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  4. /Millimeters of Mercury to Torr Converter

Millimeters of Mercury to Torr Converter

Last updated: March 28, 2026

Calculator

Results

Pressure (Torr)

760.000108

torr

Pressure (Pa)

101,324.72

Pa

Pressure (atm)

1

atm

Results

Pressure (Torr)

760.000108

torr

Pressure (Pa)

101,324.72

Pa

Pressure (atm)

1

atm

The Millimeters of Mercury to Torr Converter converts pressure from millimeters of mercury (mmHg) to torr. For all practical purposes, 1 mmHg ≈ 1 torr — the difference is only about 0.000014%, which is negligible in virtually every application. However, they are technically defined differently, and this converter provides the precise conversion.

The millimeter of mercury is defined as the pressure exerted by a 1 mm column of mercury at 0°C under standard gravitational acceleration (9.80665 m/s²). This definition ties the unit to the physical properties of mercury: its density (13,595.1 kg/m³ at 0°C) and gravity. The torr, by contrast, is defined purely mathematically as exactly 1/760 of a standard atmosphere (101,325 Pa), giving 1 torr = 133.32237 Pa.

The slight discrepancy arises because the physical mmHg column produces a pressure of 133.32239 Pa (using mercury density at 0°C and standard gravity), which differs from the torr's exact value of 133.32237 Pa by about 0.000015%. This difference is far below the accuracy of any practical pressure measurement instrument.

In medicine, blood pressure is universally measured in mmHg, though the actual measurements are now made with digital sensors rather than mercury columns. Normal blood pressure readings of 120/80 mmHg are equally 120/80 torr. In vacuum science, torr is preferred. In meteorology, millimeters of mercury appears on some barometers, particularly in countries using the metric system. Our converter provides Pascal equivalents for those needing SI units.

Visual Analysis

How It Works

The formula: torr = mmHg × 1.000000142. In practice, torr ≈ mmHg since the difference is only 0.000014%. Both units are approximately 133.322 Pa.

For Pascals: Pa = mmHg × 133.322.

Understanding Your Results

Because mmHg and torr are nearly identical, reference values are the same for both: 760 mmHg = 760 torr = 1 atm, 120 mmHg = 120 torr (systolic blood pressure), 1 mmHg ≈ 1 torr ≈ 133.322 Pa.

Worked Examples

Standard Atmosphere

Inputs

mmhg760

Results

torr760.000108
pa101324.72

760 mmHg ≈ 760 torr = 1 atm

Blood Pressure

Inputs

mmhg120

Results

torr120.000017
pa15998.64

120 mmHg ≈ 120 torr

Frequently Asked Questions

For all practical purposes, yes. The difference is about 0.000014% — far below any instrument's accuracy. They are technically defined differently, but produce identical results in practice.

mmHg is defined by the physical properties of mercury (density at 0°C and standard gravity). Torr is defined mathematically as 1/760 of an atmosphere. These definitions produce slightly different values (133.32239 Pa vs 133.32237 Pa).

In medicine: mmHg (traditional). In vacuum science: torr (standard). In practice, the values are interchangeable.

Normal blood pressure is below 120/80 mmHg (systolic/diastolic). Hypertension (high blood pressure) is defined as sustained readings above 130/80 mmHg.

1 mmHg ≈ 133.322 Pa. Standard atmospheric pressure of 760 mmHg equals 101,325 Pa.

Historically, blood pressure was measured using mercury sphygmomanometers — the height of the mercury column directly indicated the pressure. The unit persists even though modern devices use electronic sensors.

760 mmHg = 1 atm = 101,325 Pa = 101.325 kPa = 1.01325 bar = 14.696 PSI = 29.921 inHg.

Yes, but torr is more standard in vacuum science. They give the same numerical values. Vacuum levels below 1 mmHg (torr) are common in laboratory applications.

It dates to Torricelli's 1643 barometer experiment. He observed that atmospheric pressure supported a mercury column about 760 mm high, establishing both the mmHg unit and the concept of atmospheric pressure.

Technically, the values differ by only 0.14 ppm. For any real-world application, you can treat mmHg and torr as identical. This converter exists for completeness and cases requiring absolute precision.

Sources & Methodology

BIPM SI Brochure (2019); NIST SP 811 (2008); Giacomo, P. (1982). 'Equation for the Determination of the Density of Moist Air'; ISO 80000-4:2019
R

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