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Who Decides How Long a Second Is? The Science of Timekeeping

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The Quest to Define a Second: From Ancient Calendars to Atomic Clocks

Time, a fundamental aspect of our existence, has been measured and defined in various ways throughout history. But have you ever wondered how we arrived at the precise definition of a second we use today? The journey involves ancient civilizations, the spread of the Gregorian calendar, and the groundbreaking development of atomic clocks.

The Evolution of Time Measurement

  • Ancient Civilizations and the Night Sky: For most of human history, time was tracked using calendars based on the movements of celestial bodies.
  • The Gregorian Calendar: The concept of the second wasn't introduced until the late 1500s with the Gregorian calendar, which divided a day into 24 hours, each hour into 60 minutes, and each minute into 60 seconds.
  • A Mathematical Idea: Initially, the second was more of a theoretical concept than a practical unit of time. Measuring days and hours sufficed for most tasks in agrarian societies.

The Need for Precision

The advent of railways and interconnected cities necessitated a more precise agreement on timekeeping. By the 1950s, various global systems demanded that every second be accounted for with the utmost accuracy. This need for precision led scientists to explore the atomic scale.

Atomic Clocks: A New Foundation for Timekeeping

  • Harnessing the Laws of Physics: As early as 1955, researchers began developing atomic clocks, which rely on the unchanging laws of physics to establish a new foundation for timekeeping.
  • The Atom's Consistent Frequency: Atoms consist of negatively charged electrons orbiting a positively charged nucleus at a consistent frequency. This frequency can be harnessed for precise time measurement.
  • Tuning into Vibrations: By exposing an atom to an electromagnetic field, scientists can create a vibration that resembles a ticking pendulum. Unlike regular pendulums, electrons can maintain this "tick" for centuries.
  • Vaporizing Atoms for Consistency: To ensure consistency and ease of measurement, atoms are vaporized, converting them to a less interactive state without slowing down their remarkably fast ticking.
  • Unparalleled Resolution: Some atoms can oscillate over nine billion times per second, giving atomic clocks an unparalleled resolution for measuring time.
  • Consistency Across the Globe: Since every atom of a given elemental isotope is identical, researchers using the same element and electromagnetic wave can produce perfectly consistent clocks.

The Cesium-133 Standard

In 1967, the Thirteenth General Conference of the International Committee for Weights and Measures convened to determine which atom would be best suited for atomic timekeeping. The ideal element needed to possess:

  • Long-lived, high-frequency electron oscillation
  • Reliably measurable quantum spin
  • Simple energy level structure
  • Ease of vaporization

The winner was Cesium-133. By 1968, cesium clocks were commercially available.

Defining the Second

The conference then determined how many ticks of a cesium atom would constitute a second. Using the most precise astronomical measurement of a second available at the time, they formally defined one second as exactly 9,192,631,770 ticks of a cesium-133 atom.

The Impact of Atomic Clocks

Today, atomic clocks are used worldwide, from radio signal transmitters to satellites for global positioning systems. These devices have been synchronized to help us maintain a globally consistent time with unparalleled precision.

In conclusion, the definition of a second has evolved from ancient observations of the night sky to the precise measurement of atomic oscillations. Atomic clocks have revolutionized timekeeping, enabling us to maintain a globally consistent time with remarkable accuracy.