Barometric Pressure or Atmospheric Pressure Solution

STEP 0: Pre-Calculation Summary
Formula Used
Atmospheric Pressure = Density*[g]*Height of Mercury Column
Patm = ρ*[g]*hm
This formula uses 1 Constants, 3 Variables
Constants Used
[g] - Gravitational acceleration on Earth Value Taken As 9.80665
Variables Used
Atmospheric Pressure - (Measured in Pascal) - Atmospheric pressure, also known as barometric pressure, is the pressure within the atmosphere of Earth.
Density - (Measured in Kilogram per Cubic Meter) - Density of a material shows the denseness of that material in a specific given area. This is taken as mass per unit volume of a given object.
Height of Mercury Column - (Measured in Meter) - Height of Mercury Column is defined as the height of the mercury column above the free surface.
STEP 1: Convert Input(s) to Base Unit
Density: 997.3 Kilogram per Cubic Meter --> 997.3 Kilogram per Cubic Meter No Conversion Required
Height of Mercury Column: 0.76 Meter --> 0.76 Meter No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
Patm = ρ*[g]*hm --> 997.3*[g]*0.76
Evaluating ... ...
Patm = 7432.9307542
STEP 3: Convert Result to Output's Unit
7432.9307542 Pascal --> No Conversion Required
FINAL ANSWER
7432.9307542 7432.931 Pascal <-- Atmospheric Pressure
(Calculation completed in 00.020 seconds)

Credits

Created by Ayush gupta
University School of Chemical Technology-USCT (GGSIPU), New Delhi
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University of Hawaiʻi at Mānoa (UH Manoa), Hawaii, USA
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8 Pressure and its Measurement Calculators

Force at Point 1 using Pascal's Law
Go Force at Point 1 = Force at Point 2*(Area at Point 1/Area at Point 2)
Force at Point 2 using Pascal's Law
Go Force at Point 2 = Force at Point 1*(Area at Point 2/Area at Point 1)
Area at Point 1 using Pascal's Law
Go Area at Point 1 = Area at Point 2*(Force at Point 1/Force at Point 2)
Area at Point 2 using Pascal's Law
Go Area at Point 2 = Area at Point 1*(Force at Point 2/Force at Point 1)
Barometric Pressure or Atmospheric Pressure
Go Atmospheric Pressure = Density*[g]*Height of Mercury Column
Force acting on Surface
Go Force acting on Surface = Pressure Intensity*Area of Surface
Vacuum Pressure given Atmospheric Pressure
Go Vacuum Pressure = Atmospheric Pressure-Absolute Pressure
Gauge Pressure given Absolute Pressure
Go Gauge Pressure = Absolute Pressure-Atmospheric Pressure

Barometric Pressure or Atmospheric Pressure Formula

Atmospheric Pressure = Density*[g]*Height of Mercury Column
Patm = ρ*[g]*hm

What is Fluid Mechanics?

Fluid dynamics is “the branch of applied science that is concerned with the movement of liquids and gases”. It involves a wide range of applications such as calculating force & moments, determining the mass flow rate of petroleum through pipelines, predicting weather patterns, understanding nebulae in interstellar space, and modelling fission weapon detonation.

What is Viscosity?

Viscosity is a measure of a fluid’s resistance to flow. The SI unit of viscosity is poiseiulle (PI). Its other units are newton-second per square metre (N s m-2) or pascal-second (Pa s.). The viscosity of liquids decreases rapidly with an increase in temperature, and the viscosity of gases increases with an increase in temperature. Thus, upon heating, liquids flow more easily, whereas gases flow more slowly. Also, viscosity does not change as the amount of matter changes, therefore it is an intensive property.

How to Calculate Barometric Pressure or Atmospheric Pressure?

Barometric Pressure or Atmospheric Pressure calculator uses Atmospheric Pressure = Density*[g]*Height of Mercury Column to calculate the Atmospheric Pressure, The Barometric Pressure or Atmospheric Pressure formula is defined as the product of density of liquid filled in barometer, gravitational acceleration and height of mercury column above free surface. Atmospheric pressure is measured by a device called a barometer; thus, the atmospheric pressure is often referred to as the barometric pressure. The Italian Evangelista Torricelli (1608–1647) was the first to conclusively prove that the atmospheric pressure can be measured by inverting a mercury-filled tube into a mercury container that is open to the atmosphere. A frequently used pressure unit is the standard atmosphere, which is defined as the pressure produced by a column of mercury 760 mm in height at 0°C (𝜌 Hg = 13,595 kg/m3 ) under standard gravitational acceleration (g = 9.807 m/s2 ). If water instead of mercury were used to measure the standard atmospheric pressure, a water column of about 10.3 m would be needed. Atmospheric Pressure is denoted by Patm symbol.

How to calculate Barometric Pressure or Atmospheric Pressure using this online calculator? To use this online calculator for Barometric Pressure or Atmospheric Pressure, enter Density (ρ) & Height of Mercury Column (hm) and hit the calculate button. Here is how the Barometric Pressure or Atmospheric Pressure calculation can be explained with given input values -> 7432.931 = 997.3*[g]*0.76.

FAQ

What is Barometric Pressure or Atmospheric Pressure?
The Barometric Pressure or Atmospheric Pressure formula is defined as the product of density of liquid filled in barometer, gravitational acceleration and height of mercury column above free surface. Atmospheric pressure is measured by a device called a barometer; thus, the atmospheric pressure is often referred to as the barometric pressure. The Italian Evangelista Torricelli (1608–1647) was the first to conclusively prove that the atmospheric pressure can be measured by inverting a mercury-filled tube into a mercury container that is open to the atmosphere. A frequently used pressure unit is the standard atmosphere, which is defined as the pressure produced by a column of mercury 760 mm in height at 0°C (𝜌 Hg = 13,595 kg/m3 ) under standard gravitational acceleration (g = 9.807 m/s2 ). If water instead of mercury were used to measure the standard atmospheric pressure, a water column of about 10.3 m would be needed and is represented as Patm = ρ*[g]*hm or Atmospheric Pressure = Density*[g]*Height of Mercury Column. Density of a material shows the denseness of that material in a specific given area. This is taken as mass per unit volume of a given object & Height of Mercury Column is defined as the height of the mercury column above the free surface.
How to calculate Barometric Pressure or Atmospheric Pressure?
The Barometric Pressure or Atmospheric Pressure formula is defined as the product of density of liquid filled in barometer, gravitational acceleration and height of mercury column above free surface. Atmospheric pressure is measured by a device called a barometer; thus, the atmospheric pressure is often referred to as the barometric pressure. The Italian Evangelista Torricelli (1608–1647) was the first to conclusively prove that the atmospheric pressure can be measured by inverting a mercury-filled tube into a mercury container that is open to the atmosphere. A frequently used pressure unit is the standard atmosphere, which is defined as the pressure produced by a column of mercury 760 mm in height at 0°C (𝜌 Hg = 13,595 kg/m3 ) under standard gravitational acceleration (g = 9.807 m/s2 ). If water instead of mercury were used to measure the standard atmospheric pressure, a water column of about 10.3 m would be needed is calculated using Atmospheric Pressure = Density*[g]*Height of Mercury Column. To calculate Barometric Pressure or Atmospheric Pressure, you need Density (ρ) & Height of Mercury Column (hm). With our tool, you need to enter the respective value for Density & Height of Mercury Column and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
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