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  1. the air is greater than that for dry air: the specific heat of dry air is about 1 Joule per kilogram per degree while the value for water vapour is 1.84 J/kg.C. This is a large difference but because air at 10°C and 40%RH contains very little water vapour, the increase

  2. The new condition of the air is calculated and this new point and the process will be automatically drawn in the diagram. Customizations Set the chart according to your needs: Chart Style: Mollier/ Psychrometric-Chart. The x/y-axes will be flipped; Units-system can be set to Metric(SI) or Imperial(I-P). This affects the chart, input values and ...

  3. Apr 6, 2022 · 15.2.3 Use of Psychrometric Chart to Obtain Properties of Moist Air. Psychrometrics is the study of moist air. The properties of moist air can be determined from the psychrometric chart [3, 4]. Figure 15.2 illustrates the general layout and the parameters used in the psychrometric chart. The state point of moist air can be located on the chart ...

  4. Mar 26, 2024 · The 1.08 in the sensible heat formula is the product of the density of air (0.075 lb/ft3), specific heat of air (0.24 btu/lb/°F) and the conversion from cubic feet per hour to cubic feet per minute (60). The original form of the sensible heat formula is: Qs = mcΔT. Qs = (ρv)cΔT. Qs = (0.075 x 60 x 0.24) x CFM x ΔT.

  5. Psychrometric Chart. Although engineers and technicians need to know how the values of such properties of air as specific humidity, sensible and latent heat, and relative humidity in our designs, the actual computation of these quantities is much too burdensome for everyday operations. Even the use of prepared tables of values is time consuming ...

  6. Sep 19, 2020 · Adiabatic mixing is an analytical model used to describe mixing of two air streams (e.g., recirculated return air and fresh air) in a HVAC system. This video...

  7. Outdoors, we see water droplets in the air as fog, clouds, or rain and we see ice crystals in the air as snow or hail. The psychrometric chart only considers the conditions up to the saturation point; therefore, it only considers the effects of water in the vapor phase and does not deal with water droplets or ice crystals. b.