The triple point is the exact temperature and pressure at which a substance exists as a solid, liquid, and gas all at the same time. It’s not a range or a zone, but a single, precise point on a phase diagram where all three states of matter coexist in perfect equilibrium. For water, this happens at 0.01 °C and a pressure of about 611.7 Pascals, which is less than 1% of normal atmospheric pressure.
Why It’s a Single Fixed Point
The triple point isn’t something you can nudge. You can’t raise the temperature slightly and still keep all three phases in balance. This rigidity comes from a principle in thermodynamics called the phase rule, which calculates how many variables (like temperature or pressure) you’re free to change while keeping a system in equilibrium. For a single pure substance with three phases present, the math works out to zero degrees of freedom. That means both temperature and pressure are completely locked in place. Change either one, even slightly, and at least one phase disappears.
This is different from, say, a pot of water boiling on your stove. At boiling, you have two phases (liquid and gas), which gives you one degree of freedom. You can adjust the pressure and find a new boiling temperature. But at the triple point, there’s no wiggle room at all.
What It Looks Like in Practice
If you could watch a substance sitting at its triple point, you’d see something genuinely strange: the material appears to boil and freeze simultaneously. Bubbles of vapor form in the liquid while ice crystals grow at the same time. The three phases cycle between each other, with molecules constantly moving from solid to liquid to gas and back again, all while the temperature holds perfectly steady. It’s one of those rare physical phenomena that looks almost impossible until you understand the thermodynamics behind it.
Water’s Triple Point and Temperature Calibration
Water’s triple point has played a central role in how we measure temperature. For decades, the Kelvin scale was formally defined by assigning the triple point of water a value of exactly 273.16 K (0.01 °C). Because the triple point is so precisely fixed by physics, it gave scientists worldwide a perfectly reproducible reference temperature. No matter where you are or what equipment you use, pure water will always hit its triple point at the same conditions.
In 2019, the definition of the kelvin was updated. It’s now based on a fundamental physical constant (the Boltzmann constant) rather than a property of water. But the triple point of water didn’t lose its practical importance. Laboratories still use it daily to calibrate precision thermometers.
The device used for this is called a triple point cell: a sealed glass flask containing ultrapure water with all the air pumped out. You chill the cell overnight, then form a thin mantle of ice around an inner test tube. Once the ice, liquid water, and water vapor reach equilibrium inside the sealed flask, the cell sits at 0.01 °C with extraordinary stability. A platinum resistance thermometer inserted into the inner well will settle on the triple point within about an hour. From that single known temperature, the thermometer can be calibrated to measure any other temperature accurately. Even a homemade version using ordinary distilled water from a grocery store can produce surprisingly good results.
Carbon Dioxide: Why Dry Ice Doesn’t Melt
Not every substance has a triple point at low pressure like water does. Carbon dioxide’s triple point sits at about minus 56.6 °C and 5.18 bar, which is roughly five times normal atmospheric pressure. This detail explains something you’ve probably noticed: dry ice (solid CO₂) doesn’t melt into a puddle. It sublimates, going directly from solid to gas, skipping the liquid phase entirely.
At normal atmospheric pressure of about 1 bar, you’re well below the 5.18 bar needed to sustain liquid CO₂. So there’s simply no pressure regime at everyday conditions where liquid carbon dioxide can exist. To get liquid CO₂, you need a pressurized container. This is exactly what happens inside a CO₂ fire extinguisher, where the contents are stored at high enough pressure for the liquid phase to be stable.
Substances With Multiple Triple Points
The familiar triple point involves solid, liquid, and gas. But some substances have more than one solid form, with atoms or molecules arranged in different crystal structures. Each distinct crystal structure counts as a separate phase, which means a substance can have several triple points where different combinations of three phases meet.
Iron is a well-studied example. At everyday conditions, iron atoms arrange themselves in a body-centered cubic crystal pattern. Under extreme pressure, they shift to a hexagonal arrangement. At high temperatures, yet another crystal structure appears. Each boundary between these crystal forms creates the possibility of a new triple point. One of iron’s triple points, where two solid crystal forms meet the liquid phase, occurs at roughly 0.94 megabars (about 940,000 times atmospheric pressure) and around 2,970 °C. This particular triple point matters for geophysics because it helps scientists model what’s happening in Earth’s core, where iron exists under extreme pressure and temperature.
Reading a Phase Diagram
A phase diagram is a graph with pressure on the vertical axis and temperature on the horizontal axis. Lines on the diagram mark the boundaries where two phases coexist: solid-liquid, liquid-gas, and solid-gas. The triple point is where all three boundary lines converge into a single dot. To the left and below the triple point, you’re in the region where the substance sublimates directly from solid to gas. To the right and above, you can move through familiar melting and boiling transitions.
Because four or more phases of a single pure substance cannot all coexist at equilibrium, the triple point represents the maximum number of phases you’ll ever see together. The phase rule guarantees this: adding a fourth phase would require a negative number of degrees of freedom, which is physically impossible.
One useful takeaway from looking at a phase diagram is that whether a substance melts or sublimates depends entirely on whether the surrounding pressure is above or below the triple point pressure. Water’s triple point pressure is extremely low (611.7 Pa), so at any pressure we normally experience, ice melts into liquid before becoming vapor. Carbon dioxide’s triple point pressure is well above atmospheric pressure, so at normal conditions, the solid can only sublimate. The same underlying physics governs both substances; the only difference is where their triple points happen to fall.

