how much energy was transferred) • The amount of moisture condensed, if any • The entering and leaving dew point temperature • The entering and leaving wet bulb temperature 30 0 5 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com DEFINITIONS AND USEFUL EQUATIONS 15 90 85 80 75 70 65 55 50 40 45 10 DRY BULB TEMPERATURE - °F 20 Y IDIT HUM 110 35 10 35 30 15 25 10 25 20 20 15 15 5 10 0 5 0 0 -5 -5 10 30 VE ATI REL 8% 6% 4% 2% 105 25 5 30 40 20 % 15 100 45 0 550 40 95 35 30 55 60 40 5 60 70 50 25 % 80 55 45 0 65 90 15 60 EN TH AL PY -B TU 60 .016 .015 .01445 .013 .012 .011 .010 .009 40 .008 .007 .006 .00535 .004 .003 .002 .001 120 70 20 PE R PO UN D O F 65 115 DR Y AI R 75 25 HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR .017 70 10 50 30 20 25 ENTHALPY - BTU PER POUND OF DRY AIR 19 Learn More about Using a Psych Chart HTML version at: http://www.buildingcontrolworkbench.com Downloadable .pdf at: http://customer.honeywell.com/techlit/pdf/770000s/77-E1100.pdf DEFINITIONS AND USEFUL EQUATIONS 20 AFA2D Definitions • Cooling A process that removes energy. For a space, this is often accomplished by circulating air through it at a temperature below the required set point. For an airstream, this is often accomplished by passing it over a surface that is below the required supply temperature. If the surface is below the dew point of the air stream, dehumidification (moisture removal) will also occur. DEFINITIONS AND USEFUL EQUATIONS 21 AFA2D Definitions • Heating A process that adds energy. For a space, this is often accomplished by circulating air through it at a temperature above the required set point. For an airstream, this is often accomplished by passing it over a surface that is above the required supply temperature. DEFINITIONS AND USEFUL EQUATIONS 22 AFA2D Definitions • Freezing A condition that occurs when water is cooled to the point where it changes phase from a solid to a liquid. DEFINITIONS AND USEFUL EQUATIONS 23 AFA2D Definitions • Water Damage A condition that occurs after frozen water contained in a HVAC coil changes back to the liquid phase. DEFINITIONS AND USEFUL EQUATIONS 24 AFA2D Definitions • Expletive A generic reference to the field terminology used to describe and discuss water damage when it occurs. DEFINITIONS AND USEFUL EQUATIONS 25 AFA2D Definitions • Preheat A process that heats a fluid stream to prepare it for a subsequent HVAC process. In air handling systems, this process is used to raise subfreezing air above freezing to protect water filled elements down stream from damage due to freezing. See the Functional Testing Guide (www.peci.org/ftguide) Air Handling System Reference Guide Chapter 5 – Preheat, Table 5.1 to contrast preheat, reheat and heating applications DEFINITIONS AND USEFUL EQUATIONS 26 AFA2D Definitions • Reheat A process that uses heat to warm air being delivered to a zone to prevent over cooling. The temperature of the air was set by the need to hit a dehumidification target or by the requirements of another zone, so it can not be raised at the central system. The volume can not be reduced because it has been set to assure proper ventilation (contaminant control). In the limit, reheat will raise the supply temperature to the zone temperature but not above it. DEFINITIONS AND USEFUL EQUATIONS 27 AFA2D Definitions • Economizer Process An HVAC process designed to minimize the energy required to cool a building DEFINITIONS AND USEFUL EQUATIONS 28 AFA2D Definitions • Constant Volume System An air handling or pumping process that, in general terms, is always moving the same amount of water or air. Pump or fan energy is fairly steady state. Supply and return temperature differences will tend to vary with load. In water systems, the control valves will tend to be three-way valves. DEFINITIONS AND USEFUL EQUATIONS 29 AFA2D Definitions • Variable Volume System/Variable Air Volume System (VAV) An air handling or pumping process that varies the flow of water or air to match the requirements of the load.. Supply and return temperature differences will tend to hold steady regardless of load. In water systems, the control valves will tend to be two-way valves. DEFINITIONS AND USEFUL EQUATIONS 30 Benchmarks Contrasting Utility Consumption with Your Peers DEFINITIONS AND USEFUL EQUATIONS 31 Average Daily Consumption Analysis Contrasting Utility Consumption with Other Metrics Peak electrical consumption may be driven by the need to cool DEFINITIONS AND USEFUL EQUATIONS 32 Occupancy may also be a driver for electrical consumption, but maybe not FOCUSING OUR EFFORT 33 Gas consumption tends to be driven by the need to heat FOCUSING OUR EFFORT 34 Gas consumption seems to be unrelated to occupancy, which is not always true for a hotel due to the domestic hot water loads FOCUSING OUR EFFORT 35 Interval Data Consumption Analysis Looking at Variations in Hour by Hour Patterns DEFINITIONS AND USEFUL EQUATIONS 36 Sensible Heating or Cooling Loads DEFINITIONS AND USEFUL EQUATIONS 37 Where did the Units Conversion Constant Come From? DEFINITIONS AND USEFUL EQUATIONS 38 Where did the Units Conversion Constant Come From? DEFINITIONS AND USEFUL EQUATIONS 39 Specific Heat and Density of Air versus Temperature 0.260 0.24 0.250 0.20 0.240 0.16 0.230 0.12 0.220 0.08 0.210 0.04 0.200 -100 0 100 200 300 400 Density, lb/cubic foot Specific Heat, btu/lb-°F Physical Properties can Vary … 0.00 500 Temperature,°F Specific Heat Density of Dry Air DEFINITIONS AND USEFUL EQUATIONS Density of Saturated Air 40 … so Conversion Constants Only are Valid for a Range of Conditions Versus 1.08 in the equation in common use DEFINITIONS AND USEFUL EQUATIONS 41 … so Conversion Constants Only are Valid for a Range of Conditions Virtually the same as for cold dry air DEFINITIONS AND USEFUL EQUATIONS 42 … so Conversion Constants Only are Valid for a Range of Conditions Versus 1.08 in the equation in common use DEFINITIONS AND USEFUL EQUATIONS 43 … so Conversion Constants Only are Valid for a Range of Conditions Significantly different from hot saturated air and the value in the equation in common DEFINITIONS AND USEFUL EQUATIONS 44 Latent Load DEFINITIONS AND USEFUL EQUATIONS 45 Total Load DEFINITIONS AND USEFUL EQUATIONS 46 Water Side Load DEFINITIONS AND USEFUL EQUATIONS 47 The Relationship Between Flow and Velocity DEFINITIONS AND USEFUL EQUATIONS 48 The Relationship Between Velocity and Velocity Pressure DEFINITIONS AND USEFUL EQUATIONS 49 Fan Power DEFINITIONS AND USEFUL EQUATIONS 50 Unit Conversions for Working with SI Units DEFINITIONS AND USEFUL EQUATIONS 51 Pump Power DEFINITIONS AND USEFUL EQUATIONS 52 Unit Conversions for Working with SI Units DEFINITIONS AND USEFUL EQUATIONS 53 Calculating Kw Into the Pump Motor DEFINITIONS AND USEFUL EQUATIONS 54 Calculating Kw Into the Pump Motor (Continued) DEFINITIONS AND USEFUL EQUATIONS 55 Calculating Power Into the Fan Motor as kW DEFINITIONS AND USEFUL EQUATIONS 56 Calculating Energy Use What can cause the load to vary? • Changes in ambient conditions • Changes in internal conditions • Changes in a production process Just About Everything! DEFINITIONS AND USEFUL EQUATIONS 57 The Square Law DEFINITIONS AND USEFUL EQUATIONS 58 Conservation of Mass and Energy The Goes Inta’s gotta equal the Goes Outa’s Dr. Al Black The tee where the building return meets the bypass line is a node in the system ‒ Energy into and out of the node must be equal ‒ Mass flow into and out of the node must be equal Re Bypass Flow at Bypass Temperature Chiller Flow at Chiller Entering Temperature DEFINITIONS AND USEFUL EQUATIONS Return Flow at Return Temperature 59 Conservation of Mass and Energy The Goes Inta’s gotta equal the Goes Outa’s Dr. Al Black The tee where the building return meets the bypass line is a node in the system ‒ Energy into and out of the node must be equal ‒ Mass flow into and out of the node must be equal ‒ This is a steady state, steady flow process described by the continuity equation Re Bypass Flow at Bypass Temperature Chiller Flow at Chiller Entering Temperature DEFINITIONS AND USEFUL EQUATIONS Return Flow at Return Temperature 60 Conservation of Mass and Energy The Goes Inta’s gotta equal the Goes Outa’s Dr. Al Black The tee where the building return meets the bypass line is a node in the system ‒ Energy into and out of the node must be equal ‒ Mass flow into and out of the node must be equal ‒ This is a steady state, steady flow process described by the continuity equation ‒ For a tee in the pipe, the continuity equation can be simplified Re Bypass Flow at Bypass Temperature Chiller Flow at Chiller Entering Temperature DEFINITIONS AND USEFUL EQUATIONS Return Flow at Return Temperature 61 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 62 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 63 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 64 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 65 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 66 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 67 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 68 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 69 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 70 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 71 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 72 Conservation of Mass and Energy Doing the Algebra DEFINITIONS AND USEFUL EQUATIONS 73