TED Talks · Level C2 Mixing
Who decides how long a second is
In 1967, researchers from around the world gathered to answer a long-running scientific question:
Level: C2 · 78 sentences
Transcript
- In 1967,
- researchers from around the world gathered to answer a long-running scientific question:
- just how long is a second?
- It might seem obvious at first.
- A second is the tick of a clock, the swing of a pendulum,
- the time it takes to count to one.
- But how precise are those measurements?
- What is that length based on?
- And how can we scientifically define this fundamental unit of time?
- For most of human history,
- ancient civilizations measured time with unique calendars
- that tracked the steady march of the night sky.
- In fact, the second as we know it wasn't introduced until the late 1500's,
- when the Gregorian calendar began to spread across the globe alongside British colonialism.
- The Gregorian calendar defined a day as a single revolution of the Earth about its axis.
- Each day could be divided into 24 hours,
- each hour into 60 minutes,
- and each minute into 60 seconds.
- However, when it was first defined,
- the second was more of a mathematical idea than a useful unit of time.
- Measuring days and hours was sufficient for most tasks in pastoral communities.
- It wasn't until society became interconnected through fast-moving railways
- that cities needed to agree on exact timekeeping.
- By the 1950's,
- numerous global systems required every second to be perfectly accounted for,
- with as much precision as possible.
- And what could be more precise than the atomic scale?
- As early as 1955,
- researchers began to develop atomic clocks,
- which relied on the unchanging laws of physics
- to establish a new foundation for timekeeping.
- An atom consists of negatively charged electrons
- orbiting a positively charged nucleus at a consistent frequency.
- The laws of quantum mechanics keep these electrons in place,
- but if you expose an atom to an electromagnetic field such as light or radio waves,
- you can slightly disturb an electron's orientation.
- And if you briefly tweak an electron at just the right frequency,
- you can create a vibration that resembles a ticking pendulum.
- Unlike regular pendulums that quickly lose energy,
- electrons can tick for centuries.
- To maintain consistency and make ticks easier to measure,
- researchers vaporize the atoms,
- converting them to a less interactive and volatile state.
- But this process doesn't slow down the atom's remarkably fast ticking.
- Some atoms can oscillate over nine billion times per second,
- giving atomic clocks an unparalleled resolution for measuring time.
- And since every atom of a given elemental isotope is identical,
- two researchers using the same element and the same electromagnetic wave
- should produce perfectly consistent clocks.
- But before timekeeping could go fully atomic,
- countries had to decide which atom would work best.
- This was the discussion in 1967,
- at the Thirteenth General Conference
- of the International Committee for Weights and Measures.
- There are 118 elements on the periodic table,
- each with their own unique properties.
- For this task, the researchers were looking for several things.
- The element needed to have long-lived and high frequency electron oscillation
- for precise, long-term timekeeping.
- To easily track this oscillation,
- it also needed to have a reliably measurable quantum spin,
- meaning the orientation of the axis about which the electron rotates,
- as well as a simple energy level structure,
- meaning the active electrons are few and their state is simple to identify.
- Finally, it needed to be easy to vaporize.
- The winning atom? Cesium-133.
- Cesium was already a popular element for atomic clock research,
- and by 1968, some cesium clocks were even commercially available.
- All that was left was to determine how many ticks of a cesium atom were in a second.
- The conference used the most precise astronomical measurement of a second available at the time,
- beginning with the number of days in a year and dividing down.
- When compared to the atom's ticking rate,
- the results formally defined one second
- as exactly 9,192,631,770 ticks of a cesium-133 atom.
- Today, atomic clocks are used all over the Earth and beyond it.
- From radio signal transmitters to satellites for global positioning systems,
- these devices have been synchronized to help us maintain a globally consistent time
- with precision that's second to none.