Millimeter Mercury to Inch 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 — 760 mmHg at sea level. Nearly 400 years later, we still use his column height as a pressure unit in medicine and vacuum science.

For all practical purposes, they are identical — 1 torr = 1/760 atm ≈ 133.322 Pa, and 1 mmHg ≈ 133.322 Pa. The difference is about 0.00015% and arises from the torr being defined from the atmosphere while mmHg is defined from mercury density. Medicine uses mmHg; vacuum physics uses torr. They are interchangeable in any real-world measurement.

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.

American HVAC systems inherited the inch-pound measurement system, and duct static pressures fall neatly in the 0.1–4 inH₂O range — tidy numbers that are easy to read on a manometer or Magnehelic gauge. Converting to pascals (25–1,000 Pa) gives larger, less memorable values. Since the entire US supply chain — ductwork charts, fan curves, filter specs — is calibrated in inH₂O, switching would mean rewriting decades of engineering tables.

Total external static pressure should generally stay below 0.5 inH₂O for most residential furnaces. Supply-side static pressure is usually 0.2–0.3 inH₂O and return-side 0.1–0.2 inH₂O. Readings above 0.7 inH₂O indicate a problem — dirty filters, undersized ducts, or too many sharp bends. High static pressure forces the blower motor to work harder, raising energy bills and shortening equipment life.

1 inH₂O ≈ 249 Pa ≈ 0.0361 psi. The pascal conversion is handy for international specs: a 2 inH₂O reading is about 498 Pa. The psi conversion shows how small HVAC pressures are — 4 inH₂O is only 0.14 psi, which is why psi gauges are useless for duct work (the needle would barely leave zero). Inches of water occupy the Goldilocks zone for air-handling pressures.

It stands for "inches water gauge" — the same as inH₂O. "Gauge" means the reading is relative to atmospheric pressure (not absolute). You may also see "in. w.c." (inches water column). All three abbreviations — inH₂O, in. w.g., in. w.c. — refer to exactly the same unit. European equivalents would be listed in pascals or mmH₂O.

Yes, with a cheap U-tube manometer (under $20) or a digital differential pressure gauge. Drill a small test port in the supply and return plenums, connect the manometer with vinyl tubing, and read the water level difference. Many energy auditors and HVAC DIY forums recommend this as a first diagnostic step — high static pressure is the single most common cause of poor airflow and uneven room temperatures.