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
50
ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0
55
.025
45
-
0.8
SENSIBLE HEAT TOTAL HEAT
0 300
0.4
.024
2.0
Qs Qt
-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
.023 55
80
40
0
85
.022
0
h W
.020
35
75
.019 80
30
90
65
15
60 45
30 25
0
5
Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com
20
10
DEFINITIONS AND USEFUL EQUATIONS
15
90
85
80
75
70
65
60
55
50
45
40
10
35
30
15
25
10
35
30
25
20
20
5
15 15
10 10
0
5
0 0
-5
-5
5
30
40
20
0
% 15
VE ATI REL 8% 6% 4% 2%
105
35
0 550 40
100
40
55
95
45
DRY BULB TEMPERATURE - °F
60
10
Y IDIT HUM
110
50
25 %
80
55 70
EN TH AL PY
-B
TU
60
.016 .015 .014 45 .013 .012 .011 .010
40
.009 .008 .007 .006 .005 35 .004 .003 .002
115
UN D
PE R
PO
70
20
HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR
DR Y
AI R
75
25
65
5
50
.017 70
O F
• Psychrometric Chart Scary, complicated looking graph.
.018
.001 120
Definitions
.021
500
1000
150 0
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
50
ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0
55
.025
45
-
0.8
SENSIBLE HEAT TOTAL HEAT
0 300
0.4
.024
2.0
Qs Qt
-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
.023 55
80
40
0
85
.022
0
Definitions
.021
500
1000
150 0
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
70
90
65
15
60
45
30 25
0
5
Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com
20
10
DEFINITIONS AND USEFUL EQUATIONS
15
90
85
80
75
70
65
60
55
50
45
40
10
35
30
15
25
10
35
30
25
20
20
5
15 15
10 10
0
5
0 0
-5
-5
5
30
40
20
0
% 15
VE ATI REL 8% 6% 4% 2%
105
35
0 550 40
100
40
55
95
45
DRY BULB TEMPERATURE - °F
60
10
Y IDIT HUM
110
50
25 %
80
55
70
EN TH AL PY
-B
TU
60
.015 .014 45 .013 .012 .011 .010
40
.009 .008 .007 .006 .005 35 .004 .003 .002
115
20
PE R
PO
UN D
O F
65
.016
.001 120
DR Y
AI R
75
25
HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR
.017
70
5
50
30
20 25 ENTHALPY - BTU PER POUND OF DRY AIR
13
50
ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0
55
.025
45
-
0.8
0 300
20 00
0.2 0.1
5000
0.4
-2000 -100 0
0 -4. .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1
0 .5
.024
2.0 4. -8.0 0 -8 .0
Qs Qt
0
0
.023 55
80
40
85
.022 .021
500
1000
150 0
ENTHALPY HUMIDITY RATIO
h W
.020
35
75
.019 80
.018
30
70
PE R
20
65
90
55
35
45
30 25
0 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com
20
90
85
80
75
70
65
60
55
50
45
10
35
30
15
25
10
30
25
20
35
40
15 20
5
10
0
5
0 0
-5
-5
5
10
15
0
% 15
30
40
20
0 550 40
Dry Bulb Temperature Axis and Lines 5 1 1 2 0
5
DEFINITIONS AND USEFUL EQUATIONS
8% 6% 4% 2%
REL
H VE ATI
105
40
55
100
45
DRY BULB TEMPERATURE - °F
60
10
Y IDIT UM
110
70
50
25 %
80
Increasing temperature 60 and energy content
95
15
EN TH
AL PY
-B
TU
60
.016 .015 .014 45 .013 .012 .011 .010
40
.009 .008 .007 .006 .005 35 .004 .003 .002
115
PO UN D
O F
65
HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR
75
25
DR Y
AI R
70
5
50
.017
.001 120
SENSIBLE HEAT TOTAL HEAT
0.3
0.6
30
25 0 ENTHALPY - BTU PER POUND OF DRY AIR
14
50
ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0
55
.025
45
-
0.8 -100 0
0
0
.023 55
80
40
85
.022 .021
500
1000
150 0
ENTHALPY HUMIDITY RATIO
h W
.020
35
75
.019 80
.018
30
PE R
20
65
90
15
45
25
0 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com
5
20
10
15
DEFINITIONS AND USEFUL EQUATIONS
90
85
80
75
70
65
60
55
50
45
10
35
30
15
25
10
30
25
20
35
40
15 20
5
10
0
5
0 0
-5
-5
5
10
15
0
30
40
20
% 15
8% 6% 4% 2%
95
35
0 550 40
REL
H VE ATI
105
40
55
100
45
DRY BULB TEMPERATURE - °F
60
10
Y IDIT UM
110
60
70
50
25 %
80
55
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
.014 45 .013 .012 .011 .010
40
.009 .008 .007 .006
.005 35 .004 .003 .002
115
DR Y
AI R
75
25
30
50
.017 70
5
Specific Humidity Axis and Lines
0 300
20 00
0.2 0.1
5000
0.4
-2000
0 -4. .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1
0 .5
.024
2.0 4. -8.0 0 -8 .0
Qs Qt
.001 120
SENSIBLE HEAT TOTAL HEAT
0.3
0.6
30
20 25 ENTHALPY - BTU PER POUND OF DRY AIR
15
50
ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0
55
.025
45
-
0.8
SENSIBLE HEAT TOTAL HEAT
0 300
20 00
0.2 0.1
5000
0.4
.024
2.0 4. -8.0 0 -8 .0
Qs Qt
0 -4. .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1
0 .5 0.3
0.6
-2000 -100 0
0
0
.023 55
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)
65
AL PY
90
-B
TU
60
45
30 25
0 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com
5
20
10
15
DEFINITIONS AND USEFUL EQUATIONS
90
85
80
75
70
65
55
50
45
10
35
30
15
25
10
30
25
20
35
40
15 20
5
10
0
5
0 0
-5
-5
5
10
15
0
30
40
20
% 15
8% 6% 4% 2%
95
35
60
5
0 550 40
REL
H VE ATI
105
40
55
100
45
DRY BULB TEMPERATURE - °F
60
10
Y IDIT UM
110
60
70
50
25 %
EN TH
80
55
.016 .015 .014 45 .013 .012 .011 .010
40
.009 .008 .007 .006 .005 35 .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
50
ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0
55
.025
45
-
0.8
0.2 0.1
5000
0.4
0 300
20 00
0 -4. .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1
0 .5
.024
2.0 4. -8.0 0 -8 .0
Qs Qt
-2000 -100 0
0
0
.023 55
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
PE R
20
60 65
AL PY
90
-B
TU
Wet Bulb temperature Axis15 and Lines
45
30 25 20
0 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com
5
20
10
15
DEFINITIONS AND USEFUL EQUATIONS
90
85
80
75
70
65
60
55
50
45
10
35
30
15
25
10
30
25
20
35
40
15 20
5
10
0
5
0 0
-5
-5
5
10
15
0
E TIV ELA R %
30
40
8 6% 4% 2%
105
35
.016 .015 .014 45 .013 .012 .011 .010
40
.009 .008 .007
.006 Increasing temperature % .005 35 15 and energy content ITY
0 550 40
100
40
55
95
45
ID HUM
110
60
10
DRY BULB TEMPERATURE - °F
60
70
50
25 %
EN TH
80
55
.004 .003 .002
115
O F
65
HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR
75
25
DR Y
AI R
70
5
50
.017
.001 120
SENSIBLE HEAT TOTAL HEAT
0.3
0.6
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
55
.025
45
-
0.8
SENSIBLE HEAT TOTAL HEAT
.024
-2000
-100 0
0
0
.023 55
80
40
85
.022 .021
500
h W
.020
35
75 Increasing enthalpy or 80 energy content
30
.019 .018
75
25
DR Y
AI R
70
PO UN D
O F
65 70
PE R
20
65
90
15
45
30 25
0 Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com
5
20
10
15
DEFINITIONS AND USEFUL EQUATIONS
90
85
80
75
70
65
60
55
50
45
10
35
30
15
25
10
30
25
20
35
40
15 20
5
10
0
5
0 0
-5
-5
5
10
15
0
30
40
20
% 15
8% 6% 4% 2%
95
35
0 550 40
REL
H VE ATI
105
40
55
100
45
DRY BULB TEMPERATURE - °F
60
10
Y IDIT UM
110
60
70
50
25 %
80
55
EN TH
AL PY
-B
TU
60
5
50
.017 HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR
1000
150 0
ENTHALPY HUMIDITY RATIO
.016 .015 .014 45 .013 .012 .011 .010
40
.009 .008 .007 .006 .005 35 .004 .003 .002
115
0 300
20 00
0.2 0.1
5000
0.4
2.0 4. -8.0 0 -8 .0
Qs Qt
0 -4. .0 -2 -1.0 .5 -0 -0.4 -0.3 -0.2 -0.1
0 .5
0.3
0.6
.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
50
ALTITUDE: SEA LEVEL BAROMETRIC PRESSURE: 29.921 in. HG ATMOSPHERIC PRESSURE: 14.696 psia 1.0 1.0
55
.025
45
-
0.8
SENSIBLE HEAT TOTAL HEAT
0 300
0.4
.024
2.0
Qs Qt
-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
.023 55
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
70
90
65
15
60
45
30
25
0
5
Chart by: AKTON PSYCHROMETRICS, www.aktonassoc.com
20
10
DEFINITIONS AND USEFUL EQUATIONS
15
90
85
80
75
70
65
60
55
50
45
40
10
35
30
15
25
10
35
30
25
20
20
5
15 15
10 10
0
5
0
0
-5
-5
5
30
40
20
0
% 15
VE ATI REL 8% 6% 4% 2%
105
35
0 550 40
100
40
55
95
45
DRY BULB TEMPERATURE - °F
60
10
Y IDIT HUM
110
50
25 %
80
55
70
EN TH AL PY
-B
TU
60
.015 .014 45 .013 .012 .011 .010
40
.009 .008 .007 .006 .005 35 .004 .003 .002
115
20
PE R
PO
UN D
O F
65
.016
.001 120
DR Y
AI R
75
25
HUMIDITY RATIO - POUNDS MOISTURE PER POUND DRY AIR
.017
70
5
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 Power Into the Pump Motor as kilowatts
DEFINITIONS AND USEFUL EQUATIONS
54
Calculating Power Into the Fan Motor as kW
DEFINITIONS AND USEFUL EQUATIONS
55
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
56
The Square Law
DEFINITIONS AND USEFUL EQUATIONS
57
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
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 ‒ 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
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 ‒ 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
60
Conservation of Mass and Energy Doing the Algebra
DEFINITIONS AND USEFUL EQUATIONS
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