ΣEngineering Suite B2BChemical engineering calculators Home Thermodynamics · Çengel & Boles
θThermoLab SuiteTechnical calculation workspace

ThermoLab · Chapters 1 and 2

Pressure, temperature and general energy balance

Converts units, solves fluid columns and closes energy balances with traceable signs.

Motor listo
TLCalculation engine · Base SI
⌁ Main index

Engineering results

NOT RUN
Chart generated from the current input data.Rango validado
Detailed calculation reportEquations · substitution · verification

Run the calculation to generate the report.

Engineering directory

13 linked modules on a single calculation base

Open any tool without losing your chosen unit system. Each page works on its own and keeps its navigation, report and export.

Engineering framework

Theory, equations and conditions of use

Pressure changes with the weight of the fluid column, and total energy changes with the transfers that cross the system boundary.

Fundamento

Absolute and gauge pressure

Absolute pressure is measured from vacuum; gauge pressure takes the local atmosphere as its reference.

\(P_{abs}=P_{atm}+P_{man}\)

Fundamento

Hydrostatic relation

For constant density and gravity, the vertical difference integrates directly.

\(\Delta P=\rho g h\)

Fundamento

Balance general

Energy is conserved by recording inflows and outflows under a consistent sign convention.

\(\Delta E_{system}=E_{in}-E_{out}\)
Base documentalÇengel & Boles, 7th edition · SI appendices A-1 to A-28
USCS conversionA-1E to A-27E, via exact factors from the SI base
AlcancePreliminary design, teaching and independent verification

Engineering FAQ

Preguntas frecuentes

Can I enter a negative height?+

Yes. The sign indicates rising or falling relative to the reference point.

When does density change?+

In tall gas columns, or where temperature varies widely, ρ(z) must be integrated.

Is atmospheric pressure always 101.325 kPa?+

No; it depends on altitude and weather. That value is the standard atmosphere.

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