Explosive atmosphere zones 0, 1, 2 and 20, 21, 22 explained
Updated: 2026-08-13 · ISKRIT
A zone number answers one question only: how often, and for how long, an explosive atmosphere is present in that place. It says nothing about how large the zone is, and confusing the two is the most expensive mistake in area classification.
The three gas zones
Zone 0 is a place where an explosive gas or vapour atmosphere is present continuously or for long periods, conventionally more than 1000 hours a year. Zone 1 is a place where it is likely to occur occasionally in normal operation, between 10 and 1000 hours. Zone 2 is a place where it is not expected in normal operation and, if it occurs, persists only briefly, under 10 hours a year.
The hour figures are a convention rather than a measurement. In practice the zone follows from the grade of release: a continuous grade of release gives zone 0, a primary grade gives zone 1, a secondary grade gives zone 2, and the classification argument is about which grade a given source has.
The dust series
Dust gets a parallel series with the same logic: zone 20 for a cloud present continuously, zone 21 for one arising in normal operation, zone 22 for one arising only on a fault. Dust differs from gas in two ways that matter. A layer that is not airborne today can be raised into a cloud tomorrow, so housekeeping is part of the classification. And a dust only forms an explosive cloud at all if its lower explosive limit is low enough, in the range of tens of grams per cubic metre.
Fire-hazardous areas are a separate question
Not every place with combustibles has an explosive atmosphere. Combustible liquids with a high flash point, solid combustibles and fibres that never go airborne create a fire risk without an explosion risk, and Russian practice classifies them in their own series, P-I to P-III under federal law 123-FZ article 18, rather than forcing them into the explosive zones. The distinction is worth keeping in any jurisdiction: equipment selected for a dust cloud is not what a stack of pallets requires.
Ventilation moves the number
The same release in the same room classifies differently depending on how reliably the air moves. Good dilution with reliable ventilation can hold a secondary release at zone 2 or even leave the volume unclassified; poor dilution promotes it. This is why ventilation availability, graded as good, fair or poor, is an input to the classification and not an afterthought, and why an interlock that stops the process when a fan fails is a classification measure as much as a safety one.
Number against extent
The zone number and the zone extent are two separate results. The number comes from frequency and duration. The extent, the distance in metres to which the zone reaches, comes from a quantitative calculation of the release rate and the hypothetical volume of the flammable cloud under IEC 60079-10-1. A small release into a well ventilated space can be declared of negligible extent and the place treated as unclassified, while the same release in a still corner reaches several metres. Equipment cost follows the extent, which is why that calculation is the part the market charges for.
Questions
Does the zone number set the equipment category? Yes: zone 0 and 20 need category 1 equipment, zone 1 and 21 category 2, zone 2 and 22 category 3.
Is the inside of a tank a zone? Usually zone 0 for a flammable liquid, since the vapour space is above the explosive limit or within it for long periods.
Determine the zone class from the medium and the frequency of the mixture, alongside the room category and the printable signs, in the fire load density calculator.
Rotating shift patterns: covering the posts and balancing the hours
Calibration intervals: setting them, shortening them, defending them
Turning an estimate into a bill of quantities that foots
Progress billing: percent complete, carry-forward and retention
Checking claimed quantities: the design schedule and the survey
Pile capacity from CPT: how the LCPC method reads a cone trace
Driven and bored piles: why the same soil gives different capacity
What belongs on a borehole log, and what quietly gets left off
Drawing a cross section: correlating layers between boreholes
From an AGS4 file to a laboratory summary: what the groups carry
Characteristic values: turning a set of test results into one number
Void ratio, porosity and saturation from one density test
When one soil layer is really two: splitting geotechnical units
ASTM D4253 and D4254: maximum and minimum index density
Relative density Dr and density index Id are not the same number
USCS classification step by step: ASTM D2487
Cu and Cc: what the two gradation coefficients actually tell you
Dual symbols in USCS: the 5 to 12 percent fines band
EN ISO 14688-1 against USCS: two different size ladders
AGS4 file validation: what the rules actually check
AGS4 syntax: the five rules that break a delivery
ASTM D2435 oedometer test: from the curve to Cc, mv and Eoed
Converting oedometer modulus to Young’s modulus
EN ISO 17892-5 and ASTM D2435: where the two diverge
ASTM D1196 plate load test: modulus and subgrade reaction
DIN 18134: Ev1, Ev2 and the compaction ratio
Ménard pressuremeter modulus: ASTM D4719 and EN ISO 22476-4
Permeability from a pumping test: the Dupuit formulas
Shewhart control chart constants: A2, A3, B3, B4, D3, D4, d2, c4
The eight out of control tests on a Shewhart chart
Repeatability and reproducibility limits: where 2.77 comes from
How rebar cutting plans are optimised: the cutting stock problem
Cutting waste in rebar fabrication: what percentage is normal
Rebound hammer calibration: why the factory curve is not enough
Kerf and offcut: what a linear cutting plan has to account for
Earthwork volume from survey points: grid, TIN and cross sections
Fire load density: the formula, the calorific values and the traps
Pollution charges per tonne: how the over-limit multiplier works
The Russian environmental fee: who pays, when, and how the advances work