Superheat & Subcooling →
Delta T →
Refrigerant Charge →
Imperial (°F / psig)
Metric (°C / kPa)
Pressure → Temp
Temp → Pressure
Refrigerant
R-410A
R-32
R-454B
R-22
R-404A
Reading Taken On
Suction / vapour line (dew point, for superheat)
Liquid line (bubble point, for subcooling)
Gauge Pressure (psig)
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Saturation Temperature
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Enter a value above and click calculate.
R-410A PT Chart
Pressures are gauge (psig). R-410A has a single saturation curve, so one pressure column covers liquid and vapour.
Temp (°F) Pressure (psig)
-40 10.7
-35 14.0
-30 17.7
-25 21.8
-20 26.2
-15 31.0
-10 36.3
-5 42.0
0 48.2
5 54.9
10 62.2
15 70.0
20 78.4
25 87.4
30 97.0
35 107.4
40 118.4
45 130.2
50 142.6
55 156.6
60 170.7
65 185.8
70 201.8
75 218.7
80 236.5
85 255.5
90 275.4
95 296.4
100 318.5
105 341.9
110 366.4
115 392.3
120 419.4
125 448.0
130 477.9
135 509.4
140 542.5
145 578.2
150 613.9
How It Works
A PT chart lists the pressure at which a refrigerant boils or
condenses (its saturation point) at each temperature. Wherever liquid
and vapour exist together — inside the evaporator and the condenser —
the pressure on your gauge tells you the refrigerant's temperature.
Using it on a service call
Superheat = Suction Line Temp − Saturation Temp at Suction Pressure
Subcooling = Saturation Temp at Liquid Pressure − Liquid Line Temp
Read the suction pressure, look up its saturation temperature, and
compare it to the actual suction line temperature to get superheat. Do
the same on the liquid line for subcooling. The
Superheat & Subcooling calculator
does both steps for you.
Blends and glide
R-454B and R-404A are zeotropic blends: they boil across a small
temperature range instead of at one point. This is called
glide — about 2°F (1°C) for R-454B and under 1.5°F for
R-404A. Use the dew point (vapour) for superheat and
the bubble point (liquid) for subcooling. R-410A's glide
is small enough to ignore, and R-32 and R-22 have none.
Gauge vs absolute pressure
All pressures here are gauge pressure (psig or kPa gauge) — what a
manifold or digital gauge reads. Like printed PT charts, it assumes
sea-level atmospheric pressure; at high elevation a gauge reads slightly
higher for the same saturation temperature (about 2.5 psi / 17 kPa at
5,000 ft). Values between published rows are linearly interpolated.