Millimeter Mercury to Meter Water (4 °C)

Clinical medicine is deeply conservative about units because misreadings kill people. Doctors, nurses, and patients worldwide have memorized "120/80 is normal" in mmHg. Converting to kPa (16.0/10.7) would require retraining millions of clinicians and rewriting every guideline. The WHO considered the switch and decided the risk of transcription errors during transition outweighed the elegance of SI compliance. So mmHg stays — likely for decades more.

The top number (systolic) is the peak pressure when the heart contracts and pushes blood into the arteries — typically 90–120 mmHg. The bottom number (diastolic) is the lowest pressure between beats when the heart relaxes — typically 60–80 mmHg. A reading of 140/90 mmHg or above is classified as hypertension. The gap between the two (pulse pressure) also matters: a wide gap above 60 mmHg may signal stiff arteries.

In 1643, Evangelista Torricelli filled a glass tube with mercury, inverted it into a dish of mercury, and watched the column drop to about 760 mm. The empty space above was the first laboratory vacuum. The height of the mercury column became the measurement of atmospheric pressure — approximately 760 mmHg at sea level. Nearly 400 years later, we still use his column height as a pressure unit in medicine and vacuum science.

They closely agree, but their definitions are different. One torr is exactly 1/760 of a standard atmosphere: 101,325/760 Pa, or approximately 133.322368421 Pa. The conventional mmHg instead adopts a mercury density of 13,595.1 kg/m³ and standard gravity of 9.80665 m/s², giving exactly 133.322387415 Pa for a 1 mm column. This converter preserves that full conventional factor, so 1 mmHg converts to approximately 1.000000142466 torr. Values such as 133.3224 Pa/mmHg in conversion tables are rounded approximations, not a different reference frame. The exactness belongs to the adopted convention, not to the accuracy of a real mercury barometer. Medicine commonly uses mmHg and vacuum science uses torr; precise conversions keep the units distinct.

Intraocular pressure (glaucoma screening): normal is 10–21 mmHg, above 21 is suspicious. Partial pressure of oxygen in arterial blood (PaO₂): normal is 80–100 mmHg. Central venous pressure: 2–6 mmHg. Intracranial pressure: normal below 15 mmHg, dangerous above 20 mmHg. Carbon dioxide in blood (PaCO₂): 35–45 mmHg. The unit pervades clinical monitoring far beyond the blood pressure cuff.

Because pump engineers think in terms of how high the pump can lift water. A pump rated at 30 mH₂O can push water 30 meters straight up — no conversion needed to figure out if it can reach the tenth floor. The unit also makes friction-loss calculations intuitive: if a 100-meter horizontal pipe run has 5 mH₂O of friction loss, you subtract that directly from the pump's head rating.

Approximately 1 meter in fresh water. The unit references water at 4 °C under standard gravity; actual column pressure depends on water density and local gravity, so a real pool does not necessarily reproduce that reference exactly. Seawater is about 2.5% denser, so 1 meter of seawater corresponds to roughly 1.025 mH₂O of gauge pressure.

Municipal water mains deliver 20–60 mH₂O (roughly 2–6 bar or 30–85 psi) at the meter. A gravity-fed rooftop tank 10 meters above the tap provides about 10 mH₂O — barely enough for a decent shower, which is why booster pumps are common in buildings with rooftop storage. High-rise buildings need pressurisation systems because gravity alone cannot push water above about 60 mH₂O without boosting.

10.33 mH₂O ≈ 1 atmosphere ≈ 1.013 bar. For quick math: 10 mH₂O ≈ 1 bar (error about 2%). This rule of thumb is used constantly in plumbing and fire protection: a building with a water tank 40 m above ground level has roughly 4 bar of static pressure at the base. Multiply meters by 0.1 and you have bar — close enough for pipe sizing.

Temperature affects water density and therefore column pressure. The 4 °C reference is close to water's maximum density and specifies the conditions for comparing water-column units. This converter uses the fixed reference density of 999.972 kg/m³ and standard gravity, producing 9,806.3754138 Pa per meter. The metric and imperial factors retain the complete result while preserving their exact height relationships. This computational precision does not imply that a real manometer reproduces the reference density or gravity exactly.