Sidereal Day to Planck Time Converter
Convert sidereal days to Planck times with our free online time converter.
Quick Answer
1 Sidereal Day = 1.598295e+48 Planck times
Formula: Sidereal Day × conversion factor = Planck Time
Use the calculator below for instant, accurate conversions.
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Sidereal Day to Planck Time Calculator
How to Use the Sidereal Day to Planck Time Calculator:
- Enter the value you want to convert in the 'From' field (Sidereal Day).
- The converted value in Planck Time will appear automatically in the 'To' field.
- Use the dropdown menus to select different units within the Time category.
- Click the swap button (⇌) to reverse the conversion direction.
How to Convert Sidereal Day to Planck Time: Step-by-Step Guide
Converting Sidereal Day to Planck Time involves multiplying the value by a specific conversion factor, as shown in the formula below.
Formula:
1 Sidereal Day = 1.5983e+48 Planck timesExample Calculation:
Convert 60 sidereal days: 60 × 1.5983e+48 = 9.5898e+49 Planck times
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View all Time conversions →What is a Sidereal Day and a Planck Time?
What Is a Sidereal Day?
A sidereal day is the time required for Earth to complete one full rotation (360 degrees) on its axis relative to the fixed background stars.
Precise value: 1 sidereal day = 86,164.0905 seconds (mean sidereal day) = 23 hours, 56 minutes, 4.0905 seconds
Sidereal vs. Solar Day
Sidereal day (stellar reference):
- Earth's rotation relative to distant stars
- Duration: 23h 56m 4.091s
- Used by astronomers for telescope pointing
Solar day (Sun reference):
- Earth's rotation relative to the Sun
- Duration: 24h 00m 00s (mean solar day)
- Used for civil timekeeping (clocks, calendars)
The difference: ~3 minutes 56 seconds
Why Are They Different?
The sidereal-solar day difference arises from Earth's orbital motion around the Sun:
- Start position: Earth completes one full 360° rotation relative to stars (1 sidereal day)
- Orbital motion: During that rotation, Earth has moved ~1° along its orbit around the Sun
- Extra rotation needed: Earth must rotate an additional ~1° (~4 minutes) to bring the Sun back to the same position in the sky
- Result: Solar day = sidereal day + ~4 minutes
Analogy: Imagine walking around a merry-go-round while it spins. If you walk one full circle relative to the surrounding park (sidereal), you'll need to walk a bit farther to return to the same position relative to the merry-go-round center (solar).
One Extra Day Per Year
A surprising consequence: There is one more sidereal day than solar day in a year!
- Solar year: 365.242199 solar days
- Sidereal year: 365.256363 sidereal days
- Extra sidereal days: 366.256363 - 365.242199 ≈ 1 extra day
Why? Earth makes 366.25 full rotations relative to the stars during one orbit, but we only experience 365.25 sunrises because we're moving around the Sun.
What is Planck Time?
Planck time (symbol: tP) is a fundamental unit of time in the Planck system of natural units, representing the time required for light traveling at speed c (the speed of light in vacuum) to traverse a distance of one Planck length (ℓP).
Mathematical definition:
tP = √(ℏG/c⁵)
Where:
- ℏ (h-bar) = reduced Planck constant = 1.054571817 × 10⁻³⁴ J·s
- G = gravitational constant = 6.67430 × 10⁻¹¹ m³/(kg·s²)
- c = speed of light in vacuum = 299,792,458 m/s (exact)
Numerical value:
tP ≈ 5.391247 × 10⁻⁴⁴ seconds
Or written out in full: 0.000000000000000000000000000000000000000000053912 seconds
Alternative calculation (from Planck length):
tP = ℓP / c
Where:
- ℓP = Planck length ≈ 1.616255 × 10⁻³⁵ meters
- c = speed of light ≈ 2.998 × 10⁸ m/s
This gives: tP ≈ 1.616 × 10⁻³⁵ m ÷ 2.998 × 10⁸ m/s ≈ 5.39 × 10⁻⁴⁴ s
Physical Significance
Planck time represents several profound concepts in physics:
1. Shortest meaningful time interval:
- Below Planck time, the uncertainty principle combined with general relativity makes the very concept of time measurement meaningless
- Energy fluctuations ΔE required to measure sub-Planck-time intervals would create black holes that obscure the measurement
2. Quantum gravity timescale:
- At durations approaching Planck time, quantum effects of gravity become comparable to other quantum effects
- Spacetime curvature fluctuates quantum-mechanically
- Classical smooth spacetime breaks down into "quantum foam"
3. Fundamental temporal quantum:
- Some theories (loop quantum gravity, causal sets) suggest time may be fundamentally discrete at the Planck scale
- Continuous time may be an emergent property valid only above Planck time
- Spacetime may consist of discrete "chronons" of duration ~tP
4. Cosmological boundary:
- The Planck epoch (0 to ~10⁻⁴³ s after Big Bang) is the earliest era describable only by a theory of quantum gravity
- Before ~1 Planck time after the Big Bang, our current physics cannot make predictions
Why Planck Time is a Limit
Heisenberg Uncertainty Principle + General Relativity:
To measure a time interval Δt with precision, you need energy uncertainty ΔE where:
ΔE · Δt ≥ ℏ/2
For extremely small Δt (approaching Planck time), the required ΔE becomes enormous:
ΔE ≈ ℏ/Δt
When Δt → tP, the energy ΔE becomes so large that:
ΔE/c² ≈ mP (Planck mass ≈ 2.18 × 10⁻⁸ kg)
This mass concentrated in a region of size ℓP (Planck length) creates a black hole with Schwarzschild radius comparable to ℓP, making measurement impossible—the measurement apparatus itself becomes a black hole that obscures what you're trying to measure!
Conclusion: You cannot meaningfully measure or discuss events happening faster than Planck time because the act of measurement destroys the very spacetime you're trying to probe.
Planck Time vs. Other Small Times
Planck time is incomprehensibly smaller than any directly measurable duration:
Attosecond (10⁻¹⁸ s):
- Shortest time intervals directly measured by physicists (attosecond laser pulses)
- 10²⁶ times longer than Planck time
- Used to study electron motion in atoms
Zeptosecond (10⁻²¹ s):
- Time for light to cross a hydrogen molecule
- 10²³ times longer than Planck time
- Measured in 2020 experiments
Chronon (hypothetical):
- Proposed discrete time quantum in some theories
- Possibly equal to Planck time (5.39 × 10⁻⁴⁴ s)
- Unproven experimentally
Planck time is to one second as one second is to ~10²⁶ times the age of the universe!
Natural Units and Dimensional Analysis
In Planck units (also called natural units), fundamental constants are set to 1:
- c = 1 (speed of light)
- ℏ = 1 (reduced Planck constant)
- G = 1 (gravitational constant)
- kB = 1 (Boltzmann constant, sometimes)
In this system:
- Planck time = 1 tP (the fundamental unit)
- Planck length = 1 ℓP
- Planck mass = 1 mP
- All physical quantities expressed as dimensionless ratios
Example: The age of the universe ≈ 4.35 × 10¹⁷ seconds ≈ 8 × 10⁶¹ tP (in Planck units)
Advantage: Equations simplify dramatically. Einstein's field equations become cleaner, and fundamental relationships emerge more clearly.
Disadvantage: Numbers become extremely large (for macroscopic phenomena) or extremely small (for everyday quantum phenomena), making intuitive understanding difficult.
Note: The Sidereal Day is part of the imperial/US customary system, primarily used in the US, UK, and Canada for everyday measurements. The Planck Time belongs to the imperial/US customary system.
History of the Sidereal Day and Planck Time
Ancient Observations (2000-300 BCE)
Babylonian astronomy (circa 2000-1500 BCE):
- Babylonian astronomers tracked stellar positions for astrological and calendrical purposes
- Noticed stars rose earlier each night relative to the Sun's position
- Created star catalogs showing this gradual eastward drift
Greek astronomy (circa 600-300 BCE):
- Thales of Miletus (624-546 BCE): Used stellar observations for navigation
- Meton of Athens (432 BCE): Discovered the 19-year Metonic cycle, reconciling lunar months with solar years
- Recognized that stellar year differed from seasonal year
Hipparchus and Precession (150 BCE)
Hipparchus of Nicaea (circa 190-120 BCE), one of history's greatest astronomers:
Discovery: By comparing ancient Babylonian star catalogs with his own observations, Hipparchus discovered precession of the equinoxes—the slow westward drift of the vernal equinox against the stellar background
Sidereal measurements: To detect this subtle effect (1 degree per 72 years), Hipparchus needed precise sidereal positions, implicitly understanding the sidereal day concept
Legacy: His work established the difference between:
- Sidereal year: One orbit relative to stars (365.256363 days)
- Tropical year: One cycle of seasons (365.242199 days)
The ~20-minute difference between these years arises from precession.
Ptolemy's Almagest (150 CE)
Claudius Ptolemy compiled Greek astronomical knowledge in the Almagest, including:
- Star catalogs with sidereal positions
- Mathematical models for predicting stellar rising times
- Understanding that stars complete one full circuit of the sky slightly faster than the Sun
Though Ptolemy's geocentric model was wrong, his sidereal observations were accurate and useful for centuries.
Islamic Golden Age (800-1400 CE)
Islamic astronomers refined sidereal timekeeping:
Al-Battani (850-929 CE):
- Measured the tropical year to high precision
- Created improved star catalogs using sidereal positions
Ulugh Beg (1394-1449 CE):
- Built the Samarkand Observatory with advanced instruments
- Produced star catalogs accurate to ~1 arcminute using sidereal measurements
Copernican Revolution (1543)
Nicolaus Copernicus (De revolutionibus orbium coelestium, 1543):
Heliocentric model: Placing the Sun (not Earth) at the center explained the sidereal-solar day difference:
- Earth rotates on its axis (sidereal day)
- Earth orbits the Sun (creating solar day difference)
- The 4-minute discrepancy results from Earth's ~1° daily orbital motion
This was strong evidence for heliocentrism, though it took decades for acceptance.
Kepler's Laws (1609-1619)
Johannes Kepler formulated laws of planetary motion using sidereal periods:
Third Law: The square of a planet's orbital period is proportional to the cube of its orbit's semi-major axis
Application: Calculating planetary positions required precise sidereal reference frames, not solar time
Rise of Telescopic Astronomy (1600s-1700s)
Galileo Galilei (1609):
- Telescopic observations required tracking celestial objects as they moved across the sky
- Sidereal time became essential for predicting when objects would be visible
Royal Observatory, Greenwich (1675):
- Founded by King Charles II with John Flamsteed as first Astronomer Royal
- Developed accurate sidereal clocks to time stellar transits
- Greenwich Mean Sidereal Time (GMST) became the astronomical standard
Paris Observatory (1667):
- French astronomers developed precision pendulum clocks for sidereal timekeeping
- Cassini family produced detailed planetary observations using sidereal coordinates
Precision Timekeeping (1800s)
19th century: Mechanical sidereal clocks achieved second-level accuracy:
Sidereal clock design: Modified to tick 366.2422/365.2422 times faster than solar clocks (accounting for the extra sidereal day per year)
Observatory operations: Major observatories (Greenwich, Paris, Harvard, Lick, Yerkes) used sidereal clocks as primary timekeeping for scheduling observations
Photography: Long-exposure astrophotography required tracking objects at the sidereal rate to prevent star trailing
IAU Standardization (1900s)
International Astronomical Union (IAU) formalized definitions:
Mean sidereal day: 86,164.0905 seconds (exactly, by definition)
Greenwich Mean Sidereal Time (GMST): Standard sidereal time referenced to Greenwich meridian
Vernal equinox reference: Traditional sidereal time measures Earth's rotation relative to the vernal equinox (intersection of celestial equator and ecliptic)
Modern Era: ICRF (1997-Present)
International Celestial Reference Frame (ICRF):
Problem: The vernal equinox shifts due to precession, making it an imperfect reference
Solution: ICRF uses ~300 distant quasars (billions of light-years away) as fixed reference points
Accuracy: Defines celestial positions to milliarcsecond precision
Atomic time: Sidereal time is now calculated from International Atomic Time (TAI) and Earth orientation parameters measured by Very Long Baseline Interferometry (VLBI)
Modern sidereal clocks: Digital, GPS-synchronized, automatically updated for Earth rotation variations
Max Planck and the Birth of Natural Units (1899-1900)
1899: Planck's Blackbody Radiation Problem
Max Planck was investigating blackbody radiation—the spectrum of light emitted by hot objects. Classical physics (Rayleigh-Jeans law) predicted infinite energy at short wavelengths (the "ultraviolet catastrophe"), which obviously didn't match experiments.
October 1900: Planck's Quantum Hypothesis
To resolve this, Planck proposed that energy is emitted in discrete packets (quanta):
E = hν
Where:
- E = energy of quantum
- h = Planck's constant ≈ 6.626 × 10⁻³⁴ J·s
- ν = frequency of radiation
This radical idea—energy quantization—launched quantum mechanics.
1899: Planck Derives Natural Units
While developing his theory, Planck realized he could define fundamental units using only universal constants, independent of human conventions:
Planck's original natural units:
- Planck length: ℓP = √(ℏG/c³) ≈ 1.616 × 10⁻³⁵ m
- Planck mass: mP = √(ℏc/G) ≈ 2.176 × 10⁻⁸ kg
- Planck time: tP = √(ℏG/c⁵) ≈ 5.391 × 10⁻⁴⁴ s
- Planck temperature: TP = √(ℏc⁵/Gk²B) ≈ 1.417 × 10³² K
Planck's 1899 statement:
"These necessarily retain their meaning for all times and for all civilizations, including extraterrestrial and non-human ones, and can therefore be designated as 'natural units.'"
Planck recognized these weren't practical units for measurement but represented fundamental scales where quantum effects (ℏ), gravity (G), and relativity (c) all become equally important.
Irony: Planck himself thought his quantum hypothesis was a temporary mathematical trick, not a fundamental truth. He spent years trying to eliminate the quantum from his theory, unaware he'd discovered one of physics' deepest principles!
Early Quantum Mechanics: Ignoring Planck Units (1900-1950s)
For the first half of the 20th century, physicists focused on developing quantum mechanics and general relativity as separate theories:
Quantum Mechanics (1900s-1930s):
- Bohr model (1913)
- Schrödinger equation (1926)
- Heisenberg uncertainty principle (1927)
- Dirac equation (1928)
- Quantum electrodynamics (1940s)
No gravity involved—Planck time seemed irrelevant.
General Relativity (1915-1950s):
- Einstein's field equations (1915)
- Black holes (Schwarzschild 1916, Kerr 1963)
- Expanding universe (Hubble 1929)
- Big Bang cosmology (Lemaître 1927, Gamow 1948)
No quantum mechanics involved—Planck time seemed irrelevant.
Problem: The two theories use incompatible frameworks:
- Quantum mechanics: Probabilistic, discrete, uncertainty principle
- General relativity: Deterministic, continuous, smooth spacetime
At normal scales, you can use one or the other. But at Planck scales (Planck time, Planck length), you need both simultaneously—and they clash!
John Wheeler and Quantum Foam (1950s-1960s)
1955: John Archibald Wheeler's Quantum Geometry
Princeton physicist John Wheeler began exploring what happens when quantum mechanics meets general relativity at extreme scales.
Wheeler's key insight (1955): At the Planck scale, spacetime itself undergoes quantum fluctuations, creating a foamy, turbulent structure he called "quantum foam" or "spacetime foam."
Quantum Foam visualization:
- At durations longer than Planck time: Spacetime appears smooth
- At durations approaching Planck time: Spacetime becomes violently fluctuating
- Virtual black holes constantly form and evaporate
- Wormholes appear and disappear
- Topology of space changes randomly
Wheeler (1957):
"At very small distances and times, the very structure of spacetime becomes foam-like, with quantum fluctuations creating and destroying tiny wormholes."
Significance of Planck time:
- Below tP, the concept of a fixed spacetime background breaks down
- Geometry itself becomes a quantum variable
- Time may not even be fundamental—could emerge from deeper, timeless quantum processes
1967: Wheeler coins "black hole"
Wheeler's work on extreme gravity (black holes) and quantum mechanics (uncertainty) converged at Planck scales, making Planck time a central concept in quantum gravity.
Big Bang Cosmology and the Planck Epoch (1960s-1980s)
1965: Cosmic Microwave Background Discovered
Penzias and Wilson detect CMB radiation, confirming Big Bang theory. Cosmologists trace the universe backward in time toward the initial singularity.
The Planck Epoch Problem:
Standard Big Bang cosmology describes:
- t = 10⁻⁴³ s (near Planck time): Universe extremely hot (~10³² K), quantum gravity dominates
- t = 10⁻³⁵ s: Electroweak unification breaks, inflation begins (possibly)
- t = 10⁻¹¹ s: Quark-gluon plasma forms
- t = 1 s: Nucleosynthesis begins (protons, neutrons form)
But before t ≈ 10⁻⁴³ s (the Planck epoch):
- General relativity predicts a singularity (infinite density, infinite curvature)
- Quantum mechanics says you can't have infinite precision (uncertainty principle)
- Our physics breaks down!
Conclusion: The Planck epoch (from t = 0 to t ≈ tP) is the ultimate frontier—we need quantum gravity to describe it, but we don't have a complete theory yet.
1970s-1980s:
- Inflation theory (Alan Guth, 1980): Exponential expansion possibly beginning near Planck time
- Hawking radiation (Stephen Hawking, 1974): Black holes evaporate quantum-mechanically, connecting quantum mechanics and gravity
- No-boundary proposal (Hartle-Hawking, 1983): Time may become space-like before Planck time, eliminating the initial singularity
String Theory and Loop Quantum Gravity (1980s-2000s)
Two major approaches to quantum gravity emerged, both treating Planck time as fundamental:
String Theory (1980s-present):
Core idea: Fundamental entities are 1-dimensional "strings" vibrating in 10 or 11 dimensions, not point particles.
Planck time significance:
- Strings have characteristic length ~Planck length, vibration period ~Planck time
- Below Planck time, spacetime may have extra compactified dimensions
- String interactions occur on timescales of Planck time
Predictions:
- Minimum measurable time ≈ Planck time (spacetime uncertainty relation)
- Smooth spacetime emerges only above Planck scale
Loop Quantum Gravity (1980s-present):
Core idea: Spacetime itself is quantized—space is a network of discrete loops (spin networks), time consists of discrete steps.
Planck time significance:
- Fundamental "quantum of time" is exactly Planck time
- Below Planck time, continuous time doesn't exist
- Time evolution proceeds in discrete jumps of tP
Predictions:
- Planck time is the smallest possible duration
- Big Bang singularity replaced by a "Big Bounce" occurring at Planck-scale densities
Current status (2024): Neither theory is experimentally confirmed. Both agree Planck time marks the limit of classical spacetime.
Modern Developments (2000s-Present)
2010s: Causal Set Theory
Proposal: Spacetime is fundamentally a discrete set of events (points) with causal relations, not a continuous manifold.
Planck time: Natural timescale for spacing between discrete events.
2015: Planck Satellite Data
ESA's Planck satellite measures cosmic microwave background with unprecedented precision, probing conditions at t ≈ 10⁻³⁵ s after Big Bang—still 9 orders of magnitude later than Planck time, but the closest we've ever looked to the beginning.
2020s: Quantum Gravity Phenomenology
Physicists search for testable predictions of quantum gravity effects:
- Modified dispersion relations for light (different colors travel at slightly different speeds over cosmic distances)
- Violations of Lorentz invariance at Planck scale
- Quantum fluctuations of spacetime affecting gravitational wave signals
No conclusive evidence yet, but experiments are improving.
Current understanding:
- Planck time is universally accepted as the boundary where quantum gravity becomes necessary
- No experiment will ever directly probe Planck time (would require particle colliders the size of galaxies!)
- Theoretical understanding remains incomplete—quantum gravity is one of physics' greatest unsolved problems
Common Uses and Applications: sidereal days vs Planck times
Explore the typical applications for both Sidereal Day (imperial/US) and Planck Time (imperial/US) to understand their common contexts.
Common Uses for sidereal days
1. Telescope Pointing and Tracking
Professional observatories use sidereal time to point telescopes:
Right Ascension (RA): Celestial equivalent of longitude, measured in hours of sidereal time (0h to 24h)
Local Sidereal Time (LST): The current RA crossing the meridian
Pointing formula: If LST = 18h 30m, objects with RA ≈ 18h 30m are currently at their highest point (zenith)
Tracking rate: Telescope motors rotate at the sidereal rate (1 rotation per 23h 56m 4s) to follow stars across the sky as Earth rotates
Example:
- Vega: RA = 18h 37m
- When LST = 18:37, Vega crosses the meridian (highest in sky)
- Observer can plan observations when object will be optimally placed
2. Astrophotography
Long-exposure astrophotography requires tracking at the sidereal rate:
Problem: Earth's rotation makes stars trail across the image during long exposures
Solution: Equatorial mounts with sidereal drive motors:
- Rotate at exactly 1 revolution per sidereal day
- Keep stars fixed in the camera's field of view
- Enables exposures of minutes to hours without star trailing
Adjustment: Solar rate ≠ sidereal rate; photographers must use sidereal tracking for stars, solar tracking for Sun/Moon
3. Satellite Orbit Planning
Satellite engineers use sidereal time for orbit design:
Sun-synchronous orbits: Satellites that always cross the equator at the same local solar time
- Orbital period is chosen to precess at the solar rate, not sidereal rate
Geosynchronous orbits: Satellites that hover over one point on Earth
- Orbital period = 1 sidereal day (23h 56m 4s)
- NOT 24 hours! Common misconception.
Molniya orbits: High-eccentricity orbits with period = 0.5 sidereal days for optimal high-latitude coverage
4. Very Long Baseline Interferometry (VLBI)
Radio astronomers use VLBI to achieve ultra-high resolution:
Technique: Combine signals from radio telescopes across continents
Timing requirement: Sidereal time must be synchronized to nanosecond precision across all telescopes
Result: VLBI can resolve features 1,000 times smaller than Hubble Space Telescope (angular resolution ~0.0001 arcseconds)
Application: Measures Earth's rotation variations by observing quasars at precise sidereal times
5. Navigation and Geodesy
Sidereal time is used for precise Earth orientation measurements:
Earth Orientation Parameters (EOPs):
- Polar motion (wobble of Earth's axis)
- UT1 (Earth rotation angle, related to Greenwich sidereal time)
- Length of day variations
GPS accuracy: GPS navigation requires knowing Earth's orientation to ~1 meter precision, necessitating sidereal time corrections
Tidal forces: Moon and Sun create tidal bulges that affect Earth's rotation, causing sidereal day variations at the millisecond level
6. Space Navigation
Spacecraft use sidereal reference frames:
Star trackers: Autonomous spacecraft orientation using star patterns
- Compare observed stellar positions with catalog
- Catalog uses sidereal coordinates (RA/Dec)
Interplanetary navigation: Voyager, New Horizons, and other deep-space probes navigate using sidereal reference frames (ICRF)
Mars rovers: Use Martian sidereal time ("sols") for mission planning
- 1 Mars sol = 24h 39m 35s (Mars rotates slower than Earth)
7. Amateur Astronomy
Amateur astronomers use sidereal time for planning:
Planispheres: Rotating star charts that show which constellations are visible at any given sidereal time and date
Computerized telescopes: GoTo mounts require accurate sidereal time for automatic star finding
Observation logs: Record sidereal time of observations for repeatability
When to Use Planck times
1. Theoretical Physics and Quantum Gravity
Primary use: Planck time defines the scale where quantum gravity effects become important.
String Theory:
- Fundamental strings have vibration modes with periods ~Planck time
- String interactions (splitting, joining) occur on Planck-time timescales
- Calculations use Planck time as the natural unit
Loop Quantum Gravity:
- Discrete time steps ("chronons") of duration Planck time
- Spacetime evolution proceeds in jumps of tP
- Continuous time is emergent approximation above Planck scale
Causal Set Theory:
- Discrete spacetime events separated by intervals ~Planck time
- Fundamental structure: causal relations between events, not continuous time
Quantum Foam Models:
- Virtual black holes form and evaporate on Planck-time timescales
- Spacetime topology fluctuates with characteristic time ~tP
All quantum gravity approaches treat Planck time as the fundamental temporal quantum.
2. Early Universe Cosmology (Planck Epoch)
The Planck Epoch: From Big Bang singularity to t ≈ 10⁻⁴³ seconds
Why it matters:
- Before ~tP, standard cosmology (general relativity) breaks down
- Conditions: Temperature ~10³² K, energy density ~10¹¹³ J/m³
- All four forces (gravity, electromagnetic, strong, weak) were unified
- Physics: Requires quantum gravity—no complete theory exists
Modern cosmological models:
Inflationary cosmology:
- Some models have inflation beginning near Planck time
- Exponential expansion may solve horizon and flatness problems
- Planck-scale quantum fluctuations seed later galaxy formation
Cyclic/Ekpyrotic models:
- Universe may undergo cycles of expansion and contraction
- "Bounce" at Planck-scale densities, avoiding singularity
- Planck time sets timescale for bounce
Quantum cosmology (Hartle-Hawking):
- "No-boundary proposal": Universe has no beginning, time becomes space-like before Planck time
- Planck time marks transition from Euclidean (imaginary time) to Lorentzian (real time) spacetime
Observational consequence: We can never directly observe the Planck epoch—it's forever hidden behind the opaque plasma of the early universe. Our best observations (CMB) reach back to ~380,000 years after Big Bang, billions of orders of magnitude later than Planck time.
3. Black Hole Physics
Schwarzschild radius and Planck mass:
A black hole with mass equal to Planck mass (mP ≈ 2.18 × 10⁻⁸ kg) has:
- Schwarzschild radius = 2GmP/c² ≈ Planck length (ℓP ≈ 1.62 × 10⁻³⁵ m)
- Light crossing time = ℓP/c ≈ Planck time (tP ≈ 5.39 × 10⁻⁴⁴ s)
Significance: Planck-mass black holes are the smallest possible black holes before quantum effects dominate.
Hawking radiation timescale:
Black holes evaporate via Hawking radiation. Evaporation time:
tevap ≈ (5120π/ℏc⁴) × G² M³
For Planck-mass black hole (M = mP):
tevap ≈ tP (approximately Planck time!)
Meaning: The smallest quantum black holes evaporate in about one Planck time—they're extremely short-lived.
Larger black holes:
- Solar-mass black hole (M☉ = 2 × 10³⁰ kg): tevap ≈ 10⁶⁷ years
- Supermassive black hole (10⁹ M☉): tevap ≈ 10¹⁰⁰ years (googol years)
Near the singularity: Deep inside a black hole, approaching the singularity, spacetime curvature becomes extreme. At distances ~Planck length from the singularity, quantum gravity effects on timescales ~Planck time become important. Classical general relativity predicts infinite curvature; quantum gravity (unknown) likely prevents true singularity.
4. Limits of Measurement and Computation
Heisenberg Uncertainty Principle:
To measure time interval Δt with energy uncertainty ΔE:
ΔE · Δt ≥ ℏ/2
For Δt = tP:
ΔE ≈ ℏ/(2tP) ≈ mPc² (Planck energy ≈ 10⁹ J)
Problem: This energy concentrated in a Planck-length region creates a black hole, making measurement impossible.
Conclusion: Planck time is the fundamental limit on time measurement precision.
Bremermann's limit (computational speed):
Maximum rate of information processing for a self-contained system of mass M:
Rate ≤ 2Mc²/ℏ (operations per second)
For mass confined to Planck length (creates Planck-mass black hole):
Maximum rate ≈ c⁵/ℏG = 1/tP ≈ 1.855 × 10⁴⁴ operations/second
Meaning: Planck time sets the absolute speed limit for any computational process—no computer, even in principle, can perform operations faster than ~10⁴⁴ per second per Planck mass of material.
Ultimate laptop: A 1 kg laptop operating at this maximum rate would:
- Perform 10⁵² operations/second (far beyond any current computer)
- Require energies approaching Planck scale (would become a black hole!)
- Theoretical limit only—physically impossible to approach
5. Dimensional Analysis and Natural Units
Fundamental equations simplify in Planck units (c = ℏ = G = 1):
Einstein's field equations:
Standard form: Gμν = (8πG/c⁴) Tμν
Planck units (G = c = 1): Gμν = 8π Tμν
Much simpler! Planck units reveal fundamental relationships without clutter of conversion factors.
Schwarzschild radius:
Standard: rs = 2GM/c² Planck units: rs = 2M (where M is in Planck masses)
Hawking temperature:
Standard: T = ℏc³/(8πGMkB) Planck units (also kB = 1): T = 1/(8πM)
Theoretical physics calculations: High-energy physicists and cosmologists often work in natural units where ℏ = c = 1, making Planck time the fundamental timescale. Results are later converted back to SI units for comparison with experiment.
6. Philosophy of Time
Is time fundamental or emergent?
Planck time raises profound questions about the nature of time itself:
Discrete time hypothesis:
- Some quantum gravity theories (loop quantum gravity, causal sets) suggest time consists of discrete "ticks" of duration ~Planck time
- Below Planck time, "time" doesn't exist—it's like asking what's north of the North Pole
- Continuous time is an illusion, valid only at scales >> Planck time
Emergent time hypothesis:
- Time may not be fundamental at all—could emerge from timeless quantum entanglement (Wheeler-DeWitt equation suggests timeless universe)
- Planck time marks the scale where the emergent approximation breaks down
- At Planck scale, "before" and "after" may be meaningless concepts
Block universe and eternalism:
- If spacetime is a 4D block (past, present, future all equally real), Planck time sets the "grain size" of this block
- Events separated by less than Planck time may not have well-defined temporal ordering
Implications for free will, causality: If time is discrete at Planck scale, does strict determinism hold? Or do quantum fluctuations at Planck time introduce fundamental randomness into time evolution?
These remain open philosophical and scientific questions.
7. Speculative Physics and Limits of Knowledge
Can we ever test Planck-scale physics?
Direct particle collider:
- Energy required: Planck energy ≈ 10⁹ J (≈ energy of lightning bolt, concentrated in one particle!)
- LHC (most powerful collider, 2024): 10⁴ TeV = 1.6 × 10⁻⁶ J per collision
- Shortfall: Need 10¹⁵ times more energy
- Size: Planck-energy collider would need radius ~10¹³ light-years (larger than observable universe!)
Indirect observations:
Quantum gravity phenomenology:
- Search for deviations from standard physics caused by Planck-scale effects
- Example: Lorentz invariance violation—different photon colors travel at slightly different speeds due to quantum foam
- Current limits: No violations detected, but experiments improving
Gravitational waves:
- LIGO/Virgo detect spacetime ripples from black hole mergers
- Future detectors might detect quantum fluctuations of spacetime at Planck scale
- Challenge: Effects are stupendously small
Cosmic microwave background:
- CMB fluctuations may preserve imprint of Planck-epoch quantum fluctuations
- Planck satellite (2013-2018) measured CMB with unprecedented precision
- Indirect window into physics near Planck time, but not direct observation
Conclusion: We will likely never directly probe Planck time experimentally. Understanding Planck-scale physics requires theoretical breakthroughs (complete quantum gravity theory), not bigger experiments.
Additional Unit Information
About Sidereal Day (sidereal day)
How long is a sidereal day in standard time?
Answer: 23 hours, 56 minutes, 4.091 seconds (or 86,164.091 seconds)
This is the time for Earth to rotate exactly 360 degrees relative to distant stars.
Precise value: 1 mean sidereal day = 86,164.0905 seconds
Comparison to solar day:
- Solar day: 86,400 seconds (24 hours)
- Sidereal day: 86,164.091 seconds
- Difference: ~236 seconds shorter (~3 min 56 sec)
Important: This is the mean sidereal day. Earth's actual rotation rate varies slightly (milliseconds) due to tidal forces, atmospheric winds, earthquakes, and core-mantle coupling.
Why is a sidereal day shorter than a solar day?
Answer: Because Earth orbits the Sun while rotating—requiring extra rotation to bring the Sun back to the same sky position
Step-by-step explanation:
-
Starting point: The Sun is directly overhead (noon)
-
One sidereal day later (23h 56m 4s): Earth has rotated exactly 360° relative to stars
- But Earth has also moved ~1° along its orbit around the Sun
- The Sun now appears slightly east of overhead
-
Extra rotation needed: Earth must rotate an additional ~1° (taking ~4 minutes) to bring the Sun back overhead
-
Result: Solar day (noon to noon) = sidereal day + ~4 minutes = 24 hours
Orbital motion causes the difference: Earth moves ~1°/day along its 365-day orbit (360°/365 ≈ 0.986°/day). This ~1° requires ~4 minutes of extra rotation (24 hours / 360° ≈ 4 min/degree).
Consequence: Stars rise ~4 minutes earlier each night relative to solar time, shifting ~2 hours per month, completing a full cycle annually.
Is sidereal time the same everywhere on Earth?
Answer: No—Local Sidereal Time (LST) depends on longitude, just like solar time zones
Key concepts:
Local Sidereal Time (LST): The Right Ascension (RA) currently crossing your local meridian
- Different at every longitude
- Changes by 4 minutes for every 1° of longitude
Greenwich Mean Sidereal Time (GMST): Sidereal time at 0° longitude (Greenwich meridian)
- Global reference point, like GMT/UTC for solar time
Conversion: LST = GMST ± longitude offset
- Positive (add) for east longitudes
- Negative (subtract) for west longitudes
Example:
- GMST = 12:00
- New York (74°W): LST = 12:00 - (74°/15) = 07:04
- Tokyo (139.75°E): LST = 12:00 + (139.75°/15) = 21:19
Duration is universal: A sidereal day (23h 56m 4s) is the same length everywhere—only the current sidereal time differs by location.
Do geosynchronous satellites orbit every 24 hours or 23h 56m?
Answer: 23h 56m 4s (one sidereal day)—NOT 24 hours!
This is one of the most common misconceptions about satellites.
The physics: For a satellite to remain above the same point on Earth's surface, it must orbit at Earth's rotational rate relative to the stars, not relative to the Sun.
Why sidereal?
- Earth rotates 360° in one sidereal day (23h 56m 4s)
- Satellite must complete 360° orbit in the same time
- This keeps satellite and ground point aligned relative to the stellar background
If orbit were 24 hours: The satellite would complete one orbit in one solar day, but Earth would have rotated 360° + ~1° (relative to stars) during that time. The satellite would drift ~1° westward per day, completing a full circuit westward in one year!
Geostationary orbit specifics:
- Altitude: 35,786 km above equator
- Period: 23h 56m 4.091s (1 sidereal day)
- Velocity: 3.075 km/s
Common examples: Communications satellites, weather satellites (GOES, Meteosat)
How many sidereal days are in a year?
Answer: Approximately 366.25 sidereal days—one MORE than the number of solar days!
Precise values:
- Tropical year (season to season): 365.242199 mean solar days
- Sidereal year (star to star): 365.256363 mean solar days
- Sidereal days in tropical year: 366.242199 sidereal days
One extra day: There is exactly one more complete rotation relative to stars than we experience sunrises.
Why?
- Earth makes 366.25 complete 360° rotations relative to stars per year
- But we experience only 365.25 sunrises because we orbit the Sun
- One rotation is "used up" by Earth's orbit around the Sun
Thought experiment: Stand on a rotating platform while walking around a lamp. If you walk one complete circle around the lamp (1 orbit), you'll have spun around 2 complete times relative to the room walls (2 rotations): 1 from walking the circle + 1 from the platform spinning.
Can I use a regular clock to tell sidereal time?
Answer: Not directly—sidereal clocks run about 4 minutes faster per day than solar clocks
Clock rate difference:
- Solar clock: Completes 24 hours in 1 solar day (86,400 seconds)
- Sidereal clock: Completes 24 sidereal hours in 1 sidereal day (86,164.091 seconds)
- Rate ratio: 1.00273791 (sidereal clock ticks ~0.27% faster)
Practical result: After one solar day:
- Solar clock reads: 24:00
- Sidereal clock reads: 24:03:56 (3 min 56 sec ahead)
Modern solutions:
- Sidereal clock apps: Smartphone apps calculate LST from GPS location and atomic time
- Planetarium software: Stellarium, SkySafari show current LST
- Observatory systems: Automated telescopes use GPS-synchronized sidereal clocks
Historical: Mechanical sidereal clocks used gear ratios of 366.2422/365.2422 to run at the correct rate
You can calculate: LST from solar time using formulas, but it's complex (requires Julian Date, orbital mechanics)
Why do astronomers use sidereal time instead of solar time?
Answer: Because celestial objects return to the same position every sidereal day, not solar day
Astronomical reason:
Stars and galaxies are so distant they appear "fixed" in the sky:
- A star at RA = 18h 30m crosses the meridian at LST = 18:30 every sidereal day
- Predictable, repeatable observations
If using solar time: Stars would cross the meridian ~4 minutes earlier each night, requiring daily recalculation of observation windows
Practical advantages:
1. Simple telescope pointing:
- Object's RA directly tells you when it's overhead (LST = RA)
- No date-dependent calculations needed
2. Repeatable observations:
- "Observe target at LST = 22:00" means the same sky position regardless of date
3. Right Ascension coordinate system:
- Celestial longitude measured in hours/minutes of sidereal time (0h to 24h)
- Aligns naturally with Earth's rotation
4. Tracking rate:
- Telescopes track at sidereal rate (1 revolution per 23h 56m 4s)
- Keeps stars fixed in the field of view
Historical: Before computers, sidereal time made astronomical calculations much simpler
What is the difference between a sidereal day and a sidereal year?
Answer: A sidereal day measures Earth's rotation; a sidereal year measures Earth's orbit
Sidereal Day:
- Definition: Time for Earth to rotate 360° on its axis relative to stars
- Duration: 23h 56m 4.091s (86,164.091 seconds)
- Reference: Distant "fixed" stars
- Use: Telescope tracking, astronomy observations
Sidereal Year:
- Definition: Time for Earth to orbit 360° around the Sun relative to stars
- Duration: 365.256363 days (365d 6h 9m 9s)
- Reference: Position relative to distant stars (not seasons)
- Use: Orbital mechanics, planetary astronomy
Key distinction:
- Day = rotation (Earth spinning)
- Year = revolution (Earth orbiting)
Tropical vs. Sidereal Year:
- Tropical year: 365.242199 days (season to season, used for calendars)
- Sidereal year: 365.256363 days (star to star)
- Difference: ~20 minutes, caused by precession of Earth's axis
The 20-minute precession effect: Earth's axis wobbles with a 26,000-year period, causing the vernal equinox to shift ~50 arcseconds/year westward against the stellar background. This makes the tropical year (equinox to equinox) slightly shorter than the sidereal year (star to star).
Does the Moon have a sidereal day?
Answer: Yes—the Moon's sidereal day is 27.322 Earth days, but it's tidally locked to Earth
Moon's sidereal rotation: Time for Moon to rotate 360° relative to stars = 27.322 days
Tidal locking: The Moon's rotation period equals its orbital period around Earth (both 27.322 days)
Consequence: The same face of the Moon always points toward Earth
- We only see ~59% of Moon's surface from Earth (libration allows slight wobbling)
- The "far side" never faces Earth
Moon's "solar day" (lunar day):
- Time from sunrise to sunrise on Moon's surface: 29.531 Earth days
- Different from Moon's sidereal day (27.322 days) for the same reason Earth's solar day differs from sidereal day
- Moon orbits Earth while rotating, requiring extra rotation to bring the Sun back to the same position
Lunar missions: Apollo missions and rovers used "lunar days" for mission planning—each day-night cycle lasts ~29.5 Earth days (2 weeks daylight, 2 weeks night)
How is sidereal time measured today?
Answer: Using atomic clocks, GPS, and Very Long Baseline Interferometry (VLBI) observations of distant quasars
Modern measurement system:
1. International Atomic Time (TAI):
- Network of ~450 atomic clocks worldwide
- Defines the second with nanosecond precision
- Provides base timescale
2. UT1 (Universal Time):
- Earth's rotation angle (actual rotation measured continuously)
- Monitored by VLBI observations of quasars
3. VLBI technique:
- Radio telescopes across continents simultaneously observe distant quasars
- Time differences reveal Earth's exact orientation
- Accuracy: ~0.1 milliseconds (0.005 arcseconds rotation)
4. ICRF (International Celestial Reference Frame):
- Defines "fixed" stellar background using ~300 quasars billions of light-years away
- Replaces older vernal equinox reference (which shifts due to precession)
5. GPS satellites:
- Amateur astronomers and observatories use GPS for accurate time and location
- Software calculates LST from UTC, GPS coordinates, and Earth orientation parameters
Calculation chain:
- Atomic clocks provide UTC
- Earth orientation parameters (EOP) give UT1
- Sidereal time formulas convert UT1 → GMST
- Longitude correction gives LST
Accuracy: Modern systems know Earth's orientation to ~1 centimeter (as a position on Earth's surface), requiring sidereal time precision of ~0.001 seconds
Why so complex? Earth's rotation is not uniform:
- Tidal forces (Moon/Sun) slow rotation by ~2.3 ms/century
- Atmospheric winds cause daily variations (milliseconds)
- Earthquakes can shift rotation by microseconds
- Core-mantle coupling affects long-term drift
Continuous monitoring ensures astronomical observations remain accurate.
Will sidereal time ever be replaced by something else?
Answer: Unlikely—it's fundamental to astronomy, tied directly to Earth's rotation and stellar positions
Why sidereal time persists:
1. Physical basis: Directly tied to Earth's rotation relative to the universe
- Not an arbitrary human convention like time zones
- Essential for understanding celestial mechanics
2. Coordinate system: Right Ascension (celestial longitude) is measured in sidereal hours
- All star catalogs, telescope systems, and astronomical databases use RA/Dec
- Replacing it would require re-cataloging billions of objects
3. Telescope tracking: All telescope mounts track at the sidereal rate
- Mechanically and electronically built into equipment
- Solar tracking is used only for Sun/Moon
4. International standards: IAU, observatories, space agencies globally use sidereal time
- Standardized formulas and software
5. No alternative needed: Sidereal time does its job perfectly for astronomy
Evolution, not replacement:
- Old reference: Vernal equinox (shifts due to precession)
- New reference: ICRF quasars (effectively fixed)
- Future: Increasingly precise atomic timescales and Earth rotation monitoring
Non-astronomical contexts: Civil society will continue using solar time (UTC) for daily life—there's no need for most people to know sidereal time
Conclusion: Sidereal time is here to stay as long as humans do astronomy from Earth. Even space-based observatories use sidereal coordinate systems for consistency with ground observations.
About Planck Time (tP)
What is the value of Planck time in seconds?
Planck time (tP) = 5.391247 × 10⁻⁴⁴ seconds (approximate value based on current measurements of fundamental constants).
Written in full decimal notation: 0.000000000000000000000000000000000000000000053912 seconds
This is derived from fundamental constants:
tP = √(ℏG/c⁵)
Where:
- ℏ = reduced Planck constant = 1.054571817 × 10⁻³⁴ J·s
- G = gravitational constant = 6.67430 × 10⁻¹¹ m³/(kg·s²)
- c = speed of light = 299,792,458 m/s (exact by definition)
Uncertainty: Because G is the least precisely known fundamental constant (~0.002% uncertainty), Planck time has corresponding uncertainty. Future more precise measurements of G will refine the Planck time value slightly.
Is Planck time the absolute shortest possible time?
It's complicated—Planck time may be the shortest meaningful time, but whether it's the absolute shortest possible time depends on the true nature of quantum gravity, which we don't yet understand.
Three perspectives:
1. Epistemological limit (what we can know):
- Yes, effectively: Below Planck time, quantum uncertainty prevents any measurement or observation
- Energy needed to probe sub-Planck durations creates black holes that obscure the measurement
- Planck time is the shortest duration we can ever meaningfully discuss or measure
2. Ontological limit (what exists) - Discrete time hypothesis:
- Maybe: Some quantum gravity theories (loop quantum gravity, causal sets) suggest time is fundamentally quantized
- Minimum time step = Planck time (or close to it)
- Below tP, "time" doesn't exist—like asking "what's half a photon?"
- Continuous time is an emergent approximation above Planck scale
3. Continuous time hypothesis:
- No: Time remains fundamentally continuous even below Planck scale
- Planck time merely marks where our current theories (QM + GR) break down
- A complete theory of quantum gravity might describe physics at arbitrarily small durations
- Planck time is a practical limit, not an absolute one
Current status: We don't have experimental evidence or complete theory to decide between these options. Most physicists lean toward discrete or emergent time, but it remains an open question.
Analogy: Is absolute zero (0 K) the coldest possible temperature? Yes, in the sense that you can't extract more energy from a system with zero thermal energy. Similarly, Planck time may be the "absolute zero" of duration—the limit below which "colder" (shorter) loses meaning.
Can we ever measure Planck time directly?
No—direct measurement of Planck time is almost certainly impossible, both practically and fundamentally.
Practical impossibility:
To probe Planck-time durations requires energies approaching Planck energy (EP ≈ 10⁹ J = energy in 1 billion joules):
Energy needed: EP = mPc² ≈ 2 × 10⁹ J (equivalent to ~500,000 kWh, or burning 60,000 kg of gasoline, in a single particle!)
Current capability:
- LHC (Large Hadron Collider): ~10⁴ TeV = 1.6 × 10⁻⁶ J per collision
- Shortfall: Need 10¹⁵ times more energy per particle
Required collider size:
- To reach Planck energy: Collider circumference ~10¹³ light-years
- Observable universe diameter: ~10¹⁰ light-years
- Impossible: Collider would need to be 1,000 times larger than the observable universe!
Fundamental impossibility:
Even if you had unlimited resources:
Heisenberg + General Relativity:
- To measure time Δt = tP, you need energy uncertainty ΔE ≈ ℏ/tP ≈ Planck energy
- This energy in a region of size ℓP (Planck length) creates a black hole with event horizon ~ℓP
- The black hole obscures the very measurement you're trying to make!
Conclusion: The act of measuring Planck time destroys the measurement apparatus (turns it into a black hole), making the measurement impossible even in principle.
Indirect observation (maybe):
We might observe effects of Planck-scale physics indirectly:
- Quantum gravity corrections to particle physics
- Spacetime quantum fluctuations affecting gravitational waves
- Violations of Lorentz invariance at extreme energies
- CMB signatures of Planck-epoch quantum fluctuations
But even these require significant technological advances and may be undetectable in practice.
How does Planck time relate to the Big Bang?
Planck time defines the earliest comprehensible moment of the universe—the Planck Epoch.
The Planck Epoch: From t = 0 (Big Bang singularity) to t ≈ 10⁻⁴³ seconds (few Planck times)
What happened (speculative, no complete theory exists):
At t < tP (before ~1 Planck time):
- Our current physics (general relativity + quantum mechanics) completely breaks down
- Temperature: ~10³² K (Planck temperature)
- Energy density: ~10¹¹³ J/m³
- All four fundamental forces (gravity, electromagnetic, strong nuclear, weak nuclear) were unified into a single force
- Spacetime may not have existed in recognizable form—possibly "quantum foam" with no classical geometry
- We cannot describe what occurred—requires complete theory of quantum gravity
At t ≈ tP to 10⁻⁴³ s (Planck epoch end):
- Quantum gravity effects dominate
- Universe expands, cools slightly
- Gravity begins to separate from other forces (possibly)
- Spacetime geometry emerges from quantum state (maybe)
At t > 10⁻⁴³ s (post-Planck epoch):
- Gravity is distinct force
- Spacetime becomes classical (smooth, continuous)
- Standard cosmology (general relativity) takes over
- Universe continues expanding and cooling through GUT epoch, electroweak epoch, etc.
Key insight: The Planck epoch is the ultimate "cosmic censorship"—we can never observe or calculate what happened before ~tP. The earliest observable universe (CMB from t ≈ 380,000 years) is trillions upon trillions of times later than Planck time.
Theoretical models:
Inflationary cosmology:
- Exponential expansion may begin near Planck time
- Quantum fluctuations at Planck scale seed galaxies billions of years later
Quantum cosmology (Hartle-Hawking):
- "No-boundary proposal": Universe has no t = 0 singularity
- Before Planck time, time dimension becomes space-like (imaginary time)
- Universe emerges from "nothing" spontaneously via quantum tunneling
Loop quantum cosmology:
- Big Bang singularity replaced by "Big Bounce"
- Universe contracts to Planck-scale densities, then bounces back
- Bounce occurs on timescale ~Planck time
All speculative—we don't have observational evidence to distinguish these models.
Why do we need quantum gravity to understand Planck time?
Because at Planck scales, both quantum mechanics and general relativity are essential, but they're mathematically incompatible—we need a unified theory.
Quantum mechanics (QM) alone:
- Describes microscopic world (atoms, particles)
- Fundamental features: Uncertainty principle, superposition, probability
- Ignores gravity (assumes flat spacetime background)
- Fails at Planck scale: Doesn't account for spacetime curvature
General relativity (GR) alone:
- Describes gravity as curved spacetime
- Deterministic, continuous, smooth geometry
- No quantum uncertainty
- Fails at Planck scale: Predicts infinite curvature (singularities), which quantum uncertainty forbids
Why both matter at Planck scale:
Energy scales: At Planck time (tP ≈ 5.39 × 10⁻⁴⁴ s), characteristic energy is Planck energy:
EP ≈ ℏ/tP ≈ 10⁹ J (per particle!)
This energy:
- Requires quantum mechanics: Massive energy fluctuations → quantum uncertainty dominates
- Requires general relativity: EP/c² = Planck mass concentrated in Planck volume → extreme spacetime curvature
Incompatibility:
QM says: Spacetime is a fixed background; particles have uncertain positions/energies GR says: Spacetime itself is dynamic; matter curves spacetime
At Planck scale:
- Energy fluctuations (QM) create spacetime curvature (GR)
- Spacetime curvature (GR) affects energy measurements (QM)
- Circular feedback: Spacetime and quantum fields affect each other
- Neither theory accounts for this—they're fundamentally incompatible!
What quantum gravity must do:
A complete theory of quantum gravity must:
- Unify QM and GR into single consistent framework
- Describe spacetime as quantum entity (subject to uncertainty)
- Resolve singularities (black holes, Big Bang) using quantum effects
- Predict what happens at and below Planck time
Candidate theories (incomplete):
- String theory
- Loop quantum gravity
- Causal dynamical triangulations
- Asymptotic safety
- None fully tested or universally accepted
Bottom line: Planck time marks the boundary where our two best theories clash. Understanding physics at Planck time requires solving one of physics' deepest unsolved problems: quantum gravity.
What is the Planck length, and how does it relate to Planck time?
Planck length (ℓP) is the shortest meaningful distance in physics, and it relates to Planck time through the speed of light.
Definition:
ℓP = √(ℏG/c³) ≈ 1.616255 × 10⁻³⁵ meters
Written out: 0.000000000000000000000000000000000016163 meters
Relationship to Planck time:
tP = ℓP / c
Where c = speed of light ≈ 3 × 10⁸ m/s
Physical meaning: Planck time is the duration light takes to travel one Planck length in vacuum.
Calculation: tP = (1.616 × 10⁻³⁵ m) / (2.998 × 10⁸ m/s) ≈ 5.39 × 10⁻⁴⁴ s ✓
Interpretation:
- Planck length and Planck time define the fundamental "pixel size" and "frame rate" of spacetime (if spacetime is discrete)
- Below ℓP and tP, spacetime quantum fluctuations dominate
- Just as tP is shortest meaningful time, ℓP is shortest meaningful distance
Scale comparison:
Planck length to familiar sizes:
- Planck length to proton diameter (~10⁻¹⁵ m): Like proton to 100 light-years!
- Planck length to human hair (10⁻⁴ m): Like atom to observable universe!
Planck length is to an atom as an atom is to the solar system.
Why both matter: Quantum gravity effects become important when:
- Spatial scale ≈ Planck length, AND/OR
- Temporal scale ≈ Planck time, AND/OR
- Energy scale ≈ Planck energy, AND/OR
- Mass density ≈ Planck density (ρP ≈ 5.16 × 10⁹⁶ kg/m³)
All are related by fundamental constants (ℏ, G, c).
Can time exist below the Planck time scale?
We honestly don't know—this is one of the deepest open questions in physics.
Three possibilities:
1. Discrete time (time is quantized):
- Hypothesis: Time consists of indivisible "chronons" of duration tP (or close to it)
- Below tP, time doesn't exist—like asking "what's between two adjacent integers?"
- Continuous time is an emergent approximation above Planck scale
- Support: Loop quantum gravity, causal set theory
- Analogy: Digital video (24 fps) appears continuous, but consists of discrete frames
2. Continuous but unobservable time:
- Hypothesis: Time remains fundamentally continuous down to arbitrarily small durations
- Planck time is merely the limit of observability, not existence
- A complete quantum gravity theory might describe sub-Planck processes
- Support: Some string theory approaches, continuous manifold models
- Analogy: You can't see atoms with naked eye, but they exist; maybe sub-Planck time exists but is unobservable
3. Emergent time (time is not fundamental):
- Hypothesis: Time emerges from timeless quantum entanglement or other structures
- At Planck scale, "time" concept breaks down completely
- The question "does time exist below tP?" is meaningless—like asking the temperature of a single atom
- Support: Wheeler-DeWitt equation (timeless Schrödinger equation for universe), some quantum gravity approaches
- Analogy: Temperature emerges from molecular motion; below certain scales, "temperature" loses meaning. Similarly, "time" may emerge from deeper physics.
Experimental evidence: None yet. We have no way to test these ideas with current technology.
Theoretical status: Different quantum gravity theories make different assumptions, but none are complete or experimentally confirmed.
Philosophical implication: If time is discrete or emergent, it has profound consequences:
- Free will and determinism
- Nature of causality
- Beginning of universe (what does "beginning" mean if time is quantized?)
Honest answer: We don't know if time exists below Planck time. It's one of the most exciting frontiers in physics!
How was Planck time calculated?
Planck time is calculated using dimensional analysis on three fundamental constants of nature.
The three constants:
-
Reduced Planck constant (ℏ): Quantum scale
- ℏ = h / (2π) where h = Planck's constant
- ℏ ≈ 1.054571817 × 10⁻³⁴ J·s
- Dimensions: [Energy × Time] = ML²T⁻¹
-
Gravitational constant (G): Gravity scale
- G ≈ 6.67430 × 10⁻¹¹ m³/(kg·s²)
- Dimensions: M⁻¹L³T⁻²
-
Speed of light (c): Relativity scale
- c = 299,792,458 m/s (exact by definition since 1983)
- Dimensions: LT⁻¹
Dimensional analysis method:
Goal: Find a combination of ℏ, G, c that has dimensions of time [T].
Try: ℏᵃ Gᵇ cᶜ should have dimensions of time.
Dimensions:
- (ML²T⁻¹)ᵃ × (M⁻¹L³T⁻²)ᵇ × (LT⁻¹)ᶜ = T
Expanding:
- Mᵃ⁻ᵇ × L²ᵃ⁺³ᵇ⁺ᶜ × T⁻ᵃ⁻²ᵇ⁻ᶜ = M⁰ L⁰ T¹
Solve for a, b, c:
- Mass: a - b = 0 → a = b
- Length: 2a + 3b + c = 0 → 2a + 3a + c = 0 → c = -5a
- Time: -a - 2b - c = 1 → -a - 2a + 5a = 1 → 2a = 1 → a = 1/2
Therefore: a = 1/2, b = 1/2, c = -5/2
Result:
tP = ℏ^(1/2) G^(1/2) c^(-5/2) = √(ℏG) / c^(5/2) = √(ℏG/c⁵)
Numerical calculation:
tP = √[(1.054571817 × 10⁻³⁴ J·s) × (6.67430 × 10⁻¹¹ m³/(kg·s²))] / (299,792,458 m/s)^(5/2)
Numerator: √(7.039 × 10⁻⁴⁵) ≈ 8.390 × 10⁻²³
Denominator: (2.998 × 10⁸)^2.5 ≈ 1.557 × 10²¹
tP ≈ 8.390 × 10⁻²³ / 1.557 × 10²¹ ≈ 5.391 × 10⁻⁴⁴ seconds
Uniqueness: This is the only combination of ℏ, G, c that yields dimensions of time. Other Planck units (length, mass, energy, temperature) are derived similarly using dimensional analysis.
Precision: Limited by precision of G measurement (~0.002% uncertainty). As G measurements improve, Planck time value is refined.
Are there any practical applications of Planck time?
No direct practical applications—Planck time is a purely theoretical construct far beyond any technological relevance.
Why no applications:
1. Impossibly small timescale:
- Planck time is 10²⁶ times shorter than attoseconds (shortest measured events)
- No technology will ever operate on Planck-time timescales
- Even light travels only Planck length (10⁻³⁵ m) in Planck time—far smaller than any atom
2. Requires inaccessible energies:
- Probing Planck time needs Planck energy (~10⁹ J per particle)
- Largest particle collider (LHC) achieves ~10⁻⁶ J per collision
- 10¹⁵ times too weak!
3. Fundamental limit of physics:
- Below Planck time, known laws break down
- No device can exploit physics we don't understand
Indirect "uses" (theoretical and educational):
1. Theoretical physics:
- Foundation for quantum gravity theories (string theory, loop quantum gravity)
- Natural unit system simplifies complex equations
- Benchmark for testing new theories
2. Cosmology:
- Defines earliest meaningful moment of universe (Planck epoch)
- Sets limit on Big Bang singularity studies
- Helps theorists understand early universe conditions
3. Fundamental limits:
- Bremermann's limit on computation: Maximum ~10⁴⁴ operations per second per Planck mass
- Holographic bound on information storage: Maximum entropy scales with area in Planck units
- Sets ultimate limits on any physical process
4. Philosophy of science:
- Illustrates limits of human knowledge
- Shows interconnection of quantum mechanics, relativity, gravity
- Demonstrates predictive power of dimensional analysis
5. Education and outreach:
- Helps communicate extreme scales to public
- Illustrates unification goals of physics
- Inspires interest in fundamental science
Future possibilities (highly speculative):
If we ever develop complete quantum gravity theory and if it's testable, then Planck time might indirectly inform:
- Quantum computing limits (ultimate speed bounds)
- Spacetime engineering (wormholes, time travel—pure speculation!)
- Ultra-high-energy physics experiments (far beyond current tech)
Bottom line: Planck time is a fundamental theoretical concept with profound implications for our understanding of reality, but it has zero practical applications in the sense of technology, engineering, or everyday life. Its value is purely scientific and philosophical.
Conversion Table: Sidereal Day to Planck Time
| Sidereal Day (sidereal day) | Planck Time (tP) |
|---|---|
| 0.5 | 799,147,570,024,114,300,000,000,000,000,000,000,000,000,000,000 |
| 1 | 1,598,295,140,048,228,700,000,000,000,000,000,000,000,000,000,000 |
| 1.5 | 2,397,442,710,072,342,800,000,000,000,000,000,000,000,000,000,000 |
| 2 | 3,196,590,280,096,457,300,000,000,000,000,000,000,000,000,000,000 |
| 5 | 7,991,475,700,241,142,000,000,000,000,000,000,000,000,000,000,000 |
| 10 | 15,982,951,400,482,285,000,000,000,000,000,000,000,000,000,000,000 |
| 25 | 39,957,378,501,205,710,000,000,000,000,000,000,000,000,000,000,000 |
| 50 | 79,914,757,002,411,420,000,000,000,000,000,000,000,000,000,000,000 |
| 100 | 159,829,514,004,822,850,000,000,000,000,000,000,000,000,000,000,000 |
| 250 | 399,573,785,012,057,100,000,000,000,000,000,000,000,000,000,000,000 |
| 500 | 799,147,570,024,114,200,000,000,000,000,000,000,000,000,000,000,000 |
| 1,000 | 1,598,295,140,048,228,400,000,000,000,000,000,000,000,000,000,000,000 |
People Also Ask
How do I convert Sidereal Day to Planck Time?
To convert Sidereal Day to Planck Time, enter the value in Sidereal Day in the calculator above. The conversion will happen automatically. Use our free online converter for instant and accurate results. You can also visit our time converter page to convert between other units in this category.
Learn more →What is the conversion factor from Sidereal Day to Planck Time?
The conversion factor depends on the specific relationship between Sidereal Day and Planck Time. You can find the exact conversion formula and factor on this page. Our calculator handles all calculations automatically. See the conversion table above for common values.
Can I convert Planck Time back to Sidereal Day?
Yes! You can easily convert Planck Time back to Sidereal Day by using the swap button (⇌) in the calculator above, or by visiting our Planck Time to Sidereal Day converter page. You can also explore other time conversions on our category page.
Learn more →What are common uses for Sidereal Day and Planck Time?
Sidereal Day and Planck Time are both standard units used in time measurements. They are commonly used in various applications including engineering, construction, cooking, and scientific research. Browse our time converter for more conversion options.
For more time conversion questions, visit our FAQ page or explore our conversion guides.
Helpful Conversion Guides
Learn more about unit conversion with our comprehensive guides:
All Time Conversions
Other Time Units and Conversions
Explore other time units and their conversion options:
- Second (s) • Sidereal Day to Second
- Minute (min) • Sidereal Day to Minute
- Hour (h) • Sidereal Day to Hour
- Day (d) • Sidereal Day to Day
- Week (wk) • Sidereal Day to Week
- Month (mo) • Sidereal Day to Month
- Year (yr) • Sidereal Day to Year
- Millisecond (ms) • Sidereal Day to Millisecond
- Microsecond (μs) • Sidereal Day to Microsecond
- Nanosecond (ns) • Sidereal Day to Nanosecond
Verified Against Authority Standards
All conversion formulas have been verified against international standards and authoritative sources to ensure maximum accuracy and reliability.
National Institute of Standards and Technology — Official time standards and definitions
Bureau International des Poids et Mesures — Definition of the SI base unit for time
Last verified: December 3, 2025